EPA-600/9-77-022                                         AUGUST 1977
                   THE DEGRADATION OF
            SELECTED PESTICIDES IN SOIL:
                A REVIEW  OF THE PUBLISHED
                         LITERATURE
                                              ->„

                                              • "•»»
                         '- &v'L;;,,,:. ,,11 PROTECTION
                        .-.:l, ii, L  08^17
              MUNICIPAL ENVIRONMENTAL RESEARCH LABORATORY
                 OFFICE OF  RESEARCH AND DEVELOPMENT
                 U.S. ENVIRONMENTAL PROTECTION AGENCY
                       CINCINNATI, OHIO 45268

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The nine series are.

      1.  Environmental Health  Effects Research
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                                        EPA-600/9-77-022
                                        August 1977
THE DEGRADATION OF SELECTED PESTICIDES IN SOIL:
      A REVIEW OF THE PUBLISHED LITERATURE
                        by
                 James R. Sanborn
                B. Magnus Francis
                Robert L. Metcalf
          Illinois Natural History Survey
             University of Illinois
              Urbana, Illinois  61801
              Grant  No. R 803591-01
                 Project Officers

         Richard Carnes and Rosa Raskin
   Solid and Hazardous Waste Research Division
   Municipal Environmental Research Laboratory
             Cincinnati, Ohio  45268
   MUNICIPAL ENVIRONMENTAL RESEARCH LABORATORY
       OFFICE OF RESEARCH AND DEVELOPMENT
      U.S. ENVIRONMENTAL PROTECTION AGENCY
             CINCINNATI, OHIO  45268
                                    fiOM

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                         DISCLAIMER







This report has been reviewed by the Municipal Environmental




Research Laboratory, U.S. Environmental Protection Agency, and




approved for publication.  Approval does not signify that the




contents necessarily reflect the views and policies of the




U.S. Environmental Protection Agency, nor does mention of trade




names or commercial products constitute endorsement or recom-




mendation for use.
                              11

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                                 FOREWORD
The Environmental Protection Agency was created because of increasing
public and government concern about the dangers of pollution to the health
and welfare of the American people.  Noxious air, foul water, and spoiled
land are tragic testimony to the deterioration of our natural environment.
The complexity of that environment and the interplay between its components
require a concentrated and integrated attack on the problem.
Research and development is that necessary first step in problem solution
and it involves defining the problem, measuring its impact, and searching
for solutions.  The Municipal Environmental Research Laboratory develops
new and improved technology and systems for the prevention, treatment, and
management of wastewater and solid and hazardous waste pollutant discharges
from municipal and community sources, for the preservation and treatment
of public drinking water supplies, and to minimize the adverse economic,
social, health, and aesthetic effects of pollution.  This publication is one
of the products of that research; a most vital communications link between
the research and the user community.
The following report contains a  literature summary on the  degradation
of forty-five pesticides in soil.   Some preliminary conclusions are
presented as  to the suitability  of  certain pesticides for  soil disposal.
                                   Francis T. Mayo, Director
                                   Municipal Environmental Research
                                   Laboratory
                                     111

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                               ABSTRACT
This report contains a literature summary on the degradation of forty-five
pesticides in soil.  The point of beginning of each literature review
is the year of issue of the patent for the particular pesticide.  After
compilation of the literature data for each pesticide, conclusions were
formulated regarding the suitability of soil disposal of these pesticides.
On the basis of the data collected in this report it was suggested that
ten pesticides are suitable for soil disposal, twenty-one are not suitable
for disposal, and the data for fourteen are insufficient to formulate
any conclusions regarding their suitability for soil disposal.

This report was submitted in fulfillment of Grant No.  R 803591-01 by the
Illinois Natural History Survey,  University of Illinois,  under the partial
sponsorship of the U.S.  Environmental Protection Agency.   This report covers
the period from February 1975 to  May 1976.
                                    IV

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                               CONTENTS
Abstract                                                            iii

Foreword                                                             iv
List of Figures                                                     vii

List of Tables                                                       ix

Acknowledgments                                                      xv
  I  Introduction                                                     1
       References for Introduction                                    5
       Source References                                              6

 II  Conclusions                                                     14
III  Herbicides
       Atrazine                                                      16
       Bromacil                                                      35
       COM                                                          39
       Chloramben                                                    41
       2,4-D and 2,4,5-T                                             43
       Dicamba                                                       69
       Diquat and Paraquat                                           76
       Diuron, Linuron, Monolinuron and Monuron                      89
       EPIC                                                         115
       Nitralin and Trifluralin                                     121
       Picloram                                                     134
     References                                                     149
 IV  Insecticides
       Chlorinated Hydrocarbon Insecticides                         213
         DDT and Dicofol                                            222
         Methoxychlor                                               262
       Cyclodiene Insecticides
         Aldrin, Dieldrin and Endrin                                268
         Chlordecone and Mirex                                      300
         Chlordane and Heptachlor                                   307
         Endosulfan                                                 335
         Toxaphene                                                  343
       Conclusions                                                  352
     References                                                     353

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                       CONTENTS(CONTINUED)
         Organophosphate Insecticides
           Methyl Parathion and Parathion                       416
           Malathion                                            446
           Diazinon                                             461
           Disulfoton and Phorate                               475
           Azinphosmethyl                                       488
         References                                             495
         Carbamate Insecticides
           Carbaryl                                             533
           Metalkamate                                          547
         References                                             550
 V     Fungicides and Fumigants
         Captan                                                 562
         Dodine                                                 570
         Maneb, Nabam and Zineb                                 573
         Methyl Bromide                                         583
         Pentachlorophenol                                      586
       References                                               593
VI     Synthesis                                                611
                                 vx

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                                FIGURES
Number
   1      Outline of the review of the literature for each
          of 45 pesticides	      5
   2      Proposed pathways of microbial metabolism of 2,4-D .     47
   3      Photolytic degradation of diquat 	     78
   4      Degradation of trifluralin in soil	    123
   5      Residues of 4.48 kg/ha residues of picloram (sodium
          salt) in Nova Scotia sandy loam	    143
   6      Degradation pathways of DDT	    224
   7      Effect of concentration on loss of aldrin, lindane,
          and DDT from a Miami silt loam, application in
          lb/6A	    228
   8      Degradation pathways of dieldrin 	    272
   9      Degradation pathways of endrin 	    273
  10      Loss of aldrin from a silt L>am as affected by
          temperature	    290
  11      Products of chlordane and chlordene	    309
  12      Products of heptachlor	    310
  13      Variations in the total organically bound chloride
          contents of soil samples, expressed as persistent
          curves	    322
  14      Metabolism of endosulfan	    338
  15      Structures of toxaphene components 	    345
                                 vii

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                         FIGURES(CONTINUED)

Number
  16      Degradation pathways for parathion (Modified from
          Haque and Freed 1975).  Degradation pathways for
17
18
19
20


Degradation of ethylenebisdithiocarbamates 	
Feasibility of soil disposal of herbicides 	
Feasibility of soil disposal of chlorinated

— r _K. i
536
575
612

613
  21      Feasibility of soil disposal of organophosphate
          insecticides and miscellaneous pesticides 	    614
                                viii

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                                 TABLES

Number                                                           Page
   1      Feasibility of soil disposal for the 45 pesticides
          reviewed in this report	      2
   2      Persistence of atrazine in soil	     27
   3      Degradation of 2,4-D by soil microorganisms  ....     45
   4      Persistence of 2,4-D, 2,4,5-T and TCDD in soil and
          water	     52
   5      Effects of 2,4-D on soil processes	     54
   6      Effects of 2,4-D on soil enzymes and soil elements .     56
   7      Effects of 2,4-D on classes of bacteria  	     57
   8      Effects of 2,4-D on classes of fungi	     58
   9      Effects of 2,4-D on species of soil microorganisms:
          Bacteria	     59
  10      Effects of 2,4-D on species of soil microorganisms:
          Fungi	     61
  11      Effects of 2,4-D on species of soil microorganisms:
          Algae	     62
  12      Persistence of dicamba in soil	     73
  13      Effects of diquat on soil processes	     83
  14      Effects of diquat on microorganisms  	     84
  15      Physical characteristics of monuron, diuron, linu-
          ron and monolinuron	     90
  16      Degradation of monuron and diuron by soil microor-
          ganisms	     91
                                  ix

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                          TABLES(CONTINUED)

Number                                                           Page
  17      Degradation of monolinuron and linuron by soil
          microorganisms 	    92
  18      Persistence of monuron and diuron in soils	   101
  19      Persistence of linuron and monolinuron in soils  .   .   102
  20      Effects of diuron on soil processes	   106
  21      Effects of linuron, monuron, and monolinuron on
          soil processes	   107
  22      Effects of diuron on soil microorga.nisms	   108
  23      Effects of diuron on aquatic microorganisms  ....   109
  24      Persistence of nitralin in soil	   128
  25      Persistence of trifluralin in soil	   129
  26      Effects of trifluralin on soil processes, actino-
          mycetes, and fungi	   131
  27      Effects of trifluralin on soil microorganisms and
          bacteria	   132
  28      Degradation of picloram by microorganisms  	   135
  29      Movements of picloram in soils	   139
  30      Persistence of picloram in soil	   141
  31      Disappearance of Tordon herbicide  (picloram) from
          soils	   142
  32      Effects of picloram on soil processes	   146
  33      Residues of pesticides found in soils	   215
  34      Relative mobilities of pesticides  in  soil pesti-
          cides listed in decreasing order of mobility  ....   216

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                         TABLES(CONTINUED)

Number                                                           Page
  35      Relative persistence of pesticides in soil as de-
          termined in seven studies including chlorinated
          hydrocarbon insecticides.  Pesticides listed in de-
          creasing order of persistence	    220
  36      Relative toxicities of pesticides to mammals, fish,
          and bees:  Pesticides listed in decreasing order
          of toxicity	    221
  37      Degradation of DDT by microorganisms under labora-
          tory conditions including the organisms and the
          products formed.  Structures for named compounds
          are shown in Figure 6	    225
  38      Degradation of DDT by microorganisms under labora-
          tory conditions including the culture conditions
          and the products formed.  Structures for named
          compounds are shown in Figure 6	    226
  39      Vertical distribution of DDT analogs and metabolites
          in orchard soils, 1970	    234
  40      Changes in vertical distribution of total DDT, 1965-
          1970	    235
  41      Degradation of DDT under field conditions  	    244
  42      The effects of DDT on soil microorganisms and soil
          processes	    249
  43      The effects of DDT on bacteria	    250
  44      The effects of DDT on fungi	    251
  45      The effects of the DDT analogs, ODD, and Dicofol
          on soil microorganisms and soil processes	    252
  46      Degradation of aldrin, dieldrin, and endrin under
          laboratory conditions	    270
                                  XI

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                          TABLES(CONTINUED)

Number
  47      Residues and rate of degradation of aldrin, diel-
          drin, isodrin, and endrin under field conditions .  .     287
  48      The effects of aldrin on soil microorganisms and
          soil processes	     292
  49      The effects of dieldrin on soil microorganisms and
          soil processes	     293
  50      The effects of endrin on soil microorganisms and
          soil processes	     294
  51      Effects of chlordecone and mirex on soil processes
          and microorganisms	     304
  52      Degradation of heptachlor and chlordane by micro-
          organisms under laboratory conditions	     311
  53      Residues and rates of degradation of chlordane in
          soil under field conditions	     320
  54      Residues and rates of degradation of heptachlor
          under field conditions 	     321
  55      The effects of chlordane on soil microorganisms and
          soil processes	     326
  56      The effects of heptachlor on soil processes	     328
  57      The effects of heptachlor on soil microorganisms .  .     329
  58      Biological degradation of endosulfan 	     337
  59      Biodegradation of methyl parathion 	     418
  60      Biodegradation of parathion	     420
  61      Persistence of parathion in soils	     429
  62      Persistence of methyl parathion, paraoxon, and
          aminoparathion in soils	     431
                                xii

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                          TABLES(CONTINUED)

Number                                                           Page
  63      Effects of parathion on soil microorganisms	    435
  64      Effects of parathion on species of microorganisms. .    436
  65      Effects of p-nitrophenol and methyl parathion on
          soil microorganisms	    437
  66      Degradation of malathion in three soils over a 10
          day period	    447
  67      Biological degradation of malathion	    448
  68      Persistence of malathion in soil, in water, and
          on organisms	    454
  69      Effects of malathion on aquatic microorganisms .  . .    458
  70      Effects of malathion on soil organisms and soil
          processes	    458
  71      Degradation of diazinon by microorganisms and in
          soil	    462
  72      Persistence of diazinon in soil	    469
  73      Effects of diazinon on soil microorganisms and soil
          processes	    472
  74      Degradation of phorate and disulfoton	    476
  75      Persistence of disulfoton in soil	    481
  76      Persistence of phorate in soil	    482
  77      Effects of disulfoton on soil microorganisms and
          soil invertebrates	    483
  78      Effects of phorate on soil microorganisms and
          soil invertebrates	    484
  79      Number of days required for 50% loss of azinphos-
          methyl from soil at three temperatures and two
          levels of moisture	    489
                                xiii

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                          TABLES(CONTINUED)
Number
  80      Residues of azinphosmethyl in soil after contami-
          nation with undiluted (18.1%) and diluted (0.045%)
          emulsified concentrate solutions and diluted solu-
          tions (0.045%) of wettable powder,,	    491
  81      Degradation of carbaryl by bacteria	    534
  82      Degradation of carbaryl by fungi	    535
  83      Effects of carbaryl on soil microorganisms	    541
  84      Effects of carbaryl on aquatic microorganisms. .   .  .    542
  85      Effects of captan on soil processes	    566
  86      Effects of captan on soil microorganisms other than
          fungi	    567
  87      The effects of maneb on soil organisms other than
          fungi	    578
  88      The effects of nabam on soil organisms other than
          fungi	    579
  89      The effect of zineb on soil organisms other than
          fungi	    580
  90      Effects of pentachlorophenol on soil microorganisms.    591
                                  xiv

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                            ACKNOWLEDGMENTS

The authors would like to thank the following people for their assis-
tance during the preparation of this report:   P.  Drews,  G.  K.  Francis,
L. George, J. Richards, E. J. Traub.
                                 xv

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                        SECTION I  INTRODUCTION
The use of pesticides has steadily increased in the thirty years since
the introduction of DDT  and is unlikely to decline in the near future,
despite the known and suspected consequences of environmental pollution.
Of 33 billion acres of land surface on the earth, approximately three
billion acres are cultivated, with 93 percent planted to food crops and
most of the rest planted to cotton (Holm 1969).  Some of the cropped
soils receive a pre-emergence herbicide, fungicide, nematocide, systemic
insecticide, postemergent herbicide, one or more postemergent insecti-
cides or fungicides, and a defoliant, all in a single season (Nash 1967).
Some pesticides are also used on forested land, and large amounts are
used industrially and domestically.
In 1972, the U. S. production of synthetic organic pesticides exceeded
1,157,609,000 pounds, excluding compounds with major nonpesticidal
uses.  Of this total, herbicides accounted for more than 451 million
pounds, insecticides for more than 563 million pounds, and fungicides
for almost 143 million pounds (von Rumker et al. 1974).
In addition to the intended dispersal of these pesticides onto and
into soil and water, considerable amounts must be disposed of without
being used:  unwanted leftovers, residues remaining in emrty containers,
and unused stocks of compounds which have been banned.  The most common
and simplest form of disposal is in so±\ and the suitability of soil
disposal is obvious for compounds  that  readily decompose to naturally
occurring substances without endangering soil processes, soil micro-
organisms, or higher organisms in the interim.  It is the purpose of
this report to evaluate the feasibility of disposing of large quantities

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of a selected number of pesticides in the soil, but alternative modes of
disposal are also considered, since not all compounds lend themselves
to soil disposal.
The primary contraindication to soil disposal is undue persistence.
Alexander (1965) stressed the principle of microbial fallibility:
   "When the nature of the resistant configuration or backbone is
   established we can only speculate	why an organism which
   does not exist is unable to decompose a compound which does."
Long persistence has, in the past thirty years,  led to worldwide con-
tamination by immobile compounds, to poisonings  of species other than
the intended targets, and to the accumulation of recalcitrant metabo-
lites of greater or lesser toxicity than the parent compound.  There-
fore, both the mobility and the ramifications of contamination by each
pesticide, and/or of its terminal residues, must be considered before
large-scale soil disposal is attempted.
This report reviews the published literature on  the behavior of 45
pesticides (17 herbicides, 20 insecticides, six  fungicides, one fumi-
gant and one acaricide) in soil.  For each pesticide, an exhaustive
search was made of the literature pertaining to  soil persistence and
degradation by soil microorganisms, leaching through soil, and volati-
lization from soil.  Because all pesticides on which enough data exist
were found to migrate from soil into water, data on persistence, trans-
port, and degradation in water were also included.  A thorough search
of the literature pertaining to the effects of each pesticide on the
non-target microorganisms of soil and water was  also made.  Data on
the toxicity of each compound to other non-target species are included,
but these data are reviewed selectively.  Particular attention was paid
to the hazards of chronic exposure to low levels of pesticides, which
would be the most likely consequence of improper disposal, and some data
on acute effects are given for comparison.  The  outline of the review
for each pesticide is shown in Figure 1.

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Introduction
     Nomenclature, Physical Properties,  Synthesis

Degradation
     Biological
     Chemical and Physical
     Photolytic

Transport
     Within Soil
     Between Soil and Water
     Volatilization
     Into Organisms

Persistence

Effects on Non-target Species
     Microorganisms
     Invertebrates
     Plants
     Fish and Amphibians
     Birds
     Mammals

Conclusions
                           Figure 1
           Outline of the review of the literature
                  for each of 45 pesticides

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Sources of the data in this report are:  Chemical Abstracts, computer
searches, monographs, review articles, and original articles.  Each re-
ference contains the source of the data cited.  If no additional infor-
mation is given, the original article was used.  If the Chemical Ab-
stracts number is cited, data were taken from this abstract.  In the few
cases in which a computer search identified an otherwise unascertained
article, the name of the program (e.g. TOXLINE) is given as part of the
reference.  When a review article or monograph was the source of the
information, the author of the review is cited.  In short, the actual
source of the information is cited, as well as the original author when
Chemical Abstracts was the source.  A list of source references, many
of which are not specifically quoted in the text per se3 follows the
references for this section.
Only published literature was reviewed, and theses abstracted in Thesis
Abstracts were excluded from the definition of published literature.
The literature search for each compound began with the patent issue
date, and the latest articles cited include several published in 1976,
although the search was complete only through September 1975.  The last
issue of Chemical Abstracts to be scanned was number 13 of Volume 83
(September 29, 1975).  Journal searches ended with September 1975 is-
sue in most cases, but exceptions consisted of extended rather than ab-
breviated searches.
The literature search was exhaustive rather than critical, and many of
the studies cited can undoubtedly be criticized.  No attempt has been
made to evaluate each study in the text, but the conclusions for each
compound are based on the excellence as well as on the mass of data
supporting them.

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References for Introduction
Alexander, M.; 1965.  Persistence and biological reactions of pesti-
  cides in soils.  Soil Sci. Soc. Amer., Proc. 29:1-7.
Holm, L.; 1969.  Weed problems in developing countries.  Weed Sci. 17:
  113-118.
Nash, R. G.; 1967.  Phytotoxic pesticide interactions in soil.  Agron.
  J. 59:227-230.
von Rumker, R., E. W. Lawless and A. F. Meiners; 1974.  Production,
  distribution, use and environmental impact potential of selected pes-
  ticides.  EPA 540/1-74-001.

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Source References
Adams, R. S., Jr.; 1973.  Factors influencing soil adsorption and bio-
  activity of pesticides.  Residue Reviews 47:1-54.
Ahlrichs, J. L., L. Chandler, E. J. Monke and H. W. Reuszer; 1970.  Ef-
  fect of pesticide residues and other organotoxicants on the quality
  of surface and ground water resources.  NTIS PB-211 080.
Atkins, P. R.; 1972.  The pesticide manufacturing industry-Current waste
  treatment and disposal practices.  Water Pollution Control Research
  Series, EPA #12020 FYE 01/72.
Bailey, G. W., A. P. Barnett, W. R. Payne and C. N. Smith; 1974.  Her-
  bicide runoff from four coastal plain soil types.  Environmental Pro-
  tection Technology Series EPA-660/2-74-017.
Barnes, J. M.; 1974.  Toxicology of agricultural chemicals.  Outlook
  Agric. 7:97-101.
Brooks, G. T.; 1974.  Chlorinated Insecticides.   Vol. 1:  Technology and
  Application.   Vol. 2:  Biological and Envii'onmental Aspects.  CRC
  Press; Cleveland, Ohio; 1974.
Burnam, W. , M. L. Alexander, H. Kerby, T. Freiitag and E. Thomas; 1975.
  Initial scientific and minieconomic review of methyl parathion.  Sub-
  stitute Chemical Program EPA-540/1-75-004.
Chemagro Division Research Staff.  Guthion (azinphosmethyl):  Organophos-
  phorus insecticides.  Residue Reviews 51:123-180.
Chesters, G. and G. B. Lee; 1971.  Insecticide adsorption by lake sedi-
  ments as a factor controlling insecticide accumulation in lakes.  U.S.
  Nat. Tech. Inform. Serv., PB Rep. No. 206303:91 pp.
Courtenay, W. R., Jr. and M. H. Roberts, Jr.; 1973.  Environmental ef-
  fects on toxaphene toxicity to selected fishes and crustaceans.  Eco-
  logical Research Series EPA-R3-73-035.

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Crawford, N. H. and A. S. Donigan, Jr.; 1973.  Pesticide transport and
  runoff.  Model for agricultural lands.  Environmental Protection Ag-
  ency Series EPA-660/2-74-013.
Cutkomp, L. K.; 1974.  A tissue enzyme assay for chlorinated hydrocar-
  bon insecticides.  Environmental Protection Technology Series EPA-
  660/2-73-027.
Edwards, C. A.; 1973.  Persistent Pesticides in the Environment* 2nd
  ed.  CRC Press, Cleveland, Ohio 44128.
Edwards, C. A. and A. R. Thompson; 1973.  Pesticides and the soil fauna,
  Residue Reviews 45:1-80.
EPA; 1975.  Substitute chemical program:  Initial scientific and mini-
  economic review of malathion.  U.S. EPA Office of Pesticide Programs,
  EPA-540/1-75-005.
EPA; 1975.  Substitute Chemical Program;  Initial screening and mini-
  economic review of bromacil.  U.S. EPA Office of Pesticide Programs,
  EPA 540/1-75-006.
EPA; 1975.  Substitute Chemical Program:  Initial scientific and mini-
  economic review of captan.  U.S. EPA Office of Pesticide Programs,
  EPA 540/1-75-012.
EPA; 1975.  Substitute Chemical Program:  Initial scientific and mini-
  economic review of monuron.  U.S. EPA Office of Pesticide Programs,
  EPA 540/1-75-028.  Available NTIS, Springfield, Va. 22151.
EPA; 1975.  DDT:  A review of scientific and economic aspects of the
  decision to ban its use as a pesticide.
EPA; 1973.  Pesticide reference standards and supplemental data.  Pes-
  ticide and Toxic Substances Effects Laboratory Nation Environmental
  Research Center, Office of research and development.  U.S. EPA, Nov.
  1973.
EPA; 1975.  Miscellaneous Chemicals Industry.  Development Document for
  effluent limitations guidelines and standards of performance.  Feb.
  1975.
EPA; 1975.  ORD publications summary.  Technical Information Division.

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  Office of Monitoring and Technical Support.  EPA-600/9-75-001b.
Ernst, W.; 1967.  Der Stoffwechsel von Pesticiden in Saugetieren.  Res-
  idue Reviews 18:131-157.
Eto, M.; 1974.  Organophosphorus Pesticides:  Organic and Biological
  Chemistry.  CRC Press, Cleveland, Ohio.
Evans, J. 0. and D. R. Duseja; 1973.  Herbicide contamination of sur-
  face runoff waters.  U.S. Nat. Tech. Inform. Serv., PB Rep 222283/4
  106 pp.  Available GPO-$1.25.
Farmer, W. J.; 1974.  Volatilization losses of pesticides from soils.
  Environmental Protection Technology Series-EPA 660/2-74-054.
Floyd, E. P.; 1970.  Occurrence and significance of pesticides in solid
  wastes.  U.S. Dept. of Health, Education, and Welfare.  Open File Re-
  port (RS-02-68-15).
Foy, C. L. and S. W. Bingham; 1969.  Some research approaches toward
  minimizing herbicidal residues in the environment.  Residue Reviews
  29:105-135.
Fromm, P. 0.; 1970.  Toxic reaction of water soluble pollutants on
  freshwater fish.  U.S. Nat. Tech. Inform. Serv., P.B. Rep. No. 201650,
  59 pp.
Gerakis, P. A. and A. G. Sficas; 1974.  The presence and cycling of pes-
  ticides in the ecosphere.  Residue Reviews 52:69-87.
Goring, C. A. I. and J. W. Hamaker; 1972.  Organic Chemicals in the En-
  vironment, 2 volumes.  Marcel Dekker, Inc. New York.
Guenzi, W. D.; 1974.  Pesticides in Soil and Water.  Soil Sci. Soc.
  Amer. Madison, Wis.
Haile, C. L., G. D. Veith, G. F. Lee and W. C. Boyle; 1975.  Chlorina-
  ted hydrocarbons in the Lake Ontario Ecosystem.  (IFYGL).  Ecological
  Research Series EPA-660/3-75-022.
Haque, R. and V. H. Freed; 1974.  Behavior of pesticides in the envi-
  ronment:  "Environmental chemodynamics".  Residue Reviews 52:89.
Haque, R. and V. H. Freed; 1975.  Environmental Dynamics of Pesticides.
  Plenum Press, N.Y. and London.

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Harris, C. I.; 1969.  Movement of pesticides in soil.  J. Agr. Food
  Chem. 17:80-82.
Hayes, W. J., Jr.; 1967.  Safe use of pesticides in public health.
  World Health Organ., Tech. Rep. Ser. No. 356, 65 pp.
Hermanson, H. P., F. A. Gunther, L. D. Anderson and M. J. Garber; 1971.
  Installment application effects upon residue content of a California
  soil.  J. Agr. Food Chem. 19:722-726.
Honea, F. I., D. Punzak, E. W. Lawless, L. J. Shannon and D. Wallace;
  1975.  Pesticides Industry.  Environmental Catalog of Industrial Pro-
  cesses-EPA.
Hoover, R. and J. F. Fraumeni, Jr.; 1975.  Cancer mortality in U.S.
  counties with chemical industries.  Environmental Research 9:196-207.
Howard, P. H., J. Saxena, P. R. Durkin and L-T. Ou; 1975.  Review and
  evaluation of available techniques for determining persistence and
  routes of degradation of chemical substances in the environment.  Of-
  fice of Toxic Substances EPA-560/5-75-006, PB-243 825.
Hurlbert, S.; 1975.  Secondary effects of pesticides on aquatic ecosys-
  tems.  Residue Reviews 57:81-148.
Ingle, L.; 1965.  A monograph on chlordane.  Velsicol Chemical Corp.
Jukes, T. H.; 1974.  Insecticides in health, agriculture, and the en-
  vironment.  Naturwissenschaften 61:6-16.
Kaiser, P., J. J. Pochon and R. Cassini; 1970.  Influence of triazine
  herbicides on soil microorganisms.  Residue Reviews 32:211-233.
Kearney, P. C. and D. D. Kaufman; 1969.  Degradation of Herbicides.
  Marcel Dekker, Inc. N. Y.
Kearney, P. C. and J. R. Plimmer.  Relation of structure to pesticide
  decomposition.  Crops Research Division, Agr. Res. Serv. U.S. Dept.
  of Agr.
Kearney, P. C., E. A. Woolson, J. R. Plimmer and A. R. Isensee; 1969.
  Decontamination of pesticides in soils.  Residue Reviews 29:137-149.
Kraybill, H. F., Ed.; 1969.  Biological effects of pesticides in mam-
  malian systems.  Ann. N.Y. Acad. Sci. 160:1-422.  New York Academy
  of Sciences, N.Y.

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Lawless, E. W., T. L. Ferguson and A. F. Meiners;  1974.  Methods for
  disposal of spilled and unused pesticides.  Proc. Nat'l. Conf. Contr.
  Hazardous Spills 324-335.
Lawless, E. W., T. L. Ferguson and A. F. Meiners;  1975.  Guidelines for
  the disposal of small quantities of unused pesticides.  Environmental
  Protection Technology Series EPA-670/2-75-057.
Lawless, E. W., R. Von Rumker and T. L. Ferguson;  1972.  The Pollution
  Potential in Pesticide Manufacturing.  NTIS PB213-782. Prepared for
  EPA June 1972.
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  idues in soils.  Their translocation into crops.  Arch. Environ.
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  Research on Persistent Pesticides.  C. C. Thomas, Springfield, 111.
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  Control use of Pesticides.  Socioeconomic Environmental Studies Series
  EPA-600/5-74-018.
                                    10

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Nash, R. G.;  1967.  Phytotoxic pesticide interactions in soil.  Agron.
  J. 59:227-230.
O'Brien, R. D., R. L. Doutt, M. L. Fairchild, S. D. Faust, F. K. Kino-
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Reese, C. D.; 1972.  Pesticide study series-4.  Development of a case
  study of the total effect of pesticides in the environment.  Non-
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Ricci, B. and R. 0. Beauchamp, Jr.; 1973.  Toxicity of toxaphene:  a
  bibliography TIP 1250.  Toxicology Information Response Center.
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Rosenberg, D. M.; 1975.  Food chain concentration of chlorinated hydro-
  carbon pesticides in invertebrate communities:  a re-evaluation.
  Quaest. Ent. 11:97-110.
Rumker, R. v., E. W. Lawless and A. F. Meiners; 1974.  Production, dis-
  tribution,  use and environmental impact potential of selected pesti-
  cides.  EPA 540/1-74-001.
Schacht, R. A.; 1974.  Pesticides in the Illinois waters of Lake Michi-
  gan.  Ecological Research Series.  EPA-660/3-74-002.
Schlagbauer,  B. G. L. and A. W. J. Scjlagbauer; 1972.  The metabolism
  of carbamate pesticides - a literature analysis.  Residue Reviews 42:
  1-90.
Schrader, G.; 1963.  Konstitution und Wirkung organischer Phosphorver-
                                   11

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  bindungen.  Z. Naturforsch.  18b:965-975.
Schultz, D. P. and P. P. Harman; 1974.  A review of the literature on
  the use of 2,4-D in fisheries.  Bureau of Sport Fisheries and Wild-
  life.  NTIS PB-235 457.
Sethunathan, N.; 1973.  Microbial degradation of insecticides in flood-
  ed soil and in anaerobic cultures.  Residue Reviews 47:143-166.
Sheets, T. J., J. R. Bradley, Jr. and M. D. Jackson; 1972.  Contamina-
  tion of surface and ground water with pesticides applied to cotton.
  Water Resources Research Institute of the Univ. of North Carolina
  report #60.  PB-210 148.
Smith, G. E. and F. D. Whitaker; 1974.  Losses of Fertilizers and Pes-
  ticides from claypan soils.  Environmental Protection Technology Se-
  ries EPA-660/2-74-068.
Summers, W. K. and Z. Spiegel; 1974.  Ground Water Pollution.  A Bib-
  liography.
Sutton, W. W.; 1975.  Development of a biological monitoring network—
  A test case—Suitability of livestock and wildlife as biological mon-
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  Series EPA-680/4-75-003.
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  46-85.
U. S. Dept. of the Interior.  Office of Water Resources Research.
  WRSIC 72-203.  Aldrin and Endrin in Water.  A bibliography.
Weidner, C. W.; 1974.  Degradation in ground water and mobility of her-
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  Pestic. Monit. J. 6:194-228.
WSSA; 1974.  Herbicide Handbook of the Weed Science Society, 3rd ed.
                                   12

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Yoss, J. K., J. W. Blaylock, M. J. Schneider, L. C. Schwendiman, C. J.
  Touhill, Jr., W. L. Templeton, R. E. Wildung and D. B. Menzel; 1970.
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  vironmental health service volume IV.  Pesticides Model Case study.
  Battelle Memorial Institute, Columbus laboratories.  Contract No.
  CPS-69-005.
                                  13

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                        SECTION II CONCLUSIONS
Of the forty-five pesticides reviewed in this report, ten are suitable
for soil disposal, twenty-one are unsuitable., and the available data are
insufficient for any conclusions in fourteen cases.  The feasibility of
soil disposal for each pesticide is listed in Table 1.
Since most of the available data deal with relatively small amounts of
well-dispersed pesticides and degradation is almost invariably inverse-
ly correlated with concentration, bulk disposal of most pesticides will
lead to long periods of persistence of the parent compound  and/or its
degradation products.  Transport of persistent compounds through soil
is inevitable and transport into ground or surface waters extremely
probable.  Therefore any large deposits of pesticides in soil must be
carefully monitored until decomposition has obviated the possibility
of environmental contamination.
In contrast to soil disposal, thermal disposal can present hazards due
to formation of toxic gases and other wastes.  Decontamination procedures
for most of these products of combustion (e.g., chlorine and hydrogen
chloride) are well known.  While not enough data are available to suggest
burning all pesticides, incineration is a rapid and can be a most efficient
mode of disposing of many of the pesticides reviewed here.
                                    14

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                         SECTION III HERBICIDES
Atrazine
Atrazine is the common name for 6-chloro-ff-eth.yl-.ff'-(l-methylethylJ-
l^S-e-triazine^^-diamine, a pre- and postemergent herbicide intro-
duced by the Geigy Chemical Co. in 1957.  It is used for general weed
control and for selective weed control in corn, sorghum, sugar cane
and pineapple under the trade names AAtrex in the USA and Gesaprim or
Primatol in Europe.
Atrazine is a white crystalline solid with a melting point of 173-175 C,
a vapor pressure of 3.0 x 10  mm mercury at 20 C and a water solubility
of 33 ppm at 27°C.  Its solubility in ethyl acetate is 28,000 ppm; in
dimethyl sulfoxide, 183,000 ppm at 27 C.  It is synthesized by reacting
cyanuric chloride with one equivalent of isopropylamine and one equi-
valent of ethylamine in the presence of acid acceptors (WSSA 1974).  A
lengthy review of the triazine herbicides including atrazine was pub-
lished in Residue Reviews 32 (1970).
Degradation-
Biological—The major degradative process undergone by atrazine in soil
is its conversion to hydroxyatrazine by loss of the chlorine at the C-6
position (Beynon et^ a^. 1972, Harris 1967, Roeth &t_ al_. 1969, Knuesli
et^ al. 1969).  Microbial attack reportedly resulted in deethylated at-
razine as the major metabolite and deisopropylated atrazine as a minor
metabolite  (Sirons et al. 1973).  Decomposition is more rapid in nor-
mal than in sterilized soil, and is enhanced by repeated applications
of atrazine (Gigineishvili and Dzhugeli 1973).  McCormick and Hiltbold
                                   16

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(1966) suggested that atrazine was only incidentally or nonpreferential-
ly involved in microbial metabolism, a situation to which Alexander
(1972) has given the name cometabolism.  Under laboratory conditions,
however, atrazine can serve as a carbon source for Fusari-wn Tosewn
(Couch jet_ al. 1965), Rhisopus stolonifer and several species of Aspeic-
gillus and Fusarium (Kaufman and Blake 1970) and for Mueor spinosim,
Aspergillus nidulans and Peniailliion tardwn (Nepomiluev and Kuzyakina
1972).  Also under laboratory conditions, fungi could be adapted  to use
atrazine as a nitrogen source (Manorik and Malichenko 1971), giving
half the rate of growth of controls in cultures of Cephalosporiim aoTi-
moni-wn3 Ctadospoviwn herbarwn3 and in several Peniaill-ium and Aspepgil-
lus species.  Atrazine did not, however, suffice as a carbon source in
this study (Mickovski and Verona 1967).  Soil bacteria decomposed 70
percent of an unspecified level of atrazine in 18 days, with Baaillus
megatep-ilm and B. aglomeratus identified as most active (Voinova  and
Bakalivanov 1970).
The degradation of atrazine by soil fungi is restricted to the side
chains, and possibly only to laboratory cultures (Kaufman and Blake
1970).  When ring-labeled atrazine was incubated in anaerobic (flooded)
organic soil, only 0.02 to 0.59 percent of the radioactive label  was
converted to carbon dioxide.  Addition of starch or ammonium sulfate
              14
increased the   C09 evolution somewhat, as did aeration of the soil
(Goswami and Green 1971).  When chain-labeled atrazine was incubated in
soil at 25 C and 80 percent of field moisture capacity, only one  per-
cent of the radioactive label was converted to carbon dioxide.  At lower
                                               14
temperatures or in less moist soils, even less   CO- was evolved  (Roeth
et al. 1969).
In cultures of 21 planktonic algae, atrazine was not removed from water
by the algae (Butler et al. 1975).  Degradation in soil followed  first-
order kinetics with no lag period (Zimdahl et al. 1970).
In fish, exposure to ten ppm atrazine did not result in significant ac-
                                    17

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cumulation in muscle tissue, and the atrazirie was rapidly degraded
(Bathe et_ a^. 1972).  Dairy cows did not excrete atrazine in their milk,
but two percent was excreted in the urine as unaltered atrazine.  No
metabolites were identified (St. John et^ a^. 1964).  Paulson (1975) in
his review of the animal metabolism of atrazine, stated that 6-chloro-
triazines are eliminated more slowly than 6-methoxy- or 6-methylthio-
triazines, and that dealkylation is inversely related to the length of
the side chain.  No ring cleavage has been reported in animals, and
almost none of the many metabolites reported have been identified.  In
rat liver in vitro, dealkylation was the primary mode of degradation
and no dechlorination occurred (Dauterman arid Muecke 1974).
Photolytic—Atrazine in aqueous solution was converted to hydroxyatra-
zine by ultraviolet light at 253.7 nm (Pape and Zabik 1970), a reaction
which also occurred in natural sunlight (Pape and Zabik 1972).
Chemical and physical—The nonenzymatic decomposition of atrazine in
soil is unlikely under anaerobic conditions in the absence of adsorp-
tion (Hance 1967) but feasible if adsorption occurs (Hance 1969).  Non-
enzymatic hydrolysis was considered the major mechanism of atrazine de-
toxification in some studies (Best and Weber 1974, Zimdahl at al. 1970).
In comparisons between sterilized and unsterilized soil, however, only
13.6 percent of atrazine was decomposed after one month in sterile soil,
but 23 percent in unsterilized soil.  The differences were even more
marked when repeated applications of atrazirie were made to the soils
(Gigineishvili and Dzhugeli 1973).  Brown arid White (1969) found atra-
zine to be less susceptible to hydrolysis than trietazine, chlorazine,
propazine, ipazine or simazine, although the observed hydrolysis was
relatively great since atrazine was not as heavily adsorbed by the clay.
Armstrong and Chesters (1968) did not consider adsorption hydrolysis
common, and also argued against the nonbiological hydrolysis of atra-
zine as a major method of degradation under normal conditions.  Among
the factors favoring atrazine degradation under environmental conditions
were increasing temperatures (Roeth jat_ aJ^. 1969, McCormick and Hiltbold
                                    18

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1966).
Paris and Lewis (1973) summarized the welter of data by noting that de-
alkylation does not destroy the phytotoxicity of atrazine, whereas hy-
drolysis does; the former is presumed to be biological and the latter
nonbiological.
Concentrations of 50 to 100 ing/liter of atrazine were decomposed by 20
to 30 minute contact with five to 20 mg of chlorinated lime  (Martynuk
and Gzhegotskii 1967).  Metallic sodium and liquid ammonia decomposed
atrazine 100 percent, while substituting lithium for sodium resulted
in 17.5 percent intact atrazine (Kennedy et_ _al_. 1972a) .  Atrazine
could also be partially decomposed by 15N ammonium hydroxide  (Kennedy
et.al. 1972b).
When atrazine was heated in a muffle furnace, 87.8 percent was decom-
posed at 600°C, and 89 percent at 1000°C (Kennedy et_ al. 1969).  The
volatile products of burning atrazine at 900 C were carbon monoxide,
carbon dioxide, hydrochloric acid and ammonia (Kennedy et al. 1972a,
1972b).  Some decomposition occurred at temperatures as low as 250 C,
turning atrazine into yellow flakes which were tentatively identified
as primary or secondary amines (Stojanovic _et_ a!L. 1972b) .  Tadik and
Ries (1971) identified the decomposition of atrazine between  240 C and
250 C to consist of elimination of the isopropylamino and ethylamino
chains, possibly with a cyclic transition state.  They also decomposed
triazine herbicides by sonication, but did not conclusively identify
the products.
Transport-
Within soil—Transport of atrazine is inversely correlated with adsorp-
tion of the herbicide to soil and soil constituents (Rodgers  1968) .
Several attempts have been made to fit the data for atrazine  adsorption
to theoretical or empirical models (Hayes et_ a^. 1968, Hance  1969b,
Guth 1972, Bailey and White 1972, Huggenberger et_ al. 1973).  Although
                                   19

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qualitative fit was achieved, the models were not considered good pre-
dictors of atrazine behavior in the field  (Huggenberger et a]^. 1973,
Crawford and Donigan 1973).
The major factors influencing the adsorption of atrazine on soil are
the soil composition, soil moisture, pH, and temperature.  Atrazine is
heavily adsorbed on organic matter in soil  (Hilton and Yuen 1963) or
activated charcoal (Jordan and Smith 1971).  In the laboratory it has
been shown atrazine binds to the insoluble lignin or hutnic acid frac-
tions of soil, with only minor binding associated with polysaccharide
components and virtually none with ethanol-soluble components (Dunigan
and Mclntosh 1971).  Plant residues, fungal resting structures, fecal
pellets and animal cysts adsorbed atrazine heavily (Grossbard et al.
1970).  Aliphatic hydroxyl groups, aliphatic carboxyl groups and phe-
nolic hydroxyl groups are thought to be active in the soil binding
process (Turski and Steinbrich 1972).
Adsorption of atrazine on charcoal increased its persistence in soil,
as did addition of clay to the soil (Moyer et_ al. 1972a) but Hance
(1974) argued that adsorption of atrazine by soil organic matter did
not affect degradation.  Weber (1970b) noted that reversible adsorption
could lead to increased, delayed or decreased phytotoxicity.  The rela-
tive adsorption of atrazine on different soils was:  marsh > fine grain
> light, sandy soil (Gorzelak 1972); silt or silty clay > sandy loam
(Harris 1966); chernozem > Kraznozem > sod podzol (Khlebnikova 1974) .
On clay, atrazine adsorption is dependent both on pH and the cation ex-
change capacity of the clay (Hance 1969a).  Adsorption on montmorillo-
nite, but not on peat, was reversible even when the adsorbent was dried
and re-wet (Moyer £t_ al_. 1972b), and adsorption on kaolinite was fully
reversible (Scott and Lutz 1971).  Under some experimental conditions,
atrazine is not adsorbed by kaolinite (Talbert and Fletchall 1965).
At pH less than six, increasing the temperature resulted in both in-
creased binding and in increased recovery of atrazine when temperature
                                   20

-------
varied:  from 85 percent  recovery at 0.5 C  to  98 percent  recovery at
40 C, while recovery at pH  7 was only 69 percent (McGlamery and  Slife
1966).  Adsorption of atrazine usually decreased as pH  increased above
pH 7  (Hance 1969a, Weber  1970a, Nearpass 1967, Green and  Corey 1971,
Colbert e£ al. 1975) but  two silt loam soils with natural pH 8.5 and
9.6 adsorbed atrazine very  well (Colbert et^ al^ 1975).
Increasing the temperature  from three to 25 C  produced  a  four-fold in-
crease in  the binding of  atrazine to humic  acid (Li and Fellbeck 1972)
and temperature affected  atrazine adsorption on bentonite but not on
muck  (Harris and Warren 1974).  Talbert and Fletchall (1965), however,
reported decreased adsorption of atrazine at higher temperatures.
When  the soil to water ratio was  soil : water :: 1 : 10, adsorption of
atrazine on soil was five times as great as when the ratios were soil :
water :: 3 : 1.  The data suggested that the size of the  soil aggregates
affected adsorption (Grover and Hance 1970).
The relative adsorption of  herbicides on soil was:  2,4-D < fluometron
< prometone < simazine, atrazine, diphenamid < prometryne « chlorpro-
pham  « trifluralin « benefin (Scott and Phillips 1972)  and, among
triazines:  propazine < atrazine < simazine < prometone < prometryne
(Talbert and Fletchall 1965).  On a six point scale of  soil mobility,
atrazine was rated at 2.7 in silty clay loam and as 3.5 in sandy loam,
which is considered moderately mobile (Harris 1967).  Among the  tria-
zines, the chlorotriazines  are less mobile than the analogous methoxy-
triazines but more mobile than the 5"-methyl triazines (Helling et al.
1971).
The relative leaching of  seven s-triazines was:  atratone > propazine
> atrazine > simazine > ipazine > ametryne > prometryne (Rodgers 1968).
Increasing soil bulk inhibits the diffusion of atrazine through  soil,
while high soil moisture enhances it (Ritter e£ a^. 1973, Lavy 1970).
Granular atrazine leached further if formulated on ammonium sulfate
than on limestone (Cast 1962).   Agricultural soils have a greater than
                                   21

-------
necessary capacity for binding agricultural levels of atrazine  (Snel-
ling et_ al_. 1969), but the precise binding capacity depends on  the state
of decomposition of the organic matter as well as on its amount  (Walker
and Crawford 1968).  Electrolytes can also alter the adsorptive  capa-
city of soil (Hurle and Freed 1972).
Studies on the leaching of atrazine in soil columns and under field
conditions demonstrate the variability of soil penetrance.  In  quartz
sand in 30 cm soil columns, atrazine penetrated no more than ten cm
when ten cm water were used for leaching, and no more than 20 cm if the
sand was leached with 20 cm of water (Vega 197^-).  In soil columns
leached with three cm water per day, atrazine penetrated to 2.4  inches
(60 cm) with 18 inches of water in silt loam arid in sandy loam,  but
only to 20 inches  (50 cm) in loam.  With three inches (7.5 cm)  water,
phytotoxic amounts of atrazine leached to three or four inches  (<_ 10 cm)
in loam, six inches (15 cm) in sandy loam, and eight to ten inches
(>_ 25 cm) in silt loam (Ivey and Andrews 1965).,
When applied to the top two cm of chernozem and podzolic sandy  loam,
atrazine penetrated seven to eight cm in the former, but more than 13
cm in the latter within six months (Trzecki and Kowalski 1974)  while
four to six kg/ha penetrated light chestnut soils to ten cm (Stepanova
1965).  Ten to 12 kg/ha of atrazine leached to 20 cm in tea plantations,
but 12 and 14 kg/ha penetrated 30 cm in orchard soils (Tabagua  1975).
In chernozem-smolnitsa soil, 1.5 kg/ha of atrazine was most phytotoxic
in the four to six cm layer for two to three months, and in the ten to
12 cm layer thereafter until it decomposed (Andreeva-Fetvadzieva 1967).
In moist subtropical soils, atrazine leached only 40 cm during  1.5 to
two months in waterlogged soil, but 50 to 70 cm in red soil (Spiridonov
et_ a^. 1970b).  At temperatures below ten C, five to 20 kg/ha persisted
long enough to leach to 70 cm, but at 20 C, more rapid decomposition de-
creased the penetration to 30 cm  (Spiridonov and Yakovlev 1967). Re-
peating atrazine treatment had neither increased nor decreased  the degree
                                     22

-------
of penetration after three annual applications (Spiridonov et al. 1970a),
In red soils under subtropical conditions, atrazine penetrated 50 cm
within forty days after application of ten kg/ha, and to 70 cm 40 days
after 20 kg/ha were applied (Spiridonov et_ al. 1968).  Khubutiya and
Gigineishvili (1971) detected residues from 16 kg/ha or less of atra-
zine at 40 cm in brown forest soils within 60 days.  After 25.8 cm
precipitation spread over a winter, atrazine had leached to 20 cm in
loam, but to 80 cm in sand (Pop et al. 1968) whereas White and co-wor-
kers (1967) recorded only three inch penetration (7.5 cm) after 2.5
inches (6.3 cm) of simulated rain.  Bailey and White concluded that the
depth of pesticide penetration into soil depends not only on the degree
of reversible and irreversible absorption, but also on chemical reac-
tions of the pesticide, its solubility, the amount applied, and on the
average flow velocities, the pore geometry of the soil, and the soil
moisture at the time of application.  Degradation was suggested as a
major factor determining the penetration of atrazine into the soil
(Green et_ al. 1968, Harris ert a^. 1969).
In assessing the information available on the dissipation of atrazine
in the soil, and its effects on the environment during such dissipation,
two elements must be stressed:  first, atrazine is by function a soil
treatment whose action depends on its persistence and most studies
dealt with the herbicidal persistence of atrazine and its phytotoxic
metabolites in the plow layer and/or root growth layer of the soil;
secondly, application of atrazine to the soil was in amounts and prac-
tices which might approximate agricultural usage, essentially all of
the atrazine so applied is accessible to soil, if not to air, sun, and
plants.  It was estimated that the half-life of atrazine at 20 C in
sterile soil would be 9 to 116 years (Hance 1967).  The estimate, ex-
trapolated from data of herbicide slurries at 85-107 C, was criticized
because adsorption is an exothermic process which would be decreased at
the high temperatures of the slurries (Armstrong and Chesters 1968).
What the consequences of preventing adsorption would be has not been
                                   23

-------
considered, but virtually all data point to greater biological persis-
tence, and/or greater leaching, in light soils with little adsorption.
Between soil and water—On thin-layer chromatography, atrazine was
found to be more mobile than its metabolites, and to migrate indepen-
dently of them.  Under laboratory conditions, water transport at 25°C
             —8   2
was 15.3 x 10   cm /second (Helling 1971).  When fallow soil was treated
with atrazine, a 2.5 inch simulated rainfall caused the largest loss
of atrazine soon after application, and the Largest losses in such a
rain occurred in the first portion of the rainfall.  The amount depen-
ded on the soil temperature, but was of the order of 2.3 ppm in the run-
off when 2.2 kg/ha of atrazine had been applied (White et_ al_. 1967).
When rain fell after seven days, about 0.15 percent of the atrazine was
lost in runoff from contour-planted soil; ridge-planting reduced the
runoff and consequently the atrazine losses.
Of the atrazine lost in runoff, proportionally more was sediment-asso-
ciated than water-associated (Ritter et al. 1974).  In a heavy-texture
soil, four to six times as much sediment was lost from conventionally
tilled plots as from no-till plots, and surface water contained more
atrazine than did the water in drainage tiles (Schwab et al. 1973).
Atrazine polluted groundwater in wet years and in the spring in which
it was applied (Leh 1968).
In an aquifer, when 1.28 ppm of several pesticides were introduced into
a dual function well, atrazine migrated 30 feet from the point of entry
after 50 to 150 hours, but never more than 150 feet during the ten days
before the aquifer was decontaminated (Schneider et al. 1971) .  After
application in fish ponds, water residues decreased 90 percent in two
weeks, and atrazine levels in sludge exceeded water levels within days.
After eight weeks, water levels were at approximately one percent of
the original levels (Maier-Bode 1972).  Another indication of the con-
tamination of water by atrazine is the occurrence of atrazine and its
metabolite in the drinking water of New Orleans (Anonymous 1974b).
                                   24

-------
Volatilization—Approximately 80 percent of the atrazine on aluminum
planchets volatilized within 48 hours, but the addition of even small
amounts of co-extracted plant materials reduced volatility sharply
(Walker 1972).  Under infra-red lamps at 52° to 61°C, 95 percent vola-
tilized from planchets in 24 hours  (Foy 1963) but only 11 percent evap-
orated from the soil surface in two days at 40 C at an air velocity of
two liters/minute.  Decreasing the temperature or the air velocity sig-
nificantly reduced losses due to volatilization (Burt 1974).  More at-
razine volatilized from wet sand than from dry (Kearney et al. 1964) .
Jordan et al. (1970) reported a 65 to 85 percent loss of phytotoxicity
in 60 days when atrazine was exposed to light, but the effects of
photolysis and volatilization were not separated.
Into organisms—Pond treatment with atrazine led to accumulation of the
herbicide by algae and by water fleas (Daphnia), but carp, although they
also accumulated atrazine, eliminated it rapidly (Maier-Bode 1972).  In
the terrestrial-aquatic model ecosystem (Metcalf et al. 1971), the eco-
logical magnification values (EM) for atrazine in the alga, snail and
fish were only 75.6, 7.5 and 11.0, respectively.  These organisms also
contained two dealkylated metabolites of atrazine which had EM values
similar to those of atrazine itself.  Atrazine was judged unlikely to
be heavily accumulated in aquatic food chains (Sanborn 1974, Metcalf
and Sanborn 1975).  When laying hens were fed 0.5 ppm atrazine for six
weeks, no residues were detected in the yolks of their eggs (Foster et
al. 1972).
Persistence-
Atrazine was less persistent than either amiben or 2,3,6-TBA (Burnside
1965).  Bryant and Andrews (1967) stated that atrazine phytotoxicity
was lost after 16 weeks in clay loam and after 24 weeks in silt loam,
but considerable experience suggests that phytotoxicity can carry over
to the next season (WSSA 1974).  Andreeva-Fetsadzhieva (1967) stated
that atrazine phytotoxicity persisted for 4.5 months in chernozem-smol-
                                   25

-------
nitsa soil when 427 cm of rain fell, but persisted longer during droughts.
In a Nebraska loam, atrazine phytotoxicity from treatment with ten Ibs/A
(11.2 kg/ha) persisted into the third growing season  (Burnside et al.
1965) and similar results were observed in the USSR from 20 kg/ha (Ark-
harova 1973).  Persistence increased as concentration increased (Hance
and McKone 1971) but decreased as temperatures increased (Roeth et al.
1969) and as humidity above anaerobic soils approached 60 percent (Spi-
ridonov and Kamenskii 1970).
The climate did not affect atrazine persistence as much as the soil
characteristics, but a drier climate led to greater persistence than a
wet climate.  Coarse soil led to greater atrazine carryover between
seasons than did fine soil (Burnside et^ al_. 1969).  In Austria, phyto-
toxic persistence increased with increasing soil humus in dry weather
but decreased with increasing soil humus in wet weather (Neururer 1972) .
Clay or charcoal added to soil decreased phytotoxic persistence of at-
razine (Harvey 1973, Moyer et^ al^. 1972a) and persistence was greater
in silty clay loam than in loam (Burnside et ai_. 1971) .
In silty loam, atrazine persisted longer at 90 cm than at 40 cm, and
the lowest persistence occurred at 15 cm (Lavy et al. 1973).   (See Table
2).  When placed in tubes at three, nine and 15 inches in the soil at
twelve locations in the United States and Puerto Rico, persistence was
61 percent greater after three months at 15 inches (37.5 cm) than at
three inches (7.5 cm).  Geographical variations in persistence were not
entirely explainable  (Harris et^ al. 1969).
In Puerto Rican sugarcane soil, atrazine was more persistent than diuron
(Liu et^ al. 1971).  Under field conditions the relative persistence of
six herbicides was:  simazine and diuron > trifluralin and atrazine
> fluometron > prometryne (Horowitz 1969).  Atrazine was also found in
14.1 percent of 199 soils with a history of atrazine usage (Wiersma et
al. 1972).
                                    26

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27

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Effects on Non-Target Species-
Microorganisms—Of the numerous studies on the effects of atrazine on
soil respiration, only one showed an effect at less than 20 kg/ha:
Spiridonov and Spiridonova (1971) claimed five to ten kg/ha of atra-
zine stimulated soil respiration while 20 kg/ha depressed it.  Depres-
sion of soil respiration was also observed by Whitworth et al. (1965),
Liu and Cibes-Viade (1972), Eno (1962), Bartha and Lanzilotta (1967),
but in all cases more than 160 kg/ha were applied.  Stimulation of soil
respiration for 30 days at over 1000 kg/ha was observed by Bartha and
Lanzilotta (1967); inhibition occurred after the 30 day period.  Atra-
zine also stimulated soil respiration at levels not exceeding 25 kg/ha
(Spiridonov and Spiridonova 1971, Liu and Cibes-Viade 1972, Balicka and
Sobieszcsanski 1969).  Most common, however, were reports of no effect
(Liu and Cibes-Viade 1972, Kulinska 1967a, Eglite and Folkmane 1967,
Corke and Robinson 1960) at levels up to 512 ppm (1138 kg/ha) (Eno 1962)
In an experiment specifically designed to guage the effects of soil
disposal of pesticides, Stojanovic et al. (1972a) concluded that five
tons/A of pure atrazine   (5,000 ppm) inhibited soil respiration by 22
percent over a 56 day period, while formulated atrazine inhibited soil
respiration by 43 percent over 56 days.  These data fit the theory that,
whereas agricultural levels of atrazine do not inhibit soil respiration,
massive amounts do.
At levels approximating its agricultural use, atrazine almost always
stimulated nitrification and soil nitrate levels (Zavarzin 1966, Tula-
baev and Tamikaev 1967, 1968, Tsvetkova 1966, Belobrov 1972, 1974, An-
dreeva-Fetvadzhieva and Kolcheva 1970), although Siradze (1969) noted
that the stimulation of nitrification occurred the second and third
growing season after atrazine application.  Stimulation of nitrifica-
tion was not observed above 15 kg/ha, but Eno (1962) noted no signifi-
cant effect of atrazine at levels below 512 ppm  (1,138 kg/ha) with in-
hibition at higher levels.  Casely and Luckwill  (1964) and Thorneburg
                                    28

-------
and Tweedy (1973) observed no significant effects on nitrification at
levels of 12.4 kg/ha and 26.7 to 53 kg/ha, respectively.
Four kg/ha stimulated ammonification in the second and third season
after atrazine was applied (Siradze 1969), but Zavarzin and Belyaeva
(1966) reported that unspecified levels of atrazine inhibited ammoni-
fication.  The available potassium and phosphate levels in the soil were
increased in podzol (Tsvetkova 1966) and in Ukrainian forest steppes
treated with six to ten kg/ha (Belobrov 1972) but not in chernozem
treated with six to ten kg/ha (Belobrov 1974).  Four kg/ha caused in-
creases in soil phosphate levels in the second and third season after
atrazine treatment (Siradze 1969).
Atrazine increased the total numbers of soil microorganisms at three
kg/ha in light chestnut soil (Stepanova 1969) and at five to ten kg/ha
(Spiridonov and Spiridonova 1971), but higher levels were inhibiting
(Spiridonov and Spiridonova 1971, Kuz'mina 1968).  In peat-podzolic soil,
however, 75 kg/ha stimulated the main groups of microorganisms (Mashta-
kov et^ al_. 1962).  The effect observed depended on time of observation,
since an immediate decrease in the total number of microorganisms in
light chestnut soils was followed, after two months, by an increase to
twice the numbers in control soil (Stepanova 1967).  Pantera (1972)
considered atrazine to be less potent an inhibitor of soil microorganisms
than monuron, but more potent than either prometryne or Antiperz.  Zu-
bets (1970) considered atrazine to be a strong microbial inhibitor.  At
100 ppm, atrazine did not affect microflora in Macedonian soils (Mick-
ovski 1968).
The effects of atrazine on nitrogen-fixing bacteria vary from inhibi-
tion (Rankov 1968, Wegrzyn 1971, Tulabaev 1971, Zubets 1973) through no
significant effects (Peshakov et_ _al. 1969, Casely and Luckwill 1964) to
stimulation (Zubets 1970, Spiridonov and Spiridonova 1971, Andreeva-
Fetvadzhieva and Kolcheva 1970).  Although higher levels tended to be
inhibitory and lower levels stimulatory, no conclusions could be drawn
                                    29

-------
as to absolute values to achieve either.
Atrazine inhibited ammonifying bacteria under unspecified conditions
in soil (Peshakov et_ aJL 1969), at three kg/ha on meadow soil  (Tulabaev
and Tamikaev 1968), and cellulolytic bacteria were probably inhibited
in light soils (Klyuchnikov et^ £LU 1964, Stepanova 1967) although no
significant effect was reported in one study (Amantaev et al.  1963).
Stimulation of cellulolytic bacteria occurred on peat-bog soil  (Gwrino-
vich et al. 1962) and at five to 20 kg/ha  (Spiridonov and Yakovlev  1968,
Spiridonov and Spiridonova 1971).  Bacterial cellulolytes were more sen-
sitive to atrazine than cellulolytic fungi, and no resistance was ob-
served in cultures from atrazine-treated soil (Sobieszanski 1968).
Effects on cellulolytic microorganisms were not, however, as severe as
effects on nitrifying bacteria (Tulabaev 1971) .
AzotobaateT was inhibited by unspecified levels of atrazine (Peshakov
et al. 1969) and by three kg/ha (Tulabaev  1971) but not by one ppm  or
ten ppm in cultures (Wegrzyn 1971) .  Bacillus subtilis was inhibited in
cultures containing unspecified levels of  atrazine (Kuz'mina 1968)  and
Coooaaeae increased relative to Bacillaoeae (Ghinea 1967) but  no effect
on Apthpobaotev was seen in the presence of two to five percent  (20,000
to 50,000 ppm) atrazine if sugar was added to the culture (Micev and
Bubalov 1972).
Inhibition of soil fungi was reported repeatedly (Bakalivanov  1971,
1972, Klyuchnikov et_ al. 1964, Spiridonov  and Spiridonova 1971, Zubets
1973, Simon-Sylvestre 1974) as was no effect (Peshakov et al.  1969,
Amantaev et_ al. 1963, Tulabaev and Tamikaev 1968, Belobrov 1972).   Sti-
mulation of fungi was also reported at two or 12 kg/ha in sod-podzolic
soil  (Zubets 1973) and at about nine to 18 kg/ha (Kuzyakina 1971) and
occasionally for low levels of atrazine in cultures  (Manturovskaya  1970),
At low levels, saprophytic fungi were stimulated more than pathogenic
fungi while at higher levels  (17.5 ppm) all species were inhibited
(Richardson 1970).
                                   30

-------
When five tons per acre of atrazine (5,000 ppm) were incorporated into
loam soil, a slight stimulation of fungi occurred.  StTeptomyees were
stimulated by analytical grade atrazine but inhibited slightly by for-
mulated atrazine (80 percent wettable powder)  (Stojanovic et al. 1972a).
Actinomycetes were stimulated by ten kg/ha in moor soil  (Kuz'mina 1968)
and their numbers unaffected by two or 12 kg/ha in sod-podzol (Zubets
1973) but their taxonomy was altered in the absence of numerical ef-
fects (Ghinea 1967).  Trichoderma growth was inhibited for ten months
on peat-bog soil (Gwrinovich et_ al_. 1962) and even 0.01 kg/ha depress-
ed growth of Fusayiuni, but not of Penicillium or Aspergillus3 on turf-
podzol (Gorlenko et al. 1969).  Atrazine more drastically affected fun-
gi than either simazine or prometryne (Manturovskaya 1970).
Voets, Meerschman and Verstraete (1974) analyzed the effects of 15
years treatment of orchard soil with atrazine, at four kg/hg/year.
Changes in microbial population included temporary increases in the
numbers of ammonifying and proteolytic organisms, and temporary de-
creases in the numbers of nitrifying, amylolytic and denitrifying or-
ganisms.  The numbers of Asotobaater increased permanently, and perma-
nent decreases occurred in the numbers of anaerobic, spore-forming, and
cellulolytic microorganisms.  There was a concomitant loss of ground
cover and soil organic matter.
Atrazine inhibited soil algae (Mikhailova and Kruglov 1973), particu-
larly at high levels (Pantera 1970), but was less toxic than ametryne,
neburon, or diuron (Hollister and Walsh 1973).  Pillay and Tchan (1972)
ranked the relative toxicity of six herbicides to algae as:  diuron »
neburon > monuron > atrazine > simazine > atratone.  Five ppm atrazine
caused 75 percent inhibition of Chloroaoceim in culture, and 0.5 ppm
caused 70 percent inhibition of Chtorella.  Even 70 ppm did not totally
inhibit the growth of these algae, however (Virmani e_t^ al_. 1975).  Pid-
gaiko (1971) considered atrazine toxic to zooplankton reproduction, but
the level of treatment was not available.
                                  31

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Besides differences in rates of application, soils, species examined,
and types of measurements made, the experiments cited are heterogeneous
with respect to the length of time of observation.  As noted by Stepa-
nova (1967), the application of herbicide may alter conditions by al-
tering moisture retention and the amount of organic matter present on
or in the soil.  The effects would differ in preemergence weed control
in a plowed field from general weed control in an orchard or fallow
field.   In the first case, atrazine would tend to minimize the amount
of organic material accumulating in or on the soil, and maximize mois-
ture loss.  In the latter cases, decaying organic matter would be in-
creased by herbicide treatment.  The responses of soil microorganisms
might well differ.  It is known that some molds and some bacteria can
utilize atrazine as a nitrogen source and, to a lesser extent, as a
carbon source (Goswami et_ al_. 1971, Nepomiluev and Kuzyakina 1972,
Mickovski and Verona 1967, and Kaiser e_t al_. 1970).  Manorik and Mali-
chenko (1971) suggested that there is adaptation by soil organisms to
the presence of triazines, a phenomenon which could explain shifts in
overall soil respiration as well as increases in particular species.
Plants—In addition to its herbicidal effects, atrazine is mutagenic in
barley (Hordeim vulgare) (Wuu and Grant 1966, Sharma 1973) although
Stroev (1968) did not induce mutations in barley at 12 hours' exposure
               _3
to less than 10  M concentrations of atrazine.  A metabolite of atra-
zine produced by atrazine-treated corn (Zea mays) is mutagenic in both
corn and yeasts (Galston 1976, Gentile and Plewa 1976, Plewa and Gen-
tile 1975, 1976a, 1976b, 1976c).
Invertebrates—At levels greater than 19 ppm, atrazine synergized para-
thion toxicity to fruit flies or mosquitos (Aedes aegypti-) (Liang and
Lichtenstein 1974).  In grassland soil, agricultural levels of atrazine
decreased the numbers of wireworms, springtails and earthworms, but not
of millipedes or mites.  The effect may have been secondary to changes
in vegation (Fox 1964).  Numerous species of aquatic invertebrates were
                                   32

-------
reduced by atrazine treatments of 0.5 to two ppm, but water beetles and
damselfly nymphs increased  (Pimentel 1971) .  One mg/ml  (1000 ppm) in-
creased fertility in the first generation  of water fleas  (Scapholeberis
muoronata and Ceveodaphnia quadrangula) in the first generation but de-
creased fertility in subsequent generations (Shcherban  1972).
Fish and amphibians—Schlueter (1970) considered atrazine toxic if used
carelessly near water, but not if carefully used.  Darwazeh and Mulla
(1974) noted no toxicity of 10 ppm atrazine to mosquito fish (Gambusia
affinis) after 48 hours, but one pound per acre (1.12 kg/ha) killed 26
percent of the fish after four days.  Hiltibran (1967)  reported that
bluegill fry and green sunfish fry survived eight to ten days' exposure
to ten ppm of atrazine.  The 48-hour LC    for rainbow trout was 12.6
ppm (Pimentel 1971).
Birds—The LC   of atrazine for two week old quail, pheasants, bobwhites
and mallards was above 5,000 ppm, but seven percent of  the quail and
30 percent of the mallards died when fed 5,000 ppm for  three days (Heath
j^ ajU 1972).  The hatching rate of hens'  eggs was not  reduced by 100
ppm atrazine injected into the yolk sac, and was reduced by only ten
percent when 200 ppm were injected (Dunachie and Fletcher 1967, 1970).
Mammals—The acute oral LD   of atrazine in rats is 3,000 to 3,080 mg/
kg (Pimentel 1971, Bashmurin 1974).  Atrazine caused bone marrow inhi-
bition and chromosomal aberrations when 0.033 to 0.1 x LD,.-. was inject-
ed intraperitoneally into rats (Kulakov 1970) and morphologica.1 changes
leading to death at 20 mg/kg/day in rats (Nezefi 1971) .
Conclusions-
Neither the persistence of atrazine itself nor its effects on soil mi-
croorganisms is extreme.  Nevertheless, there is no conclusive evidence
for degradation of the triazine ring under environmental conditions.
Atrazine and one of its metabolites have been detected in the New
Orleans water supply, suggesting widespread pollution and/or considera-
                                   33

-------
ble mobility of these compounds.  Large-scale soil disposal of an al-
ready pervasive contaminant of uncertain biodegradability cannot be
recommended.
                                   34

-------
Bromacil
Bromacil is the common name for 5-bromo-3-sec-butyl-6-methyluracil, a
general herbicide introduced by E. I. DuPont de Nemours Chemical Co.
in 1962 as Hyvar, and also marketed by U.S. Borax Co. as Hibor.  Bro-
macil is a white, odorless, crystalline solid with a melting point of
158° to 159°C and a water solubility of 815 ppm at 25°C.  Its solubi-
lity in ethanol is 134,000 ppm at 25 C.  Formulations include granules
and liquids, alone or in combination with other herbicides.  A review
of the toxicology, environmental fate, chemistry, production and use of
bromacil has recently been published (Burnam et al. 1975).
Degradation-
                                                         14
Biological—Wolf and Martin (1974) applied 2.88 ppm of 2-  C-bromacil
to a neutral sandy loam soil.   After 115 days, 53 percent of the bro-
mine content of the soil was still present as bromacil in one study,
                         14                  14
but  22.1 percent of the   C was released as   CO- over a 600 day ob-
servation period if soil water-holding capacity was maintained at 60
percent.  When soil water was at 100 percent of capacity, less than
                   14             14
0.5 percent of the   C evolved as   CO- in 145 days but all the broma-
cil had been altered to some extent.  Gardiner et^ al. (1969b) reported
                     14                         14
that 25.3 percent of   C-bromacil decomposed to   CO- after nine weeks
in the laboratory, but not in the field.  Metabolites included 5-bromo-
3-sec-butyl-6-hydroxymethyluracil; 5-bromo-3-(2-hydroxy-l-methylpropyl)-
6-methyluracil; and 5-bromo-3-(3-hydroxy-l-methylpropyl)-6-methyluracil.
The mutagen 5-bromouracil was not found.  Zimdahl and co-vorkers (1970)
characterized the degradation of bromacil in soil as following first-
order kinetics with no preliminary lag phase.  No data on specific mi-
croorganisms which degrade bromacil were available.
Rats fed 1,250 ppm bromacil for one month metabolized it to 5-bromo-3-
sec-butyl-6-hydroxymethyluracil which was excreted in their urine,
                                  35

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mostly in conjugated form.  Five or six other metabolites, but not 5^
bromouracil, were also found (Gardiner et_ al. 1969a).  Dairy cows fed
five ppm of bromacil excreted 0.019 ppm in their milk; excretion in-
creased to 0.13 ppm when 30 ppm bromacil were fed.  No urinary or fe-
cal bromacil was found, but no attempt was made to identify metabolites
(Gutenmann and Lisk 1970).
Photolytic—When one to ten ppm of bromacil in aqueous solution were
exposed to summer sunlight for four months, very little was converted
to 5-bromo-6-methyluracil.  Recovery of bromacil was almost quantita-
tive (Moilanen and Crosby 1974).
Chemical and physical—Liquid ammonia and metallic sodium decomposed
100 percent of analytical grade bromacil (Kennedy et al. 1972a) but
I8N H2SO,  only partially decomposed it (Kennedy et al. 1972b) .  At 250
C, broraacil was changed from a white to a black solid; the major decom-
position product was tentatively identified as 3-sec-butyl-methyl-ura-
cil (Stojanovic et^ al_. 1972b) .  When bromacil was heated to 600 C in a
muffle furnace, 88.8 percent of the formulated herbicide (80 percent
wettable powder) was lost; at 1000 C, 91.3 percent was lost (Kennedy et
al. 1969).  The volatile products of burning bromacil at 900 C were car-
bon monoxide, carbon dioxide, chlorine, hydrogen chloride and HN_.  Hy-
drogen bromide was not produced (Kennedy et aL_. 1972a) .
Transport-
Adsorption of bromacil to soil corresponds to a Freundlich isotherm,
suggesting physical rather than chemical adsorption (Rhodes &t_ al_. 1970,
Hague and Coshow 1971).  After six to seven years' application of bro-
macil to loam orchard soil, less than three percent of the bromacil was
recovered at depths of one meter although considerable leaching to the
10-20 cm layer had occurred.  Leistra et al. (1975) considered this less
leaching than was implied by the mobility of bromacil on thin-layer chro-
matographs.
                                    36

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Persistence-
Bromacil was more persistent in sandy than in clay  soil, and more per-
sistent in lower soil layers than in surface layers  (Stecko 1971).  One
year after the last of six to seven annual applications of bromacil to
loam soil at 1.5 to 3.0 kg/ha/year, 54 percent of an annual dose was
present in the soil.  Leistra and co-workers (1975) calculated  this to
correspond to a loss of 35 percent per year.  The persistence in soil
was even greater than these data suggest, since 20  to 30 percent of
the bromacil could have been taken up by plants (Leistra et_ al_. 1975).
In California agricultural soils bromacil persisted for over 30 months
(Lange et_ al. 1968).  Weber and Best (1972) estimated that full weed
control by bromacil persisted for over 18 weeks, and a half-life of five
to six months was estimated by Gardiner et al. (1969) in silt loam when
four Ibs/A (4.48 kg/ha) were applied.  Persistence  in the laboratory
was much shorter as 25.3 percent of the bromacil decomposed to CO- af-
ter nine weeks (Gardiner et al. 1969).
Effects on Non-Target Species-
Microorganisms—In the laboratory, 2.88 ppm bromacil did not alter car-
bon dioxide evolution in neutral sandy loam (Wolf and Martin 1974) nor
did four ppm in sandy loam (Steyn and Wolff 1969) or 100 ppm in two
clay loams or in sandy loam (Liu and Cibes-Viade 1972) .
When pure bromacil was incorporated into loam soil  at five tons per acre
(5000 ppm), 16 percent inhibition of carbon dioxide evolution occurred,
but formulated bromacil inhibited carbon dioxide evolution by only nine
percent.  Bacteria were stimulated by pure and by formulated bromacil
at 5000 ppm, fungi were stimulated by 5000 ppm pure bromacil, and strep-
tomycetes by 5000 ppm of either pure or formulated bromacil (Stojanovic
jet^ ajL. 1972a) .  Algal growth, in contrast, was strongly inhibited by
0.32 ppm of bromacil (Pillay and Tchan 1972), a result not surprising
for an inhibitor of photosynthesis.  Bromacil was not mutagenic in a
                                   37

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bacteriophage, and did not inhibit the mutagenicity of 5-bromouracil
(McGahen and Hoffmann 1966).
The median tolerance limit for bluegills and rainbow trout was about
100 ppm at 24 hours, falling  to 75 or 80 ppm at 48 hours (WSSA 1974).
The eight-day LC   for bobwhite quail and for mallard ducklings was
over 10,000 ppm, and the acute oral LD   for rats was 5200 mg/kg (WSSA
1974).
Conclusions-
The few data on bromacil transport and persistence in soil do not sug-
gest major problems resulting from its disposal in soil.  Since it is
moderately persistent and moderately mobile, care would be required to
prevent its leaching into planted areas before it is degraded.
                                  38

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CDAA
CDAA is the common name for 2-chloro-./l/,]l/-di-2-propenylacetamide, a se-
lective pre- and post-emergence herbicide introduced by Monsanto Co. in
1957 as Randox.  An oily amber liquid with a boiling point of 74 C at
0.3 mm mercury, CDAA decomposes at 125 C and has a vapor pressure of
9.4 x 10~  mm mercury at 20°C.  Its water solubility is 20,000 ppm at
25 C and 200,000 ppm in kerosene at 49 C.  It is synthesized by reac-
ting chloracetyl chloride with diallylamine.
Degradation-
Pseudomonas striata degraded 36.8 percent, and an Achromobaetep species
degraded 24.5 percent, of CDAA during six days' incubation with soil
(Kaufman and Blake 1973) .  Dairy cows which were fed five ppm of CDAA
for four days excreted no intact CDAA in their milk, feces or urine (St.
John and Lisk 1974).  Microbial degradation is thought to be the major
detoxifying process in soil, with chemical hydrolysis secondary (WSSA
1974).
Transport-
Gentz (1960) considered CDAA to leach little, and noted that soil-ad-
sorbed CDAA retains its phytotoxicity.  Deming (1963) noted' that CDAA
leaches through soil, but did not present data.  The adsorption of CDAA
to soil is directly proportional to soil colloid content and, in the ab-
sence of adsorption, four Ibs/A (4.48 kg/ha) of CDAA volatilized in less
than eight hours at temperatures above 7 C (WSSA 1974).  Volatilization
increased with increasing water saturation of soil colloids and with de-
creasing organic matter content of soil; on occasion, volatilization de-
creased with increasing temperature (Deming 1973).  No data were avai-
lable on transport between soil and water.
                                    39

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Persistence-
CDAA applied to soil at eight Ibs/A (8.96 kg/ha) persisted four weeks
in moist soil and somewhat longer in dry soil.  Persistence was greater
in soil at 80°F or 100°F than at 40°F or 60°F (Gantz 1960).  Increasing
temperatures decreased its persistence in moist soil (Otten et al. 1957)
Within three months, 160 ppm CDAA in soil had lost all phytotoxicity
(Sheets 1959).  The usual length of persistence of agricultural levels
of CDAA is considered to be less than five weeks (Sweet et al. 1958) or
three to six weeks (WSSA 1974).
Effects on Non-Target Species-
In the laboratory, unspecified levels of CDAA inhibited nitrification
in soil (Otten et_ a^. 1957b).  In culture, Rhizoetonio., ScleToti-wn Tol-
fsii3 and Scleroti-um batatioolo. were completely inhibited by 24 hours'
exposure to two Ibs/A (2.24 kg/ha) of CDAA, suggesting it is fungicidal
at agricultural levels (Bain 1961).  Streptomyoes was not affected by
CDAA at levels of six to 300 Ibs/A (6.72-336 kg/ha) (Pimentel 1971).
The LC,.0 for quail was reportedly greater than 5620 ppm, and for rain-
bow trout and bluegills, the median tolerance levels were 2.0 ppm and
6.6 ppm, but no length of exposure was given (WSSA 1974).  The acute
oral LD 0 of CDAA to rats was 750 mg/kg (WSSA 1974) .
Conclusions-
The short persistence of CDAA would make it suitable for soil disposal
but for the complete lack of data concerning its degradation products,
their persistence and their effects on soil processes.  Data on trans-
port through soil are also insufficient for valid conclusions to be
drawn.
                                    40

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Chloramben
Chloramben is the common name for 3-amino-2,5-dichlorobenzoic acid, a
selective pre-emergence herbicide introduced in 1958 by Amchem Products,
Inc. as Amiben or Vegiben.  Chloramben is a white, odorless amorphous
powder which melts at 201 C and has a water solubility of 700 ppm at
25 C.  It is synthesized by nitration of the 2,4-dichlorobenzoic acid
to produce 2,4-dichloro-3-nitrobenzoic acid, which is reduced to pro-
duce chloramben.
Degradation-
Chloramben is degraded by microorganisms, but no specific species or
products were identified (WSSA 1974).  Detoxification in highly organic
soils is slow and not affected by pH within the normal soil range (Cor-
bin and Upchurch 1967).  In aqueous solution chloramben is decomposed
                                            _3
by sunlight or ultraviolet light:  when a 10  M aqueous solution (206
ppm) was exposed to sunlight, 49 percent remained after six hours.  Ex-
posed to a sun lamp, 51 percent persisted for six hours.  In glass jars,
4 lbs/40 gal. (1,200 ppm) water was not significantly decomposed by ex-
posure to sunlight for six hours, and the triethylamine salt was less
sensitive to sunlight than pure chloramben (Sheets 1963).  No data on
physical or chemical decomposition were available.
Transport-
Chloramben was less readily adsorbed by activated carbon than were CIPC,
trifluralin, 2,4-D or diphenamid (Coffey and Warren 1969).  It is little
adsorbed by soils in comparison with most herbicides, but adsorbs more
readily to organic soils than to sand or clay (Donaldson and Foy 1965).
In consequence of its slight adsorption, chloramben leaches readily
(Donaldson and Foy 1965) even in muck albeit more in sand or silt loam
(Eshel and Warren 1967).  On a scale of six, chloramben was ranked 5.2
                                  41

-------
in silty clay loam and 5.7 in sandy loam, both indicating high mobility.
Only dicamba was more mobile on these soils (Harris 1967).
Persistence-
In silty clay loam at temperatures between 15° and 35°C, chloramben was
less persistent at higher temperatures.  Although the usual persistence
of chloramben in soil is six to eight weeks (WSSA 1974) and the usual
period of phytotoxicity in Nebraska soils is four to six weeks, no de-
gradation of chloramben was seen after 11 months in moist soil at 15
C.  At 25 C and 35 C, 42 and 46 percent decomposed in eleven months, in-
cluding a lag period of five to six months (Burnside 1965).
Effect on Non-Target Species-
At agricultural levels, chloramben did not affect soil respiration
(Corke and Robinson 1960), mobile nitrates, phosphates, or potassium
compounds, soil microorganisms or the redox enzymatic activity of soil
(Geshtovt et. .al. 1974).  At 0.4 kg/ha Pashkin (1971) observed an in-
crease in soil nitrates and soil potassium, and four to six kg/ha de-
pressed soil catalase for ten days (Soldatov et al. 1971).  At five
kg/ha, Azotobacter growth was inhibited one month after application of
chloramben (Shkola 1970).  Of crayfish exposed to 0.3 to 3.0 mg/liter
(0.3-3.0 ppm) for an unspecified length of time, one third survived
(Sestokas 1967), while up to 1000 ppm of chloramben in 60 percent suc-
rose was not toxic to bees (Morton and Moffett 1972).  The acute oral
LD   of chloramben to rats was 3500 mg/kg (WSSA 1974) or 5620 mg/kg
(Pimental 1971).
Conclusions-
There is not enough information on the degradation of chloramben, or on
its persistence in soil, to permit conclusions as to the feasibility of
its disposal in soil.
                                   42

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2,4-D and 2,4,5-T
2,4-D is the common name for the systemic herbicide 2,4-dichlorophen-
oxyacetic acid, introduced by Amchem Products, Inc. in 1942.  Salts and
esters of 2,4-D are its most common herbicidal formulations.  The free
acid is white, crystalline, and odorless if pure; it has a melting
point of 140° to 141°C for pure 2,4-D, 135° to 138°C for technical 2,4-D,
and a boiling point of 160 C at 0.4 mm mercury.  Its solubility at 25 C
is 900 ppm in water, 850,000 ppm in acetone and 1,300,000 ppm in etha-
nol.  It is produced by the interaction of 2,4-dichlorophenol and sod-
ium monochloracetate.  The sodium salt of 2,4-D has a water solubility
of 25,000 ppm at room temperature and is soluble in aqueous alkali and
in alcohol, but insoluble in petroleum oils.  Martin (1968) lists the
many other salts of 2,4-D with their melting points and water solubi-
lity.  The most common ester used is the isopropyl ester, an almost
colorless liquid with a boiling point of 130 C at one mm mercury.
2,4,5-T is the common name for the herbicide 2,4,5-trichlorophenoxy-
acetic acid, introduced by Amchem Products, Inc. in 1944.  The acid is
a white, crystalline solid with a melting point of 154  to 155 C, a de-
composition temperature above 200 C and a water solubility of 238 ppm
at 30°C.  Its solubility in ethanol is 590 ppm at 50°C (WSSA 1974).
The salts of 2,4,5-T are soluble in petroleum oils.  The technical acid
is 98 percent pure with a melting point of 150° to 151°C (Martin 1968).
2,4,5-T is produced by the interaction of sodium monochloracetate with
2,4,5-trichlorophenol.
Degradation-
Biological—Two modes of degradation have been established for 2,4-D:
dechlorination (Rogoff and Reid 1954, Bell 1957, 1960) and breakdown of
the side chain (Taylor and Wain 1962, Steenson and Walker 1957).  Warm,
moist conditions and the addition of organic matter to the soil accele-
                                   43

-------
rate 2,4-D disappearance  (Loos 1969).  Audus (1949, 1950, 1951, 1952)
conclusively established  the microbial degradation of phenoxyacetic
acid herbicides.  Data on the degradation of 2,4-D and 2,4,5-T by soil
microorganisms are shown  in Table 3.  Bell (L957) observed a lag before
Aohromobaoter degraded 2,4-D, and suggested that the necessary enzymes
were induced.  Altom and  Stritzke (1973) reported a five day lag before
2,4,5-T degradation began in forest soil, and no lag, or a less than
five day lag, for 2,4-D degradation.  While 2,4-D was equally rapidly
degraded in all three soils, 2,4,5-T was more rapidly degraded in soil
taken from under grass than from under trees.
Rogoff and Reid (1954) isolated a Corynebaoteri-um which dechlorinated
1,000 ppm of the sodium salt of 2,4-D in as Little as three days, and
80 percent of 1,000 ppm in solution at a pH of 7.1, within four hours.
A Flavobactevi-wn isolated by MacRae and Alexander (1963) cleaved the
side chains of 2,4-dichlorophenoxypropionic acid, but not of 2,4-D;
longer side chains were more readily degraded than the propionic moiety,
and odd-numbered carbon-chains were more readily degraded than even-
numbered chains.  A similar result was obtained by Taylor and Wain
(1962), who concluded that in the ortho/para position, Cl did not inter-
fere in side chain cleavage, while a Cl at the para position inhibited
ortho-CI removal.  In their study, Noeardia ooeliasa, Pseudomonas3 and
Mi,evocooaus successfully  degraded omegra-phenoxyalkane carboxylic acids
while AchpomobaeteT and Flavobacteviwn did not.
Faulkner and Woodcock (1965) reported that bacterial degradation of
phenoxyacetic acids included ring fission while fungal detoxification
consisted of nonspecific hydroxylation of the ring without fission.
An increase in the speed  of degradation by microorganisms occurred with
repeated 2,4-D applications (Torstensson et_ aj^. 1975).  Skryabin et al.
(1974), however, were unable to culture microorganisms using 2,4-D as
the sole source of carbon and concluded that 2,4-D was cometabolized to
the extent of partial side chain oxidation, but that the aromatic
                                   44

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nucleus was intractable.  Cultures of planktonic algae removed signi-
ficant amounts of 2,4-D from cultures but its fate was not ascertained
(Butler et al. 1975).
Phenoxyalkanoic acids with a Cl in the meta position, such as 2,4,5-1,
are considerably more resistant to metabolism (Alexander and Aleem 1961,
Jensen 1963).  When 30 pg/ml (30 ppm) of 2,4-D and 2,4,5-T were placed
in nutrient solution,  2,4-D was degraded within ten days, while 2,4,5-T
persisted unaltered for three months (Whiteside and Alexander 1960).
The pathways of microbial metabolism of 2,4-D are shown in Figure 2.
When five tons per acre (11,227 kg/ha) of 2,4-D and 2,4,5-T were mixed
with soil, CO- evolution was depressed by the pure chemicals, but en-
hanced by formulated compounds, suggesting that the carriers are readily
biodegradable (Stojanovic et_ a^. 1972a).  The degradation of the 2,4,5-T
contaminant 2,3,5,7-tetrachloro-dibenzo-p-dioxin (TCDD) in soil has not
been demonstrated (Helling et al.  1973) .
The fate of 2,4-D and 2,4,5-T in animals has been reviewed by Paulson
(1975) who concluded that the nature of the metabolites in tissues,
urine, and feces is not well understood.  Neither 2,4-D (Bache et _al.
1964) nor 2,4,5-T (St. John et^ al. 1964) is excreted in cows' milk.  In
dogs, a 5 mg/kg dose of 2,4,5-T had a plasma half-life of 77 hours and
a body-clearance half-life of 86.6 hours.  In rats the plasma clearance
half-life ranged from 4.7 hours for a 5 mg/kg dose to 25.2 hours for 200
mg/kg.  The body clearance half-life ranged from 13.6 hours for 5 mg/kg
to 28.9 hours for 200 mg/kg (Piper e£ a^. 1973).  The half-life of an
unspecified level of radioactive 2,4,5-T was 97 hours in newborn rats
but 3.4 hours in adult female rats (Fang et al. 1973).  Five men ex-
creted unaltered 2,4,5-T in their urine with a 23.1 hour plasma clear-
ance half-life and a 23.06 hour body clearance half-life (Gehring et al.
1973) .
Photolytic—In the presence of UV light and of photo-activated ribofla-
vin, 2,4-D was converted to 2,4-dichlorophenol and other phenols.  The
                                    46

-------
              OCM,COOH
       3-CHLOROCATECHOL
   0         T 0
HO-C-CH=CH-CH=C-C-0!H
              CL
 "-CHLOROMUCONIC ACID
       COOH
                                                   3, j-DICHLOROCATECIIOL
                        HO-C-CH=C-CH=C-C-OH
                                CL   CL
                      a,Y-DICHLOROMUCO'IIC ACID
                             I
0
C-OH
H2c/ cnoH ^ —
0=C C-CL
\ */
c
H
a-CHLOROMALEYL-
ACETIC ACID
w
0
C- OH
- ^V=0
"/ '
CNc,C-CL

Y-CARBPXYM'
a-rm nRO-A™-1
 HOOC-C')2-CH-COOH  ~
          CL
CHLOROSUCCINIC ACID
                                                            ETHYLENE-
Hnoc-CH2-cii2-cooM

  SUCCINIC ACID
            PROPOSED PATHWAYS OF rucROBiAL M,ETAEOLisfi OF
                            (AFTER HENZIE
                              Figure  2
                                  47

-------
precise composition of the degradation products depended on the initial
concentration and pH of the solutions (Bell 1956) .  Ultraviolet light
above 290 nm converted the water-dispersed ethyl and 2-methylheptyl es-
ters of 2,4-D to 2,4-D acid and hydrogen chloride.  Dechlorination was
light-dependent, while the side chain cleavage was essentially a dark
reaction catalyzed by the HC1 produced by dechlorination.  The yields
were sufficiently great to suggest that these, reactions are significant
under field conditions (Binkley and Oakes 1974) .  Baur and Bovey (1974)
noted that 2,4-D in so-called polymer formula.tions was more susceptible
to degradation by long-wave UV light than were conventional 2,4-D for-
mulations.  Photolytic degradation of 2,4-D on silica gel chromatogra-
phic plates was enhanced slightly but definitely by xanthone, benzo-
phenone, and 4,4'-dichlorobenzophenone, and more extensively by anthra-
quinone (Ivie and Casida 1971).
Long-wave (356 nm) UV light decomposed the potassium salt of 2,4,5-T,
but not 2,4,5-T acid, at 30° and 60°C (Baur j£ a^. 1973).  In water,
2,4,5-T was very slowly photolysed to 2,4,5-trichlorophenol and 2-OH£
4,5-dichlorophenoxyacetic acid.  Some 4,6-dichlororesorcinol, 4-chloro-
resorcinol, and 2,4-dichlorophenol were also formed, as well as 4£
chlororesorcinol and unidentified polymeric compound.  No 2,3,6,8-tet-
radichlorodibenzo-p-dioxin (TCDD) was detected (Crosby and Wong 1973).
TCDD was photolytically extremely stable in soil, and almost as stable
in water (Helling et^ al. 1973) .
Chemical and physical—In natural surface waters in the laboratory, the
isopropyl, isooctyl and isobutyl esters of 2,4-D were hydrolyzed to the
free acid and corresponding alcohol in nine days.  The alcohols decom-
posed further, but 2,4-D acid persisted for up to 120 days.  After con-
siderable microbial adaptation, lake muds decomposed 81 to 88 percent
of 2,4-D within 24 hours (Aly and Faust 1964).
Complete degradation of 2,4-D and 2,4,5-T occurred in the presence of
liquid ammonia plus either metallic sodium or lithium (Kennedy et al.
                                   48

-------
1972a).  Partial decomposition of 2,4-D was achieved with 70 percent
Ca(C10)9, 8N NaOH and 18N H_SO .   Partial decomposition of 2,4,5-T oc-
       £*                   £  ^r
curred in the presence of 8N NaOH and I8N H^O^ (Kennedy at al.  1972b).
Storage of 2,4-D in cardboard boxes resulted in a ten percent loss after
three years, and 30 percent after six years but glass containers de-
creased these losses (Chorbadzhiiska 1966).
Polymeric formulations were less easily destroyed by heat than were
conventional formulations of 2,4-D (Baur and Bovey 1974).  Hee and
Sutherland (1974) determined that the methylamine and n-butylamine salts
of 2,4-D decomposed to form maximum amounts of the amide at 140  to
150 C, while the dimethylamine salt required temperatures above 160 C
for amide formation and the n-dodecylamine and n-tetradecylamine salt
formed amides most rapidly between 150  and 170 C.  Other decomposition
products included 2,4-dichlorophenol, imines and lactones.  The amides
of 2,4-D decomposed above 200°C.
When 2,4-D and 2,4,5-T were heated in muffle furnaces, over 99 percent
of both compounds had decomposed at temperatures below 600 C.  For
2,4,5-T, 27.4 percent decomposed below 200°C (Kennedy .et al. 1969).
Heating 2,4-D or 2,4,5-T to 900°C resulted in formation of the volatile
compounds carbon monoxide, carbon dioxide, chlorine, hydrogen chloride
gas and oxygen (Kennedy et_ al. 1972a, 1972b).  Although the thermal de-
gradation of both 2,4-D and 2,4,5-T is eminently feasible, the possi-
bility of dioxin production during pyrolysis makes it inadvisable with-
out rigorous monitoring of the conditions.
Transport-
Of ten herbicides, 2,4-D was least readily soil adsorbed.  The order
was:  2,4-D < fluometron < prometone < simazine, atrazine and diphena-
mid < prometryne « chlorpropham « trifluralin « benefin (Scott and
Phillips 1972).  On clays, the sodium salt of 2,4-D was least readily
adsorbed on bentonite and most readily on kaolin.  Both the butyl, iso-
propyl, and isooctyl esters were least readily adsorbed on kaolin and
                                   49

-------
most readily on bentonite.  Illite was intermediate in all cases (Faust
and Aly 1963).  The level of adsorption of 2,4-D on clay is always low
(Weber et al. 1965, Scott and Lutz 1971, Grover 1973) but increased to
some extent as pH increased (Helling 1971b, Frissel and Bolt 1962).
Salting out occurred at high concentrations of 2,4,5-T or 2,4-D (Frissel
and Bolt 1962).  On goethite, which is positively charged, 2,4-D was
maximally adsorbed at low ionic strength near its pK of 2.73 but its
ready desorption could lead to rapid leaching (Watson et al. 1973).
Adsorption on montmorillonite is physical (Khan 1974a, 1974c).
On humic acid, 2,4-D is probably also adsorbed physically rather than
chemically (Khan 1973a).  Esters of 2,4-D were more rapidly hydrolyzed
to the free acid in soil than in aqueous solution, and effectively be-
haved like the acid in moist soil (Grover 1973) .  Organic matter is the
major adsorbent of 2,4,5-T in soil (O'Connor and Anderson 1974).  Both
2,4-D and 2,4,5-T are minimally adsorbed by near neutral prairie soils
and strongly adsorbed by peat (Grover and Smith 1974) .
As expected from this low adsorptiveness, 2,4-D is characterized as a
mobile herbicide (Helling 1971a).  Nevertheless, little 2,4-D leached
more than five centimeters during rice field irrigation (Sokolov et al.
1974).  In North Carolina soil, 90 percent of 2.24 kg/ha of 2,4,5-T had
disappeared from the soil without penetrating significantly below 7.5
cm and without moving more than 12 meters downhill.  The low rate of
downhill movement was correlated with a low level of runoff (Lutz et al.
1973).  In calcareous silty loam in greenhouses, ten cm of irrigation
resulted in 35 cm leaching by 2,4,5-T (O'Connor and Wierenga 1973).
When plots treated with 2.2 or 4.4 kg/ha of 2,4-D were watered with
simulated rains of varying intensity, 26 percent of the 2,4-D butyl es-
ter, but only five percent of the amine salt, were washed off by the
strongest simulated rain, calculated as occurring once in a century.
For a storm calculated to occur once a year., 13 percent of the butyl
ester and four percent of the amine salt were washed off.  Most of the
                                   50

-------
2,4-D remained in the top 7.5 cm of soil.  TCDD, the dioxin contaminant
of 2,4,5-T, is highly immobile in soil  (Helling et a^. 1973).
Between soil and water—In a survey of western streams, 2,4,5-T was the
most frequently encountered contaminant, while 2,4-D reached the highest
levels:  0.99 pg/liter  (0.99 ppb) (Schulze et al_. 1973).  Treatment of
a pond with 2,4-D resulted in water residues of up to 0.067 ppm and per-
sisting 24 days, but soil residues persisted for over 85 days, decreas-
ing from 4.96 ppm on the first day to 0.1 ppm on the 95th (Frank and
Comes 1967).  The washoff from cultivated fallow sandy loam soil con-
tained no more than one ppm of the amine salt of 2,4-D but up to 4.2
ppm of the isooctyl and butyl esters  (Barnett et al. 1967).  Leaching
is expected to be great if rain is heavy and occurs soon after 2,4-D is
applied (Scott and Lutz 1971).  On grass-covered Houston black clay,
five sprayings of 2,4,5-T and picloram at 1.12 kg/ha resulted in soil
levels of up to 238 ppb, while runoff water contained 400 to 800 ppb of
pesticides if heavy rain followed application of the herbicides.  If
rain was delayed for over a month, runoff contained less than five ppb
of the herbicides (Bovey et al. 1974) .  After two applications per year
for three years, 2.24 kg/ha of a 1:1 mixture of picloram and 2,4,5-T
had contaminated groundwater.  Even a single treatment of 1.12 kg/ha
of the mixture led to water levels of one to four ppb picloram (Bovey
et al. 1975).
When 2,4-D was tested in the model ecosystem, no 2,4-D residues were
found in any of the organisms after 33 days (Sanborn 1974, Metcalf and
Sanborn 1975).
Persistence-
The average losses per day of 2,4-D and 2,4,5-T are shown in Table 4.
In all studies in which both herbicides were examined 2,4,5-T was more
persistent, which Alexander and Aleem (1961) attributed to meta-CI.
O'Connor and Wierenga (1973) noted that repeated application enhanced
                                   51

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the degradation of 2,4,5-T while high levels  (64 kg/ha) enhanced per-
sistence.  The maximum rate of degradation resulted in decomposition of
2,4,5-T at 40 ppm in 43 days in calcareous silty loam.  Altom and Stritz-
ke (1973) noted a lag of more than five days before 2,4,5-T degradation
began but no lag for 2,4-D degradation.
When 2,4-D was placed in field pits, the rate of degradation decreased
with increasing soil depth.  In anaerobic soils, degradation was extreme-
ly slow at all depths (Lavy et^ a!U 1973).  The optimum pH for 2,4-D de-
toxification was 5.3 (Corbin and Upchurch 1967).
The dioxin contaminant of 2,4,5-T, TCDD, persisted less than six years
in soil when 1,060 kg/ha of 2,4,5-T were applied to Lakeland sand (Hel-
ling ej^ al_. 1973).  The propyleneglycolbutylether ester of 2,4-D re-
mained in containers at the rate of 24 ml per five gallon drum and 146
ml per 55 gallon drum and was more persistent than emulsifiable con-
centrates of parathion (Archer 1975).
Effects on Non-Target Species-
Microorganisms—The effects of 2,4-D on soil processes and soil micro-
organisms are shown in Tables 5 through 11.  Among the consequences of
2,4-D application are an increase in the organic carbon content of soil
(Oh 1973) and an irreversible genetic effect  (sis) on Streptomyees glo-
bisporus and Stveptomyces fasciculus (Kiss 1966).  Resistance to 2,4-D
can be selected for (Sokolov et al. 1975).  Aerobacter aerogenes growth
was depressed for 25 generations in the presence of 1,000 ppm of 2,4-D
with a concomitant increase in the length of the lag phase before 2,4-D
was degraded.  At 5,000 ppm, however, the lag phase decreased even
though growth was inhibited for 91 serial subcultures (Dean and Law
1964).  Strains of AzobaoteT which were selected for resistance to 2,4-D
sometimes lost their ability to produce vitamins BI and B~ (Hammouda
1974).  Facultatively anaerobic bacteria were more sensitive to 2,4-D
under anaerobic than under aerobic conditions, while gram negative
                                   53

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    bacteria within each metabolic group were less sensitive than gram-posi-
    tive bacteria  (Hart and Larson 1966).  The sodium salt of 2,4-D was
    considered toxic to microorganisms in peat-podzolic soil at unspecified
    high levels  (Mashtakov at al. 1962).
    Metabolism in Tetrdhymena pyviformi-s was inhibited by 0.5 to 0.9 mM of
    2,4,5-T; cell division stopped for up to one hour and mitochondrial ox-
    ygen uptake  slowed.  Sensitivity decreased with time  (Silberstein and
    Hooper 1975).  In sandy or muddy soil five ppm of 2,4,5-T inhibited ni-
    trification while ten to 15 ppm enhanced nitrification (Cervelli et al.
    1974).
    Mixtures of dalapon and 2,4-D inhibited soil respiration of soddy-pod-
    zolic soil at two or 20 kg/ha but enhanced respiration at six and 60
    kg/ha (Bliev 1973).  Dicamba counteracted the inhibiting effect of un-
    specified levels of 2,4-D on phosphorus-mobilizing organisms, nitrifi-
    cation, and on saccharase and urease activity in leached chernozem
    soils (Svyatskaya 1972).
    Invertebrates—Beran and Neururer (1955) reported that 2,4,5-T, the so-
    dium salt of 2,4-D, and the butyl esters of 2,4-D and 2,4,5-T were not
    toxic to bees, but Kirkor and Giese (1960) found 0.01 percent (100 ppm)
    of 2,4-D in sugar to be toxic to bees.  Newly emerged honeybees were not
    acutely sensitive even to 1,000 ppm of 2,4-D or 2,4,5-T, but their mean
    lifespan was decreased by the esters of either acid (Morton et^ al.
    1972a).  Neither agricultural levels of 2,4-D butyl ester nor ten times
    agricultural levels affected soil microarthropods significantly after
    ten days or four months (Rapoport and Cangioli 1963) .  In the labora-
    tory the order of toxicity of eight herbicides to beetles (Bemb'i-d-ion)
    was:  sodium chlorate < dalapon < simazine plus amitrole < pyrazon
    < diquat < 2,4-D < chlorpropham (Mueller 1971).  Treatment with 40 Ibs/A
    (44.8 kg/ha) of an emulsifiable concentrate of the amine salt of 2,4-D
    did not affect the numbers of springtails, wire worms, or mites in
    grassland soil (Fox 1964).
                                       63
    

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    No mortality was found among oysters (Cras so street virginioa") exposed to
    0.1 ppm 2,4-D butoxyethanol ester for seven days or among pigtoe mussels
    (Pleurobena oordatvm) exposed to 100 Ibs/A (50 ppm) for 72 hours, to
    1000 Ibs/A (500 ppm) for 48 hours or to five ppm for seven days.  The
    oysters accumulated 18 ppm of 2,4-D which was eliminated after seven
    days in clear water (Butler 1965).  Secondary effects of 2,4-D and
    other herbicides in aquatic ecosystems have been reviewed by Hurlbert
    (1975).
    Fish and amphibians—At agricultural levels, 2,4-D is not toxic to the
    larvivorous fish Aplocheilus latipes and Zaooo platypus (Shim and Self
    1973).  Schlueter (1969) warned that 2,4-D and 2,4,5-T were toxic to
    fish if carelessly used.  Differences in toxicity between 2,4-D and
    2,4,5-T were not as great as differences between formulations:  the 24
    hour TL  of 2,4-D isopropyl ester to bluegills (.Lepomis maaroch-irus')
    was 0.9 ppm while the TL  of the alkanolamine salts approached 900 ppm.
    For 2,4,5-T, the 24 hour TL  was 1.4 ppm for the butoxyethanol ester,
    but 144 ppm for the dimethylamine salt (Davis and Hughes 1963, Hughes
    and Davis 1963).  Davis and Hardcastle (1959) calculated the 24 hour
    TL  of 2,4-D acid to be 350 to 390 ppm in bluegills (Lepomis maarochirus)
      m
    and 350 to 375 ppm in largemouth bass (MiaTOpterus salmoides) .  Commer-
    cial salts of 2,4-D and 2,4-D acid were not toxic to green sunfish (Le-
                              -4
    pomis QyanelZus") at 5 x 10  M (110.5 ppm) but the butoxyethanol ester
    was (Sergeant e_t al. 1970).
    The effects of 2,4-D and 2,4,5-T on fertilized fish eggs and fish fry
    of bluegills (Lepomis maoToahirus'), green sunfish  (L. oyanellus), small
    mouth bass (Micropterus dolomi&u) lake chub-suckers (Erimyzon suoetta)
    and stonerollers (Campestoma anomalwri) also depended on formulations,
    with 2,4-D toxicity at two ppm for the propylene glycol butoxyethanol
    ester but only at 100 ppm for the sodium salt.  For 2,4,5-T, the sodium
    salt was toxic at 50 ppm, and the isooctyl ester was toxic at one ppm
    if in liquid formulation, and at ten ppm if in granules (Hiltibran 1967) .
                                        64
    

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    In carp (Cyprinus carp-io) hatching was delayed by five ppm of the so-
    dium salt of 2,4-D while 50 ppm caused massive deaths of fry five days
    after hatching (Matlak 1972, Kamler 1972).
    Birds—The acute oral LD,_n of 2,4-D acid was greater than 1,000 mg/kg
    for mallards, was 472 mg/kg for pheasants, and 668 mg/kg for coturnix
    quail (Pimentel 1971).  The LCSQ for 2,4,5-T was greater than 5,000 ppm
    for coturnix quail and for mallards; and between 1,250 and 2,500 ppm
    for pheasants (Heath et al. 1972).  The LCC-. of 2,4-D acetamide and
                         	                OU
    2,4-D butoxyethanol ester were over 5,000 ppm for two-week old quail
    (Heath et^ al_. 1972) while chicks were unaffected by 2,4-D or 2,4,5-T
    at up to 100 ppm (Andersson et_ ail_. 1962).
    Oil solutions of the butyl esters of 2,4-D and 2,4,5-T were more toxic
    than aqueous suspensions when given orally to chicks (Stupnikov 1972).
    Roberts and Rojers (1957) fed 62 mg/kg 2,4,5-T per day to turkeys for
    11 days without affecting their growth.  Kenaga (1975) reviewed the data
    and concluded that at the usual levels of 2,4,5-T spraying, birds would
    not be affected adversely.
    The effects of 2,4-D on avian reproduction are disputed.  Dunachie and
    Fletcher (1967, 1970) observed a 50 percent decline in the hatchability
    of hens' eggs injected with 200 ppm 2,4-D (10 mg/egg), and a 30 percent
    decline in the hatchability of hens' eggs injected with 100 ppm (five mg/
    egg).  Pheasants given 75 to 150 mg technical 2,4-D or its amine salt
    produced normal numbers of eggs with only two percent abnormalities
    (Solomon et^ al. 1973) .  Grolleau e_t^ al. (1974) sprayed the dimethylamine
    salt of 2,4-D over the eggs of quail (Coturnix COturnix), of grey par-
    tridges (Perdix perdix) and of red partridges (Aleotoris rufd) at levels
    equal to 1.2, 2.4 and 6.0 kg/ha.  No toxic effects were noted except a
    possible decrease in Perdix egg viability at six kg/ha, and few residues
    of 2,4-D were found in any of the eggs.  A series of studies on the ef-
    fects of 2,4-D, 2,4,5-T, picloram and DDT on chickens demonstrated that
    the pesticides penetrated the eggs between days five and 19, but hardly
                                       65
    

    -------
    at all between days three and five (Somers et al. 1974a).  Even treat-
    ment with 33.6 kg/ha of 2,4-D did not adversely affect eggs in compari-
    son with controls (Somers et al. 1974c).  Similarly negative results
    were obtained with studies on pheasants (Phasianus oolohius) in which
    2,4-D mixed with picloram or 2,4,5-T actually increased the hatching
    rate (Somers et al. 1974b).  These studies are unfortunately marred by
    the extraordinarily high incidence of malformations in control embryos:
    12.5 to 23 percent in chicken studies (Somers &t_ al_. 1973) and 50 per-
    cent in the pheasant study (Somers et_ al. 1974b) .  Lutz and Lutz-Oster-
    tag (1970) presented data showing that 2,4-D sprayed on pheasant, red
    partridge, and gray partridge eggs caused abnormalities and high mor-
    tality in the offspring although a lack of quantitative data on con-
    trols weakened this study.
    Mammals—The considerable controversy over the effects of 2,4,5-T and/
    or its contaminant TCDD (3,4,7,8-tetrachlorodibenzo-p-dioxin) has been
    reviewed repeatedly (Anonymous 1971, Whiteside 1971, Gribble 1974, Anon-
    ymous 1974a).
    The acute oral LD5Q of 2,4-D and 2,4,5-T in rats are 400 to 500 mg/kg
    and 300 to 800 mg/kg, respectively (Jones e£ aJU 1968).  Stupnikov
    (1962) listed the 100 percent lethal dose of the butyl acetate salt of
    2,4-D as 900 mg/kg in mice, 2,000 mg/kg in rats, 1,000 mg/kg in rabbits
    and 1,500 mg/kg in guinea pigs.  Buslovich (1962) noted that the acute
    oral toxicity of 2,4-D acid and its sodium salt were the same in mice,
    but the acid was more toxic to rats than the salt.  Among the effects
    claimed for sublethal doses of 2,4-D Fire uncoupling of oxidative phos-
    phorylation in rats (Graff 1972) and inhibition of the tuberculosis
    bacillus in vitro (Mahishi et^ a_^. 1965).  Liver damage occurred in field
    mice given 200 mg/kg 2,4-D butyl ester orally.  The damage was not al-
    ways reversible and was less severe when pure rather than technical
    butyl ester was given (Skokova 1972) .
                                       66
    

    -------
    Gehring et^ a^. (1973) fed ten mg/kg/day of 2,4,5-T to five male human
    volunteers and found no clinical effects, but after three days continu-
    ous feeding plasma levels were calculated to reach a plateau at 17 times
    the daily intake.
    In tissue culture, 0.4 mg/ml (400 ppm) of the diethylamine salt of
    2,4-D caused chromosome aberrations in human fibroblasts (Berin et al.
    1973) and three hours' exposure of cultured human lymphocytes to 0.1 yM
    or to 250 yM 2,4-D (22.1 to 55,250 ppm) caused chromosome aberrations.
    In mice, 100 to 300 mg/kg of 2,4-D increased the in vivo incidence of
    bone marrow chromosome aberrations (Pilinskaya 1974).  No effect of
    2,4,5-T or 2,4-D against Ehrlich ascites carcinoma was observed by
    Schultz and Norman (1965) and no increase in tumors was observed among
    Swedish railroad workers occupationally exposed to 2,4-D or 2,4,5-T
    (Axelson and Sundell 1974).  Effimenko (1974) increased chromosomal ab-
    errations in rats by feeding 0.01 to 10 mg/kg (0.01 to 10.0 ppm).  These
    data are not sufficiently definitive to vitiate Rosival's (1970) con-
    clusion that the effects of the phenoxyacetic herbicides on carcinoge-
    nesis and mutagenesis are unknown.  In contrast, the data on the re-
    productive effects are unequivocal in that 2,4,5-T contaminated by
    greater than 0.1 ppm TCDD is teratogenic (Anonymous 1971, Anonymous
    1974).  Pure TCDD was both embryotoxic and teratogenic in mammals
    (Neubert et_ al^ 1973).  No embryotoxic effects were seen at 0.003 ppm
    in rats (Lucier et a^. 1975).  The butyl ester of 2,4,5-T is both em-
    bryotoxic and teratogenic in rats (Sokolik 1973, Konstantinova 1974a,
    1974b) .  The acid itself, contaminated by less than 0.05 ppm dioxin
    (TCDD) was not teratogenic in rhesus monkeys (Macaco, mulatta) (Dough-
    erty et_ al. 1975).  Lindquist and Ullberg (1971) established the accu-
    mulation of both 2,4-D and 2,4,5-T in murine yolk sacs and fetal tis-
    sues.  They noted that 2,4-D dissipated faster than 2,4,5-T.  Haus
    (1973), in his survey of pesticide residues in the environment, identi-
    fied the fsooctyl, isobutyl and -£sopropyl esters of 2,4-D as teratogenic
    in mice, and 2,4,5-T as teratogenic in rats and mice.
                                       67
    

    -------
    Conclusions-
    The effects of 2,4-D and 2,4,5-T on soil and soil organisms are not
    sufficiently great to prohibit soil disposal of these herbicides.  Since
    2,4-D is readily degraded, the major concern in its disposal should be
    its herbicidal effects rather than environmental side effects.  The
    same cannot be said for 2,4,5-T, which is both more persistent than
    2,4-D and most probably contaminated, however slightly, with the ex-
    tremely toxic and highly persistent TCDD.  Disposing of large quantities
    of 2,4,5-T in or on soil, carries an unknown risk of TCDD contamination
    of soil, plants, and animals.  The relative merits of burning 2,4,5-T,
    with the possibility of dioxin formation, or of burying it, with the
    probability of disseminating dioxins, cannot be determined on the basis
    of the data now available.
                                       68
    

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    Dicamba
    Dicamba is the common name for 3,6-dichloro-o-anisic acid, introduced
    by Velsicol Chemical Co. in 1959 as Banvel.  Technical dicamba is a
    brown crystalline solid, and pure dicamba is a white, odorless crystal-
    line solid with a melting point of 114 to 116 C, a solubility of 0.45
    g/lOOg water (4500 ppm) and 92.2 g/lOOg ethanol (922,000 ppm), and a
    vapor pressure of 3.75 x 10   mm mercury at 100 C.  It is formulated as
    the diethylamine salt with a water solubility of more than 72 g/lOOml
    (720,000 ppm).   Dicamba is synthesized from 1,2,4-dichlorobenzene by a
    three stage process in which trichlorobenzene is treated with methanol
    and sodium hydroxide to produce 2,5-dichlorophenol which, treated with
    carbon dioxide under pressure produces 2-hydroxy-3,6-dichlorobenzoic
    acid.  The latter is reacted with dimethyl sulfate (Martin 1968).
    Degradation-
    Biological—The optimum pH for detoxification of dicamba on highly or-
    ganic soils was 5.3 (Corbin and Upchurch 1967).  Detoxification of 1.1
    kg/ha was completed between May and October or October and May in un-
    sterilized prairie soil.  Essentially no degradation occurred in sterile
    soil during a four week period, but over 50 percent degradation occurred
    in two weeks in unsterilized soil (Smith 1973a) and 95 percent decomposed
    in five weeks in Regina heavy clay.  Degradation of 3,6-dichlorosalicylic
    acid was 28 percent complete after five weeks in the heavy clay, and no
    5-hydroxy-dicamba was found (Smith 1973b).  Dicamba detoxification was
    unaffected by microbial adaptation to the herbicide MCPA (Kirkland and
    Fryer 1972) but occurred more rapidly as temperature and soil moisture
    levels increased (Burnside and Lavy 1966).  Berezovskii and Nikhotin
    (1972) reported that 13 percent of dicamba was converted to 3,6-dichloro-
    salicyclic acid.  The latter compound persisted for long periods (Bere-
    zovskii 1974) .
                                        69
    

    -------
    Krumzdorf (1974) identified 3,6-dichlorosalicylic acid, p-aminobenzoic
                                                                     14
    acid and benzoic acid as dicamba metabolites.  In prairie soils,   C^"
                             14                                         ~~
    dicamba was converted to   CO- and 3,6-dichlorosalicylic acid, with the
    latter decomposing more slowly than dicamba.  No other metabolites were
    detected, little or no metabolism occurred in sterilized soils and only
    four to five percent were lost when dicamba was incubated in soil in
    sealed flasks, presumably because of anaerobic conditions (Smith 1974).
    In water, dicamba was most rapidly lost in unsterilized water in the
    presence of light.  Neither vegetation nor turbidity affected the rate
    of loss, nor did the presence of sediments.  Dissipation was presumed
    to be microbial (Scifres et al. 1973).   Burnside and Lavy (1966) noted
    that dicamba was more biodegradable than either amiben or atrazine, and
    that little degradation occurred in autoclaved soil.
    Photolytic—Dicamba is relatively resistant tc ultraviolet light (WSSA
    1974).  Degradation was not enhanced by exposure to long wave (356 nm)
    UV light for seven days at 30° or 60°C (Baur et al. 1973) .  In conven-
    tional formulations dicamba was more susceptible to decomposition by UV
    light than were its so-called polymeric formulations.  The ratio of
    volatilization to photolysis was 46:21 for polymeric dicamba, and 60.1:
    37.9 for ordinary dicamba, with degradation accounting for 21 percent
    and 37.9 percent of the initial amounts, respectively (Baur and Bovey
    1974).
    Chemical and physical—Dicamba was partially decomposed by 18/V sulfuric
    acid or 70 percent Ca(C10)_, but not by 8N sodium hydroxide, 100 per-
    cent monoethanolamine or 100 percent triethanolamine (Kennedy et al.
    1972b) .  Dicamba was also 100 percent decomposed by metallic sodium or
    lithium in the presence of liquid ammonia  (Kennedy et al. 1972a).  When
    heated in a muffle furnace, over 98 percent of dicamba was decomposed
    at 600°c (Kennedy e± al. 1969).  The volatile products of burning dicam-
    ba at 900 C included carbon monoxide, carbon dioxide, chlorine, hydrogen
    chloride, oxygen and ammonia  (Kennedy et^ al_. 1972a, 1972b) .  Dicamba
                                       70
    

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    heated to 210 C was changed to a clear liquid  (Stojanovic et_ aJ^. 1972b) .
    Transport-
    Within soil—Dicamba adsorbed to kaolinite to  a considerable extent, but
    only a small amount adsorbed to muck  (Burnside and Lavy 1966).  The ad-
    sorption of dicamba on montmorillonite was affected by the saturation
    ion and by the degree of saturation of the clay (Carringer et al. 1975).
    Adsorption on near-neutral prairie soils was minimal, and when several
    adsorbents were compared, the degree  of adsorption was:  charcoal > anion
    exchange resin > peat > cellulose triacetate   (Grover and Smith 1974) .
    Dicamba was rated as highly mobile in both silty clay loam and sandy
    loam (Harris 1967) and its mobility increased  as pH increased and also
    increased with increased flux (Helling 1971).  In soil columns of 6.25
    mm x 1.8 m, dicamba retention time was only 2.6 minutes, indicative of
    its possibly leaching to 1.5 meters in soil.   In forest soils, dicamba
    was highly mobile even when the soil  contained eight percent organic
    matter and 50 percent clay (Norris and Montgomery 1975).
    Between soil and water—When dicamba was applied to the soil surface,
    more was lost to surface water from sod than from fallow soil (Trichell
    et^ aJ^. 1968).  When applied to a heavy-textured soil, two to seven per-
    cent of dicamba was lost to drainage water.  Up to 5.5 times as much
    was lost from conventionally-tilled as from no-till plots, runoff in
    surface water was greater than runoff into drainage tiles, and more was
    lost if rain occurred soon after application than if rain was delayed
    (Schwab e_t al. 1973).
    Norris and Montgomery (1975) considered stream contamination by dicamba
    unlikely because stream detritus and  stream biota readily adsorbed the
    herbicide, resulting in rapid decreases in the water levels.
    In the aquatic-terrestrial ecosystem, unchanged dicamba was the major
    component of the water after 33 days.  There was no evidence of accumu-
    lation in aquatic food chains and very little uptake whatever by the
                                       71
    

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    organisms.  Ten percent of the dicamba had been converted to 5-hydroxy-
    dicamba (Sanborn 1974, Yu e_t al_. 1975, Metcalf and Sanborn 1975).
    Volatilization-
    Little dicamba was lost to volatilization from silty clay loam after
    eight weeks with relative humidities between zero and 100 percent, but
    50 percent volatilized from planchets in 11 weeks (Burnside and Lavy
    1966) .
    Persistence-
    The persistence of dicamba in soil is summarized in Table 12 .  At pH
    7.5, traces were found for three years, but persistence is usually
    estimated in weeks rather than in months.  It is noteworthy, however,
    that 2,3-dichloro-salicylic acid is considerably more persistent than
    dicamba.  Berezovskii (1974) noted its accumulation over a three year
    period.  Krumzdorov (1974) detected 3,6-dichlorosalicylic acid in corn
    plants sown two and three years after dicamba was applied to soil.  Up
    to 55 percent of 3,6-dichlorosalicylic acid was adsorbed by sandy loam
    soil (Smith 1974).  Dicamba decomposed faster in soil taken from under
    grass than in soil taken from under trees (Altom and Stritzke 1973) or
    from litter-covered forest soil than from cleared forest soil (Brady
    1975), but was rapidly decomposed under all the preceding conditions.
    In soil under five inches of bracken litter, however, dicamba residues
    could be detected for three years (Parker and Hidgson 1966) .  In Nebraska
    soils, dicamba was less persistent than either picloram or 2,3,6-TBA
    (Burnside &t_ al. 1971) .
    In water, dicamba dissipated as a logarithmic function of concentration
    with time, and dissipation was enhanced by light, especially in the
    presence of sediment (Scifres et al. 1973).
    Effect on Non-Target Species-
    Microorganisms—At 0.12 kg/ha, dicamba was net toxic to soil microorga-
    nisms from 20 to 80 days after soil treatment (Bezuglov et al. 1973) .
                                       72
    

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    In a sod-podzolic soil, dicamba applied at an unspecified level inhibi-
    ted aerobic bacteria (Kozarev and Laptev 1972).  Five tons per acre
    (5000 ppm) of dicamba incorporated with a calcareous loam slightly in-
    hibited respiration and soil bacteria whether the analytical standard
    or the formulated liquid was used.  Streptomycetes were markedly in-
    hibited by pure dicamba and only slightly by formulated dicamba, and
    fungi were stimulated by pure dicamba (Stojanovic et al. 1972a).
    Invertebrates—Honeybees were extremely sensitive to dicamba, with an
    estimated LD   of 3.6 yg/bee, while the 24-hour and 48-hour LC,-n for
    the amphipod Gammarus looustris were 10 ppm and 5.8 ppm, respectively
    (Pimentel 1971).
    Vertebrates—The 24-hour and 48-hour LC   of dicamba for juvenile coho
    salmon (Onchophynehus kusutoh) were 151 ppm and 120 ppm (Bond et al.
    1965) but for rainbow trout (Salmo gaivdnerii} and bluegills (Lepomis
    maaroehirus) the 48-hour LC   were 35 and 130 ppm, respectively (Pimen-
    tel 1971).  The acute oral LD   in pheasants (.Phaisanus aolchis) was
    673 mg/kg in females and 800 mg/kg in males (Pimentel 1971).  The acute
    oral ID,... in male rats was 757 mg/kg, with 95 percent confidence limits
    of 449 to 1278 mg/kg while the acute oral LDr^ of formulated dicamba to
    male rats was 1100 mg/kg with 95 percent confidence limits of 925 to 1308
    mg/kg (Edson and Sanderson 1965).
    Khristov  (1975) noted that dicamba at concentrations of 0.1 to 10 ppm
    was mutagenic in corn and caused chromosome damage.  No data on its
    mutagenesis in animals or bacterial systems were available.  Levels of
    800 ppm for three months, or 500 ppm for two years, were not  overtly
    toxic to rats or dogs, and three generations of rats fed dicamba were
    reproductively normal (WSSA 1974) .
    Conclusions-
    Although dicamba is not a highly persistent herbicide, it can persist
    for long periods under certain conditions.  Moreover, its metabolite,
    3,6-dichlorosalicylic acid, may be considerably more persistent than
                                        74
    

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    dicamba itself.  Dicamba cannot be recommended for soil disposal until
    more is known of its terminal residues.
                                       75
    

    -------
    Diquat and Paraquat
    Dlquat, the common name for the 6,7-dihydro (l,2-a:2T,l'-c) pyrazine-
    diium ion, is the active ingredient of diquat: dibromide, introduced by
    J. C. I. Plant Protection Ltd. in 1958 as Reglone.  It is marketed as
    Ortho Diquat by Chevron Chemical Co. in the United States.  Diquat di-
    bromide monohydrate, a yellow solid which decomposes above 300°C with-
    out melting, is highly soluble in water (700.,000 ppm) and is corrosive
    to most common metals.  It is a contact herbicide which is highly sus-
    ceptible to decomposition by ultraviolet light but essentially nonvo-
    latile.  It is synthesized by condensing 2,2v-dipyridyl with ethylene
    dibromide.
    Paraquat is the common name for l,l'-dimethyl-4,4-bipyridinium ion, the
    active ingredient of the contact herbicide paraquat dichloride, which
    was introduced by J. C. I. Plant Protection Ltd. in 1958 as Gramoxone.
    It is marketed in the U. S. by Chevron Chemical Company under the name
    Ortho-Paraquat.  Pure paraquat dichloride is a white crystalline solid
    with a faint ammoniacal odor, which decomposes at about 300 C.  It is
    completely soluble in water and is formulated only in aqueous solution.
    Technical paraquat dichloride is a dark red solution, which is corrosive
    to most common metals.  It is synthesized by direct quaternization of
    4,4'-bipyridyl with methyl chloride under pressure (WSSA 1974).
    Degradation-
    Biological—Both diquat and paraquat are degraded by microorganisms.
    Atkinson (1973) reported an Aehromobacter> which reduced diquat and Nam-
    deo  (1972) isolated nine actinomycetes, one Streptomyces and one Noaar-
    di-a capable of decomposing paraquat with l-methyl-4-carboxypyridylium
    ion as a degradation product.  Funderburk and Bozarth (1967) also found
    a bacterium capable of degrading paraquat by demethylation followed by
                                       76
    

    -------
    ring cleavage.  The l-methyl-4-carboxypyridinium ion was identified as
    a product.
    Picolinamide, a photolytic product of diquat, is degraded by bacteria
    (Menzie 1974).  The degradation of the 4-carboxy-l-methyl-pyridinium
    ion by Aohpomo'baoter D and that of /l/-methylisonicotinate by a gram-f^
    positive and a gram-negative bacterium have also been shown (Menzie
    1974).  Microorganisms have been cultured which can use paraquat as
    their sole source of nitrogen  (Funderburk 1966).  These data make it
    apparent that, at least in the laboratory, microbial degradation of
    diquat and paraquat is plausible.  In soil under field conditions, ad-
    sorption radically reduces the plausibility of microbial decomposition
    (Weber and Coble 1968) .  Fryer and co-workers (1975) concluded that
    paraquat may not break kown at all in soil, and that if microbial degra-
    dation occurs, it is extremely slow.  Funderburk and Bozarth (1967)
    stated that both herbicides are quite stable in higher plants.
    In animals, bipyridylium compounds are poorly absorbed from the gut and
    are excreted, unchanged, in the feces.  Paulson (1975), reviewing the
    fate of herbicides in animals, states that partial metabolism occurs,
    but that the nature of the products has not yet been reported.  The
    role of microorganisms in the gut in metabolizing diquat and paraquat
    has also not been established.
    Photolytic—Dry paraquat and diquat were 50 percent decomposed by UV
    light in 48 hours.  No diquat remained in an aqueous solution exposed
    to ultraviolet light for 192 hours (Funderburk and Bozarth 1967).  In
    aqueous solution, paraquat was totally decomposed within three days to
    the //-methylbetaine of nicotinic acid, with subsequent formation of
    methylamine hydrochloride and nicotinic acid (Slade 1965) .  The 1-methyl-;
    4-carboxypyridinium ion was obtained from paraquat in aqueous solution
    exposed to 240-260 nm UV light.  On planchets, inactivation was 50 per-
    cent completed in 48 hours, and 75 percent completed in 96 hours (Fun-
    derburk et al. 1966).  The photolytic degradation of diquat is shown in
    Figure 3.
                                        77
    

    -------
                          BR
                 DIQ'JAT
                   I
                                        I       NH,
                 VOLATILE FRAGMENTS
    PHOTOLYTIC  DEGRADATION OF DInUAT
          (AFTER  MENZIE 1974)
             Figure  3
                   78
    

    -------
    Chemical and physical—Hance  (1967) considered the chemical degradation
    of paraquat on soil to be extremely slow due to adsorption and relative-
    ly low temperatures.  In water, at pH > 8, 0.03 mg/ml paraquat was oxi-
    dized by C1CL within one minute (Gomaa and Faust 1971) and at neutral
    or acid pH, paraquat is very  stable (Hiltibran e* a^. 1972, WSSA 1974).
    Paraquat was not at all decomposed by treatment with 100 percent meth-
    anolamine  (Kennedy &t_ <&_• 1972b) but was 99.9 percent decomposed by
    either metallic sodium or lithium with liquid ammonia and 95 percent
    was decomposed by sodium biphenyl  (Kennedy et_ a\._. 1972a) .  At 600 C,
    98.3 percent of paraquat in commercial formulations decomposed (Kennedy
    et al. 1969).  Volatile products of burning analytical-grade paraquat
    at 900 C in a muffle furnace were carbon monoxide, carbon dioxide, and
    ammonia (Kennedy et al. 1972b).
    Transport-
    Within soil—The major factor  determining the mobility of paraquat and
    diquat in soil is their adsorption by clay and by organic matter (Burns
    and Hayes 1974, Khan 1974, Hayes et al. 1975).  The adsorption of the
    bipyridylium ions on montmorillonite is generally considered irreversi-
    ble under field conditions (Tomlinson £t^ al^. 1968, Weber &t_ a^. 1965,
    Gamar and Mustafa 1975, Mithyantha and Perur 1975).  The complete re-
    covery of bipyridylium herbicides from soil required four hours of re-
    fluxing with 18^17 sulfuric acid (Tucker et al. 1967) .  Adsorption was a
    function of the cation exchange capacity of the clays (Malquori and
    Radaelli 1966, Weber et^ a^. 1965) and charge-transfer complexes are ap-
    parently formed between diquat or paraquat and soil organoclay complexes
    (Khan 1973).  Tucker et^ al^ (1967) recognized two types of binding be-
    tween soil and bipyridilium herbicides:  tight and loose, the former ir-
    reversible and the latter reversible when the soil was leached with con-
    centrated salt solutions.  The ratio of tightly bound to loosely bound
    paraquat or diquat was 1:4 in  loam, 1:27 in sand and 1:107 in muck
    (Tucker e_t^ ^1^. 1967).  Adsorption to kaolinite, but not to montmorillonite,
                                         79
    

    -------
    could be reversed by liming or fertilizing (Weber et al. 1965) and de-
    sorption from bentonite was easier than from muck (Harris and Warren
    1964) .  Adsorption of paraquat was greater on acid than neutral soils
    (Weber and Best 1972).  On humic acid or humin, paraquat was more stron-
    gly adsorbed to strongly acidic sites, but diquat to weakly acidic
    sites (Best et al. 1972).  The relative adsorbability of the dipyridy-
                                           I j             i
    lium cations on organic matter was:  Ca   - humus > H  - humus > lignin
    > epidium roots > oats > clover, lucerne or wheat  (Radaelli and Fusi
    1968).
    Unlike most pesticides, diquat and paraquat directly influence the sta-
    bility of the soil, due to the dipyridyl cation, particularly in clay
    soils with few water-stable aggregates (Malquori and Radaelli 1968).
    Gomar and Mustafa (1975) calculated that 1,930 tons per acre of diquat,
    and up to 4,500 tons per acre of paraquat, could be adsorbed by arid-
    zone soils and that less than one percent of such adsorbed herbicide
    could be released by water.  Such an enormous and tenacious capacity
    of adsorption is, as expected, correlated with an extremely low mobil-
    ity (Helling 1971a).  Nevertheless, paraquat applied to a sandy-loam
    soil was found in significant amounts at the 25 to 35 cm level (Fryer
    et al. 1975).
    Between soil and water—Since paraquat and diquat are frequently used as
    aquatic herbicides, contamination of water by direct application is most
    common.  Calderbank (1972) noted that diquat and paraquat were adsorbed
    by mud after the aquatic weeds died, and that: no desorption from mud
    occurred.  After six months, 36 percent of the paraquat applied to the
    water remained in the top two inches of hydrosoil, while water levels
    fell from 2.5 ppm to 0.01 ppm within two weeks (Calderbank 1970).  At-
    kinson (1973) estimated that free diquat persisted no more than two
    hours in water, being adsorbed by sediment thereafter.   In reservoirs,
    74 percent of diquat and paraquat were adsorbed by sediment within half
    an hour  (Yeo 1967).  As Hiltibran and co-workers (1972) suggested, the
                                       80
    

    -------
    hydrosoil may well be  the  ultimate  repository  of  diquat,  and  probably
    also of paraquat.
    Into organisms—Diquat and paraquat are  taken  up  by  plants  to some  ex-
    tent even though  their herbicidal activity  is  by  contact  (WSSA 1974).
    Water  levels of one  ppm led  to  112  ppm paraquat in the  aquatic plant
    Myriophyllum spicatim  in two days (Calderbank  1972) .  Cattle  fed  200  to
    400 ppm paraquat  did not secrete it in their milk or muscles,  and fish
    accumulated paraquat only  in skin,  gills and viscera, not in  their  edi-
    ble tissues (Calderbank 1972).  Rainbow  trout  exposed to  one  ppm  did
    not concentrate paraquat in  their tissues  (Calderbank 1970).
    Persistence-
    Paraquat does not retain its phytotoxicity  when adsorbed  to clay, and
    retains very little  when adsorbed to  soil organic matter.  Phytotoxic
    persistence is, therefore, not  very great  (WSSA 1974).  In an orchard
    soil in Ontario 2.24 kg/ha paraquat applied in early June each year
    from 1963 to 1971 led  to residues of  4.36 ppm  in  the top  15 cm of soil
    in July of 1971, and 4.12  ppm 16 weeks later (Khan et_ al_. 1975).  This
    constituted approximately  50 percent  of  the total 20.16 kg/ha  applied
    over the nine-year period—a remarkable persistence  for a foliage-ap-
    plied herbicide subject  to photolysis.  Fryer, Hance and  Ludwig (1975)
    found that essentially all the  paraquat  applied to a sandy loam soil
    remained in the soil for two years,  and  suggested that paraquat is not
    degraded at all in soil.
    Water levels of diquat  decreased from 1,000 ppb to nine ppb in 12 days
    in reservoirs, and paraquat applied at 250-2,500  ppb declined  to  less
    than 180 ppb in 13 days  (Yeo L967).   In some New  York lakes,  four Ibs/A
    (4.48 kg/ha) of diquat  applied  to water declined  to  less  than  0.005 ppm
    within eight days (Sewell  1970).  Most of the  dissipated  paraquat and
    diquat are merely absorbed to hydrosoil according to Hiltibran et al.
    (1972) and Frank  (1967).
                                      81
    

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    Effects on Non-Target Species-
    Microorganisms—Paraquat and diquat are only toxic to soil processes and
    soil microorganisms at very high levels in situ, probably because they
    are so completely inactivated by clay as well as by soil organic matter.
    Of nine herbicides tested, only dichlobenil was less toxic to ammonia
    oxidation than paraquat:  picloram, 2,3,6-TBA, Chlorthiamid, bromoxynil,
    chlorfluorazole, ioxynil and propanil were more inhibitory (Debona and
    Audus 1970).  The effects of diquat on soil processes and soil micro-
    organisms are shown in Tables 13 and 14.
    Overall bacterial numbers were decreased by 500 ppm of paraquat  (Pokor-
    ny 1971).  Proteolytic bacteria were inhibited for four days, beginning
    two days after treatment, by 400 ppm paraquat, while cellulolytic bac-
    teria were stimulated for eight days, inhibited between the 8th and 10th
    day, and then returned to normal levels.  Even at 400 ppm, paraquat had
    no effect on ureolytic bacteria (Giardina et al. 1973).  Overall bac-
    terial populations were depressed for at least 56 days by five tons/acre
    (5,000 ppm) of paraquat, whether pure or formulated (Stojanovic et al.
    1972a) but not by low levels (Debona and Audus 1970), and 5.6 kg/ha
    were even stimulatory (Camper e_t^ al^. 1973).
    Bacterial species varied widely in the levels of paraquat required for
    inhibition, from 10   mg/liter (one ppm) for Azotobaeter ehroococcum
    in a nitrogen-free medium (Manninger et_ al^. 1972) to one mg/ml (1,000
    ppm) for Bacillus subtilis (Thomas et al. 1973).  One Bacillus species
    was inhibited by ten liters of Gramoxone per hectare (Langkramer 1970)
    and another by five ppm (Breazeale and Camper 1972).  Paraquat inhibi-
    ted the growth of Pseudomonas fluovesoens, Erwinia cayotovoTa, and Es-
    cheviokia coli at 25, 50 and 50 ppm, respectively (Breazeale and Cam-
    per 1972, Wallnoefer 1968).
    Inhibition of fungi was reported at 56 ppm and  stimulation at 2.8 ppm
    paraquat (Camper et_ a^. 1973).  Stojanovic e_^ al^. (1972a) stimulated
                                       82
    

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    Streptomyees by incorporating 5,000 ppm pure paraquat  into  loam, but
    formulated paraquat at levels of 5,000 ppm inhibited Streptomyoes.  Of
    thirteen fungal species tested by Szegi (1973), all except  four FUSOP-
    vum species were depressed by 25 ppm of paraquat.  The inhibited species
    were:  Aspergillus aandidus, A. ustus, Stachybotris atva, Verticill-iwn
    aandellabrum, a Peniaiflium species, and two species of Fusarium.  Fu-
    sariwn oxysporwn was not inhibited by 20 ppm (Rodriguez-Kabana and Curl
    1972) but Suillus var-iegatus was inhibited by 2.3 ppm  (Sobotka 1970).
    These data make it abundantly clear that, even though  paraquat does not
    depress soil respiration at five tons per acre (5,000  ppm)  (Stojanovic
    et al. I972a), the balance among soil microflora will  be  sharply alter-
    ed as sensitive species are replaced by resistant species.  Celluloly-
    tic bacteria are inhibited by paraquat levels of 500 ppm  or more (Szegi
    1973, Szegi and Gulyas 1971).  Rankov (1970) considered paraquat to
    have no effect on cellulolytic bacteria in soil, but did  not  specify
    levels.
    The effects of paraquat on aquatic systems are extreme:   0.6  ppm was
    toxic to freshwater bacteria, freshwater algae and freshwater protozoa
    (Huess 1972).  Bluegreen algae were affected for up to 28 days by 20
    ppm (Da Silva et al. 1975) and 100 ppm was toxic to Chlorella on paper
    disc culture (Thomas et_ al. 1973).
    Molds were less sensitive to diquat and paraquat than  were  bacteria
    (Wallnoefer 1968).  In pure cultures, ten to 100 ppm inhibited growth
    of Trichoderrr?*. vivide and Khizopus stolonifer but not  of Fusarium aut-
    moTvm or Aspepgillus niger.  In mixed cultures, both paraquat and di-
    quat reversed the usual dominance of P. stolonifex1 over A.  nigev (Wil-
    kinson 1969).  On agar, 100 ppm paraquat resulted in selection for res-
    istant bacteria (Kokke 1970a) and resistance was observed in  fungi from
    paraquat-treated soil (Szegi and Gulyas 1971) .  Gene conversion was in-
    duced in Sacchapomyaes oeTewis'lae by 100 to 900 ppm paraquat  (Namdeo and
    Dube 1973).  Rosival (1970) included both diquat and paraquat among the
                                       85
    

    -------
    pesticides exerting direct chemical effects on DNA.
    Invertebrates—Even at one ppm diquat affected aquatic arthropods and
    molluscs, albeit indirectly, through habitat destruction  (Hilsenhoff
    1966).  In a New Zealand stream, three 30 minute exposures to two ppm
    of paraquat destroyed 95 percent of the amphipods within days, but in-
    creased the numbers of Trichoptera after one year (Burnett 1972) .  The
    96-hour TL^ of diquat for pond invertebrates ranged from 0.048 ppm in
    the amphipod Hyallella azeteoa to over 100 ppm for dragon flies  (.L-Vbel-
    lula) and damselflies (Endllagmd) (Wilson and Bond 1969).  No short-term
    effect on aquatic macro-invertebrates was incurred when 0.11 ppm diquat
    and 0.17 ppm endothall were used (Berry et_ aJ^. 1975).
    The toxicity of paraquat to entomophagous mites and insects was consid-
    ered too great to permit its use in an integrated pest control program
    (Kock and Yeargan 1973).  Under laboratory conditions, the relative tox-
    icities of eight herbicides to beetles (Bembidion') were:  sodium chlor-
    ate < dalapon < simazine < simazine plus amitrole < pyrazon < diquat
    < 2,4-D < chlorpropham  (Mueller 1971).
    Fish and amphibians—The 96-hour LC   of diquat to striped bass  (Roccus
    saxatilis') in aquaria was 0.25 ppm (Wellborn 1969) while the TL^ of
    paraquat for bluegills (Lepomis maarochirus) was 400 ppm at 24 hours
    and 100 ppm at 48 hours (Davis and Hughes 1963).  Gilderhus (1967) found
    that bluegills accumulated increasing amounts of diquat for ten days
    after water treatment and that residues persisted for six to twelve
    weeks.  At high concentrations (275 ppm), diquat increased the time of
    onset for the toxicity of aldrin, DDT or parathion without decreasing
    its severity (Krieger and Lee 1973).  Despite the indubitable toxicity
    of diquat and paraquat for fish, Schlueter (1970) considered it a suit-
    able aquatic herbicide if carefully handled.  Hiltibran (1967) consid-
    ered the no-effect level of diquat for bluegill eggs and fry to be ten
    ppm and concluded that, at ordinary levels of application, diquat would
    not seriously harm fish.  The 24-hour LC,.,. of paraquat for Fowlers toad
    tadpoles (Bufo woodhousii fowleri} was 54 ppm (Pimentel 1971).
                                       86
    

    -------
    Birds—The five day LC5Q of diquat for two-week old quail was 1,346
    mg/kg with 95 percent confidence limits of 1,178 to 1,540 mg/kg; 3,742
    rag/kg with 95 percent confidence limits of 3,329 to 4,220 for pheasants;
    2,933 mg/kg with 95 percent confidence limits of 1,181 to 5,256 mg/kg
    for bobwhites; and mallard mortality was 30 percent at 5,000 mg/kg.
    For paraquat, the five day LC_Q was 970 mg/kg (823-1,140 mg/kg) for
    quail; 981 (784-1,213 mg/kg) for bobwhite; 1,468 (1,287-1,673) mg/kg
    for pheasants; and 4,048 (3,432-4,886 mg/kg) for mallards (Heath et al.
    1972).
    When diquat was injected into fertilized hens' eggs, ten percent hatch-
    ed if 0.5 mg  (ten ppm) were injected and 60 percent hatched after five
    ppm were injected (Dunachie and Fletcher 1967).  Paraquat was lethal
    to over half the chick embryos even at 0.15 ppm injected on the first
    day of incubation.  One ppm permitted survival of 25 percent of embryos
    treated on day two, and of 94 percent treated on day 16 (Dunachie and
    Fletcher 1970).  At 0.1 ppm injected, egg hatch was as high as in con-
    trols (Dunachie and Fletcher 1967) .  Fletcher (1967) considered the
    levels injected into the eggs to correspond to feeding the hens 40 ppm
    of paraquat.
    Mammals—The acute oral LD n of paraquat in rats was 100 to 110 mg/kg
    with 95 percent confidence limits between 85 and 134 mg/kg (Gaines
    1969).  Howe and Wright (1965) cited 200 mg/kg paraquat and 400 mg/kg
    diquat in rats and 40 to 50 mg/kg paraquat in cats.  The no-effect lev-
    els for dogs fed paraquat or diquat for three years was 7.5 mg/kg, a
    level rats could tolerate over their whole life span.  Paraquat repor-
    tedly altered the fight-flight response of rats at levels above five
    percent of the LD   (Billewicz-Stankiewicz and Pawlowski 1971).   Both
    diquat and paraquat affected spermatogenesis, but not preimplantation
    mortality, in rats (Pasi et_ a^. 1974).
    Conclusions-
    The absolute lack of evidence for any degradation of paraquat or diquat
                                       87
    

    -------
    in soil makes these compounds unsuitable for soil disposal.   Use of
    sunlight to decompose these herbicides in water might be possible if
    contact with adsorptive surfaces such as hydrosoil is prevented.  Pyro-
    lysis is also a feasible method of disposal.
    

    -------
    SUBSTITUTED UREA HERBICIDES
    Diuron, Linuron, Monuron and Monolinuron
    The urea herbicides monuron [/!/'- (4-chlorophenyl) -/7-methoxy-^-methyl-
    urea], diuron  IN'- (3,4-dichlorophenyl)-/l/,71f-dimethylureaJ  and  linuron
    L3-(3,4-dichlorophenyl)-l-methoxy-l-methylurea] were  introduced  by  E.  I.
    duPont de Nemours  in 1951, 1955 and  1960, respectively.   Monolinuron
    L/!/'-(4-chlorophenyl)-/l/~methoxy-.Af-methylureaJ was  introduced by Farbwerke
    Hoechst AG in  1960.  All are used as selective herbicides to  some ex-
    tent, but monuron  and diuron are used primarily for week  control in un-
    cropped areas, while linuron and monolinuron are  primarily preemergent
    herbicides.
    Monuron is synthesized by the reaction of 4-chlorophenyl  isocyanate
    with dimethylamine and diuron is synthesized by reacting  3,4-dichloro-
    phenyl isocyanate with methylamine.  Linuron is prepared  by the  reac-
    tion of 3,4-dichlorophenyl isocyanate with (^//-dimethyl hydroxylamine,
    whereas monolinuron is synthesized by the reaction of hydroxylamine and
    4-chlorophenyl isocyanate followed by reaction with dimethyl  sulfate.
    The characteristics of each compound are shown in Table 15.
    Degradation-
    Biological—The substituted urea herbicides are decomposed by many  soil
    organisms to some  extent.  Breakage  of the bond between the carbonyl
    carbon and nitrogen atoms absolutely requires a urease, but methyl  de-
    alkylation is  far  less specifically  catalyzed (Kearney 1966) .  Boerner
    (1967) noted that demethylation is carried out by numerous microorgan-
    isms.  The initial products consist  of methyl- and methoxyureas, chlor-
    inated anilines, and carbon dioxide  derived from  the  side chains (Tables
    16 and 17).  Boerner (1967) reported that 3,4-dichloroaniline was also
    rapidly degraded in loamy soil but Menzie (1974)  considered aniline for-
    mation to be of some concern.
                                       89
    

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    Baoi-fius sphaevieus degraded monolinuron and linuron but not monuron
    or diuron  (Engelhardt  et al. 1971).  The decomposition consisted  of
    removal of the ureido portion of the molecule from W-methoxy-compounds
    with formation of p-chloroaniline and the latter was reportedly resis-
    tant to further degradation  (Wallnoefer 1969, Wallnoefer and Bader
    1970, Wallnoefer and Engelhardt 1971).  Wallnoefer et_ al^.  (1973) repor-
    ted that Rh-izopus japonieus dealkylated both monuron and monolinuron.
    Mueller and Korte (1975) observed that while some monolinuron was  deme-
    thylated during waste composting, 86.2 percent was unaltered.  Kaufman
    and Blake  (1973) cultured ten microorganisms which decomposed propham,
    propanil,  solan, and SWEP, of which three (Aspergillus usius, Fusar-ium
    oxyspoTum  and Aohromobacter) also degraded diuron.  Aspergillus versi-
    colov3 three strains of Penioill-iian, Fusarium solanwn and  T^iohoderma
    wivide did not decompose diuron.  Lopez and Kirkwood (1974) obtained
    growth, but no diuron degradation, when FusaviiMn and two bacteria  were
    cultured with 20 ppm diuron for two weeks.  After 80 days, 3.5 percent
                                        14
    of the radioactive label evolved as   C0~ and increasing the soil  tem-
    perature by 10 C between 10  and 30  tripled diuron degradation.   Of
    ten ppm diuron, 6.3 ppm remained after 12 weeks in loamy sand, 5.5 ppm
    after 12 weeks in clay loam  (McCoraick and Hiltbold 1966).
    Murray and co-workers (1969) compared the degradation of five substi-
    tuted urea herbicides by three strains of Asperg-illus.  The herbicide
    fenuron, with no chlorine, was most readily decomposed by  all three
    strains, while diuron was most resistant.  Norea, fluometron and mon-
    uron were  intermediate.  Some growth was achieved by A. sydowi and A.
    tamavii even at 1000 ppm of monuron, but A.  rigger was completely in-
    hibited by 100 ppm.   Rankov  (1968b) found that 0.01 percent monolinuron
    (100 ppm)  served as nitrogen source for five of 25 strains of soil bac-
    teria, and ten of 20 strains of actinomycetes, while 100 ppm of linu-
    ron served as nitrogen source for five of 25 bacteria, but only two of
    twenty actinomycetes.  Five of 15 strains of fungi could use linuron or
                                       93
    

    -------
    monolinuron as a nitrogen source.  Maximum degradation of monolinuron
    occurred when soil water levels were at 30 percent of the soil's water
    capacity and after repeated applications (Suess 1970).  Belasco and
    Pease (1969) examined soil after 12 years of annual diuron treatment
    (2.24 and 4.8 kg/ha) or after one year of linuron treatment (2.24 kg/ha)
    and found no 3,3',4,4'-tetrachloroazobenzene, while incubation of 500
    ppm linuron or diuron resulted in formation of about one ppm of dichlo-
    roaniline and no 3,3',4,4'-tetrachloroazobenzene.  As with most pesti-
    cides, increasing levels of application decreased the rate of degrada-
    tion  (Hance and McKone 1971).
                     14
    In sterile soil,   CH.,0-labeled monuron decomposed to form nine per-
         14
    cent   C09, and 28 percent ^(9-dimethylhydroxylamine, but in nonsterile
         14
    soil   C0?  accounted for 58 percent of the radioactivity and NsO-d±-
    methylhydroxylamine for only eight percent (Schuphan 1974a, 1974b) .
    The decomposition of monolinuron to .Vjf-dimethylhydroxylamine could, at
    least theoretically, lead to nitrosamine formation (Schuphan 1974b).
    In spinach, monolinuron was metabolized to 3-(4-chlorophenyl)-l-methoxy-
    1-hydroxymethylurea (Schuphan and Ebing 1975).
    The fate of urea herbicides in animals has been reviewed by Paulson
    (1975) who concluded that the urea moiety is hydrolyzed only to a limi-
    ted extent, and that the major routes of metabolism include demethyl-
    ation, demethoxylation, ring hydroxylation and conjugation.  Boehme and
    Ernst (1965a, 1965b) fed diuron to rats and found that urinary metabo-
    lites accounted for about 20 percent of the dose.  Metabolites includ-
    ed l-(3,4-dichlorophenylurea) and l-(2-hydroxy-4,5-dichlorophenyl)urea
    as a major urinary products.  The tissues and feces were not analyzed.
    Photolytic—Diuron was decomposed by UV light (Janko et al. 1970).
    Monuron and diuron were decomposed by both UV light or sunlight, but
    different products resulted from the two kinds of light (Jordan et  al.
    1964).  Weldon and Timmons  (1961) noted that most decomposition of  di-
    uron occurred between 227 nm and 249 nm, while for monuron most changes
                                       94
    

    -------
    occurred between 220 run and 245 nm.  Exposure to 28 hours of UV light
    reduced the phytotoxicity of 0.5 Ib/A (0.56 kg/ha) diuron from 50 per-
    cent kill of oat plants to zero, and of monuron from 100 percent kill
    to zero.
    The photolytic decomposition of monuron exposed to southern California
    sun for 14 days were 3-(p-chlorophenyl)-l-formyl-l-methyl-urea, l-(p£
    chlorophenyl)-3-methylurea, 4,4'-dichlorocarbanilide, 3-(4-chloro-2-C
    hydroxyphenyl)-l,l-dimethylurea.  Three additional products were tenta-
    tively identified:  l-(p-chlorophenyl)-3-formylurea, 4'-chloroformani-
    lide, and p-chloroaniline.  The degradation proceeded by stepwise photo-
    oxidation and demethylation of the ^-methyl groups, hydroxylation of
    the aromatic nucleus, and polymerization.  Degradation was hydrolytic
    and the products formed were not dependent on the initial concentra-
    tions of monuron.  Less than six percent of the monuron was decomposed
    after 14 days, and little HC1 was formed (Crosby and Tang 1969).  Maz-
    zochi and Rao (1972) photolysed monuron in methanol at 253.7 nm, under
    anaerobic conditions.  The products were 3-phenyl-l,l-dimethylurea and
    methyl-p-chlorophenylcarbamate, the latter in minor amounts.
    Linuron exposed to sunlight for two months decomposed to 3-(3-chloro£.
    4-hydroxyphenyl)-l-methoxy-l-methylurea, (13 percent), 3,4-dichloro£
    phenylurea (ten percent) and 3-(3,4-dichlorophenyl)-l-methylurea (two
    percent), while 69 percent of the linuron remained unchanged (Rosen et
    al. 1969).
    Chemical and physical—Linuron decomposed at 95 C (Janko et al. 1970).
    Extrapolating from the decomposition of diuron and linuron at tempera-
    tures of 85 C or higher, Hance (1967) estimated that their nonbiologi-
    cal degradation in soil would require more than nine years, but when
    the effects of soil adsorption were included, the model suggested that
    nonbiological degradation in soil was plausible (Hance 1969).  The de-
    composition of diuron in soil was not affected by pH (Corbin and Up-
    church 1967).
                                        95
    

    -------
    The bioactivity of 100 ppm diuron in water exposed to three Mrads of
    gamma-irradiation was less, but not significantly less, than that of
    100 ppm diuron stored for the same length of time without irradiation.
    In the solid state, diuron was not decomposed by three Mrads of gcanma£
    irradiation (Horowitz and Blumenfeld 1973).  Diuron was completely de-
    composed by liquid ammonia in the presence of metallic sodium, and 94.8
    percent by liquid ammonia in the presence of lithium (Kennedy et al.
    1972a).  At 775 C, 25 percent of technical diuron was decomposed where-
    as diuron formulated as an 80 percent wettable powder was 25 percent de-
    composed at 550 C (Kennedy e_t_ al_. 1969) .  Complete combustion at 900 C
    produced carbon monoxide, carbon dioxide, chlorine, hydrogen chloride,
    ammonia, and nitrogen oxides as volatile produ> ;  (Kennedy et al. 1972a,
    1972b).
    Transport-
    Within soil—Spiridonov and co-workers (1970) reported that monuron and
    diuron leached 100 cm during 110 days in moist subtropical soil.  Liu
    (1974) reported that diuron leached 36 inches. (90 cm) during 112 days in
    a Puerto Rican soil, and Dowler et_ al. (1968) reported 120 cm leaching
    in 90 days in Puerto Rican forests.  More tv;--i \ally, diuron and monuron
    leached 20 to 30 cm in 150 days (Sniri.knov g>nd Yakovlev 1967) or 45 cm
    in 180 days (Leh 1968).  Al r -r; V/ha, monuron and diuron leached 40 to
    50 cm, while 20 kg/ha leached nf> to 70 cm (Spiridonov £t_ al. 1968).  For
    diuron, Ivey and Andrews (196i;) reportec six inch (15 cm) soil penetra-
    tion of agricultural levels, but eight inch  (20 cm) penetration of 2.5
    times agricultural levels.  Kazarina  (1965) found that monuron applied
    to soil columns leached more readily in loamy sand than in sandy loam.
    Khubitiya and Gigineishvili (1971) observed 40 cm leaching of monuron
    during a 60 day period in early spring.
    Cool dry climates were said to inhibit both  Leaching and decomposition
    of monuron (Erickson 1965).  Granules were less mobile than other for-
    mulations (Spiridonov et al. 1968) and diuron granules remained in the
    surface layers of soil when a two to three cm layer of water was on the
                                        96
    

    -------
    soil  (Imaliev and Bersonova 1969).  Liu  (1974)  estimated  that  3.6  per-
    cent of the diuron applied to Puerto Rican Vega Alta  soil was  lost to
    leaching, with the greatest transport during  the  first week and no ob-
    servable leaching after 16 weeks.  One year after the third of three
    annual applications of monuron,  62 to 69 percent  of the residues recov-
    ered remained in the top two inches of soil,  and  86 to 100 percent re-
    mained in the top four inches (Dawson et_ al.  1968) .
    The substituted urea herbicides  are moderately  mobile, with relative
    mobilities of 2.2 to 3.3 on a scale of six for  monuron, diuron and lin-
    uron  (Harris 1967).  The precise degree of leaching depends, as always,
    on numerous factors among which  are water flux  and average pore velo-
    city  (Davidson and Santelman 1968, Davidson et^  a^. 1968), electrolytes
    (Hurle and Freed 1972) and the presence of surfactants  (Bayer  1967).
    Adsorption by soil is the major  deterrent to  leaching, and all the urea
    herbicides are readily absorbed  by organic matter (Harris and  Warren
    1964, Doherty and Warren 1969, Hilton and Yuen  1963,  Liu  e^t a±. 1970,
    MacNamara and Toth 1970, Moyer e^t al_. 1972, Green and Young 1971,  Mus-
    tafa and Gamar 1972).  Adsorption to clay is  also significant  (Scott
    and Lutz, 1971, Harris and Warren 1964, Doherty and Warren 1969, Khan
    1974, MacNamara and Toth 1970, Moyer et_ aJU 1972, Mustafa and  Gamar
    1972, Van Bladel and Moreale 1974) as is adsorption to carbon  (Hilton
    and Yuen 1963, Jordan and Smith  1971).  Models  for the mobility and ad-
    sorption of the urea herbicides  have been constructed frequently (Rhodes
    et_ al_. 1970, Khan and Mazurkewich 1974, Huggenberger  et_ al^. 1973,  Hance
    1969b, Aleshin and Yudina 1973).
    Cation exchange capacity and specific surface area affect adsorption
    (Mustafa and Gamar 1972, Doherty and Warren 1969, Liu et_  al_. 1970,
    MacNamara and Toth 1970).  On montmorillonite,  adsorption depended on
    the ionic strength of the saturating solution at  high ionic strengths
    (Van Bladel and Moreale 1974).   In dry soils, linuron formed a stable
    complex with montmorillonite (Khan 1974) .  Adsorption of  monuron on
                                       97
    

    -------
    bentonite increased with increasing temperature from 0° to 50°C, but
    adsorption on muck was not significantly affected by temperature.  De-
    sorption of monuron from bentonite occurred more readily than from muck
    (Harris and Warren 1964).  Diuron adsorption on Puerto Rican soils de-
    creased linearly with increasing temperatures (Liu et^ al. 1970).
    Relative adsorption of linuron by organic matter and clay was:  muck
    and peat > sphagnum moss >_ bentonite ^_ quartz sand  (Doherty and Warren
    1969) .  Monuron was reversibly adsorbed to peat if and only if  the peat
    was not dried, while linuron could never be completely desorbed from
    peat (Mover et al. 1972).  Harris (1966) found that monuron was adsor-
    bed least by Lakeland sandy loam, most by Chillum silt loam or Hagers-
    town silty clay, with Wehadkee silt loam intermediate; but monuron was
    mobile in all four soils.
    Monuron and diuron leached more in alluvial sandy soil than in brown
    forest soil (Khubutiya and Gigineishvili 1971).   Increased moisture
    levels, whether from rain or subirrigation, increased monuron trans-
    port in soil columns containing loamy sand or sandy loam (Kazarina 1965)
    Hance  (1965a, 1965b, 1969a, 1969b, 1974) and Grover and Hance (1970)
    examined the adsorption of urea herbicides by soils.  Among substitu-
    ted urea derivatives, adsorption increased with increasing chain length
    and with addition of chlorine or chloro-phenoxy-substituents.  The rel-
    ative adsorptivity of the compounds tested was:   urea < fenuron < meth-
    ylurea < phenylurea < monuron < monolinuron > diuron <_ linuron  < nebu-
    ron < chloroxuron (1965a, 1969b) .  The cation exchange capacity, pH,
    and clay content of the soils were not well correlated with the degree
    of adsorption (1965a, 1969a).  Adsorption of diuron on hydrophilic soil
    constituents was less than on the organic fraction of soil (1965b) .
    Linuron adsorption was determined partly by the size of the soil aggre-
    gates  (Grover and Hance 1970).
    There was no significant correlation between degradation and adsorption.
    Degradation decreased as soil organic matter was extracted, with some
                                       98
    

    -------
    suggestion that the decreased degradation was due to a less favorable
    environment for microorganisms  (Hance 1974).  On alluvial clay contain-
    ing 1.7 percent organic matter, diuron was more rapidly lost from soil
    if soil was irrigated one week  after treatment rather than immediately
    afterwards (Horowitz and Herzlinger 1974).
    Between soil and water—Monuron treatment of soil at agricultural lev-
    els led to groundwater contamination in wet years or if monuron was ap-
    plied in spring, but the levels of contamination were not specified
    (Leh 1968).  In an aquatic environment, monuron levels were higher in
    water than in soil for 32 weeks after treatment, then soil levels were
    higher than water levels (Frank 1966).  Granules of monuron were phy-
    totoxic ten meters from the point of application if transport was
    through water; soil transport was characterized as limited and levels
    of application were not available (Bersonova 1968) .  Neither linuron
    nor diuron was removed from water by slow sand filtration (Bauer 1972).
    Into organisms—All the substituted urea herbicides are absorbed by
    plants, where they interrupt photosynthesis (Martin 1968).  Residues
    of monolinuron have been found  in asparagus at harvest (Boerner 1966)
    and linuron residues were present in carrot and parsnip leaves (Del
    Rosario and Putnam 1973).  Carrots treated with linuron contained lin-
    uron, 3-(3,4-dichlorophenyl-l-methylurea; 3,4-dichlorophenylurea, and
    3,4-dichloroaniline after 117 days.  Metabolites accounted for no more
    than 13 percent of the residues (Loekke 1974) .  Auranti-aceae treated
    with ten, 13 or 16 kg/ha monuron or diuron contained traces of the her-
    bicides in unripe fruit (Khubutiya and Gigineishvili 1971).  One year
    after the last treatment of the soil cotton seeds from diuron-treated
    fields contained no residues (Dalton et al. 1966).
    Hens which were fed 0.5 ppm linuron for up to six weeks did not trans-
    mit detectable levels to the yolks of their eggs (Foster et al. 1972).
    Rats which were fed monuron at  175 mg/kg/day for 60 days accumulated
    unspecified amounts of the herbicide in their lungs, heart, liver, brain,
                                        99
    

    -------
    kidneys and milk (in decreasing order of accumulation) and also in
    their bone marrow and thyroid (Fridman 1968).
    Volatilization—Linuron was 80 percent volatilized from metal planchets
    within 48 hours but even small amounts of plant material sharply de-
    creased its volatility (Walker 1972).  In Israeli soil in July, surface^
    applied diuron dissipated most rapidly from dry soil, but was also lost
    from wet soil.  Irrigation immediately after herbicide application re-
    sulted in lower losses than irrigation one week later (Horowitz and
    Herzlinger 1974).
    Persistence-
    The persistence of monuron and diuron in soils is shown in Table 18, and
    that of linuron and monolinuron in Table 19.  In addition to these quant-
    ifiable data, numerous reports of carryover between growing seasons are
    found in the literature.  Linuron at 2.24 kg/ha persisted to the next
    growing season in sandy loam in Newfoundland (Morris and Penney 1971)
    and in Saskatchewan (Smith and Esmond 1975); monuron at ten Ibs/A (11.2
    kg/ha) was phytoxic in the third growing season after application to
    silty clay loam in Nebraska (Burnside et^ a^. 1963, 1965) and carryover
    with diuron is considered common (Bryant and Andrews 1967, Upchurch et
    al. 1969).  As with most pesticides, persistence increases with increas-
    ing levels of application and varies with soil and climate.
    Spiridonov and Kamenskii (1971) found that soil types did not affect
    the rate of degradation of monuron when comparisons were made between
    krasnoyem, meadow, chestnut, and soddy-podzolic soils, while high tem-
    perature and high rainfall decreases persistence.  Degradation of sub-
    stituted urea herbicides was, however, more rapid in red soil than in
    meadow-swampy soil under subtropical conditions (Spiridonov and Yakov-
    lev 1967).  Moyer et^ al. (1972) found that the initial concentration
    of linuron affected its rate of degradation while clay increased its
    persistence only slightly, and charcoal had no significant effect.  In
                                       100
    

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    comparisons among 11 soils, linuron decomposed more rapidly in  soils
    with a high level of organic matter, primarily due to the greater mi-
    crobial activity (Dubey et al. 1966).  Coarse soils led to greater per-
    sistence of linuron than fine soils (Burnside et^ al. 1969).
    Higher temperature and higher humidity or soil moisture decrease  per-
    sistence of substituted urea herbicides  (Burnside et al. 1969).  When
    87 to 113 kg/ha were applied to soils in the southwestern U.S., weed
    control persisted for over three years, but in Tennessee 84 to  113 kg/
    ha provided control for less than one year; soil differences as well
    as climate may have contributed (Isensee et al. 1973) .
    In Puerto Rico, monuron and diuron were more persistent than prome-
    tryne (Liu et al. 1970a, 1971) and diuron was more persistent than bro-
    macil or fenac in a Puerto Rican forest soil, but less persistent than
    prometone or picloram (Dowler e_t_ al. 1968) .  Horowitz (1969) found di-
    uron to be more persistent than atrazine, fluometron, trifluralin and
    prometryne in the field and greenhouse.  Bromacil, noruron, ametryne,
    and pyrazon were also less persistent in the greenhouse but were not
    tested in the field.  Simazine was as persistent as diuron, but no her-
    bicide was more persistent than diuron (Horowitz 1969) .  Diuron was
    also more persistent than monuron under greenhouse conditions (Arle et
    al. 1965), and more persistent than linuron in sandy loam soils (Up-
    church et al. 1969).  Linuron also decomposed faster than monolinuron
    (Homburg and Smit 1964).
    One year after the last of six annual applications of 2.4 Ibs/A (2.7
    kg/ha) of monuron, residues were 1.6 Ibs/A (1.8 kg/ha) in a silt loam
    soil.  For diuron, residues were 2.8 Ibs/A (3.1 kg/ha) one year after
    the sixth annual application of 2.4 Ibs/A (2.7 kg/ha) and 10.6 Ibs/A
    one year after the sixth annual application of 7.2 Ibs/A (8.1 kg/ha)
    (Dawson et al. 1968).
                                      103
    

    -------
    In river water which was exposed to natural and artificial light  in
    jars, 20 percent of the monuron persisted for four weeks, and none for
    eight weeks  (Eichelberger and Lichtenberg 1971).
    Effects on Non-Target Species-
    Microorganisms—As photosynthetic inhibitors, the substituted urea her-
    bicides are markedly toxic to algae.  Pillay and Tchan  (1972) ranged
    the toxicity of various herbicides to Chlovel'ia and Soenedesmus as:
    diuron > neburon > monuron > atrazine > simazine > atratone.
    When technical diuron was incubated with soil at levels equalling
    11,227 kg/ha (five tons/A), carbon dioxide evolution was inhibited over
    a 56 day period.  The inhibition was even more marked when formulated
    diuron (wettable powder) was incubated.  Bacteria and fungi were  inhi-
    bited by technical diuron, and bacteria were also inhibited for formu-
    lated diuron.  Streptomycetes were stimulated by formulated diuron but
    inhibited by technical diuron (Stojanovic et al. 1972a).  Diuron  at 0.5
    mM (116 ppm) induced mutations in Chlovella (Kvitko &t_ al. 1971) .  Pho-
    tosynthesis in ChloTetla pyrenoidosa was -':-hibited by 10  M of diuron
                   -4
    (0.023 ppm); 10  11 (23.3 ppm) inhibited .thtrmogenesis in light, and
    10  11 (2.33 ppm) inhibited all energy storage processes (Petrov et al.
    1974) .  Diuron also induced mutants which were resistant to its inhi-
    bition of phosphorylation in Chlorella pyrenoidosa (Mukhamadiev et al.
    1971).
    Zooplankton was inhibited by monuron applied to reservoirs against Mi-
    eroeystis but oxygen depletion was considered the primary cause of re-
    ductions of 25 percent, lasting up to two years (Pidgaiko and Shcherban
    1970) .  At two ppm monuron depressed reproduction of planktonic clado-
    cera by 50 percent (Shcherban 1971).
    Among bacteria, Azotobacter chroocoocion was more resistant to monuron
    and diuron than was A.  galophilion (Babak 1968).  In liquid cultures, the
    production of free amino acids by microorganisms was altered by linuron
                                       104
    

    -------
    at levels of five ppm (Balicka et al. 1970).  The inhibition of bac-
    teria and fungi by linuron lasted for more  than 145 days in sand or
    compost, but increases in both fungi and bacteria were observed (Lode
    1967).  Beck (1970) reported increases of bacteria and of C0« produc-
    tion for less than one month after monolinuron treatment; nitrification
    remained somewhat inhibited for 3.5 months, albeit not significantly.
    Fungi can to some extent be controlled by substituted urea herbicides
    (Goguadze 1966, Ebner 1965) and fungicidal  levels of linuron are muta-
    genic in Rhizobiicm (Kaszubiak 1968).
    The effects of monuron, linuron, diuron and monolinuron on soil proces-
    ses are shown in Tables 20 and 21.  The effects of diuron on soil mi-
    croorganisms and aquatic microorganisms are shown in Tables 22 and 23,
    respectively.
    At agricultural levels, linuron did not affect ammonifying bacteria
    (Rankov et al. 1967) or oligonitrophilic bacteria (Ulasevich et al.
    1973) but inhibited nitrifying bacteria (Rankov et al. 1966, Torstens-
    son 1974).  High levels of linuron also inhibited ammonifying and cell-
    ulolytic bacteria (Torstensson 1974, Rankov et^ a^. 1967).  Overall num-
    bers of soil bacteria were unaffected by four kg/ha of linuron while
    eight kg/ha in chernozem inhibited bacteria below ten cm, but stimula-
    ted their numbers above ten cm (Ulasevich et^ a^. 1970, 1973).
    When specific genera were tested, linuron almost invariably depressed
    growth.  Only Pseudomonas fluorescens at 2.5 to 4.0 ppm (Sobieszczanski
    1969) and Pseudomonas phaeseoli (Balicka and Krezel 1969) were not af-
    fected.  Azotobactev was strongly inhibited by linuron (Ulasevich et
    al. 1973, Wegrzyn 1971, Pajewska 1969) with levels as low as 1.5 ppm.
    Bacillus cereus and Rhizobiim meliloti were inhibited by 500 to 1,000
    ppm in the laboratory and under field conditions (Pajewska 1969) and
    2.5 to 4.0 ppm were toxic to Arthrobacter,  CoTynebactevium and Bacillus
    species in culture (Kosinkiewicz 1973, Sobiezczanski 1969).
    Linuron was toxic to all algae tested, Chlovella being inhibited at 0.2
                                      105
    

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    to 1.0 ppm  (Knauf and Schulze 1972).  For Andbaena  species,  inhibiting
    levels of linuron varied from one ppm to 2,000 ppm  and  for Nostoo  spe-
    cies from 100 to 500 ppm (Venkataraman and Rajyalakshmi 1971).  Da Silva
    et al. (1975) reported toxicity to algae from ten ppm linuron, and Pan-
    tera (1970) noted that high levels of linuron were  toxic  to  soil algae.
    In contrast, fungi were not severely affected (Peshakov et^ al_. 1969).
    Four kg/ha neither stimulated nor depressed actinomycetes (Ulasevich
    e£ a!L. 1970, 1973) and Bakalivanov (1972) stimulated growth  of Penio-Ll-
    l-iion with linuron; eight kg/ha inhibited this fungus in chernozem,
    however  (Ulasevich et^ ad. 1970, 1973).
    When monuron was applied to a weed-free soil at eight to  16  kg/ha,  the
    available potassium, nitrogen and phosphorus levels of  the soil were
    not changed (Spiridonov et al. 1972) but shifts in  phosphorus levels
    due to similar levels of monuron have been reported (Zavarzin 1966,
    Zavarzin and Belyaeva 1966).  Monuron stimulated soil catalase and per-
    oxidase  (Spiridonov et al. 1972).
    Agricultural levels of monuron did not affect the averall numbers  of
    soil microorganisms (Kulinska 1967a) but high levels reduced the micro-
    bial population (Pantera 1972).  Effects shifted with time:  Volynchuk
    (1974) noted that six to eight kg/ha of monuron reduced the  microbial
    population of southern chernozem for thirty days, after which microbial
    levels in treated soils rose above those of control soils.   Celluloly-
    tic bacteria in a bog soil increased above control  levels from 40  to
    70 days after the soil was treated with eight to 16 kg/ha of monuron,
    but fungal numbers decreased (Spiridonov et al. 1972).  In a meadow
    soil, 1.5 kg/ha decreased the numbers of nitrifying and ammonifying bac-
    teria, but not of cellulolytic bacteria (Tulabaev 1971, Tulabaev and
    Tamikaev 1968).  Nitrifying bacteria were also inhibited by  eight  kg/ha
    in an Armenian vineyard (Akopyan and Agaronyan 1968) .
    Monuron inhibited algal growth (Mikhailova and Kruglov  1973) :  Soil al-
    gae were stimulated by 0.001 to 0.01 ppm, but 0.1 to 1.0 ppm was toxic
                                       111
    

    -------
    (Pillay and Tchan 1972).  Nitrogen fixation by Chlovoglea was inhibi-
    ted by 10 ppm, but 25 ppm were required to stunt growth  (DaSilva et al.
    1975) .  Ukeles (1962) observed inhibition of five species of phytoplank-
    ton at 0.02 ppm, and one species (Phaeodactylum tri-aozmutum') was in-
    hibited by 0.01 ppm.
    Monolinuron did not alter the numbers of fungi or actinomycetes in soil
    (Peshakov ett al. 1969) nor the numbers of anaerobic bacteria (Sobotka
    1970) but did inhibit the growth of nitrifying, denitrifying and ammon-
    ifying bacteria (Sobotka 1970).  The fungus Suillus variegatus was not
    affected by four kg/ha (Sobotka 1970).  Azotobaotev ckpoocoaoton was
    inhibited by 100 or 1,000 ppm but not by one or ten ppm  (Wegrzyn 1971)
    but Chlorella was sensitive to 0.2 ppm monollnuron during a four day
    incubation (Knauf and Schulze 1972).
    Although effects on microorganisms other than algae range from stimu-
    lating to inhibiting, the predominance of inhibitory effects makes it
    apparent that these substituted urea herbicides do alter the numbers
    and kinds of soil microorganisms.  Moreover, Corke and Thompson (1970)
    observed that, whereas 100 ppm of linuron or diuron are required to
    inhibit nitrification for three days, 2.5 to 5.C ppm of their metabo-
    lite, 3,4-dichloroaniline, is very toxic to Nitresomonas, and 25 ppm
    of the metabolite 3-(3,4-dichlorophenyl)-l-methylurea strongly inhibit
    nitrification.
    Invertebrates—The LC  _ of linuron to Daphma magnet was six ppm, but
    to Artemia saii-ne, greater than 100 ppm.  Snails (.Lyrmaea stagnali-s)
    and aquatic worms (Tubiflex~) were not injured by 0.2 to one ppm (Knauf
    and Schulze 1972).  Shcherban (1972) observed adaptation of some Clad-
    oaeva to diuron and Braginskii and co-workers  (1972) noted that where-
    as low concentrations of diuron inhibited zooplankton, higher concen-
    trations were stimulatory.
    When clams Qievcenapia mevcencwia.} were exposed to 0.25 ppm diuron, 92
    percent of the eggs developed and larval survival was not decreased; at
                                       112
    

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    five ppm larvae also survived, but no eggs developed.  For monuron,
    five ppm inhibited neither the development of oyster eggs nor  the  sur-
    vival of their larvae  (Davis and Hidu 1969).
    Among land invertebrates, monuron was mutagenic at 0.01 percent  (100
    ppm) in Drosophila melanogaster  (Shkvar et_ al. 1969) and monolinuron
    at 0.1 mg/lOOg soil (one ppm) inhibited reproduction in Folsonria oan-
    dida (Sanocka-Woloszyn and Woloszyn 1970).  Monuron decreased  the  num-
    bers of wireworms, earthworms, springtails, millipedes, and mites  in
    grassland soil at levels above 11.2 kg/ha (Fox 1964).
    Fish and amphibians—The 48-hour LC,..-. of diuron to coho salmon (Orco-
    rhynchus kisutch) and largemouth bass (NioTopteTus salmoides)  was  42
    ppm and 16 ppm, respectively (Pimentel 1971).  Bluegills  (Lepovris  mac-
    Tochi-Tus') exposed to 3.0 ppm of diuron in ponds died as a consequence
    of oxygen depletion (McCraren et al. 1969) while roach fish  (Putilis
    Tuti-tis) developed methemoglobinemia as a consequence of diuron poi-
    soning  (Komarovskii 1973).  Popova  (1970) reported that diuron at  0.2
    mg/liter (0.2 ppm) decreased piscine hemoglobin content and the number
    of erythrocytes within five days.  Both monuron and diuron accumulated
    in roach fish exposed to 0.2 to 0.3 mg/liter  (0.2-0.3 ppm) for two to
    three months (Komarovskii and Popovich 1971).
    The 24-hour LC,.,, of monuron for the channel catfish (.lotaluvus punota-
    lus) was 75 ppm and the 48-hour LC,-n for the mullet (tfugil eephalus')
    was 16.3 ppm (Pimentel 1971).  Ten ppm of monuron were toxic to some
    freshwater fish within eight days (Pimentel 1971).
    Birds—When two-week old birds were fed diuron for five days followed
    by clean feed for three days, 14 percent of quail, 33 percent  of phea-
    sants,  and 30 percent of mallards died of 5,000 ppm, while the LC^
    for bobwhites was 1,730 ppm with 95 percent confidence limits  between
    1,482 ppm and 2,035 ppm.  No bobwhite died when fed 5,000 ppm  monuron,
    but 21 percent of the quail and ten percent of the mallards died,  while
                                       113
    

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    the LC n for pheasants was calculated to be 4,682 ppm, with 95 percent
    confidence limits of 3,902 to 5,746 ppm (Heath et_ aU 1972).  When lin-
    uron or diuron was injected into fertile hens' eggs, 100 ppm of the
    former or 200 ppm of the latter decreased the hatching rate significant-
    ly (Dunachie and Fletcher 1967, 1970).
    Mammals—The acute oral LD,-n °f diuron is 3,400 mg/kg; of linuron 4,000
    mg/kg; of monuron, 3,500 to 3,700 mg/kg; and of monolinuron, 2,250 mg/kg
    (Martin 1968, Pimentel 1971).
    Monuron is carcinogenic if rats are fed 450 mg/kg (450 ppm) per day for
    17 months (Rubenchik et^ a^. 1969, 1970) or if mice are fed six mg/week
    for 15 weeks (Rubenchik et al. 1970).  Diuron was less strongly carcin-
    ogenic, with fewer carcinomas occurring after a longer latency period
    (Rubenchik et al. 1973).   Rosival (1970) characterized urea herbicides
    as indirect mutagens, perhaps because of their demonstrated cytogenic
    effects (Khubutiya and Ugulava 1973), and their mutagenicity in micro-
    organisms and in plants (Wuu and Grant 1966).
    Dystrophic changes in rat livers due to linuron and diuron have been
    reported after chronic feeding of ten percent of the acute LD   (Ban-
    kowska and Bojanowska 1973) and monolinuron at 230 to 460 mg/kg/day
    caused damage to the liver, kidneys and spleen of rats (Pasiewicz and
    Nikodemska 1973).  Air levels of 13 mg/m  reportedly caused changes in
    the erythrocyte count of rats (Lomonova 1969).
    Conclusions-
    Despite the wealth of data on the effects of the herbicides monuron,
    linuron, diuron and monolinuron on soil processes and soil organisms,
    the consequences of disposing of these compounds in soil are unclear.
    Their extreme toxicity to algae, considerable toxicity to bacteria and
    fungi, and their relatively great mobility and persistence argues a-
    gainst soil disposal.  Bulk disposal would invite pollution of both
    soil and water for years.  Disposal of small amounts over larger areas
    would probably be acceptable at normal agricultural use levels.
                                      114
    

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    EPIC
    EPIC, the common name for 5-ethyl di-n-propyl thiocarbamate, was intro-
    duced by Stauffer Chemical Co. in 1955 under the name Eptam or Eradi-
    cane as a selective preemergence herbicide.  EPIC is a light yellow
    colored liquid with an amine odor, a boiling point of 127 C at 20 mm
    mercury, a vapor pressure of 0.1 mm mercury at 24 C and a flash point
    of 116 C.  Its water solubility is 370 ppm at 20 C and it is completely
    miscible with acetone, ethanol, and kerosene at 20 C.  EPTC is synthe-
    sized by the reaction of ethyl mercaptan and di-n-propylcarbamoyl chlor-
    ide in the presence of base, or by the reaction of di-n-propylamine with
    5-ethyl chloroformate.
    Degradation-
    In one study the degradation of EPTC proceeded at similar rates in
    sterilized and unsterilized soil, and after seven weeks in this heavy
    clay soil phytotoxicity was lost although very little carbon dioxide
    was evolved (MacRae and Alexander 1965).  Other studies contradicted
    these results.  In five soil types including peaty muck and pure sand
    inactivation decreased sharply when soil was sterilized (Koren et al.
    1968).  Sheets (1959) estimated that degradation in sterilized soil
    was one third that of non-autoclaved soil.  More rapid degradation
    occurred in loam than in heavy clay soils (Smith and Fitzpatrick 1970),
    and when soil moisture was increased (Cialono and Sweet 1963, Fang
                                                         14
    1969).  Fang (1969) suggested that the low levels of   CO  evolution
    could be due to microbial utilization of the ethyl moiety of EPTC.
    No microorganisms capable of degrading EPTC have been identified, nor
    were data available on microorganisms which failed to decompose EPTC
    (Fang 1969, Menzie 1974).
                                                      14
    Adult female rats fed 0.6 to 103 mg EPTC excreted   C0,j and six urinary
    metabolites, including urea (Menzie 1974).  In mice, degradation pro-
                                       115
    

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    ceeded by sulfoxidation followed by cleavage of the thiocarbamate ester
    group.  EPTC-sulfone was six percent degraded to carbon dioxide, but
    EPTC and its sulfoxide were 35 to 41 percent converted to carbon dioxide
    (Casida et^ al. 1975) .
    Chemical and physical—EPTC is decomposed by concentrated acids at high
    temperatures, but treatment with ION sodium hydroxide for one hour at
    95°C had little effect (Smith and Fitzpatrick 1970).
    Transport-
    Within soil—EPTC was more readily adsorbed tc dry soil than wet (Leu-
    chenko and Gortlevskii 1970, Koren and Ashton 1969) and more readily at
    low temperatures than at high (Koren and Ashton 1969).  Complexes of
    EPTC with montmorillonite were stable against some moisture increases,
    but could be reversed by complete water saturation (Mortland and Megitt
    1966).  On model aliphatic adsorbents, EPTC adsorption increased with
    increasing length of the alkyl group from C0 to C.. 0, and more EPTC ad-
                                               o     _Lo
    sorbed to the peat fraction of soil than to the humic acid fraction
    (Hance 1969b).
    In soil columns, EPTC leaching increased as temperatures dropped from
    24° to 3 C (Vernetti and Freed 1963) .  Leaching was not significant in
    dissipating unspecified levels of EPTC from a black clay loam over a
    90 day period (Yatsenko and Balkova 1971).  In a peaty muck, EPTC leach-
    ed less than five cm (Koren et^ al. 1969).  No data were available on
    the transport of EPTC from soil into water or from water into sediments.
    Volatilization—When EPTC was applied to wet soil, 22 to 38 percent vo-
    latilized within one hour and volatilization from dry soil was even
    greater (Gray 1965).  Its volatilization from peaty muck, adobe clay,
    clay loam and sandy loam was 15.1 percent, 16.4 percent, 5.3 percent,
    10.4 percent and 18.1 percent, respectively, within one hour and the
    greatest amount of volatilization was from pure sand (Koren et_ a.^. 1968,
    1969).
                                       116
    

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    Persistence-
    The phytotoxicity of agricultural levels of EPIC persists for one week
    in moist loam at 70° to 80°F (WSSA 1974) and for not more than 90 days
    in black clay loam planted to sugar beets  (Yatsenko and Komissarov
    1970).   Persistence was estimated to be less than one growing season
    when four to six kg/ha EPTC were applied in sugar beet fields, while
    eight kg/ha applied before sowing often resulted in carryover to the
    next season (Yatsenko and Blakova 1971).  Four ppm (8.96 kg/ha) of
    EPTC retained its phytotoxicity for three months and persistence was
    correlated with the organic matter, clay, and cation exchange capacity
    of the soil (Sheets 1959).  Wet clay granules were less persistent than
    dry clay granules (Cialono and Sweet 1963).
    Effects on Non-Target Species-
    Microorganisms—At agricultural levels, EPTC did not alter the overall
    numbers of microorganisms in the soil (Balicka and Sobieszczanski 1969,
    Zharasov and Chulakov 1972, Lobanov and Poddulnaya 1968).  Nitrifying
    bacteria were inhibited on dark chestnut soil (Zharasov 1972) and on
    gray podzol or chernozem (Nikolaenko 1970, Nikolaenko et^ aJU 1970), but
    stimulated after two months at an unspecified level (Novogrudskaya et al.
    1965).   In cotton fields, eight kg/ha had no effect on nitrifying bac-
    teria (Tulabaev 1970) and Azotobaoter cultures were not inhibited by one
    or ten ppm but were inhibited by 100 or 1000 ppm (Wegrzyn 1971) .
    Different types of bacteria were variably affected by EPTC with cellu-
    lolytic bacteria inhibited by levels of eight kg/ha or higher (Sobiesz-
    czanski 1969, Tulabaev 1970) and saprophytic bacteria in leached cherno-
    zem stimulated at the same level (Matsneva and Semikhatova 1973).  De-
    nitrifying bacteria in cotton fields were stimulated by eight kg/ha (Tu-
    labaev 1970) or on agar after 1.5 months exposure to EPTC (Novogrudskaya
    et al.  1965) but the same bacteria were inhibited on gray podzol or cher-
    nozem (Nikolaenko 1970).  Ammonifying bacteria in cotton fields were un-
    affected by eight kg/ha (Tulabaev 1970) but inhibited on gray podzol or
                                       117
    

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    chernozem (Nikolaenko 1970).
    When different species were tested for sensitivity to EPIC, bacilli
    were most resistant, with Bacillus megateviiffn, B. mesentericus and B.
    vulgatus being stimulated by unspecified levels in leached chernozem
    (Matsneva and Semikhatova 1973) and B. subtilts being unaffected by
    1000 ppm in paper-disc culture (Thomas et a1. 1973).  Azotobacter was
    stimulated by EPTC on leached chernozem (Matsneva and Semikhatova 1973),
    unaffected by eight kg/ha in cotton fields (Tulabaev 1970) and by one
    ppm in culture, but inhibited by 100 ppm in culture (Wegrzyn 1971).
    Fungi were inhibited by agricultural levels of EPTC as well as by 20
    mg/ml (20,000 ppm) in light and dark chestnut soils (Zharasov 1972,
    Zharasov et al. 1972) but not on leached chernozem (level unspecified)
    (Matsneva and Semikhatova 1973).  Fungal species inhibited by 4.5 kg/ha
    (10 ppm) were Cladospoman, Altevnaria., and Curvutaria (Zharasov et al.
    1972) while sclerotial growth, but not fungal numbers, of ScleToti-wn
    rolfsii was inhibited by 20 yg/g (20 ppm) EPTC (Rodriguez-Kabana and
    Curl 1972).  Soil algae were reportedly unaffected by EPTC, but levels
    were not specified (Mikhailova and Kruglov 1973).  In aquaria, 0.5 to
    1.0 mg/ml (500 to 1000 ppm) depressed the carbon dioxide evolution and
    increased the ammonia levels of the water; plcinktonic growth was not
    affected (Pischolka 1971).
    The effects of EPTC on soil processes varied.  Nikolaenko (1970) re-
    ported that ammonification was inhibited by EPTC in gray podzol or
    chernozem.  No effects on nitrification were observed when 4.5 kg/ha
    were applied to sugar beet fields of light chestnut soil (Zharasov 1971,
    Zharasov and Chulakov 1972) and unspecified amounts of EPTC stimulated
    nitrification on sandy-loamy chernozem (Lobanov and Poddubnaya 1968).
    Cell suspensions of Nitrobaeter were inhibited by ten yg/ml (10 ppm)
    (Winely and San Clemente 1970).  Soil respiration was reportedly en-
    hanced by EPTC (Karpiak and Iwanowski 1969) or unaffected (Balicka and
    Sobieszczanski 1969).  The data suggest that EPTC is somewhat fungicidal
                                       118
    

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    and affects bacteria selectively.  The toxicity of EPIC  to microorganisms
    was greater on gray podzolic soil than on chernozem, although its phyto-
    toxicity was greater on chernozem (Nikolaenko 1970).  Heavy low-humus
    chernozem resulted in lower toxicity of EPTC to nitrogen-fixing bac-
    teria than did solodized chernozem (Nikolaenko et al. 1970).  As the
    moisture content of soil fell, microbial toxicity increased (Nikolaenko
    and Geller 1969).  EPTC uncoupled oxidative phosphorylation in Nitro-
    bacter agilis to some extent (Winely and San Clemente 1971).
    Invertebrates—EPTC was not considered toxic to honey bees by Morton and
    co-workers (1972) but did inhibit development of ova and of larvae at
    100 ppmw (Morton and Moffett 1972).  The LC,-0 of EPTC for Daphnia magna
    was 4.7 ppm at 48 hours and 9.4 ppm at 96 hours (Koval'chuk et_ _ajL 1971).
    Fifty percent of white shrimp  (Penaeus setiferus) were paralyzed or
    killed by exposure to 0.63 ppm for 96 hours, and shell growth was in-
    hibited in eastern oysters (Crassostrea virginica.) exposed to five ppm
    for 96 hours (Pimentel 1971).
    Vertebrates—White mullet (Mugil aurema) had an LC _ of  20 ppm EPTC in
    48 hours (Pimentel 1971) and the 96-hour LC,._ was 17 ppm in mosquito
    fish (Gambusia affinis) (WSSA 1974).
    In bobxriiite quail (Cotinus virginianus) the oral LD__ is 20,000 ppm per
    day for seven days (WSSA 1974) and the acute LD   for chick embryos is
    0.74 mg/kg (Medved e^ al_. 1970).  No teratogenesis was seen in rats fed
    0.5 or 5.0 percent of the LD _ of EPTC throughout pregnancy but the
    higher level was highly embryotoxic (Medved et_ al. 1970).  Olefir (1973)
    reported that rats fed the maximum tolerated level of EPTC for one week
    exhibited decreased immune capacity.  The acute oral LD  n of EPTC is
    1,630 mg/kg for mice and 3,160 mg/kg for rats (Pimentel  1971).
    Conclusions-
    The disposal of EPTC in soil is feasible, since this herbicide is neither
    overly persistent nor highly toxic to soil "organisms.  Some fungicidal
                                       119
    

    -------
    activity as well as changes in the numbers and species of soil micro-
    organisms would almost certainly occur, and some leaching must be anti-
    cipated.  The degree of water pollution to be anticipated cannot be de-
    termined from the data.
                                       120
    

    -------
    Nitralin and Trifluralin
    Nitralin is the common name for 4-(methylsulfonyl)-2}6-dinitro-^ff-di£
    propylbenzamine, introduced by the Shell Chemical Co. in 1966 as a se-
    lective preemergence herbicide on numerous vegetables, fruits, turf
    and ornamentals and soybeans.  It is a yellow crystalline solid with a
    mild odor which melts at 151 C to 152 C, which has a vapor pressure of
    1.8 x 10  mm mercury at 25 C, and decomposes vigorously at 225 C, with
    an estimated heat of decomposition of 250 cal/gram.  Nitralin has a
    water solubility of 0.6 ppm , 37 percent (370,000 ppm) in acetone, and
    33 percent (330,000 ppm) in dimethyl sulfoxide at 25°C.  It is inflam-
    mable but not corrosive.
    Trifluralin is the common name for 2,6-dinitro-Af,7l/-dipropyl-4-(trif luo-
    romethyl) benzamine, introduced by Blanco Products Co. in 1959 as a
    preemergence herbicide in vegetables, fruit, nut trees and soybeans.
    It is an orange crystalline solid with a melting point of 48.5  to 49
    C, a boiling point of 96  to 97 C at 0.18 mm mercury, and a vapor pres-
                     -4                   o
    sure of 1.99 x 10   mm mercury at 29.5 C.  Its water solubility is less
    than one ppm, but it is soluble in ethanol to 7 g/100 ml (70,000 ppm)
    and in acetone to 40 g/100 ml (400,000 ppm).  Trifluralin is neither in-
    flammable nor corrosive.  Technical trifluralin is at least 95 percent
    pure and melts above 42 C.
    Helling (1976) has recently reviewed the behavior of dinitroaniline her-
    bicides in soil.
    Degradation-
    Biological—Hamdi and Tewfik (1969) reported that pseudomonads degraded
    trifluralin by splitting the nitro-groups from the aromatic moiety.
    Petrosini et al. (1970) found significantly greater decomposition of
    trifluralin in unsterilized soil than in sterilized soil, with additional
                                       121
    

    -------
    stimulation of degradation if organic matter was added to the soil.
         14
    When   CF -trifluralin was incubated with Paeoi1omyees3 Fuscari-wn oxy-
    spomm or Aspergillus fwnigatus3 less than one percent of the radio-
                        14
    activity evolved as   CCL (Laanio et al. 1973), and Willis and co-
    workers (1974) observed little correlation between trifluralin degrada-
    tion and microbial respiratory activity in soil suspensions.  Degrada-
    tion was enhanced by anaerobic conditions if the oxidation-reduction
    potential of the soil was lowered by prestimulating microbial activity
    (Willis et al. 1974) .  Nitralin degradation rates were not affected
    by activated carbon added to soil, but trifluralin degradation was  (Tal-
    bert and Kennedy 1972) .
    Trifluralin decomposed more rapidly at soil moisture equal to 160 per-
    cent of field capacity than at 80 percent of field capacity in loam
    soils (Messersmith e^ al. 1971).  In silt loam under laboratory condi-
    tions, trifluralin in aerobic autoclaved soil was not significantly de-
    composed after 20 days, but it was decomposed in unautoclaved soil.
    Most of the trifluralin losses were due to volatilization rather than
    degradation, however (Parr and Smith 1973).  The products of triflura-
    lin degradation are shown in Figure 4.  Probst and Tepe (1969) concluded
    that, although microorganisms may contribute to destruction of triflura-
    lin in soil, there is no evidence that microbial degradation predominates.
    Corbin and Upchurch (1967), investigating the effects of pH on herbicide
    detoxification in soil, concluded that trifluralin was not detoxified
    in soil.  Data on the microbial degradation of nitralin are not availa-
    ble.
                                   14
    In rats and dogs fed 100 mg/kg   CF«-trifluralin in a single oral dose,
    78 percent of the radioactivity was eliminated in the feces and 22 per-
    cent in the urine.  Urinary metabolites consisted of partially and com-
    pletely dealkylated compounds, but the CF -group remained intact.  Tri-
    fluralin was poorly absorbed from the gut, resulting in high fecal ex-
    cretion (Emmerson and Anderson 1966).  Studies of the animal metabolism
    of nitralin are not available (Paulson 1975).
                                        122
    

    -------
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                                            123
    

    -------
    Photolytic—Trifluralin on glass decomposed photolytically during four
    to six hours' exposure to 300-700 my light (Wright and Warren 1965).
    Photolytic decomposition proceeded by oxidative dealkylation, nitro-re-
    duction and cyclization.  The products included 2,3-dihydroxy-2-ethylC
    7-nitro-l-propyl-5-trifluoromethylbenzimidazoline and 2-ethyl-7-nitro£)
    5-trifluoromethylbenzimidazole 3-oxide, both of which could be further
    degraded by heat or irradiation.  Under acid conditions, 2-amino-6-nitroS
    2,2,2-trifluoro-p-toluidine was formed, and under alkaline conditions,
    2-ethyl-7-nitro-5-trifluoromethylbenzimidazole accounted for 80 percent
    of the decomposition products (Leitis and Crosby 1974).
    Using a vapor-phase reactor which simulated sunlight, Soderquist and co-
    workers (1975) identified two dinitrotoluidines and two benzimidazoles
    as photolytic products of trifluralin (Figure 4).  Up to 95 percent of
    trifluralin applied to anaerobic silt loam at 1.0 ppm and 0.1 ppm was
    recovered after 30 days in the dark, but only 18 percent after 30 days
    in the light.  But little degradation of 200 ppm occurred even in light
    (Parr and Smith 1973).  Although nitralin photodegradation may follow
    the same pattern as that of trifluralin, no data are available.
    Chemical and physical—Trifluralin was completely decomposed by liquid
    ammonia with either metallic sodium or lithium, and was 91.2 percent
    decomposed by sodium biphenyl (Kennedy et al. 1972a).  Burning formu-
    lated trifluralin at 900 C produced as volatile products:  carbon mon-
    oxide, carbon dioxide and ammonia (Kennedy et al. 1972a, 1972b) .  De-
    composition of 25 percent of trifluralin was achieved for the reference
    standard by heating to 879 C, and for the formulated (liquid) trifluralin
    at 842°C (Kennedy et^ al. 1969).  Some reduction in the phytotoxicity of
    trifluralin was achieved by exposing 10 ppm or 100 ppm to three Mrad of
    gamma-irradation (Horowitz and Blumenfeld 1973).
    Transport-
    Within soil—Helling (1971) characterized trifluralin as immobile in
    all soils.  Being highly volatile, trifluralin diffused in the vapor
                                       124
    

    -------
    phase and its diffusion in soil was not affected by variations  in  soil
    water (Scott and Phillips 1972).  Trifluralin was strongly adsorbed by
    activated carbon (Coffey and Warren 1969) and by various adsorbents in
    the order:  peat moss > wheat straw >_ cellulose triacetate > cation ex-
    change resin > anion exchange resin > silica gel and cellulose  powder
    > kaolinite > montmorillonite (Grover 1974).  Its adsorption on muck
    was sufficiently great to prevent four Ibs/A (4.9 kg/ha) from leaching
    two inches (Eshel and Warren 1967) but it could be readily desorbed
    from montmorillonite by water (Grover 1974).  When the amount of organ-
    ic matter was low and was kept constant, however, adsorption increased
    with increasing clay content (Horowitz et al. 1974).  The level of mont-
    morillonite clay in the soil did not affect trifluralin's bioactivity
    after the first year (Weber et ajU 1974).  Koren (1972) increased  the
    leaching of trifluralin by adding surfactants to the soil, but  charac-
    terized the degree of movement in dry soil as slight.
    In silt loam in the laboratory, trifluralin diffusion increased direct-
                                                 3
    ly with increases in bulk density to 1.1 g/cm , then decreased  with in-
    creasing bulk density.  Vapor diffusion increased about 50 percent for
    each ten percent increase in the air-filled porosity of the soil,  and
                                       3             3
    for bulk densities between 1.2 g/cm  and 1.4 g/cm , the magnitudes of
    vapor diffusion and solution diffusion were similar (Bode et_ al. 1973a).
    Diffusion was low in air-dry soils, increased until the soil moisture
    content reached eight to 15 percent (weight/weight) and then decreased
    again.  Diffusion also decreased if the air-filled fraction of  the soil
    fell below 40 percent (volume/volume).  A model adequate to predict tri-
    fluralin diffusion in soil included 15 parameters (Bode et al.  1973b).
    When 0.84 and 1.68 kg/ha of trifluralin were soil incorporated, 80 per-
    cent remained in the top 15 cm, and the rest above 30 cm in fine sandy
    loam.  After 15 months, residues in the zero to 15 cm layer were 0.11 ppm;
    in the 15-30 cm layer, 0.10 ppm (Miller et^ a^. 1975).  In four  southern
    soils, trifluralin leached into the two to four inch layer (five to ten
    cm) in 22 weeks (Schweizer and Holstun 1966) .
                                        125
    

    -------
    In contrast to trifluralin, both nitralin and its metabolites leached
    readily through clay loam in soil columns (Anderson et_ al. 1968).  Af-
    ter 15 months, 0.84 to 1.7 kg/ha soil-incorporated nitralin had  leached
    to the 15-30 cm layer (Miller et_ al. 1975).
    Between soil and water—Most losses of trifluralin into surface waters
    occurred when heavy rains followed herbicide treatment; but, over a
    three year period, losses into water did not exceed 0.05 percent per
    season (Willis et_ al^. 1975).  No data were available for nitralin.
    Volatilization—The phytotoxicity of surface-applied trifluralin was
    enhanced by adding adsorbents to the soil, presumably because the ad-
    sorbents decreased volatiliy (Bardsley et al. 1967).  Losses due to
    volatilization were proportional to the concentration of trifluralin,
    and increased with time and with the amount of soil water when triflu-
    ralin was applied to the soil surface.  Vapor loss decreased sharply
    when the herbicide was incorporated to a depth of 1.27 cm (Bardsley et
    al. 1968).  Increasing the application rate increased the amount of tri-
    fluralin which volatilized, while increasing the volume of the diluent
    from 2.34 kl/ha to 300 kl/ha decreased vaporization by 50 percent.  An-
    other practice which decreased vapor losses was percolating trifluralin
    into dry soil in enough water to moisten the soil, rather than spraying
    onto moist soil and then soil-incorporating it.  Regardless of the mode
    of application, vapor losses in the first twelve hours were less than
    five percent of the trifluralin applied (Swanson and Behrens 1972).
    Spencer and Cliath (1974) stressed that volatilization, rather than de-
    gradation, accounted for losses of trifluralin activity after surface
    application, but Soderquist and co-workers (1975) considered photolysis
    to precede volatilization.
    When trifluralin was applied to sand in the aquatic-terrestrial  model
    ecosystem, the trifluralin was sand-adsorbed and did not enter water
    in algicidal quantities  (Sanborn 1974) .
                                       126
    

    -------
    Into organisms—Neither trifluralin nor nitralin are taken up by fol-
    iage (WSSA 1974).  When trifluralin was tested in the aquatic terres-
    trial ecosystem, sand-applied trifluralin resulted in greater accumu-
    lation of the herbicides by snails and fish than did foliage-applied
    trifluralin  (Sanborn 1974).  Caterpillars (Estigmene aavea) feeding on
    contaminated sorghum both distributed and degraded the trifluralin more
    effectively than snails (fhysa sp.); the latter were unable to degrade
    trifluralin  (Sanborn 1974).  Metcalf and Sanborn (1975) judged triflu-
    ralin to accumulate in aquatic food chains to the same extent as meth-
    oxychlor.  The ecological magnification level of 926 in fish (Gambusia
    affinis) and of 17,872 in snails was well correlated with its low water
    solubility and high lipid solubility.  Nevertheless, 11 degradation
    products of trifluralin were found in the water of the ecosystem (Met-
    calf and Sanborn 1975) .  Model ecosystem data for nitralin were not
    available.
    Persistence-
    Trifluralin was found in 12 percent of soils with a history of regular
    trifluralin use (Stevens et^ a^. 1970) and in 3.5 percent of 1729 samples
    tested for trifluralin under the national soils monitoring program in
    1969 (Wiersma est_ a^. 1972).  The major losses of trifluralin and nitra-
    lin appear to be due to their volatilization, since an air flow of 0.04
     3
    m /hour over loamy sand soil was found to dissipate all the nitralin and
    over 75 percent of the trifluralin (Parochetti and Hein 1973).  Horowitz
    (1969) characterized trifluralin as moderately persistent, with a great-
    er persistence under field conditions than in greenhouses.  The relative
    persistence of several herbicides under field conditions was:  simazine=
    diuron > trifluralin=atrazine > fluometron > prometryne.  Under green-
    house conditions the order was:  simazine=diuron > atrazine > fluomet-
    ron=trifluralin=bromacil=noruron > prometryne=ametryne > pyrazon (Horo-
    witz 1969).  The persistence of nitralin and trifluralin in soils is
    shown in Tables 24 and 25 for those data which could be quantified.
                                       127
    

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    -------
    When trifluralin was applied to sandy loam, persistence increased with
    increasing depth of soil incorporation (Menges and Tamez 1974, Burnside
    1974) and with increasing levels of application (Savage and Barrentine
    1969).  In unsterilized Italian soil, nine to ten percent organic mat-
    ter was most conducive to trifluralin persistence, but of soils steri-
    lized by propylene oxide, clay or calcareous soils retained trifluralin
    longest (Petrosini et_ al. 1970).  Savage (1973) surveyed 250 fields
    and concluded that trifluralin persisted equally well after repeated ap-
    plications as after the first, whereas nitralin persistence decreased
    with repeated applications.  Nitralin persisted longer in soil which
    had a lower pH.
    Effects on Non-Target Species-
    Microorganisms—The data in Tables 26 and 27 show that, except at mas-
    sive levels, trifluralin does not inhibit soil processes, soil bacteria,
    or soil fungi drastically.  No data for its effects on algae were avai-
    lable.  Noguchi and Nakazawa (1971) ranked eight herbicides with res-
    pect to their effects on soil nitrification.  The order was:  prometryne
    < lenacil < diphenamid < trifluralin < vernolate < MCPA < STOP < PCP.
    Nitralin at 25 ppm stimulated the growth of Pseudomonas fluovescens
    while the same level of trifluralin had no significant stimulatory or
    inhibitory effect (Breazeale and Camper 1972).  In meadow marshy soil
    and humus-peat-gley soil, however, nine kg/ha  (4.1 ppm) and 30 kg/ha
    (14 ppm) were somewhat toxic (Tyunyalva et al. 1974).  Khikmatulaeva
    and Ibragimova (1973) reported that water levels of two ppm inhibited
    oxygen consumption, nitrification, and ammonification in reservoirs.
    Invertebrates—The 24-hour LC   for aquatic arthropods ranged from 8.8
    ppm in the amphipod Gaimamts laGustvis to 13 ppm for stoneflies (Ptero-
    narcys sp.).  The 48-hour LC_Q for the stonefly was 4.2 ppm, however,
    indicating cumulative effects.  The LCrn for waterfleas  (Daphnia pulex)
    was 0.24 ppm in 48 hours  (Pimentel 1971).  Data for nitralin were not
    available.
                                       130
    

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    Fish and amphibians—The 24-hour LC   of trifluralin for rainbow trout
    (Salmo gairdnerii) was 0.21 ppm.  For bluegills  (Lepomis maoTOchirus)
    the LC,-n decreased as time and temperature increased:  the 24-hour LC
    at 45°C was 1.3 ppm while the 96-hour LC - at 65°C was 0.13 ppm (Pimen-
    tel 1971).  The 24-hour LC.Q for Fowler's toad (Bufo woodhousii fowleri)
    tadpoles was 0.18 ppm (Pimentel 1971).  Data for nitralin were not avai-
    lable.
    Birds—The acute, oral LD   of trifluralin for mallards and pheasants
    was greater than 2000 mg/kg (Tucker and Crabtree 1970); so was the
    acute oral LD ^ for chickens (Pimentel 1971).  Data for nitralin were
    not available, and chronic feeding data were available neither for ni-
    tralin nor for trifluralin.
    Mammals—The acute oral LD,-n of trifluralin to rats was greater than
    10,000 mg/kg; for dogs and rabbits, greater than 2000 mg/kg; and for
    mice, greater than 5000 mg/kg (WSSA 1974).  No data on chronic toxi-
    city were available for trifluralin or nitralin.  The acute oral LD,_n
    of nitralin to rats was greater than 2000 mg/kg  (Jones ejt^ al. 1968).
    Conclusions-
    Although trifluralin is not particularly toxic to mammals in single
    doses, it is highly toxic to fish, amphibians, and aquatic arthropods.
    It is, moreover, highly persistent and is magnified in aquatic food
    chains.  The data are insufficient to predict disastrous consequences
    if large amounts of trifluralin are disposed of in soil, but also in-
    sufficient to be reassuring.  Data for nitralin are too sparse to per-
    mit any conclusions.
                                       133
    

    -------
    Picloram
    Piclorain, the common name for 4-amino-3,5,6-trichloropicolinic acid, was
    introduced as Tordon by the Dow Chemical Co. in 1963 as a general herbi-
    cide for woody plants and broadleaf weeds.   Pure picloram is a white
    powder with an odor similar to that of chlorine which decomposes at 215°
    C without melting.  Its water solubility is 430 ppm and its vapor pres-
    sure is 6.16 x 10   mm mercury at 35 C.  Formulations include the potas-
    sium salt in pellets or aqueous solution, the amino salts, and esters.
    The potassium salt has a water solubility of 400,000 ppm.
    Degradation-
    Biological—The biological degradation of picloram has been assumed, since
    degradation ends when soil is sterilized (Parker and Hodgson 1966) and
    because a lag period precedes picloram degradation in soil (Grover 1967) .
    The few reports of specific organisms which degrade picloram, or of de-
    gradative products, are shown in Table 28.
    In heavy clay soil, degradation of picloram wass preceded by a lag phase
    of seven days for 0.25 ppm, 30 days for 0.5 ppri, and 90 days for one ppm,
    with a soil half-life of 55, 90 and 180 days at the three levels.  Dif-
    ferences in the soil half-life were attributed entirely to the variation
    in lag periods, with a one percent per day rate of degradation thereafter
    (Grover 1967).  Degradation of one pound of picloram in soil required
    concomitant degradation of 10,000 to 100,000 pounds of organic matter
    (Youngson et al. 1967) .  The only products of picloram degradation which
    have been reported so far are the mono-dechlormated and mono-demethyl-
    ated compounds (Table 28), carbon dioxide,  and chloride ion (Goring and
    Hamaker 1971, Meikle et_ al. 1974).  Naik et_ al. (1972) considered the
    possibility of obtaining a readily biodegradable picloram to be remote,
    since most substitutions (decarboxylation,  dechlorination at C,-, deami-
    nation) decreased phytotoxicity without affecting persistence.  Adding
                                        134
    

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    -------
    carboxyl, hydroxyl or araino groups increased persistence.  Additional
    chlorine decreased persistence as did alpha- or. Z>eta-methylation, while
    gamma-methylation increased persistence.
    The rate of picloram detoxification in soil may follow half-order kine-
    tics (Hamaker et^ al. 1968), or first-order kinetics at low concentrations
    and Michaelis-Menten kinetics at high concentrations (Youngson et^ al.
    1967, Grover 1967).  Meikle et^ al. (1973) considered detoxification to
    follow 0.8-order kinetics rather than first-order kinetics, and Hance
    and McKone (1971) concluded that neither zero-order, half-order, first-
    order or Michaelis-Mentin kinetics applied.
    The sum of these data on the degradation of picloram in soil is that,
    although the herbicide is undoubtedly detoxified in soil, active micro-
    bial degradation has not been demonstrated.  Cometabolism of picloram
    by soil microorganisms is a plausible but unproven hypothesis, and de-
    gradation in soil probably proceeds no further than detoxification.
    In cattle, feeding five ppm of picloram resulted in almost quantitative
    urinary elimnation (Fisher et al. 1965).  Milk residues did not exceed
    0.2 ppm even when cows were fed 10,000 ppm picloram, but the milk was
    not tested for metabolites (Paulson 1975) .
                                                _2
    Photolytic—In water at alkaline pH, 12 x 10   M picloram  (2898 ppm) ex-
                      2
    posed to 200 yW/cm  of ultraviolet light (253.7 nm) was 20 percent de-
    composed after 48 hours.  Decomposition included destruction of the pyri-
    dine nucleus and release of two chloride ions per molecule.  Sunlight
    was both less effective and less consistent in its effects (Hall et al.
    1968).  Hedlund and Youngson (1972) considered photolysis to follow
                                                                         -4
    pseudo-first-order kinetics for concentrations of less than 4.14 x 10
    M  (99.98 ppm) and to proceed at depths of 3.65 meters even in hazy sun-
                                                      _3
    light.  Mozier and Guenzi  (1973) exposed 2.08 x 10   M of  the sodium
    salt of picloram to light between 300 nm and 380 nm.  The pH decreased
    from 9.5 to 6.0 in 34 hours and two chloride ions were released per
                                        136
    

    -------
    molecule.  The extremely limited CO- formation argued against decarboxy-
    lation as a major photolytic pathway.  Baur, Bovey and McCall (1973)
    analyzed the effects of light and temperature on the degradation of pic-
    loram as the sodium salt and as the free acid.  The acid decomposed sig-
    nificantly at 60 C and was not decomposed by UV light, whereas the salt
    was decomposed at 30°C, 60°C and by UV light at 356 nm (Baur et a^. 1973).
    Chemical and physical—Picloram was completely degraded by liquid ammo-
    nia in the presence of either metallic sodium or lithium (Kennedy et al.
    1972a) but was unaffected by 9N or 18N sodium hydroxide (Kennedy et al.
    1972b).  In soils, Corbin and Upchurch (1967) observed no detoxification
    of picloram on an organic soil, but Hance (1967, 1969) considered chemi-
    cal degradation of picloram in soils to be theoretically feasible.
    When heated to 225 C in a muffle furnace, picloram lost 48 percent of
    its weight, but remained a white solid (Stojanovic et^ aJU 1972b) .  When
    heated to 900 C, the volatile products of picloram degradation were car-
    bon monoxide, carbon dioxide, chlorine and ammonia (Kennedy et al. 1972a,
    1972b).
    Transport-
    Within soil—Adsorption of picloram decreased with increasing pH  (Farmer
    and Aochi 1974, Helling 1971b) and followed a Freundlich isotherm, char-
    acteristic of physical adsorption between the herbicide and humic acid
    molecules (Khan 1973).  Adsorption was greater with smaller soil aggre-
    gates at specific bulk densities, but pore-water velocity was more im-
    portant than either aggregate size or pore-water velocity (Davidson and
    Chang 1972).  Increasing organic matter increased picloram adsorption,
    whereas the amount of clay was of minor importance (Hamaker et al. 1966,
    Farmer and Aochi 1974) .  Adsorption decreased slightly with increasing
    temperature (Farmer and Aochi 1974).  The relative adsorption of piclor-
    am on several adsorbents was:  activated charcoal > anion exchange re-
    sins > peat moss > cellulose triacetate.  No adsorption occurred on mont-
    morillonite, kaolinite, cation exchange resins, wheat straw or cellulose
                                        137
    

    -------
    triacetate (Grover 1971).  Van Genuchten and co-workers (1974) stressed
    that picloram adsorption was not a single-valued function.
    The amount of leaching observed for picloram after various times in dif-
    ferent soils is shown in Table 29.  Most picloram in a North Carolina
    soil remained in the top layer (7.5 cm) of soil.  Less than 1.2 meter
    downslope movement occurred, probably because there were only low levels
    of runoff (Lutz et al. 1973).  In Saskatchewan, most of the picloram re-
    mained in the top six inches (15 cm) of soil, although leaching increased
    as the soil organic matter decreased (Keys and Friesen 1968) .  When pic-
    loram levels in pasture soils were monitored, residues in the 24 to 36
    inch layer (60-90 cm) of soil were greater one to three years after
    treatment than in the year of treatment, and dissipation from this lay-
    er was slow (Scifres et al. 1969).  Deeper leaching occurred on a three
    percent slope than on a one percent slope (Scifres et^ al. 1971).  Phil-
    lips and Feltner (1972) considered picloram presence at 2.4 meters to
    be the result of movement through soil cracks rather than by leaching.
    Among factors determining the extent to which picloram leached were the
    soil type, with greater leaching in sand than in clay loam (Baur et al.
    1972) and the average pore-water velocity (Davidson and McDougal 1973) .
    Both soil texture and the uniformity of soil pores affected leaching.
    Diffusion from conducting pores into adjacent mLcropores was suggested
    by Ping and co-workers (1975).  Conventional sprays and polymerized
    sprays leached to the same extent (Baur et al. L972) and adsorption was
    negatively correlated with diffusion (Walker 1970) .  Byrd and co-workers
    (1971) concluded that the lateral migration of 2.16 Ibs/A (2.42 kg/ha)
    picloram sprayed on roadsides and railbeds would not result in "undue
    hazard" to adjacent vegetation.
    Between soil and water—When 1.12 kg/ha of a one to one mixture of 2,4,5C
    T and picloram were sprayed on grassland soil in the Blacklands of Texas,
    groundwater was contaminated by one to four ppb of picloram two to nine
    months later, but not by 2,4,5-T (Bovey et_ al. 1975).  When 2.24 kg/ha
                                        138
    

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    of this mixture were applied five times at six month intervals, washoff
    from foliage accounted for most of the surface-water contamination.
    Residues on the grass were 50 to 70 ppm immediately after spraying, and
    if heavy rains occurred soon after, washoff contained 400 to 800 ppb
    picloram (Bovey e_t al. 1974).  Davis and Ingebo (1973) estimated that
    4.5 percent of the picloram applied to a chaparral watershed was lost to
    stream water.  After a heavy rain, water contained 30 to 370 ppb, and
    water contamination occurred until 40 inches of rain had fallen over a
    14 month period.
    Surveys of grasslands water sources determined that 1.1 kg/ha sprayed
    over a 32 hectare area did not contaminate soil 0.8 km downslope from
    the treated area, nor was picloram detected in wells over a two year
    period.  The dissipation of picloram from contaminated ponds proceeded
    at 14 to 18 percent per day at first, but ponds still contained 0.005
    ppm after 100 days (Haas et^ al_. 1971).  Streams 1.6 km from picloram-
    treated plots contained detectable residues for up to eight months, with
    maximum water levels of 0.04 ppm (Baur et_ a^. 1974).  In the Ogalalla
    aquifer, picloram did not move 150 feet from the point of injection dur-
    ing a ten day period (Schneider et al. 1971).
    Persistence-
    Quantifiable data on persistence of picloram in soils are summarized in
    Table 30 and Table 31, the latter summarizing a single study of picloram
    persistence in soils from several states (Goring et al. 1965).  Data for
    the disappearance of picloram in a sandy loam soil in Nova Scotia are
    shown in Figure 5.
    The relative persistence of several herbicides one and two years after
    application to Puerto Rican forest soil was:  fenac > prometone > pic-
    loram > diuron > bromacil > dicamba  when phytotoxicity was the criter-
    ion.
    After one year, residues from nine Ibs/A (10.28 kg/ha) of picloram were
    less than ten percent as high as residues from 27 Ibs/A (30.94 kg/ha)
                                       140
    

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    (Dowler et_ al_. 1968).  After three years, Parker and Hodgson  (1966) ob-
    served no further decrease in residues from four Ibs/A (4.48 kg/ha) pic-
    loram in soil underlying bracken and residues were still toxic to beans
    grown in pots.
    Picloram persistence increased with increasing soil depths (Herr et_ al.
    1966, Scifres £t al^. 1969, Hunter and Stobbe 1972) and with cool weather
    at the time of application (Scifres et_ al. 1969).  Residues from Tordon
    beads exceeded those from Tordon liquid  (Getzendaner et al. 1969) and
    residues from conventional sprays and from granules exceeded those from
    polymerized sprays (Baur et al. 1972).  Picloram disappeared more quick-
    ly from cleared forest soil than from litter-covered forest soil (Brady
    1975).  The persistence of picloram in water exposed to hazy sunlight
    was greater than 30 days in shallow containers, and greater than 56 days
    in deep containers (Hedlund and Youngson 1972).
    Effects on Non-Target Species-
    Microorganisms—The effects of massive levels of picloram on numbers of
    bacteria in soil are negative:  five tons per acre (5000 ppm) of picloram
    incorporated into a loam soil inhibited bacterial growth for at least
    56 days whether the herbicide was pure or formulated (Stojanovic et al.
    1972a).  Debona and Audus (1970) reported bacterial inhibition at less
    than 150 ppm in soil columns, but 1000 ppm was reported to have no effect
    on soil bacteria (Beynon et al. 1966) and 100-fold the normal agricultu-
    ral levels neither stimulated nor depressed bacterial growth for six
    months (Van Schreven £t_ al. 1970).  In Oregon soils, Tu and Bollen (1969)
    demonstrated that picloram inhibited bacterial numbers at ten ppm, but
    not at one ppm.
    Similarly discordant data have been reported for individual species of
    bacteria:  Asotobaoter was inhibited by  100-fold the usual agricultural
    levels (Van Schreven at_ al. 1970) but not by 1000 ppm (Beynon et al.
    1966), and Bacillus subtilis was inhibited by one ppm (Thomas et al.
                                       144
    

    -------
    1973).  Inhibition of Pseudomonas fluoreseens in culture occurred at 50
    ppm picloram  (Breazeale  and  Camper  1972).   Unaffected by 1000 ppm pic-
    loram when cultured on agar  were:   Nooard'ia opaoas  Pseudomonas aerug'i-
    nosa, Fthizobium phaesolij Aerobaoter  and Aerogenes  (Beynon et_ al. 1966).
    Fungal growth in soil was stimulated  by 5000 ppm analytical grade pic-
    loram for 56 days  (Stojanovic  et al.  1972a) and unaffected on agar by
    1000 ppm (Beynon &t^ al_.  1966).  Streptomycetes, however, were inhibited
    by 5000 ppm under the same conditions which stimulated fungal growth
    (Stojanovic et^ a^. 1972a).   On agar,  no significant effects of up to
    1000 ppm were seen in Aspergillus terreus,  Fusapium oxysporum, Penioil-
    l-iwn dig-itatwn, Rhizoctonia  solani, Pythiim ultimum,  Tviehodevma 1i-g-
    no?>iorn3 Vef-t-lailliian aWoatrum,  Streptomyaes scabies3  or Aspevgillus
    niger (Beynon et^ a]^. 1966).  In soil, formulated picloram at one and ten
    ppm inhibited the growth of  Muoov and Pen'ioi'll'Lwn species, and stimula-
    ted Aspergillus and Terreus  species (Beynon et_ al.  1966).
    Such differences in toxicity due to differences in  species and/or ex-
    perimental techniques were not found  for the effects of picloram on
    algae.  One ppm did not  inhibit the growth  of Chlorella pyvenoidosa on
    agar  (Beynon et al. 1966) but  50 ppm  depressed growth of ChloTella vul-
    gA = chlorthiamid < bromoxy-
    nil < chlorfluorazole <  ioxynil < propanil  (Debona  and Audus 1970) .
    The effects of picloram  on soil processes are shown in Table 32, and are
    seen to be minor at low  levels but  inhibiting at high levels.
                                        145
    

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    Analytical grade picloram, incorporated in soil at 5000 ppm  (five tons
    per acre) stimulated fungal growth but inhibited both streptomycetes and
    bacteria.  Formulated picloram inhibited bacteria and streptomycetes,
    but was not tested against fungi  (Stojanovic et al. 1972a).
    Invertebrates—Levels of one ppm  did not affect Daphnia over a ten week
    period (Lynn 1965).  The 48-hour  LC^ of picloram for an amphipod (Gam-
    marus lacustris) was 48 ppm, and  the 24-hour LC,.- for the  same species
    was 50 ppm.  For stone fly nymphs, the 24-hour LC-x, was estimated to be
    120 ppm (Pimentel 1971).  Snails  survived 380 ppm but not  530 ppm (Lynn
    1965) and the growth of eastern oysters (Crassostrea virgin-ica) was not
    affected by one ppm (Butler 1965).
    Fish and amphibians—The 24-hour  LC,-0 for various fish species, reviewed
    by Kenaga (1969) ranged from 2.2  ppm of the isooctyl ester for channel
    catfish (latalurus punctatus) to  less than 36 ppm of the acid for gold-
    fish (Carass-ius auratus) .  Tolerance generally increased with increasing
    temperature (Pimentel 1971).  Sergeant and co-workers (1970) noted that
    commercial formulations of picloram were toxic to fish at  concentrations
    at which picloram itself was not.  They suggested that 2-(3,4,5,6-tetra-
    chloro)-2-pyridylguanidine might  constitute a highly toxic impurity.
    Birds—The acute oral LDj-^ of picloram was over 2000 mg/kg in young mal-
    lards and young pheasants (Tucker and Crabtree 1970) and the five-day
    LC^ was greater than 5000 ppm for bobwhite, Japanese quail, Pheasants
    and mallards (Heath et^ a^. 1970).  Somers and co-workers (1973, 1974a,
    1974b,  1974c) observed no detrimental effects on hatching  success in
    pheasants or chickens when eggs were sprayed with picloram and/or 2,4-D
    and 2,4,5-T.  This study is discussed under the section on 2,4-D and
    2,4,5-T.
    Mammals—The acute oral LD-Q for  rats was 8200 mg/kg (Pimentel 1971).
    Death occurred within 14 days for half the rats fed 8200 mg/kg, for
    half the mice fed 2000 to 4000 mg/kg, and for half the rabbits fed 2000
    mg/kg (Lynn 1965).  Picloram was  tumorstatic in mice (Bradley et al.
                                       147
    

    -------
    1974).  Levels of up to 1000 mg/kg did not affect the maternal weight
    gain, litter size or resorption rate in pregnant rats if dams who died
    were excluded from the data, but fetal ossification was inhibited (Thomp-
    son et_ al. 1972).  McCollister and Young (1969) reviewed data on the tox-
    icology of picloram and noted that 0.1 percent (100 ppm) did not affect
    murine reproduction and that 3000 ppm fed to three generations of rats
    was also without reproductive effect.
    Conclusions-
    The sparse data on the biological degradation of picloram and on the na-
    ture and persistence of its terminal residues argue against its disposal
    in soil.
    In all probability the effects of picloram on soil processes and soil
    microorganisms would vary sharply with soil, temperature and other en-
    vironmental factors as well as with species.  The most probable conse-
    quence of picloram contamination would therefore be a more or less subtle
    shift in the balance of soil-dwelling species.  Since picloram persists
    for long periods in soil, the alterations would be of long duration if
    not permanent.
                                      148
    

    -------
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    -------
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                                        154
    

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                                       155
    

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    Brady, H. A.; 1975.  Picloram and dicamba persistence in forest environ-
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      bial populations in paraquat-treated soil.  Weed Res. 13:231-233.
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                                      159
    

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                                                                      14
    Deming, J. M.; 1963.  Determination of volatility losses of CDAA-C
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                                       162
    

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    Szegi, J.; 1973.  Effect of a few herbicides on the decomposition of
      cellulose.  Symp. Biol. Hung. 11:349-354. (Chem. Abstr. 79:17465j,
      1973).
    Szegi, J. and F. Gulyas; 1971.  Influence of Gramoxone on cellulose de-
      composition in soils.  Agrokem. Talajian 20:590-598. (Chem. Abstr. 77:
      125350k, 1972).
    Tabagua, M. L.;  1975.  Penetration of herbicides along a profile of re-
      claimed soils of  the Colchis plain.  Khim. Sel'sk. Khoz. 13:64-65.
      (Chem. Abstr.  82:165748f, 1975).
    Tadic, Z. D. and S. K. Ries; 1971.  Thermal and ultrasonic dealkylation
      of s-triazines via the cyclic transition state.  J. Agr. Food Chem.
      19:46-49.
    Talbert, R. E. and  0. H. Fletchall; 1965.  Adsorption of some s-tria-
      zines in soils.  Weeds 13:46-52.
    Talbert, R. E. and  J. M. Kennedy; 1972.  Effects of activated carbon on
      fluometuron, nitralin, and trifluralin activity in soil.  Proc. S.
      Weed Sci. Soc. 25:394-402.
    Taylor, H. F. and R. L. Wain; 1962.  Side chain degradation of certain
      w-phenoxyalkane carboxylic acids by Nocardia aoeliaoa and other micro-
      organisms isolated from soil.  Proc. Roy. Soc. (London), Ser. B 156
      (963):172-186.
                                       204
    

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    Teater, R. W., J. L. Mortensen and P. F. Pratt; 1958.  Effect of certain
      herbicides on rate of nitrification and carbon dioxide evolution in
      soil.  J. Agr. Food Chem. 6:214-216.
    Thomas, V. M., Jr., L. J. Buckley, J. D. Sullivan, Jr. and M. Ikawa;
      1973.  Effect of herbicides on the growth of Chlovella and Bacillus
      using the paper disc method.  Weed Sci. 21:449-451.
    Thompson, D. J., J. L. Emerson, R. J. Strebing, C. C. Gerbig and V. B.
      Robinson; 1972.  Teratology and postnatal studies on 4-amino-3,5,6-
      trichloropicolinic acid (picloram) in the rat.  Food Cosmet. Toxicol.
      10:797-803. (Chem. Abstr. 78:80574p, 1973).
    Thorneburg, R. P. and J. A. Tweedy; 1973.  Rapid procedure to evaluate
      the effect of pesticides on nitrification.  Weed Sci. 21:397-399.
    Tomlinson, T. E., B. A. G. Knight, A. W. Bastow and A. A. Heaver; 1968.
      Structural factors affecting the adsorption of bipyridinuim cations
      by clay minerals.  SCI (Soc. Chem. Ind., London) Monogr. No. 29:317-
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    Torstensson, N. T. L., J. Stark and B. Gdransson; 1975.  The effect of
      repeated applications of 2,4-D and MCPA on their breakdown in soil.
      Weed Res. 15:159-164.
    Tortensson, L.; 1974.  Effects of MCPA, 2,4,5-T, linuron, and simazine
      on some functional groups of soil microorganisms.  Swed. J. Agric.
      Res. 4:151-160.
    Trichell, D. W., H. L. Morton and M. G. Merkle; 1968.  Loss of herbi-
      cides in runoff water.  Weed Sci. 16:447-449.
    Trzecki, S. and E. Kowalski; 1974.  Translocation of Gesatop and Gesa-
      prim (simazine and atrazine) in relation to precipitation and type of
      compaction of soil.  Zesz. Nauk. Akad. Roln. Warszawie, Roln. 15:93-
      101. (Chem. Abstr. 83:73445x, 1975).
    Tsvetkova, S. D.; 1966.  The action of simazine and atrazine on agro-
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      (Chem. Abstr. 64:20578f, 1966).
                                       205
    

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    Tu, C. and W. B. Bollen; 1969.' Effect of Tordon herbicides on micro-
      bial activities in three Willamette Valley soils.  Down Earth 25(2):
      15-17.
    Tucker, B. V., D. E. Pack and J. N. Ospenson; 1967.  Adsorption of bi-
      pyridylium herbicides in soil.  J. Agr. Food Chem. 15:1005-1008.
    Tucker, R. K. and D. G. Crabtree; 1970.  Handbook of toxicity of pes-
      ticides to wildlife.  U.S. Fish Wildl. Serv.,  Bur. Sport Fish. Wildl.,
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    Tulabaev, B. D.; 1970.  Effect of herbicides on soil microflora in cot-
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    Tulabaev, B. D.; 1971.  Effect of the herbicides simazine, atrazine,
      monuron, phenuron, and diuron on the microflora of meadow soil.
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      77:30244q, 1972).
    Tulabaev, B. and N. Azimbegov; 1967.  Effect of triazine and urea deri-
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    Tulabaev, B. and S. Tamikaev; 1968.  Effects of herbicides on meadow
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      1968).
    Turski, R. and A. Steinbrick; 1974.  Possibilities of binding herbi-
      cides of triazine derivatives by humic acids.   Pol. J. Soil Sci. 4:
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    Tyunyaeva, G. N., A. K. Minenko and L. A. Pen'kov; 1974.  Effect of
      Treflan on the biological properties of the soil.  Agrokhimiya 1974:
      110-114. (Chem. Abstr. 81:115626y, 1974).
    Ukeles, R.; 1962.  Growth of pure cultures of marine phytoplankton in
      the presence of toxicants.  Appl. Microbiol. 10:532-537.
    Ulasevich, E. I., I. V. Veselovskii and Y. P. Man'ko; 1970.  Effect of
      linuron on microflora of low-humus chernozem.   Mikrobiol. Zh. (Kiev)
      32:497-502. (Chem. Abstr. 75:34336c, 1971).
                                      206
    

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    Ulasevich, E. I., S. N. Kharchenko, S. V. Yakuboskii and Yu. P. Man'ko;
      1973.  Effect of linuron on microflora of chernozem and rhizosphere
      of corn and soybeans.  Ilikrobiol. Zh. (Kiev) 35(2):231-235.  (Chem.
      Abstr. 79:74784m, 1973).
    Upchurch, R. P., F. T. Corbin and F. L. Selman; 1969.  Persistence pat-
      tern for diuron and linuron in Norfolk and Duplin sandy loam soils.
      Weed Sci. 17:69-77.
    Van Bladel, R. and A. Moreale; 1974.  Adsorption  of fenuron and monu-
      ron (substituted ureas) by two montmorillonite  clays.  Soil Sci. Soc.
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    Van Genuchten, M. Th., J. M. Davidson and P. J. Wierenga; 1974.  Evalu-
      ation of kinetic and equilibrium equations for  the prediction of pes-
      ticide movement through porous media.  Soil Sci. Soc. Amer., Proc.
      38:29-35.
    Van Schreven, P. A., D. J. Lindenbergh and A. Koridon; 1970.  Effect of
      several herbicides on bacterial populations and activity and the per-
      sistence of these herbicides in soil.  Plant Soil 33:513-532.
    Vega, L. A.; 1974.  Mobility and persistence of atrazine and metribuzin
      in four soils from Puerto Rico.  J. Agr. Univ. P.R. 58:379-380.
    Venkataraman, G. S. and B. Rajyalakshmi; 1972.  Relative tolerance of
      nitrogen-fixing blue-green algae to pesticides.  Indian J. Agr. Science
      42:119-121.
    Venkataraman, G. S. and B. Rajyalakshmi; 1971.  Interactions between,
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    Vernetti, J. B. and V. H. Freed; 1963a.  Vapor losses of thiolcarbamates
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      1966).
    Vernetti, J. B. and V. H. Freed; 1963b.  Soil behavior of four thiol-
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      (Chem. Abstr. 64:1280c, 1966).
                                       207
    

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    Vicario, B. T.; 1972.  Effect of pesticides (2,4-D ester, Agroxone 4,
      and malathion) on the phosphorus, potassium, calcium, and total ni-
      trogen levels.  Araneta Res. J. 19:103-114.
    Vinitikova, H., V. Skrdleta and M. Srogl; 1965.  Sensitivity of nodule
      bacteria to several herbicides.  Plant Microbes Relationships, Proc.
      Symp., Prague 1963:264-268. (Chem. Abstr. 63:18954a, 1965).
    Virmani, M., J. 0. Evans and R.  I. Lynn; 1975.  Preliminary studies of
      the effects of s-triazine, carbamate, urea,  and Karbutitate herbicides
      on growth of freshwater algae.  Chemosphere 4:65-71.
    Voets, J. P., P. Meerschman and W. Verstraete; 1974.  Soil microbiolo-
      gical and biochemical effects of long-term atrazine applications.
      Soil Biol. Biochem. 6:149-152.
    Voinova, G. and D. Bakalivanov;  1970.  Detoxication of certain amino-
      triazine herbicide by soil bacteria.  Med. Fac. Landouwwetensch., Rij-
      ksuniv. Gent. 35:839-846. (Chem. Abstr. 75:117414c, 1971).
    Volynchuk, I. M.; 1974.  Effect of herbicides on the biological activi-
      ty of soil.  Vestn. Sel'skokhoz. Nauki Kaz.  17:84-86.  (Chem. Ahstr.
      81:86686k, 1974).
    Walker, A.; 1970.  Diffusion coefficients for two triazine herbicides
      in six soils.  Weed Res. 10:126-132.
    Walker, A.; 1972.  Volatility of  (14C)-labeled atrazine and linuron
      from aluminum planchets.  Weed Res. 12:275-278.
    Wallnoefer, P.; 1968.  Untersuchungen fiber die antimikrobielle Wirkung
      von Deiquat und Paraquat.  Z.  Pflanzenkr. Pflanzenschutz 75:218-224.
    Wallnoefer, P.; 1969.  The decomposition of urea herbicides by Bacillus
      sphaericus, isolated from soil.  Weed Res. 9:333-339.
    Wallnoefer, P. and J. Bader; 1970.  Degradation of urea herbicides by
      cell-free extracts of Bacillus sphaericus.  Appl. Microbiol. 19:714-
      717.
    Wallnoefer, P. and G. Engelhardt; 1971.  Degradation of phenylamides by
      Bacillus sphaerieus.  Arch. Mikrobiol. 80:315-323.
                                       208
    

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    Wallnoefer, P. R. , S. Safe and 0. Hutzinger; 1973.  Microbial demethyl-
      ation and debutynylation of four phenylurea herbicides.  Pestic. Bio-
      chem. Physiol. 3:253-258.
    Watson, J. R., A. M. Posner and J. P. Quirk; 1973.  Adsorption by the
      herbicide 2,4-D on goethite.  J. Soil Sci. 24:503-511.
    Weber, J. B.; 1970a.  Adsorption of s-triazine by montmorillonite as a
      function of pH and molecular structure.  Soil Sci. Soc. Amer. Proc.
      34:401-404.
    Weber, J. B.; 1970b.  Mechanisms of adsorption of s-triazines by clay
      colloids and factors affecting plant availibility.  Residue Reviews
      32:93-130.
    Weber, J. B. and J. A. Best; 1972.  Activity and movement of 13 soilo
      applied herbicides as influenced by soil reaction.  Proc., S. Weed
      Sci. Soc. 25:403-413.
    Weber, J. B. and H. D. Coble; 1968.  Microbial decomposition of diquat
      adsorbed on montmorillonite and kaolinite clays.  J. Agr. Food Chem.
      16:475-478.
    Weber, J. B., P. W. Perry and R. P. Upchurch; 1965.  Influence of tem-
      perature and time on the adsorption of paraquat, diquat, 2,4-D, and
      prometone by clays, charcoal and an anion-exchange resin.  Soil Sci.
      Soc. Amer., Proc. 29:678-688.
    Weber, J. B., J. A. Best and W. W. Witt; 1974a.  Herbicide residues and
      weed species shifts on modified soil field plots.  Weed Sci. 22:427-
      433.
    Weber, J. B., S. B. Weed and T. W. Waldrep; 1974b.  Effect of soil con-
      stituents on herbicide activity in modified-soil field plots.  Weed
      Sci. 22:454-459.
    Wedemeyer, G. A.; 1966.  Uptake of 2,4-dichlorophenoxyacetic acid by
      Pseudomonas f1ouz>escens.   Appl. Microbiol. 14:486-491.
    Wegrzyn, T.; 1971.  Effect of some herbicides on Azotobaeter clwoococcwn.
      Acta Microbiol. Pol. Ser. B.; 3:131-134. (Chem. Abstr. 76:10869y,
      1972).
                                       209
    

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    Weldon, L. W. and F. L. Tiramons; 1961.  Photochemical degradation of di-
      uron and monuron.  Weeds 9:111-116.
    Wellborn, T. L., Jr.; 1969.  Toxicity of nine therapeutic and herbici-
      dal compounds to striped bass.  Progr. Fish Cult. 31:27-32.
    White, A. W., A. P. Barnett, B. S. Wright and J. H. Holladay; 1967.
      Atrazine losses from fallow land caused by runoff and erosion.  Envi-
      ron. Sci. Technol. 1:740-744.
    Whiteside, J. S. and M. Alexander; 1960.  Measurement of microbiologi-
      cal effects of herbicides.  Weeds 8:204-213.
    Whiteside, T.; 1971.  The Withering Rain.  E. P. Button and Co., Inc.
      N.Y.
    Whitworth, J. W., B. C. Williams and W. Garner; 1965.  The influence of
      herbicides on soil metabolism.  Proc., Western Weed Control Conf. 20:
      10.
    Wiersma, G. B., H. Tai and P. F. Sand; 1972.  Pesticide residue levels
      in soils, fiscal year 1969.  National Soils Monitoring Program.  Pes-
      tic. Monit. J. 6:194-228.
    Wilkinson, V.; 1969.  Ecological effects of diquat.  Nature 224:618-
      619.
    Wilson, D. C. and C, E. Bond; 1969.  Effects of the herbicides diquat
      and dichlobenil (Casoran) on pond invertebrates.  Trans. Amer. Fish.
      Soc. 98:438-443.
    Willis, G. H., R. C. Wander and L. M. Southwick; 1974.  Degradation of
      trifluralin in soil suspensions as related to redox potential.  J.
      Environ. Qual. 3:262-265.
    Willis, G. H., R. L. Rogers and L. M. Southwick; 1975.  Losses of diu-
      ron, linuron, fenac, trifluralin in surface drainage water.  J. Envi-
      ron. Qual. 4:399-402.
    Winely, C. L. and C. L. San Clemente; 1970.  Effects of pesticides on
      nitrite oxidation by Nitrobacter agilis.  Appl. Microbiol. 19:214-
      219.
                                       210
    

    -------
    Winely, C. L. and C. L. San Clemente; 1971.  Effect of two herbicides
      (CIPC  [isopropyl fl/-(3-chlorophenyl)carbamate] and eptam (S-ethyl di-
      ^^-propylthiocarbamate) on oxidative phosphorylation by
      agilis.  Can. J. Microbiol. 17:47-51.
    Wolf, D. C. and J. P. Martin; 1974.  Microbial degradation of bromacil-C
      2-14C and terbacil-2-  C.  Soil Sci. Soc. Amer., Proc. 38:921-925.
    Wright, W. L. and G. F. Warren; 1965.  Photochemical decomposition of
      trifluralin.  Weeds 13:329-331.
    WSSA; 1974.  Herbicide handbook of the Weed Science Society of America.
      Champaign, Illinois 61820.
    Wuu, K. D. and W. F. Grant; 1966.  Morphological and somatic chromoso-
      mal abberrations induced by pesticides in barley (Hordeum vulgare) .
      Can. J. Genet. Cytol. 8:481-501.
    Yatsenko, V. G. and E. N. Balkova; 1971.  Duration of the toxic action
      of herbicides in sugar beet seed plantings.  Khim. Sel. Khoz. 9:530-
      532. (Chem. Abstr. 75:150613q, 1971).
    Yatsenko, V. G. and L. M. Komissarov; 1970.  Infiltration and inacti-
      vation in soil of herbicides applied by banding.  Khim. Sel. Khoz.
      8:688-689. (Chem. Abstr. 74:2913b, 1971).
    Yeo, R. R. ; 1967.  Dissipation of diquat and paraquat, and effects on
      aquatic weeds and fish.  Weeds 15:42-46.
    Youngson, C. R. , C. A. I. Goring, R. W. Meikle, H. H. Scott and J. D.
      Griffith; 1967.  Factors influencing the decomposition of Tordon her-
      bicide in soils.  Down Earth 23:3-11.
    Yu, C. , D. J. Hansen and G. M. Booth; 1975.  Fate of dicamba in a model
      ecosystem.  Bull. Environ. Contam. Toxicol. 13:280-283.
    Zavarzin, V. I.; 1966.  Effect of herbicides on some agrochemical pro-
      perties of soil.  Agrokhimiya 1966:121-124. (Chem. Abstr. 65:2924f,
      1966).
    Zavarzin, V. I. and T. V. Belyaeva; 1966.  Effect of herbicides on es-
      sential plant minerals in soil.  Khim. Sel. Khoz. 4:34-36. (Chem.
      Abstr. 66:27926f, 1966).
                                      211
    

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    Zharasov, S. U.; 1971.  Effect of herbicides on the intensity of nitri-
      fication.  Vestn. Sel'skokhoz. Nauki (Alma-Ata) 14(11):41-44. (Chem.
      Abstr. 77:71254m, 1972).
    Zharasov, S. U.; 1972.  Action of herbicides on the microflora of dark
      chestnut soils in sugar beet plantings in the Alma-Ata region.  Vestn.
      Sel'skokhoz. Nauki (Alma-Ata) 15(2):25-29. (Chem. Abstr. 77:44266k,
      1972).
    Zharasov, S. U. and S. A. Chulakov; 1972.  Dynamics of the biological
      activity of light chestnut soils during the use of herbicides.  Tr.
      Kaz. Nauch.-Issled. Inst. Zashch. Rast. 11:163-170. (Chem. Abstr. 78:
      93450s, 1973).
    Zharasov, S. U., G. M. Tsukerman and S. A. Chulakov; 1972.  Effect of
      herbicides used in sugar beet plantings on soil fungi.  Khim. Sel.
      Khoz. 10:617-619. (Chem. Abstr. 77:125260f, 1972).
    Zimdahl, R. L., V.  H. Freed, M. L. Montgomery and W. R.  Furtick; 1970.
      The degradation of triazine and uracil herbicides in soil.  Weed Res.
      10:18-26.
    Zinchenko, V. A. and T. V. Osinskaya; 1969.  Change in the biological
      activity of soil during composting with herbicides.  Agrokimiya 1969:
      94-101. (Chem. Abstr. 72:2381k, 1970).
    Zinchenko, V. A., T. V. Osinskaya and N. A. Prokudina; 1969.  Effect of
      herbicides on the biological activity of the soil.  Khim. Sel. Khoz.
      7:850-853. (Chem. Abstr. 72:131326v, 1970).
    Zubets, T. P.; 1970.  Effect of herbicides on nitrifying bacteria.  Nauch.
      Tr., Sev.-Zapad.  Nauch.-Issled. Inst. Sel. Khoz. 19:46-49. (Chem.
      Abstr. 75:34340z, 1971).
    Zubets, T. P.; 1973.  Residual action of simazine and atrazine on the
      microflora and enzyme activity in sod-podzolic soil.  Nauchn. Tr.,
      Sev.-Zapadn. Nauchno-Issled. Inst. Sel'sk. Khoz. 24:103-109.
    Zurawski, H. and M. Ploszynski; 1970.  Rate of Lorox detoxication in
      light soils.  Rocz. Glebozn. 21(1):99-104. (Chem. Abstr. 74:110651y,
      1971).
                                       212
    

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                           SECTION IV INSECTICIDES
    
    CHLORINATED HYDROCARBON INSECTICIDES
    Of the numerous pesticides commonly included under the heading of "chlor-
    inated hydrocarbons" or "organochlorines", the 12 compounds to be dis-
    cussed are:  DDTS its hydroxy-analog dicofol, and its methoxy-analog
    methoxyahlorj the cyclodiene insecticides aldrin, dieldrins endrin, mi~
    rex3 kepone (chloTdecone)3 'heptaohtoTi and ohlordjane; the sulfur con-
    taining cyclodiene, endosulfan; and the chlorinated terpene mixture
    designated as toxaphene.
    The literature for each compound or group of compounds is reviewed sep-
    arately, but certain papers which compare the chlorinated hydrocarbon
    insecticides with each other and with other pesticides are reviewed be-
    low.  In this way a perspective is obtained as to the relative stabili-
    ty, mobility, persistence, and toxicity of these highly controversial
    compounds.  Similarly, conclusions for all the organochlorine insecti-
    cides are discussed at the end of the section and not after the sepa-
    rate reviews.
    Degradation-
    The ultimate fate of the millions of tons of chlorinated hydrocarbon in-
    secticides which have been dispersed into the air, the soil, and the
    water is not known.  Schuphan and Ballschmiter (1972) concluded that the
    dechlorination of the cyclodienes under the influence of the soil pH was
    essentially impossible, but considered photochemical dechlorination, as
    on leaf surfaces, of possible significance.  Alexander (1968) argued
    persuasively that biodegradation of certain molecules, including DDT,
                                       213
    

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    might occur only in the laboratory, since cometabolism is of no advan-
    tage to microorganisms outside the laboratory (c.f.  DDT, section on
    biological degradation).
    While the ultimate reality of such hypotheses remains to be tested, the
    persistence of most chlorinated hydrocarbon insecticides is demonstrated
    by the sizable residues present 16 and 21 years after application (Nash
    and Harris 1973, Bennett et^ aL. 1974, Ruhr et^ al_. 1972), and by the pre-
    sence of chlorinated hydrocarbon residues in all phases of the environ-
    ment:  in soils (Gish 1970, Wiersma et^ al. 1972), in rainwater (Wheatley
    and Hardman 1965, Tarrant and Tatton 1968) and groundwater (Achari et
    al. 1975), in the atmosphere (Risebrough ej^ al. 1968, Stanly et al.
    1971, Bidleman and Olney 1974) and in polar mammals  (Tatton and Ruzicka
    1967, Clausen et al. 1974).
    Wiersma et al. (1972) examined fifty sites in each of five cities for
    arsenic, DDT and its metabolites, dieldrin, chlordane, heptachlor and
    its epoxide, toxaphene, endrin, and organophosphates.  Considerable
    variation was found between cities, with Miami having the highest resi-
    dues and Houston the lowest; within cities, residues were higher in
    lawns than in unkempt areas.  Organophosphate residues were rare, but
    organochlorine residues were common.
    The levels of pesticide residues found in three surveys of agricultu-
    ral soils are shown in Table 33.
    Transport-
    Although the organochlorines are among the least mobile of insecticides,
    movement through soil is seen during their long persistence in soil.
    The relative mobilities of organochlorine pesticides are shown in Table
    34.
    Burkhardt and Fairchild (1967) observed that the mobility of aldrin,
    heptachlor, and three organophosphate insecticides varied with the com-
    pound, its rate of application, the soil type, soil moisture, time of
                                       214
    

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               Table 33.  RESIDUES OF PESTICIDES FOUND IN SOILS
    
    Compound
    DDT
    DDE
    ODD
    Aldrin
    Dieldrin
    Endrin
    Heptachlor
    Heptachlor epoxide
    y-chlordane
    BHC
    Malathion
    Atrazine
    2,4,5-T
    PPM^'
    97.70
    12.65
    3.33
    2.13
    3.33
    6.55
    0.40
    0.24
    0.63
    *
    *
    *
    *
    PPM^ % %-/
    1-9 45 *
    * *
    * *
    0.75 32 75
    ii it it
    * *
    0.06 9 *
    II M *
    0.86 9 *
    * 75
    * 43
    * 36
    * 24
    *Not sought
    _!/  S.W. Ontario farmland by Harris and Sans 1971.
    2J  Canadian Atlantic Provinces by Duffy and Wong 1967.
    _3/  Five W. Alabama Counties by Albright et_ aiU 1974.
    Residues are given in PPM for contaminated  soil in studies 1 and  2,
    and the percent of soils contaminated is shown for studies 2 and  3.
                                    215
    

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    Table 34.  RELATIVE MOBILITIES OF PESTICIDES IN SOIL:
      PESTICIDES LISTED IN DECREASING ORDER OF MOBILITY
    BHC                                   Aldrin
    Isodrin                               Dyfonate
    Heptachlor                            Lindane
    Endrin                                Dieldrin
    Toxaphene                             Parathion
    Dieldrin                              DDT
    Aldrin                                Diazinon
    Dilan                                 Azinphosmethyl
    Chlordane
    
    1.  Nash and Woolson 1968:  mobility within soil.
    2.  Lichtenstein and Schulz 1970:  volatilization in
          soil-water mix.
                              216
    

    -------
    year and interval of sampling.  Using bioassay of field-treated soils,
    they concluded that aldrin and heptachlor were more mobile than diazi-
    non, parathion, or phorate.  Nash and Woolson (1968) found aldrin, diel-
    drin, dilan, toxaphene and chlordane to be less evenly dispersed through
    cultivated sandy loam than were BHC or isodrin.  After fourteen years,
    the greatest concentrations of dieldrin, dilan, toxaphene, and chlor-
    dane were found in the soil at depths between 7.6 and 23 centimeters.
    Except for BHC and isodrin, 95 percent of the pesticides remained in
    the upper 23 centimeters.  Harris and Sans (1969) noted that organo-
    chlorines penetrated cultivated soil more deeply than uncultivated
    soil, and mineral soil more deeply than muck.  Carter and Stringer (1970)
    found that aldrin, dieldrin, gamma-chlordane and heptachlor penetrated
    soils to the same extent, with soil type and soil moisture the chief
    factors affecting depth of penetration.  In sandy soil, moisture af-
    fected penetration more than in muck, which retained 70 percent of all
    the pesticides in the upper soil layers regardless of moisture levels.
    Lichtenstein et al. (1971b) observed that cultivation sharply decreased
    soil residues of both heptachlor and aldrin (or dieldrin), presumably
    because cultivation increased volatilization.  For heptachlor, a resi-
    due reduction of 76 to 82 percent was recorded.
    Goerlitz and Law (1974) noted that the distribution of chlorinated hy-
    drocarbons in stream bottom material varied significantly with size,
    organic matter content, and composition of the stream-bottom particles:
    sand was free of organochlorine residues while gravel with shell mater-
    ial carried large amounts of hydrocarbons.  Ju-Chang and Liu (1970)
    compared the behavior of three organochlorines on three clays, and found
    the relative levels of adsorption to be:  DDT > dieldrin > heptachlor.
    All three pesticides were adsorbed almost instantaneously to the sur-
    face of kaolinite and illite; and DDT and heptachlor diffused, somewhat
    more slowly, into the intralamellar spaces of montmorillonite.  Diel-
    drin did not diffuse into montmorillonite.  The difference was consid-
    ered due to hydrogen-bond formation in the adsorption of DDT and hepta-
                                      217
    

    -------
    chlor onto clays, while dieldrin adsorption was attributed to interac-
    tions of its epoxide ring with oxygen molecules in the clays.  The ad-
    sorptive capacities of the clays with respect to these three pesticides
    was not correlated with their ion exchange capacities or with their
    specific surface areas.  Contamination of drinking water by DDT and
    DDE was decreased by routine water treatment, but BHC and toxaphene
    were less readily removed, apparently because the latter are carried
    in solution rather than adsorbed on particulate contaminants (Nichol-
    son et_ al. 1968) .
    Mistric and Gaines (1953) found the relative loss of insecticide from
    cotton leaf surfaces to be greatest for dieldrin and least for gamna-C
    BHC, aldrin, dieldrin, heptachlor, and methyl parathion; losses of
    toxaphene, endrin and EPM were intermediate.  That a large portion of
    the volatilized pesticides is subsequently precipitated is suggested
    by the presence of pesticides in rainwater and on unsprayed terrain.
    Hartley (1968) suggested, however, that those pesticide residues which
    escape to a height of 50 meters might, by eddy diffusion, be carried
    to the ionosphere and there undergo photolytic degradation.
    Persistence-
    Harris (1969) classified nine soil-applied pesticides as highly, moder-
    ately, or slightly residual:  The highly residual compounds, which re-
    tained full activity for 48 weeks in sandy loam, were DDT and dieldrin;
    aldrin, Dasanit, and carbofuran were moderately residual, retaining full
    activity for 16 weeks in sandy loam; parathion, diazinon, phorate and
    Dursban lost all detectible activity within four weeks in sandy loam
    and were considered to be only slightly residual.  The criterion of "ac-
    tivity" was defined by bioassay, beginning with four times the LD ^ of
    each compound.  The position of aldrin as "moderately persistent" re-
    sulted from its conversion to the less potent dieldrin.  Tests in muck
    resulted in slightly longer persistence for all compounds.
                                       218
    

    -------
    Table 35 shows the relative persistence of the most common chlorinated
    hydrocarbon pesticides with respect to each other and to other pesti-
    cides.  With the exception of methoxychlor, which was less persistent
    than parathion (Carlo et_ al_. 1952), chlorinated hydrocarbons are consis-
    tently more persistent than insecticides of other classes.
    Toxicity-
    The relative toxicities of organochlorine pesticides in mammals and
    fish are listed in Table 36.
    Macek and McAllister (1970) stated that, as a group, organochlorine in-
    secticides are more toxic to fish than either the organophosphate or car-
    bamate pesticides.  Moreover, whereas large interspecies variability
    was observed in piscine sensitivity to organophosphates, relatively
    uniform sensitivities to organochlorines were found.
                                       219
    

    -------
    
    
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    -------
       Table 36.  RELATIVE TOXICITIES OF PESTICIDES TO MAMMALS, FISH, AND
            BEES: PESTICIDES LISTED IN DECREASING ORDER OF TOXICITY
         1
       Rats
         2
       Fish
         3
       Fish
        4
      Bees
    Endrin
    Dieldrin
    Aldrin
    Toxaphene
    Heptachlor
    Endosulfan
    DDT
    Chlordane
    Dicofol
    Methoxychlor
    Endrin
    Rotenone
    Toxaphene
    Pyrethrum
    Aldrin
    DDT
    Lindane (gamma-EEC)
    Heptachlor
    Parathion
    Systox
    Dicofol
    Vapam
    Malathion
    delta-EEC
    Diazinon
    Perthane
    Ovotran
    Metasystox
    alpha-EEC
    Tedion
    Endrin
    p,p'-DDT
    Dieldrin
    Aldrin
    Dioxathion
    Heptachlor
    Lindane
    Methoxychlor
    Phosdrin
    Malathion
    DDVP
    Methyl parathion
    Azinphos
    DDVP
    Carbaryl
    DDT
    Dicofol
    1.  Martin 1968:
     acute oral LD   in rats.
    2.  Adlung 1957:  Toxicity of pesticides to the guppy, Lebistes reti-cu-
                      latus.
    3.  Eisler 1970b:  96-hour toxicity in estuarine fish.
    4.  Anderson and Atkins 1958.
                                      221
    

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    DDT and Dicofol
    DDT is the common name for the technical product in which p^p'-DDT is
    the predominant compound.  The acronym DDT stands for dichlorodiphenyl-
    trichloroethane, known as l,l,l-trichloro-2,2-bis-(4-chlorophenyl)eth-
    ane.  DDT was the first of the wide spectrum organic insecticides, in-
    troduced in 1942 by Geigy under the trade names Gesarol, Guesarol, and
    Neocid.  It is a potent nonsystemic stomach and contact insecticide
    which had little effect on phytophagous mites, aphids, or scale insects,
    but was used with striking success on a wide variety of agricultural
    and public health pests.
    DDT is synthesized by the condensation of one mole of chloral with two
    moles of chlorobenzene in the presence of sulfuric acid.  The p3p '-iso-
    mer forms colorless crystals with a melting point of 108.5 C and a va-
    por pressure of 1.9 x 10   mm mercury at 20 C.  The technical product
    contains up to 30 percent of the o^p'-isomer and is a waxy solid of
    indefinite melting point.  Pure p^p'-DDT and its O3p '-isomer are prac-
    tically insoluble in water (0.0012 ppm at room temperature), moderate-
    ly soluble in hydroxylic and polar solvents, and readily soluble in
    most aromatic and chlorinated solvents (Martin 1968).  Brooks (1974,
    vol. 1) listed the solubility of DDT in acetone, benzene, and carbon
    tetrachloride as 580, 780, and 450 mg/ml, respectively.
    Dicofol is the common name for 2,2,2-trichloro-l,l-bis-(4-chlorophenyl)
    ethanol, a nonsystemic acaricide with little insecticidal activity, in-
    troduced by Rohm and Haas in 1955 as Kelthane.  It is synthesized by
    the reaction of l,l-dichlorophenyl-l,2,2,2-tetrachloroethane with sil-
    ver acetate followed by hydrolysis of the resulting ester.  Commercial-
    ly, dicofol is formulated as an 18.5 percent or 42 percent emulsifiable
    concentrate, an  18.5 percent wettable powder, or in a dust base at 30
    percent.  The wettable powder formulations are sensitive to solvents
                                      222
    

    -------
    and surfactants, which may affect acaricidal activity or phytotoxi-
    city.
    Pure dicofol is a white solid with a melting point of 78.5 to 79.5°C,
    but the technical product is a brown viscous oil of about 80 percent
    purity, essentially insoluble in water and soluble in most aliphatic
    and aromatic solvents.  Dicofol is also a metabolite of DDT (Khan
    1975).
    DDD is the acronym for dichlorodiphenyldichloroethane, known as 1,1-5
    dichloro-2,2-bis(p-chlorophenyl)-ethane.  It is both a metabolite of
    DDT (Brooks 1974, vol. 2) and an insecticide produced by Rohm and Haas
    as Rhothane for use against lepidoptera and as a mosquito larvicide.
    DDD is also referred to as TDE.
    Degradation-
    Biological—The major degradative pathways for DDT are dehydrodechlor-
    ination to DDE and reductive dechlorination to DDD (TDE), as shown in
    Figure 6.  Some microorganisms and some insects are able to oxidize
    DDT to dicofol, but for mammals, plants, birds, and most microorganisms,
    DDD and DDE are the first, and often the only, metabolites.  DDE is
    usually considered less acutely toxic than DDT, but it is more toxic
    to pigeons (Brooks 1974, vol. 2); moreover, DDE is extremely stable
    in most organisms, with a half-life of 250 days in pigeons (Bailey et
    al. 1969a, 1969b).  DDD is readily metabolized in vertebrates via
    DDMU, as shown in Figure 6.
    The metabolism of DDT by microorganisms is summarized in Tables 37 and
    38, which show the products of DDT metabolism as well as the organism
    or conditions under which conversion occurred.  Anaerobically, DDT was
    converted principally to DDD (Guenzi and Beard 1967); addition of al-
    falfa components accelerated the reaction, but two percent oxygen in
    the medium sufficed to inhibit the dechlorination (Burge 1971) .  Guen-
    zi and Beard (1968) found that the anaerobic conversion of DDT to DDD
                                      223
    

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    /    \       \
                                               J-l
                                               fn
    224
    

    -------
      Table  37.  DEGRADATION OF DDT BY MICROORGANISMS UNDER LABORATORY
          CONDITIONS INCLUDING THE ORGANISMS AND THE PRODUCTS  FORMED.
            STRUCTURES FOR NAMED COMPOUNDS ARE  SHOWN IN  FIGURE 6
    Organism
    Actinomycetes
    AeTobaater aevogenes
    Baker's yeast
    Proteus vulgaris
    Fusar-ittm oxysporum
    Products
    DDD
    ODD
    DDD
    DDD
    DBH, DEP
    Reference
    Chacko et_ al. 1966
    Wedemeyer 1966,
    1967
    Ibid.
    Ibid.
    Engst and Kujawa
    Esahe-piehia coli
    Trichodevma
    Aerobaoter aerogenes
    MUQOV alternans
    
    Erwin-ia sp .
    
    Stpeptamyoes
    
    Ankistpodemus amallo-ides
    
    Daphn-uz pulex
    DDD
    
    DDD, DDE, Dicofol
    
    
    DDD  '' i \  r-
    
    3 hexane soluble
    2 water soluble
    
    dechlorinated ethane
    moiety
    dechlorinated ethane
    moiety
    DDE, DDD
    
    DDE
    1967
    Langlois 1967
    Matsumura and Boush
    1968
    Plimmer et_ al. 1968
    Anderson et al. 1970
    Van Dijk et_ aj^. 1973
    
    Ibid.
    
    Neudorf and Khan
    1975
    Ibid.
                                       225
    

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       Table 38.  DEGRADATION OF DDT BY MICROORGANISMS UNDER LABORATORY
      CONDITIONS INCLUDING THE CULTURE CONDITIONS AND THE PRODUCTS FORMED.
             STRUCTURES FOR NAMED COMPOUNDS ARE SHOWN IN FIGURE 6
    
    Conditions
    Soil,
    Soil,
    anaerobic
    aerobic
    20 cultures selected for
    Products
    ODD
    DDE
    ODD, DDA
    Reference
    Guenzi
    1967
    Ibid.
    Patil
    and Beard
    
    and Matsumura
      dieldrin degradation
    Nitrogen, nitrogen + C0r
    ODD, DDE
      atmosphere
    Microarthropods               DDE
    Soil, anaerobic               ODD
    Lake Michigan microorganisms  TDK and DDNS
    Estuarine films
    Marine algae
    Marine microorganisms
    
    Sewage
    
    Flooded soil
    
    Flooded soil
    Everglades muck
    TDE, DDNS, DDOH
    TDE, DDNS, DDOH
    TDE, DDNS, DDOH
    
    ODD, DDE, DBF
    
    ODD
    
    ODD
    DDE, ODD
    1968
    Parr et. al. 1970
    
    Butcher et_ al. 1970
    Burge 1971
    Matsumura et al.
    1971
    Ibid.
    Patil et.
                 1972
    Matsumura and Boush
    1972
    Pfaender and
    Alexander 1973
    Castro and Yoshida
    1974
    Farmer et al. 1974
    Parr and Smith 1974
                                      226
    

    -------
    was essentially complete after 12 weeks, with only one percent of the
    DDT remaining, and only traces of metabolites other than ODD present.
                                                        14
    Even after six months, less than one percent of the   C-DDT had been
    converted to CO .  Aerobically, degradation of DDT was much slower,
    and after six months 75 percent remained unchanged and four percent
    DDE and traces of ODD were found (Guenzi and Beard 1968).   The loss ofJ
    DDT, lindane, and aldrin from a Miami silt loam is shown in Figure 7.
    Langlois (1967) found that E. eoli were able to convert DDT to ODD,
    with the reaction 50 percent complete in two days and more than 90
    percent complete in one week; skim milk inhibited the conversion.
    Fungi were found to be ineffective in converting DDT to ODD under lab-
    oratory conditions (Chacko e^ al_. 1966).  Under anaerobic conditions,
    DDT was converted to ODD more rapidly in an argon atmosphere than in a
    nitrogen atmosphere, which in turn was more effective than C09 , which
    was more effective than CO- mixed with air (Parr et al. 1970).  The
                              /                      ~~~
    authors suggested that CO  favored fungal growth and so retarded the
    growth of DDT degrading organisms.  Both DDT and its analog, methoxy-
    chlor, were more effectively degraded in flooded anaerobic soil than
    in aerobic upland soils; ODD accumulated in the flooded soils (Castro
    and Yoshida 1971).  Fresh water diatoms, collected from mosquito breed-
    ing sites in Winnipeg, were found to convert DDT to DDE (Miyazaki and
    Thorsteinson 1972).
    Hydrogenomas species aerobically effected ring fission of the DDT ana-
    log p,p'-dichlorodiphenylmethane (DDM), but were unable either to
    cleave the DDT ring or to grow on DDM or on p-chlorophenylacetic acid
    (Focht and Alexander 1971).  Eydrogenomas species were able, anaerobi-
    cally, to carry out the conversion sequence:  DDT ->• DDM + DBF, after
    which addition of oxygen and fresh cells resulted in ring cleavage and
    in the eventual formation of p-chlorophenylacetic acid, which can be
    degraded to CO .  Alexander (1972) postulated that cometabolism, a
    process in which a compound is metabolized but not utilized by the
    degrading organism, is of no selective advantage to the organism, which
                                      227
    

    -------
                                                     100 LBS
                                                             DDT
           6              13              33              i
                               MONTHS
    EFFECTOR CONCENTRATION  ON  LOSS OF ALDRIN, LINDANE, AND
    DDT FROM A MIAMI  SILT LOAM, APPLICATION  IN LB/6A
    LICHTENSTEIN AND  SCHULZ, 1959B
                         Figure  7
                             228
    

    -------
    derives no energy from the reaction.  Therefore, even though it is
    possible to select organisms which cometabilize pesticides in the lab-
    oratory, it is not possible to select for such degradative reactions
    under field conditions, since cometabolizing organisms will not grow
    more rapidly in contaminated areas than organisms which do not cometa-
    bolize.  Cometabolism is assumed if degradation occurs in a nonsterile
    medium but not in sterile medium and no organism is found which can
    use the substrate as its sole source of carbon (Pfaender and Alexander
    1973) .   By this definition, sewage microorganisms cometabolized DDT to
    ODD, DDE, and DBF; adding glucose enhanced ODD production at the ex-
    pense of DBP synthesis (Pfaender and Alexander 1973) .
    In an Everglades muck, DDT was slowly converted to ODD and DDE.  Under
    the most favorable conditions, 10.1 percent of the DDT was converted to
    ODD, two percent to DDE, and 83.1 percent remained unaltered.  Addition
    of lime to the muck favored the degradation of DDT, either by stimula-
    ting the growth of DDT-degrading organisms, or by favoring the desorp-
    tion of DDT from the muck (Parr and Smith 1974).  Both flooding and the
    application of organic matter shifted DDT degradation from formation of
    DDE to ODD (Farmer et_ al. 1974) .
    Muaor altevnans in shake culture reportedly converted DDT into five
    metabolites, three of which were soluble in hexane and two in water.
    While the metabolites were not identified positively, they were not
    identical to ODD, DDE, DDA, DDP, dicofol, or l,l-bis(p-chlorophenyl)
    ethane.  The M, alternans spores, when placed in soil, were unable to
    degrade DDT (Anderson et_ al. 1970).  The degradation of DDT in a cell-
    free Aerobaeter1 aerogenes system suggested reduced cytochrome oxidase
    as the dechlorinating agent (Wedemeyer 1966).
    In addition to the actual conversion of DDT by microorganisms, DDT was
    adsorbed by streptomyces, bacteria, and fungi (Chacko and Lockwood
    1967) .   No particular difference in uptake was seen between fungi for
    any one pesticide, but there was positive correlation with increasing
                                      229
    

    -------
    soil moisture (Ko and Lockwood 1968b) .  Kokke (1970a) found DDT to ac-
    cumulate heavily in nursery soil, which adsorbed almost 100 percent of
    the DDT applied, while ditch water retained less than one percent.  It
    was thought that the occurrence of relatively many DDT-resistant or-
    ganisms of soil compared with relatively few resistant water organisms,
    was due to this high affinity of DDT for soil as opposed to water
    (Kokke 1970b).  Shin and co-workers (1970) found precipitation to be
    the major factor in removing DDT from water when 4 ppb DDT were present,
    In soil, adsorption was found to be increased by removal of ether- and
    alcohol-soluble fractions from mineral soil, presumably by removing
    competition for limited numbers of adsorption sites (Shin et_ al. 1970).
    Treatment of algae and protozoa with one ppm of DDT resulted in accu-
    mulation of 99 to 964 ppm, with no metabolites and no adverse effects
    observed (Gregory et al. 1969).  Of 100 samples of estuarine and ocea-
    nic films, 35 were able to convert DDT to TDE, DDNS, and DDOH during
    a 30 day incubation period.  All the active films were estuarine while
    films from open water could not transform DDT at all (Matsumura and
    Boush 1972).  Freshwater diatoms were able to convert DDT to DDE (Mi-
    yazaki and Thorsteinson 1972).  Mayfly nymphs were observed to con-
    vert 85 percent of DDT to DDE within three days, and glass shrimp
    (Palaemonetes kadiakensis Rathbun) converted DDT to ODD, DTMC, and
    DBF; neither organism had reached a plateau in its accumulation of DDT
    in three days, and glass shrimp continued to accumulate DDT In higher
    and higher quantities for seven days (Johnson et al. 1971) .  No con-
    version of DDE to PCB (polychlorinated biphenyl) occurred in a terres-
    trial-aquatic ecosystem (Metcalf et al. 1975).
    In chickens, DDT is metabolized to numerous compounds, including DDD,
    DDA, DDE, and the 3-hydroxy- and 3-methoxy- analogs of these metabo-
    lites (Feil e_t_ al. 1975) .  The metabolism of DDT in pigeons was ex-
    amined by Bailey and his co-workers (1969a, 1969b).  It was shown that
    DDT had a half-life of about 28 days in all tissues and was converted,
                                      230
    

    -------
    by separate pathways, to DDE and ODD.  DDD in turn had a half-life of
    24 days and was converted to DDMU, but DDE had a half-life of approxi-
    mately 250 days.
    In mice and hamsters, DDA was the principal metabolite of DDT.  Both
    species excreted DDT, and conjugated DDT and its metabolites with gly-
    cine or alanine before excreting them in their feces, and mice, but
    not hamsters, excreted DDE in their urine (Wallcave et_ ^1L. 1974).  In
    rats, the conversion of p^p'-DDT to p^p'-DDD was carried out by intes-
    tinal flora rather than by the rat's own enzymes (Mendel and Walton
    1966) .  McKinley and Grice (1960) reported that rats also metabolized
    dicofol to DDE.
    Photolytic—Ultraviolet radiation decomposed DDT, being less effective
    if the soil contained humus than if humus-free soil or pure DDT was
    exposed (Piasecki et al. 1970).  A free-radical mechanism for photo-
    chemical decomposition of DDT on quartz was postulated, with 4,4'-di-
    chlorobenzophenone, 1,l-dichloro-2,2-bis(p-chlorophenyl)ethane and
    l,l-dichloro-2,2-bis(p-chlorophenyl)ethylene as the chief products.
    The reaction was 80 percent complete in 48 hours and did not necessa-
    rily produce hydrogen chloride (Hosier et al. 1969) .  On silica gel
    thin layer chromatographic plates, some aromatic amines sensitized
    decomposition of DDT by sunlight (Ivie and Casida 1971).
    Seven days' exposure of solid DDT to ultraviolet light of greater than
    230 nm (quartz glass) or greater than 290 nm (pyrex glass) resulted in
    the decomposition of some DDT to CO  and HC1.  Of the initial 94 mg
    DDT, 89 were unaltered and 12 mg C09 and two mg HC1 were produced.
                                       ^_>
    Under the same conditions, 98 mg of DDE resulted in formation of ten
    mg (XL and eight mg HC1 while 85 mg DDE remained unaltered.  No chlor-
    ine gas was produced (Gaeb et_ al_. 1975).
    Light of greater than 290 nm wavelength degraded dicofol to dichloro-
    benzophenone (Archer 1974) .  When dicofol was adsorbed to almond hull
    meal at 10.2 ppm and exposed to UV light,  50 percent was lost with 157
                                     231
    

    -------
    hours and 11 percent of the adsorbed dicofol was transformed into 4,4'£;
    dichlorobenzophenone (Archer 1970).
    Chemical and physical—Diffusion of DDT on homoionic clays was asso-
    ciated with conversion of DDT to TDE; the degree of decomposition de-
    pended on the type of clay and the exchangeable cation present (De Dios
    Lopez-Gonzalez and Valenzugla-Calahorro 1970).   At temperatures above
    its melting point, DDT in the presence of metal salts decomposed to
    the noninsecticidal dichloroethylene (Balaban and Surcliffe 1945).
    DDT was partially decomposed by 9N sodium hydroxide and by 18ff sul-
    furic acid (Kennedy et al. 1972b) .  Complete decomposition was achieved
    in liquid ammonia and metallic sodium and substitution of lithium for
    the sodium gave better than 99 percent degradation (Kennedy et al.
    1972a).  Less than 20 percent of DDT was degraded by treatment with
    potassium permanganate while alkaline decomposition was successful
    (Leigh 1969).
    In the laboratory, up to 90 percent of soil-applied DDT could be de-
    composed by mildly acidic reduction with zinc.   Bis(p-chlorophenyl)
    ethane and tetrakis(chlorophenyl)tetrachlorobutane were the products
    (Sweeney and Fischer 1970, Sweeney et_ al. 1974).
    DDT could be destroyed by burning in oxygen at 900 C with the formation
    of carbon monoxide, carbon dioxide, chlorine gas and hydrogen chloride,
    as well as other unidentified substances (Kennedy &t_ al_. I972a, 1972b) .
    Complete combustion of pure DDT was actually achieved at 560 C, but
    DDT formulated as technical flakes required 850 C for complete combus-
    tion (Kennedy et al. 1969).  DDT dissolved in kerosene could also be
    destroyed in a blue-flame oil burner, and the hydrogen chloride gas
    which was generated was neutralized by an alkaline water spray.  Pow-
    dered DDT required the addition of a baffled refractory furnace and a
    water-cooled feeder system to inject the powder, which then vaporized
    and burned.  Dust formulations ranging from ten to 90 percent burned
    successfully (Whaley e£ al. 1970, Lee et_ al_. 1971).  Cutkomp (1947)
                                       232
    

    -------
    observed that water-dispersed DDT could be decomposed by heating it to
    above 90 C, but boiling appeared to result in different products than
    did autoclaving, and aged or aerated dispersions did not decompose.
    The products were not fully identified.
    Cobalt-60 g-omma-irradiation of five Mrads decomposed 75 percent of a
    five ppm solution of DDT in hexane (Lippold et al. 1969).  Woods and
    Akhtar (1974) were able to dechlorinate DDT which had been dispersed
    on silica gel suspended in water by use of g'omma-irradiation.  The
    level of irradiation was lower than that required to sterilize sewage,
    and so was considered economically feasible, but complete dechlorina-
    tion was achieved with some difficulty.  No data were available on the
    degradation of dicofol by chemicals or heat, but the results should be
    very similar to those for DDT.
    Inasmuch as none of the data suggest that DDT, dicofol, or ODD will
    decompose to naturally occurring substances in either soil or water,
    thermal or chemical degradation appear to be the only practical ways
    of disposing of these compounds.
    Transport-
    Within soil—The fate of 414 Ibs/A (207 ppm) of DDT and 22.1 Ibs/A
    (11.05 ppm) dicofol applied to an Oregon orchard between 1946 and 1967
    is shown in Table 39 and 40 (Kiigemagi and Terriere 1972).
    In a 20-year study of orchard soils, less than one percent of the fol-
    iage-applied DDT was found 30-36 in. deep in the soil; most remained
    in the upper six inches (Terriere et al. 1965).  Similarly, after 24
    years of exposure to DDT, vineyard soil retained 88 percent of the re-
    covered DDT in the top three centimeters of soil, while the figures
    were 95 percent and 92 percent respectively after 12 and six years
    (Kuhr et_ al. 1972).  In Houston black clay, with 33 inches of rain per
    year, 60-75 percent of the DDT remained in the top 12 inches of soil
    after ten years (Swoboda et^ al^ 1971).  After ten years, 30 percent of
                                      233
    

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    Table 39.  VERTICAL DISTRIBUTION OF DDT ANALOGS AND METABOLITES IN
             ORCHARD SOILS, 1970 (KIIGEMAGI AND TERRIERE 1972)
    
    Pesticide concentration, ppm
    Soil level,
    inches
    0
    7
    13
    25
    - 6
    - 12
    - 24
    - 36
    P»Pf-
    DDT
    33.1
    7.25
    1.08
    1.02
    o,p'-
    DDT
    Hood
    5.59
    1.20
    0.17
    0.11
    PtP1-
    DDE
    River
    7.61
    0.97
    0.19
    0.12
    P.P1-
    TDE
    1.59
    0.18
    0.02
    0.01
    Dicofol
    2.44
    2.32
    0.50
    0.36
    DBF
    7.25
    0.87
    0.19
    0.07
                                    234
    

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      Table 40.  CHANGES IN VERTICAL DISTRIBUTION OF TOTAL DDT,
              1965 - 1970 (KIIGEMAGI AND TERRIERE 1972)
    Soil level,                   Change,                           ,
      inches	yg/sample                Change, %—
                              Hood River
       0-6                     - 7129                     -  31
       7-12                    + 1994                     + 159
      13-24                    -  321                     -  16
      25-36                    +  861                     + 247
       0-36                    - 4595                     -  18
    a/  As percent of 1965 levels.
                                   235
    

    -------
    the DDT residues were found in the six-nine inch layer  (Lichtenstein
    et^ al. 1971a).  Balinov (1973) found 97 percent of DDT residues in the
    top 30 centimeters, with 79 percent in the top ten centimeters, after
    15-20 years; also after 15 years, DDT was found to have leached to 60
    centimeters in a light sandy soil, even though only traces were recov-
    ered at this depth (Voerman and Besemer 1970).
    In sandy loam, Stewart and Chisholm (1971) concluded there had been
    little downward or lateral movement in 15 years.  Comparing silt loam
    and muck soil, Lichtenstein (1958) found 84-96 percent of DDT in the
    top three inches in loam, and only 62-74 percent in muck; in the three
    to six inch layer, loam held 4-12 percent while muck held 19-29 per-
    cent.
    Leaching of DDT was found to increase when soil was cultivated (Harris
    and Sans 1969), when soil was treated with urea (Ballard 1971) and
    when calcium-containing rather than acidic homoionic clays were present
    (Lopes-Gonzalez and Gonzalez-Gomez 1970).  However, there was some ev-
    idence that leaching was independent of the rate of application, since
    the leachate from gravelly forest soil contained 5 pg DDT per cubic
    decimeter (Riekerk and Gessel 1968) .  After eight years of DDT appli-
    cation, DDT had leached to 30 centimeters.  More important, although
    only 0.3 mg/kg DDT (0.3 ppm) were found in the soil at the top of a
    hill, 7.25 mg/kg DDT were found in the soil at the foot of the hill
    (Naishtein e_t_ aj^. 1967).  It is therefore apparent that, albeit slowly,
    DDT moves through soil, in soil, and with soil.
    Between soil and water—Despite the virtual insolubility of DDT in
    water, contamination of rivers has occurred repeatedly  (Breidenbach
    et_ al. 1967).  Contamination of groundwater below orchards was detec-
    ted (Terriere et_ al. 1965).  Relatively little DDT reaches groundwater
    through vertical leaching, however.  Johnston and co-workers (1967)
    estimated that drainage tiles contained only about 1/7 to 1/12 the
    DDT carried by surface runoff and Johnson and Morris (1971) found DDT
                                      236
    

    -------
    was carried in runoff from fields into the rivers.  Of the DDT entering
    surface waters from cotton plots, less than three percent was in the
    water itself and over 96 percent was associated with sediment (Bradley
    e_t^ a^. 1972).  It was estimated that, in sea water, the humic acid
    fraction of the sediments carried 50 percent of the adsorptive capa-
    city and was the most important DDT repository  (Pierce et al. 1974).
    The predominant pattern of DDT contamination of aquatic environments
    consists of extremely low or undetectable levels in water with the
    levels in mud and in water organisms increased by one or more orders
    of magnitude.  Even under conditions of minimal water contamination,
    fish and aquatic invertebrates were found to be contaminated with DDT
    (Kuhr et al. 1974, Moubry et al. 1968).
    In the Everglades, DDT was present at less than 0.03 yg/liter (0.03
    ppb) in water, but levels in the underlying marsh soil were of the
    order of 30 ppm, and DDT levels in fish, omnivorous crustaceans, and
    algal mats ranged to 100 ppm (Kolipinski et^ al. 1971).  In a Long Is-
    land estuary, concentrations in water birds were approximately a mil-
    lion-fold greater than the water levels (Woodwell ej^ al. 1967).  In
    a drainage system of southwestern Ontario, concentrations of DDT and
    its metabolites in mud were 820- to 13,000-fold as great as water levels
    of DDT, while fish carried up to 80,000 times the Levels found in water
    (Miles and Harris 1971).  Other reports of DDT magnification in aquatic
    systems abound (e. g.:  Ettinger and Mount 1967, Reed 1969, Reinert
    1970, Fredeen and Duffy 1970).
    Actual degradation of DDT, even to ODD and DDE, is quite slow in aqua-
    tic systems, with no degradation observed in bottled river water after
    eight weeks (Eichelberger and Lichtenberg 1971) and no visible degra-
    dation observed in a sewage lagoon (Halvorson et al. 1971).  Albone
                                              f
    and co-workers (1972) reported that conversion of DDT to ODD occurred
    most effectively in an anaerobic sludge at 35 C; with a hydrogen at-
    mosphere.  In this study, the relative degradation of DDT to ODD was
                                      237
    

    -------
    found to be slowest in situ in the Severn estuary sediment (Albone et
    al. 1972).
    In the Ogallala aquifer, most of the DDT introduced into the water re-
    mained close to the point of entry and was not recovered (Scalf et_ al.
    1969) .  Adsorption of DDT by suspended sea water particles was found
    to be associated with humic acid fractions (Pierce et_ al. L974), and
    to be related to the size of the clay particles and the organic con-
    tent of the particles (Leland et al. 1973).  Adsorption by kaolinite
    and montmorillonite was slow, and equilibrium was reached only after
    one month (Weil et_ al_. 1972).  Off the coast of southern California,
    DDT levels increased between 1949 and 1970 in ocean and in fish with
    the residues decreasing with distance from a DDT-dumping sewer.  DDT
    levels reached a plateau before 1970, and after dumping of DDT ceased
    in 1970, DDT levels began to decrease.  DDE levels, which had been in-
    creasing steadily throughout, continued to accumulate, as did DDD, un-
    til the study ended in 1972 (MacGregor 1974).
    The extremely slow movement of DDT within soil or from soil to water
    merely delays aquatic accumulation.  In agricultural areas draining
    into south Monterey Bay, agricultural use of DDT declined sharply be-
    ginning in 1972, but DDT levels in marine sediment were still increas-
    ing in 1973 (Phillips et_ al. 1975).  It was estimated that concentra-
    tions in sediment had reached one percent of the agricultural level of
    2 Ibs/A (2.24 kg/ha) by 1973.
    Volatilization—The loss of DDT from a placid aqueous surface was
    found to occur by codistillation of DDT with water, with the rate of
    loss paralleling increasing DDT concentrations at least to 100 ppb.
    Moreover, DDT was found to have an affinity for the air-water boundary
    resulting in heterogeneous dispersal of DDT in the aqueous medium in a
    manner facilitating codistillation  (Acree etL al. 1963).  These results
    were confirmed for DDT in sand, but not in soils of high organic con-
    tent (Bowman et al. 1965).
                                      238
    

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    The rate of loss of DDT from fields was estimated to be 2 Ibs/A per
    year (2.24 kg/ha/year) in the summer, and 0.3 Ibs/A per year (0.34 kg/
    ha/year) in the winter, so that about 1/2 of the DDT applied to fields
    might be expected to volatilize (Lloyd-Jones 1971).  Freed et al.
    (1972) calculated, however, that the theoretical loss of DDT from an
    inert surface would not exceed 0.16 Ib/A (0.18 kg/ha) per year.
    Cliath and Spencer (1972) found that 66 percent of the volatile sub-
    stance over a field containing DDT residues was actually p^p'-DDE,
    which has a higher vapor pressure than DDT.  At 30 C, the volatile
    products of spraying one kg/ha of DDT consisted of:  62 percent O3p'£
    DDT, 16 percent of 0.,p'-DDE, 14 percent p}p '-DDE and eight percent
    o,p'-DDT (Spencer and Cliath 1972).
    Cliath and Spencer noted that, at 30 C, p^p'-DDE has over seven times
    the vapor pressure of pjp'-DDT.  More recently, Ware, Cahill, and Es-
    tesen (1975) compared the volatilization of DDT and DDE and concluded
    that DDE volatilizes more readily from a cool moist soil than from a
    warm dry soil.  On, but not in, dry soil, o3pf-DDT was converted to
    o.,p'-DDE.  Volatilization of O3p f-DDT was more rapid from dry soil than
    from wet soil, with conversion to DDE occurring after, as well as be-
    fore, volatilization.  On both dry and moist soil, O3p '-DDT volatilized
    more rapidly than p^p'-DDT (Ware ejt guL. 1975).
         14
    When   C-DDT was applied to different soils at levels of ten ppm and
    the soil was carried through three cycles of drying and rewetting,
    fine soil was found to maintain DDT volatilization for the longest time,
    presumably by retaining the requisite surface monolayer of water long-
    er.  Volatilization above 15 bars of water tension depended on temper-
    ature and on the adsorptive capacity of the soil.  Evaporation was
    greatest from loamy sand, followed by silty clay loam; clay permitted
    least volatilization of DDT (Guenzi and Beard 1970).  Sundaram (1974)
    found only small changes in the DDE levels from ground level to six
    feet, and found that O3p '-DDT dissipated more quickly than did pjp
                                      239
    

    -------
    In the laboratory, DDT volatilized from Gila silt loam at a rate cor-
    responding to five kg/ha/year, with volatilization increasing as air
    flow increased.  The rate of volatilization decreased with increasing
    time as the concentration of DDT in the soil decreased (Farmer et_ al.
    1972).  Flooding was found to decrease the volatilization of DDT, at
    least in part by changing the conversion product to ODD, which has a
    lower vapor pressure than the aerobically generated DDE (Spemcer e_t_ al.
    1974).  Over a 48 hour period, DDT volatilized from unflooded soil at
                               3                                 3
    an average rate of 100 ng/m  and from flooded soil at 58 ng/m .  For
                                   3            3
    ODD, volatilization was 92 ng/m  and 30 ng/m  from unflooded and flood-
    ed soil, respectively.  As expected, high wind and low rainfall in-
    creased volatilization (Willis et^ al. 1971).  Mackay and Wolkoff (1973)
    stressed that even compounds with a low vapor pressure may evaporate
    rapidly due to high activity coefficients which result in high equil-
    ibrium vapor partial pressures.
    Other modes of pesticide entry into the atmosphere included spray
    drift as particles of less than five nm, transport with soil in wind
    erosion, and transport with smoke from incinerated items contaminated
    by DDT (Brooks 1974).
    In the atmosphere, these losses of DDT to volatilization are reflected
    in the presence of 57 x 10~  g/m  of p^p'-DDT and 9 x 10~  g/m  p,p'C
    DDE over the northern equatorial Atlantic ocean (Prospero and Seba
    1972).  The pesticides were not dust-associated, and therefore were
    presumed not to be of relatively local African origin.  In Arizona,
    six to 229 ppb of DDT were found in deer mice (Pevomyseus) downwind
    from areas of DDT application and quail livers contained up to 2,800
    ppb and soil residues ranged from 3.6-6,700 ppb (Laubscher et_ al_. 1971),
    Loss of insecticidal activity in sunlight was less for DDT than for
    dieldrin, chlordane, or methoxychlor.  Formulation affected inactiva-
    tion, with wettable powders least sensitive, fuel oil or emulsified
    preparations intermediate, and kerosene solutions most sensitive
                                      240
    

    -------
    (Ginsburg 1953).  Aqueous suspensions maintained toxicity to houseflies
    longer than did emulsions (Chisholm et al. 1949).
    When five ppm DDT were applied to soil in the laboratory, the effects
    of temperature and ultraviolet light were found to interact, with loss
    of DDT from soil reaching 24 percent and 50 percent in 50 days at 30 C
    and 50 C, respectively.  Ultraviolet light of 300-400 nm added four to
    eight percent loss at 30 C and seven to nine percent loss at 50 C
    (Baker and Applegate 1970).  Level of application of DDT also affected
    loss:  at 20 ppm, loss at 30°C was 22-27 percent with ultraviolet light
    adding three to eleven percent; at 50 C, 20 ppm resulted in only 35-44
    percent loss, but the addition of ultraviolet light increased the loss-
    es by up to 32 percent.  Finally, the soil type interacted with the
    other factors:  clay was most effective in retaining DDT, while silty
    clay loam and gravel loam did not differ significantly (Baker and
    Applegate, 1970).  DDT applied to leaves is lost by first order kinet-
    ics and at the same rate regardless of the rate of application (Gunther
    et_ al.. 1946).
    In a recent review of the movement of DDT and its derivatives, Spencer
    (1975) concluded that these compounds will continue to enter the atmos-
    phere for many years after the use of DDT has been completely discon-
    tinued .
    Into organisms—In a terrestrial-aquatic ecosystem, DDT and its meta-
    bolites were present at 0.004 ppm in the water, 22.9 ppm in snails,
    8.9 ppm in mosquitos, and 54,2 ppm in mosquitofish (Gambusia).  For
    DDE, the levels were 0.008 ppm in water, 121.6 ppm in snails, 168.9
    ppm in mosquitos, and 149.8 ppm in mosquitofish.  These data illustrate
    the bio-accumulation of DDT and DDE when compared with the DDT analog,
    methoxychlor, which was present in water at 0.0016 ppm, in snails at
    15.7 ppm, in mosquitos at 0.48 ppm, and in mosquitofish at only 0.33
    ppm (Metcalf et al. 1971).
                                      241
    

    -------
    In a watershed treated with one Ib/A  (1.12 kg/ha) DDT in 1960  and  1963,
    DDTR (total DDT residues) in 1971 were between 0.031 and 17.94 ppm in
    mud (mostly in dead water or beaver ponds), 0.045 to 0.196 ppm in  cray-
    fish (Cambavus bartoni) and 0.4 to 0.9 ppm in brook trout  (Sa'lvelinus
    font-inal'is') .  Of the mud residues, 35 to 60 percent consisted  of ODD,
    30 percent of DDT, and 25 percent of DDE (Diraond et^ al^. 1974).  Schulz
    ^t_ al_.  (1975), using data from a Hawaiian canal and drainage ditch,
    suggested that small fish absorbed more DDT from the water than from
    food, while large fish absorbed more DDT from their food.
    Miles and Harris (1971) found extremely small DDT residues in  the
    water of a stream and drainage system of southwestern Ontario, but
    fish had accumulated up to 80,000 times the water levels of DDT in
    their tissues.  The sum of these data makes it abundantly clear that
    extremely low levels of water contamination by DDT are indicative  of
    nothing more than the very low solubility of the substance, and do not
    preclude high levels of contamination in aquatic organisms.
    DDT is taken up from soil into wheat seedlings, with greater absorp-
    tion from sand than from clay (Nash 1968) .  The rate of uptake was con-
    sidered minimal (Harris and Sans 1969b) and was less than the  uptake
    of dieldrin, endrin, or heptachlor (Bea.ll and Nash 1969).  When ten ppm
    of DDT were applied to the soil, rye, wheat and barley were found  to
    take up 0.014, 0.032 and 0.057 ppm, respectively (Beitz et^ al. 1970).
    Uptake into peanuts was lowest in the nuts themselves, while levels
    in both turnips and turnip greens were considered to be possibly ob-
    jectionable (Young 1969).  In the Agro "Pontino region of Italy, 0.044
    ppm of DDT in the soil resulted in residues of 0.154 ppm DDT in beet
    roots (Camoni et al. 1971).  DDT accumulated in root crops (MacPhee
    et_ al. 1960) and in grain at 0.1 to 1.2 ppm (Popov and Donev 1970).
    Uptake was not significantly correlated with soil pH, cation exchange
    capacity or clay content, but was correlated inversely with organic
    matter  (Beall and Nash 1969, Harris and Sans 1969b) .
                                      242
    

    -------
    Heinisch  (1973) found  that  141 days after application  of  dicofol  at  an
    unspecified level,  carrots  contained  from O.OA  to  0.4  ppm of dicofol.
    Grandolfo and co-workers  (1967) found  that  treatment with dicofol left
    unacceptably high residues  on lettuce  under conditions which resulted
    in acceptably low or no DDT residues.
    Uptake of DDT by foliage was found to  be in the order:  emulsifiable
    concentrates > dusts > wettable powders,  with  consequent inverse tox-
    icity to bees (Johansen and Kleinschmidt 1972).  Application of DDT  to
    spinach and cabbage leaves  resulted in some transfer of DDT, DDE,  and
    ODD to stem, roots, and soil as ascertained 18  days and 14 weeks  after
    treatment (Zimmer and Klein 1972).  Metabolites included  DDE and  DDMU
    on the leaves, and DDE, DDMU, DDD, DDA, and a DDA-conjugate and DBH-£?
    conjugate in the leaves.  Most of the  radioactivity remained in or on
    the foliage (Zimmer and Klein, 1972).
    The accumulation of DDT and DDE in animal fat is well documented  (Wood-
    ward et_ al_. 1945, Morgan and Roan 1971), including even species pre-
    sumably remote from direct  exposure, such as arctic mammals (Tatton
    and Ruzicka 1967, Clausen _et_ al_. 1974).  Beef cattle sprayed with 0.5
    percent DDT accumulated DDT in their fat and excreted it  in their milk
    (Claborn et_ al_. 1960).  Chickens fed 0.1 ppm DDT for 14 days accumula-
    ted residues in their tissues; feeding of ten to 15 ppm for five  days
    resulted in egg residues as well as residues in the abdominal fat.
    DDE residues of 0.7 ppm persisted for  26 weeks  (Stadelman  et_ a.l_.  1964).
    Persistence-
    The persistence of DDT and  its metabolites in soil is summarized  in
    Table 41 for those cases where the residues remaining after a specified
    time could be quantified.   After a total of 103.6 Ibs/A (116 kg/ha)
    had been applied to a California soil  over a five year period, the soil
    residues after the fifth application were between ten and  15 ppm.
    Four years later, four to six ppm remained in the soil (Hermanson et
    al. 1971).  In agricultural soils in Finland, the average  level of
                                     243
    

    -------
    Table 41.  DEGRADATION OF DDT UNDER FIELD CONDITIONS
    %
    Residue
    22
    40
    10.6
    39
    55
    18
    24
    33
    29
    56
    16
    50
    44
    56
    50
    64
    79
    50
    90
    97
    50
    55
    62
    100
    50
    100
    50
    # of Loss/year
    Years % Conditions Reference
    24
    20
    15-22
    17
    15
    15
    15
    12
    11
    11
    10
    9
    8
    6
    6
    4
    3
    3
    2
    1
    1
    0.75
    0.75
    0.75
    0.50
    0.50
    4
    3.25
    3.00
    4.47
    3.59
    3.00
    5.47
    5.07
    5.58
    6.45
    4.00
    8.40
    5.56
    7.00
    7.33
    8.33
    9.00
    7.00
    16.67
    5.00
    3.00
    50.00
    60.00
    50.67
    0
    100.00
    0
    12.5
    maximum dispersal Ruhr et al. 1972
    foliar sprays Terriere et al. 1956
    foliar sprays Balinov 1973
    maximum retention Nash and Woolson 1967
    sandy loam Stewart and Chisholm 1971
    10 Ibs/A Lichtenstein e£ al. 1971a
    100 Ibs/A Ibid.
    maximum dispersal Kuhr _et al . 1972
    10 Ibs/A Lichtenstein jet al. 1971a
    100 Ibs/A Ibid.
    Houston black clay Swoboda jet al. 1971
    podzol soil Krechniak 1973
    25,50 Ibs/A; bioassay Fleming and Maines 1953
    25,50 Ibs/A; bioassay Ibid.
    maximum dispersal Kuhr et _al. 1972
    25,50 Ibs/A; bioassay Fleming and Maines 1953
    25,50 Ibs/A; bioassay Ibid.
    isotope labeled Czaplicki 1969
    25,50 Ibs/A; bioassay Fleming and Maines 1953
    25,50 Ibs/A; bioassay Ibid.
    Texas soil Randolph _et al. 1960
    pots: alkaline, soil Chawla and fhopra 1967
    pots: normal soil Ibid
    bioassay Mulla 1960
    bioassay Luchev et al. 1971
    standing, percolated Yule 1967
    moist soil
    California soil Hermanson et al. 1971
                            244
    

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    DDT and its metabolites was 0.073 ppm, or about 21 percent of the
    amounts applied.  Data on the time span and the amounts applied to the
    soil were not available (Rautapaa et al. 1972).  Reran and Guth (1965)
    found DDT to be less persistent than lindane, but more persistent than
    aldrin or parathion.
    Enormous variation exists in the residues of DDT observed in different
    studies.  After 24 years of DDT treatment of vineyard soil, despite
    miximum weathering, runoff, and volatilization due to bare soil and
    repeated tilling, 22 percent of the DDT remained in the soil (Ruhr et
    al. 1972).  Under conditions favoring maximum retention (including
    soil incorporation, minimum tillage, and extremely high levels of ap-
    plication) Nash and Woolson (1967) found that 38 percent of a single
    application of DDT remained in the soil after 17 years.  At the other
    extreme, it was estimated that only 50 percent of the DDT applied to
    Texas soil remained after one year (Randolph et al. 1960), and that
    less than 16 percent remained in a Houston black clay after ten years
    (Swoboda et_ al. 1971).  The latter losses were ascribed to volatili-
    zation by the authors, who noted that soil temperatures reached 60 C.
    Alkaline soil (pH 9.5) was reportedly conducive to DDT loss (Chawla
    and Chopra 1967) but pH differences between 4.0 and 7.5 did not alter
    degradation rates (Fleming and Maines 1953).
    After DDT had been applied to a light sandy soil for 15 years, samples
    were taken at four year intervals.  No significant decrease in the
    total soil residues of o3p '-DDT or of p3p '-DDT occurred in the four
    years, even though the soil was dug up yearly and either plowed or
    planted (Voerman and Besemer 1975).
    When DDT was applied at ten Ibs/A (22 kg/ha), 29 percent remained in
    the soil after 11 years, but when 100 Ibs/A (112 kg/ha) were applied,
    56 percent remained after 11 years.  After 15 years, the corresponding
    residues were 18 percent and 24 percent (Lichtenstein et^ al. 1971a).
    After 3.5 years, a ten-fold increase in the rate of application was
                                      245
    

    -------
    found to have resulted in a two-fold increase in the rate of retention
    (Lichtenstein and Schulz 1959b).  The observation that higher levels
    of DDT result in higher rates of persistence has been made repeatedly
    (Nash and Woolson 1967, Lichtenstein et_ ?il_. 1960).
    The effects of soil must be evaluated separately for chemical persis-
    tence and biological activity.  Addition of organic matter was found
    to increase conversion of DDT to DDD (Farmer et_ _ajL. 1974) .  Organic
    colloids adsorbed DDT and reduced its volatility, so that at 186 C
    only 66-83 percent of the DDT was lost when organic soil colloids were
    added, whereas 100 percent of the DDT was lost at 80 C when colloids
    were not added (Porter and Beard 1968) .  When midwestern soils were
    ranked with respect to the length of DDT persistence, DDT was found to
    persist longer in heavily organic muck soils than in loam, but climate
    also affected the results, since soils from Kansas retained DDT longer
    than similar soils from Ohio or Wisconsin (Lichtenstein et al_. 1960) .
    DDT was found to adsorb virtually instantaneously to the surface of
    illite or kaolinite, but more gradually into montmorillonite, which is
    an expanding clay with intralamellar adsorption sites.  The adsorption
    capacities of the clays were not correlated with their ion exchange
    capacities or specific surface areas (Ju-Chang and Liao 1970) .  On
    homoionic clays, cation exchange capacity was found to affect the de-
    hydrohalogenation of DDT, and dried bentonite was found to adsorb three
    times as much DDT as dried vermiculite (Lopez-Gonzalez and Valenzugla-
    Calahorro 1970).  Clay catalyzed decomposition of DDT was also found
    to increase with decreasing pH and to decrease with increasing amounts
    of organic base (Fowkes ejt al. 1960) .
    In evaluating the edaphic aspects of pesticide disposal, it: was found
    that combinations of pesticide formulations were degraded nore readily
    than single formulations, although, no attempt was made to determine
    whether the carrier or the active ingredient was responsible for the
    increased C00 evolution (Stojanovic et al. 1972a).
                z
                                      246
    

    -------
    Paulini (1957) found colloidal clays, whether lateritic or not, to be
    highly adsorptive of DDT and suggested that ferric oxide did not in-
    activate DDT but only served as an indicator or the laterization of the
    clay.  Downs and co-workers (1951) however, found that soils of high
    iron or aluminum content actually catalyzed DDT decomposition, with
    ferric chloride accumulating in the soil.  Inactivation was not thought
    to be due to adsorption or to alkalinity of the soil, although cataly-
    sis by iron was implicated because one molecule of iron was found to
    degrade about 160 molecules of DDT before  (presumably) decomposition
    products blocked further degradation (Downs et^ al. 1951).  Gunther and
    Tow (1946) observed that ferric-catalyzed DDT composition could be in-
    hibited by picolinic acid and salicylaminoguanidine.  Iron porphyrins
    were found to mediate conversion of DDT to DDD in cell-free systems
    (Zoro et_ al. 1974) .
    Adsorption by organic matter, while apparently increasing the stability
    of DDT in the soil by decreasing its volatility and its decomposition,
    also decreased its availability to plants and insects (Harris and Sans
    1967).  When bioassays were used to measure residues, DDT was found to
    be least persistent in soils with high levels of organic matter (Flem-
    ing and Maines 1953).  In forest soils, 91 percent of the DDT was
    found in humic acid extracts and only nine percent in fulvic acid frac-
    tions (Ballard 1971).
    In orchards treated with 22.1 Ibs/A (1_ .05 ppm) of dicofol between 1946
    and 1967, Kiigemagi and Terriere (1972) found 5.62 ppm dicofol in the
    top 36 inches of soil in 1970.  As shown in Table 40, heavy residues
    of DDT-from a total application of 414 lb^;/A «rere also found.  Some of
    the dicofol may be due to conversion of DDT to dicofol, accounting for
    residues of 50 percent of the total application of 30 years.  No other
    data on soil persistence of dicofol were available.
    These results confirm the absence of microbial degradation of DDT and
    underline its incredible persistence.  Despite numerous attempts, no
                                      247
    

    -------
    evidence exists that DDT is converted to naturally occurring molecules
    under any soil conditions.
    Effects on Non-Target Species-
    Microorganisms—The data on the effects of DDT on CO- evolution, 09
    evolution, ammonification, nitrate production, and the overall numbers
    of fungi are shown in Table 42.  Tables 43 and 44 summarize the effects
    of DDT on specific fungi and on bacteria.  Table 45 shows the few data
    available on the effects of the DDT analogs, DDD and docofoL, on micro-
    organisms.  Levels of application, number of days observed and condi-
    tions of culture are also included.  The interpretations of the effects
    as increasing, decreasing, or not affecting microorganisms (+, -, and
    0, respectively) are repeated from the references cited and no critical
    reevaluation of the data was attempted.
    It is quite apparent from Table 42 that DDT does not, even at massive
    doses, alter CCL evolution very much, nor affect the overall numbers
    of bacteria and fungi.  Oxygen evolution from algal culture decreased
    sharply even at low levels (0.01 ppm) of DDT.  Fisher (1975) noted
    that DDT depresses the growth rate rather than the rate of photosyn-
    thesis in marine phytoplankton, and concluded that total marine photo-
    synthesis will probably not be diminished by DDT, even though selec-
    tive toxicity could affect herbivore populations.
    More fungi were stimulated than inhibited by DDT (Table 44), and the
    few inhibitions occurred at low levels, suggesting that DDT actually
    stimulated fungal growth, albeit only at massive doses.  Bacteria, on
    the other hand, were more often inhibited than stimulated (Table 43)
    but applications of about 1,000 ppm (560 kg/ha) were required for in-
    hibition.
    Franzke and co-workers (1970) found that fungal stimulation was act-
    ually due to a combination of inhibition by DDT and stimulation by DDD;
    the observed effect consisted of the sum of these opposing effects.
                                      248
    

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    DDE was found to be neither stimulating nor inhibiting.  Ko and Lock-
    wood (1968b) found ODD to be more antimicrobial than DDT, with only
    one part per million of ODD required to inhibit actinomycetes, whereas
    ten parts per million of DDT were required.  In soil, higher concen-
    trations were required than in soil-agar plates.  Parsenyuk and Akimen-
    ko (1970) found DDT to favor the denitrifying microflora because it
    inhibited the growth of nitrifying bacteria.
    Despite these effects of DDT, the early reports of Smith and Wenzel
    (1947) and of Wilson and Choudhri (1946) that DDT does not deleter-
    iously affect soil microorganisms have been reconfirmed.  Vashkov (1949)
    found that a small bactericidal effect of combusted DDT aerosols on
    Staphylocooci and on E. eoli was due in part to the smoke.  Trudgill
    and Widdus (1970) found DDT to have the least effect of seven insecti-
    cides on bacterial metabolism.  It was postulated by Richardson and
    Miller (1960) that fungitoxicity is positively correlated with water
    solubility and vapor pressure and therefore DDT, with its extremely
    low solubility and low vapor pressure, exerted as little effect on
    fungi as the model predicted.
    Dicofol applied at four times the normal agricultural levels did not
    decrease the yield of mushrooms (Poppe 1966).
    Invertebrates—The effects of DDT on soil invertebrates have been ex-
    haustively reviewed by Edwards and Thompson (1973) and need not be re-
    capitulated here.  DDT was not found to be mutagenic in either wasps
    (Bracon hebetev) nor in brine shrimp (Artemia), although extremely
    toxic to both organisms (Grosch and Valcovic 1967, Grosch 1967).  At
    0.05 ppm, DDT killed 90 percent of the larvae of oysters (Cvassostvea
    virginiaa) and clams (Venus mercenaries.) (Davis 1970).
    Plants—DDT at 25 Ibs/A (28 kg/ha) caused growth retardation in some
    seedlings, particularly cucurbitaceae, with some difference between
    technical and pure DDT (Cullinan 1949).   The difference in purity was
    less significant than the effect of soils:  DDT in mineral soil was
                                      253
    

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    more phytotoxic than in peat soil; the effects were considered to be
    due to decreased availability of phosphorus resulting curtailed lateral
    root development (Thurston 1953).  Goldsworthy and Foster (1950) re-
    ported that the soil accumulation of 1,000 Ibs/A (1,120 kg/ha) of DDT
    profoundly affected all plants, but that 3,000 Ibs/A (3,360 kg/ha) on
    the soil surface did not damage the plants, presumably because there
    was no root contact.  Dennis and Edwards (1964) found damage to toma-
    toes at all levels of DDT application with beans quite susceptible and
    cucumbers, carrots, and parsnips susceptible only at large doses.  Da-
    mage was limited to potted plants, however, and little or no phytotox-
    icity was seen under field conditions.  At 50 to 100 Ibs/A (56 to 112
    kg/ha), DDT delayed soybean emergence (Probst and Everly 1957).  Bos-
    well (1955) observed decreases in crop quality before either yield or
    growth were affected and more damage occurred in poor soil than in
    rich soil.  Shaw and Robinson (1960) observed an unexplained increase
    in nitrification when DDT was applied at 20 and 200 Ibs/A (22,4 and
    224 kg/ha).
    Fish and amphibians—The toxic effects of DDT on fish were pointed out
    by Pielou (1946), who noted that as little as 0.25 oz/A (.01 ppm) of
    DDT resulted in a complete kill of young fish unless weeds and mud
    were present.  In the latter case, 3 oz/A (0.21 kg/ha) caused only a
    70 percent kill (Pielou 1946).  The acute oral LD   for goldfish was
    found to be between 63 mg/kg and 200 mg/kg (Ellis et_ al_. 1944), but:
    the LC,n ranged from two ppb for largemouth bass and brown trout to
    320 ppb for mosquito fish (Pimentel 1971).  The effects of sublethal
    doses of DDT on fish included abortions in mosquitofish, changes in
    thermal acclimatization in salmon and trout, and loss of learned avoid-
    ance responses in trout (Pimentel 1971).  The metabolism of DDT to ODD
    in trout was found to be enhanced by intestinal microflora, but was
    also carried out by liver enzymes (Wedemeyer 1968) .  DDT caused changes
    in schooling behavior of goldfish (Carassius auratus) when fish were
    exposed to one ppb for seven days and then transferred to clean water
                                      254
    

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    (Weis and Weis 1974).  The 48 hour LC   for rainbow trout exposed to
    dicofol was 100 ppm  (Pimentel 1971).
    Frogs were killed by a single injection of 150 mg/kg DDT into the dor-
    sal lymph sac (Ellis et al. 1944) , but the LE>cn for a single oral dose
    was greater than 2,000 mg/kg in bullfrogs (Tucker and Crabtree 1970).
    The relative toxicity of chlorinated hydrocarbons to anurans was esti-
    mated to be endrin > aldrin and dieldrin > DDT and toxaphene and re-
    sistance of up to 200-fold was found in amphibians from treated areas
    (Ferguson and Gilbert 1967).
    Birds—The acute toxicity of DDT in birds ranged from an LD   of 800
    mg/kg in pigeons to an LD,.,. of greater than 2,200 mg/kg in mallards,
    while LC,-n levels ranged from 300 ppm in bobwhites to 3,300 ppm in
    mallards when five day feedings were used as the criterion (Pimentel
    1971).  Tucker and Crabtree (1970) stressed the high degree of cumula-
    tive action of DDT as the effective minimum lethal dose in mallards
    was 50 mg/kg/day over a 30-day feeding period and 100 ppm over a one
    year period.
    The LC   for birds fed dicofol-treated feed for five days followed by
    clean feed for three days ranged from 1,400-1,500 ppm in two-week old
    coturnix quail to 2,800-3,000 ppm in bobwhites; mallards and pheasants
    were intermediate (Pimentel 1971).
    At 500 ppm, dicofol in acetone injected into hens' eggs caused 30 per-
    cent mortality of the embryos (Dunachie and Fletcher 1969) .
    When pigeons were fed DDT, the observed increase in liver wieght was
    more closely correlated with DDE levels than with DDT levels, and was
    not observed when ODD, which is not converted to DDE, was fed (Bailey
    et al. 1969a) .  DDE was toxic in the pigeon but did not cause the ty-
    pical symptoms of organochlorine poisoning (Bailey et al. 1969b) .
    The drastic effects of chronic intake of DDT, and other chlorinated
    hydrocarbons, on avian reproduction have been adequately reviewed
                                     255
    

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    (Pimentel 1971, Menzie 1972, Edwards 1973, Stickel 1973, Ware 1975,
    Peakall 1975).  Haegele and Tucker (1974) fed 15 common pollutants to
    mallards and coturnix quail and only DDE caused eggshell thinning of
    prolonged duration after a single dose.  Eggshell thinning was also
    the result of toxic effects by other compounds, but was rapidly re-
    versed when their other symptoms waned.
    Mammals—The acute oral LD5Q of DDT in rats is 113 mg/kg (Servintuna
    1963, Martin 1968, Brooks 1974) and the dermal LD,-0 is greater than
    2,500 mg/kg (Martin 1968, Jones et_ al_. 1968).  The DDT metabolite and
    analog DDD (TDE) has an acute oral ID,.- of 400 to 3,400 mg/kg and an
    acute dermal LD   of greater than 5,000 mg/kg (Jones 1968).  The acute
    oral LD5Q for the DDT metabolites DDA and DDE is given as 740 mg/kg
    and 880 mg/kg respectively (Servintuna 1963).  In the present array
    of insecticides DDT may be classified as moderately toxic to mammals
    if acute toxicity is the only criterion.  Early evaluations generally
    concurred with the summary of Stammers and Whitefield (1947) that,
    properly used, DDT was harmless.
    Toxicity in rats and rabbits was suggested to result from the presence
    of both aromatic and aliphatic chlorine, and to decrease with decreas-
    ing chlorination of the ethane bridge (Smith et_ al_. 1946, Von Oettin-
    gen et^ al^. 1946).  Acute poisoning by DDT, other than by deliberate or
    accidental ingestion of large doses, is often allergenic, with allergic
    rhinitis, dermatitis, blood disorders, and autoantibody formation re-
    ported (Kagan et al. 1969).  Therapeutic value was claimed for DDT by
    Greim (1970), who reported that in man, 90 mg DDT per day reduced hy-
    perbilirubinemia by increasing bilirubin conjugation to glucuronic acid,
    and also found that two to five grams of DDD per day was beneficial in
    Gushing's syndrome since it decreased the excretion of 17-hydroxyster-
    oids.  A daily dietary intake of 2.2 mg/kg altered mast cell physiology
    and histamine-mediated reactions in rats (Gabliks et al. 1975).  Hrdina
    and Singhal (1975) most recently reviewed the data pertaining to the
                                       256
    

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    pharmacological basis of DDT toxicity in mammals.
    Accumulation of DDT in fat and its transmission into milk were noticed
    early (Woodward et_ ajU 1945, Stammers and Whitfield 1947).  Krasovskii
    and Shigan (1970) observed that rats fed less than 50 mg/kg/day accu-
    mulated DDT in their fat, but not in their livers, kidneys, brains, or
    hearts; compensatory increases in excretion were found as the dose of
    DDT was increased up to 50 mg/kg/day, suggesting that enzyme induction
    by DDT can modify the response to it.  When rats were fed 10 to 20 mg
    technical DDT per day, serum and fat levels of DDT remained elevated
    for one year after feeding ended.  Storage was found to be of the order:
    p^p'-DDD < c^p'-DDT < p^p'-DDT < p,p'-DDE (Morgan and Roan 1971).  The
    conversion of p,p'-DDT to p3p'-DDD was found to be mediated by intes-
    tinal flora rather than by the rat's own enzymes (Mendel and Walton
    1966).
    In rats, DDT at 70 mg/kg/day increased liver phosphofructokinase and
    phosphofructoaldolase but inhibited glucose-6-phosphatase, glucose-6-C
    phosphate dehydrogenase, and glucose-6-phosphate transketolase.  All
    of these enzymes were inhibited by 3.5 mg/kg/day (Kuz'minskaya and
    Yakushko 1970).  When 70 mg/kg/day were administered to rats, distur-
    bances of serotonin metabolism were postulated because increases of
    5-hydroxyindole-3-acetic acid were observed within two days.  Chronic
    doses over three to five months somewhat reduced the excess excreted
    (Khaikina and Shilina 1971).  Daily doses of one percent of the LD n
    to rabbits rendered them more sensitive to coronospastic agents such
    as pituitrin (Kagan et al. 1974) .  DDT is generally recognized to be
    estrogenic (Cecil et al_. 1971, 1975; Gellert et^ al. 1972, Nelson 1974).
    The DDT homologs, p^p'-DDD and DDE were not estrogenic, but DDA was
    somewhat estrogenic (Gellert et al. 1972).
    In a lengthy review of the harmful effects of DDT, Kagan (1969) cited
    the effects of chronic intake of DDT in the rat to include marked al-
    terations of liver functions at "large" doses (0.05 LD,-n per day, or
                                      257
    

    -------
    about 5 mg/kg/day).  Moderate doses (0.01 LD   per day, or about 1.2
    mg/kg/day) resulted in decreased sleep, changes in blood serum enzymes,
    and increases in the weights of liver, kidneys, and heart.  Small doses
    (0.001 to 0.005 LI>5Q» or about 0.1 to 0.05 mg/kg/day) caused minor
    changes in liver function and weight.  It was stated that, in man, the
    effects of chronic DDT intake included higher rates of liver disease,
    central nervous system disorders, more endocrine disturbances, compli-
    cations of pregnancy, spontaneous abortions, and premature births (Ka-
    gan et al. 1969).  Radomski et al. (1968) observed increased levels of
    p.,p'-DDE in patients dying of portal cirrhosis, cerebral hemorrhage,
    and hypertension.
    Interactions of DDT with other pesticides included sharp increases in
    DDT storage in beagles when aldrin was added to a fixed regimen of DDT
    intake (Deichmann et al. 1971a), decreases in the toxicity of carbaryl
    when mice were pretreated with DDT (Meksongsee et al. 1967) and in-
    creases in dieldrin metabolism in DDT-treated female rats  (Street and
    Chadwick 1967).  Wagstaff and Street (1971) reported that guinea pigs,
    unlike beagles, stored less DDT when also treated with dieldrin.  Sy-
    nergism of toxic effects was reported between endrin and DDT in mice
    (Keplinger and Deichmann 1967).
    The acute oral LD   value of dicofol for rats has been estimated to be
    1,100 mg/kg (Gaines 1969), 1,494 mg/kg, with 95 percent confidence lim-
    its of 1,039 to 2,150 mg/kg (Brown et a^. 1969), and 575 to 2,000 mg/kg
    (Jones et al. 1968).  For intraperitoneal injections the LD^ was 1,150
           —-—"- •'                                                j U
    mg/kg, with 95 percent confidence limits of 867 to 1,525 mg/kg (Brown
    et_ a^. 1969) or 17 mg/ml of a 20 percent solution (Gul'ko 1968).  The
    acute oral LD,-n of dicofol for rabbits was calculated to be 1,810 + 350
    mg/kg; for dogs, 4,000 mg/kg (Smith et_ al_. 1959).
    Chronic feeding of 1,250 ppm dicofol caused deaths in 3 months in rats
    (Smith et_ a!L. 1959) and 3,000 ppm caused deaths in five weeks  (Vers-
    chuuren et al. 1973).  Female rats were found to store more dicofol,
                                      258
    

    -------
    and excrete it less rapidly, than males while growth was inhibited by
    chronic feeding of 100 ppm in females, but required 1,250 ppm in males
    (Smith et_ al. 1959).  McKinley and Grice  (1960) suggested that most
    dicofol would be stored as its metabolite, DDE.
    After a single oral or intraperitoneal dose of dicofol, peak loads were
    observed in the heart and testes after 32 hours while in muscles, brain,
    and most other organs the peak occurred after 40 hours.  In fat and
    feces the peak occurred after more than seven days  (Brown et al. 1969).
    Non-lethal effects of dicofol parallel those of DDT, notably liver
    lesions and an increased liver weight relative to body weight (Smith
    et^ al. 1959) .  Dicofol, like DDT, increased the epoxidation of aldrin
    and of heptachlor in male rats and female quail, but it was less active
    than DDT in this respect (Gillett et_ al.  1966) .
    DDT does not appear to be teratogenic (Deichmann et_ a.1^. 1971a, Schmidt
    1973) but did cause reproductive disturbances in mink (Pimentel 1971)
    and racoons  (Menzie 1972) at environmental levels.  In beagles, 12 mg/
    day of DDT for fourteen months adversely  affected the male libido, the
    female estrus cycle, pregnancy and milk production; stillbirths in-
    creased and litter survival decreased.  Blood and fat levels in the
    adult beagles were comparable to levels found in human occupational
    exposure (Deichmann et al. 1971b).  DDT was found to cross the placen-
    ta and was stored in fetuses (Backstrom e_t_ al^. 1965, Schmidt 1973).
    When DDT or its analogs, methoxychlor, DDE or DDA, were administered
    to two, three, or four day old female rats, the rats remained anovula-
    tory and showed persistent vaginal estrus when mature; male rats treat-
    ed the same way were reproductively normal (Gellert et_ al. 1974) .
    Ozburn and Morrison (1964) were able  to select for DDT resistance in
    mice, and after nine generations the  selected line had an LD   of
    greater than 900 mg/kg to DDT.  This  resistant line showed somewhat
    increased tolerance to dieldrin and lindane as well.  In mouse lymph-
    oma cells, resistance to DDT conferred resistance to dicofol, DDD,
                                      259
    

    -------
    methoxychlor, and DDE.  The resistance to dicofol was enhanced five
    times as much as DDT resistance.  The resistance to DDT analogs was
    not due to enhanced degradation (Spalding et al. 1971).
    Epstein and Shafner (1968) concluded that DDT was not mutagenic in
    mice, but Epstein and Legator (1971) cited data showing that DDT was
    mutagenic in mice if given to males at levels of 50 to 70 mg/kg.  These
    data were later published by Palmer et^ al_. (1973), who concluded that
    DDT was marginally mutagenic.  Clark (1974) also considered DDT to be
    weakly mutagenic by the dominant lethal test in mice.  In vitro, ten
    mg/kg DDT caused chromosome breaks and exchange figures in a marsupial
    cell line (Epstein and Legator 1971).
    Considerable controversy exists- as to the carcinogenicity of DDT.
    Nakamura (1960) observed precancerous lung changes in rats sprayed
    with DDT for three months, and chromoleukemia increased in rats fed a
    high-fat, highly purified diet.   In the latter study, the diet rather
    than the DDT was considered the major carcinogen (Kimbrough e_t_ al.
    1964).  Terracini (1967) found suggestions of weak carcinogenicity of
    DDT in rats, mice, and dogs, but considered the data to be equivocal.
    Kemeny and Tarian (1966) observed an increase of tumors from 1.22 per-
    cent in controls to 5.41 percent in treated mice, and 3.51 percent of
    leukemias in treated mice compared with little or no leukemia in con-
    trols.  This study spanned five generations, and mice were fed 2.8 to
    3.0 ppm per day, corresponding to 0.002 or 0.001 of the murine LD,-Q.
    More recent evidence for carcinogenicity in mice was reported by To-
    matis and co-workers (1972) in a preliminary report on a projected
    seven generation study.  Both in the parental and F  generations, DDT£
    treated mice had larger liver tumors earlier and more frequently than
    control mice.  Aflatoxins were not present in the food, as had been
    suggested by Jukes (1970) about an earlier study.  Lung tumors were
    found significantly more often in four of six generations of inbred
    strain A mice treated with DDT (Shabad et al. 1973) and liver tumors
                                     260
    

    -------
    which were transmittahle, but did not metastasize, were found in inbred
    Balb/c mice fed 250 ppm DDT (Terracini et_ al. 1973) .  DDT was also co-
    carcinogenic with methylcholanthracene (Uchiyama et al. 1974).  DDT
    decreased the induction of tumors by dimethylbenzanthracene in rats
    (Okey 1972) and reduced the carcinogenicity of dialkylnitrosamines in
    rat, hamster, and mouse tissues (Bartsch et_ a^. 1975).
    Brown (1972) observed no effects on murine reproduction, and no tera-
    togenesis, at dicofol levels up to 225 ppm; in rats, the no effect
    level was 100 ppm, and no pathological differences between control and
    treated rats were observed in the fifth generation at this level.
                                      261
    

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    Methoxychlor
    Methoxychlor is the common name for l,l,l-trichloro-2,2-bis-(p-methoxy-
    phenyl) ethane, introduced in 1954 by J. R. Geigy AG, and by E.  I. du
    Pont de Nemours and Company, Inc. under the trade name Marlate.
    Methoxychlor, a nonsystemic contact and stomach insecticide with a
    range of effectiveness similar to that of DDT, is synthesized by the
    condensation of chloral and anisole in the presence of acidic catalyst.
    The pure p^p'-isomer forms colorless crystals melting at 89 C and the
    technical product consists of about 88 percent p3p '-methoxychlor, most
    of the rest being O3p '-methoxychlor.  Brooks  (1974, vol. 1) detailed
    alternative ways of synthesizing methoxychlor.  The technical product
    is a grey, glaky powder with a melting point of 77 C which is soluble
    in water to 0.62 ppm (Kapoor et^ al_. 1970), moderately soluble in etha-
    nol and petroleum oils, and readily soluble in most aromatic solvents.
    Brooks (1974) listed the solubilities of methoxychlor in kerosene and
    dichlorobenzene as 20,000 ppm (2 g/lOOg) and 400,000 ppm (40 g/lOOg)
    solvent.
    Degradation-
    Biological—Under laboratory conditions in Phillipine soils methoxychlor
    was degraded within one month in flooded Casiguran soil, within  two
    months in flooded Luisiana soil, and within three months in flooded
    Maahas soil, while some residues remained after three months in  flooded
    Pila soil.  Under simulated upland (aerobic) conditions, methoxychlor
    residues were found in all soils after three months (Castro and  Yoshida
    1971) .  Degradation of methoxychlor by planktonic algae  (.Chtovel'ia,
    Monopaphid-i-um, Actinostrum, Kol-lella., Carteria, Soenedesmus, and N-tta-
    okia) ranged from 20 to 80 percent.  Products were not identified  (But-
    ler et al. 1975).  Aevobaater aerogenes degraded methoxychlor to 1,1-C
    dichloro-2,2-bis(p-methoxyphenyl) ethane in two of four anaerobic cul-
                                       262
    

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    tures; the latter compound was also recovered from one of five aerobic
    cultures (Mendel et^ al. 1966).
    In the terrestrial-aquatic ecosystem, methoxychlor was significantly
    less persistent than DDT, because of the biodegradation of the aryl
    CH.,0 groups.  Whereas DDT was converted to DDE, which was heavily
    stored in animal tissues, only small amounts of the corresponding meth-
    oxychlor ethylene were stored by animals.  The principal degradation
    pathway for methoxychlor was conversion to the mono- and dihydroxy de-
    rivatives, followed by conversion to polar conjugates (Metcalf et al.
    1971, Kapoor et^ al^. 1970, 1972).  On the basis of ecosystem studies,
    methoxychlor was ranked as a moderately persistent insecticide which,
    although severely toxic to fish, was more readily degraded by them than
    DDT (Metcalf and Sanborn 1975).  The degradation products of methoxy-
    chlor found in the water of the model ecosystem were the monohydroxy-
    ethane, dihydroxyethane, dihydroxyethylene, and unidentified polar meta-
    bolites (Metcalf e£ al. 1971).
    In fish, methoxychlor was readily metabolized to 2-(p-methoxyphenyl)-2-o
    (p-hydroxyphenyl)-1,1,1-trichloroethane and 2,2-bis-(p-hydroxyphenyl)-
                                                                14
    1,1,1-trichloroethane (Reinbold et_ a^. 1971).  Excretion of   C-meth-
    oxychlor metabolites occurred chiefly through the liver and bile in
    rats  (Weikel 1957).  In mice, methoxychlor was 0-demethylated to phe-
    nolic products, the major metabolites being 2-(methoxyphenyl)-2-bis-£
    (p-hydroxyphenyl)-1,1,1-trichloroethane 2,2-bis (p-hydroxyphenyl)-1,1,l-f_"
    trichloroethane and its ethylene, and 4,4'-dihydroxybenzophenone (Ka-
    poor et_ al. 1970) .
    Chemical and physical—In aqueous alkaline solution methoxychlor loses
    hydrogen chloride to form the diphenylethylene derivative (Crosby 1969).
    Photolytic—Under UV light in water about 50 percent of an original
    methoxychlor concentration of 0.1 to 0.2 mg/liter decomposed to form
    methoxychlor-DDE (sio~) and p^p'-dimethoxybenzophenone.  In the absence
    of air, only the DDE analog was formed.  Degradation was 90 percent
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    complete after one month (Paris and Lewis 1973) .  When milk containing
    methoxychlor was exposed to UV light at 220 and 330 nm, the photopro-
    ducts were methoxyphenol, methoxychlor-DDE (sio), 1,1,4,4-tetrakis  (p£
    methoxyphenyl)-l,2,3-butatriene, and p3p '-dimethoxybenzophenone  (Li and
    Bradley 1969).
    Transport-
    Within soil—Methoxychlor was found to migrate as much as 100 cm under
    conditions in which 95 to 97 percent of the residues remained in the
    top ten centimeters of soil (Obuchowska 1972).
    Between soil and water—Treatment of the N. Saskatchewan river with
    0.309 ppm of methoxychlor resulted in water residues of 0.05 to 0.1 ppm
    21 to 22 km downstream (Fredeen et^ al. 1975).
    Into organisms—Aeyobaater aerogenes and Ba.ci.11us subtili-s accumulated
    methoxychlor directly from water.  Uptake was extremely rapid and the
    total adsorbed varied linearly with water levels of methoxychlor be-
    tween 0.5 and 5.0 yg/liter.  Bacterial levels reached 1,400 to 4,300
    times the water levels, and 80 to 90 percent of the uptake occurred
    within the first hour (Johnson and Kennedy 1973) .  In a river treated
    with 0.309 ppm of methoxychlor, some uptake by fish occurred, but resi-
    duse disappeared within 17 days (Fredeen et al. 1975) .  Cattle fed meth-
    oxychlor-sprayed hay for six months, or fed up to six gm per day for
    six months, had no methoxychlor residues in their milk.  At higher doses
    than six gm, 0.48 percent of the intake was excreted in the milk (Ely
    et al. 1953).  Normal use of cattle sprays resulted in fat storage of
    2.8 ppm after one treatment and 2.4 ppm after six treatments.  Milk
    residues were 0.7 ppm after 24 hours and persisted no more than 21 days
    (Claborn e£ al. 1960).
    Persistence-
    Obuchowska (1969) found that methoxychlor, applied to soil at a rate of
    2 mg/100 gm soil (20 ppm) essentially disappeared in 20 to 26 weeks if
                                      264
    

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    soil moisture was ten percent, and in 30 to 38 weeks if soil moisture
    was decreased to three percent.  Methoxychlor was less persistent than
    either toxaphene or parathion  (Obuchowska 1972).
    In water, methoxychlor declined from application levels of 1.5 mg/liter
    to 0.5 mg/liter after 98 to 112 days, and to 0.15 mg/liter after 155 to
    169 days.  No further decrease was observed between 169 and 460 days
    (Luczak 1969).  Agricultural residues of chlorinated hydrocarbon insec-
    ticides in Utah Lake included methoxychlor at inlets, but not at the
    lake's outlet; carp (Carpio ayprinus) were found to have residues be-
    tween 56 and 62 ppb of methoxychlor, which compared favorable with DDT
    residues at the level of parts per million (Bradshaw et al. 1972).  The
    half-life of methoxychlor in streams was two to seven days if biological
    degradation occurred, but 200 days if hydrolysis was the primary mode of
    degradation (Bender and Eisele 1971) .
    Effects on Non-Target Species-
    Microorganisms—Methoxychlor did not significantly affect the numbers
    of fungi, the evolution of carbon dioxide, or the rate of nitrifica-
    tion, when mixed with potting soil at 12.5, 50, or 100 ppm (Eno and
    Everett 1958).  Nitrification was not inhibited by methoxychlor concen-
    trations of 2,500 ppm (Jones 1956), and carbon dioxide evolution was not
    affected by 2,500 ppm methoxychlor applied to sandy loam under laboratory
    conditions (Bartha &t_ &L_. 1967).  In contrast, an 85 percent reduction
    in photosynthesis was observed when phytoplankton was exposed to one ppm
    methoxychlor for four hours (Pimentel 1971), while 20 mg/liter (20 ppm)
    killed protozoa immediately and algal filaments within five days (Cabej-
    szik 1965).  Exposure of Chlorella pyrenoidosa to 0.1 ppm methoxychlor
    for 164 hours decreased growth by 19 percent (Kricher e_t_ aJ^. 1975).
    Invertebrates—Methoxychlor was toxic to the aquatic annelids Asellus
    aquatiaus and Lumbriculus viviegatus at 0.001 and 0.44 mg/liter, respec-
    tively (Lakota 1974).  Daphnia magna were killed by eight mg/liter of
    commercial methoxychlor within 24 hours.
                                       265
    

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    Plants—Methoxychlor did not significantly decrease root or top growth
    in beans at 12.5, 50 and 100 ppm in pot culture  (Eno and Everett 1958).
    Pish—The 48 hour LC,.-. for rainbow trout  (Salmo gai-rdneri-i) was 0.0072
    ppm; for guppies (Lebistes retieulatus),  the 96 hour LC -. was 0.12 ppm
    (Pimentel 1971).  The toxicity of methoxychlor to trout and bluegills
    (Leporrris maapoahipus) decreased with increasing temperatures, especially
    during the first 24 hours (Macek et al. 1969).
    Fathead minnows  (Pimephales promelas) exposed to methoxychlor for 96
    hours in continuous flow bioassays had a  TL,.,, of 8.63 yg/liter, but
    hatching of eggs was inhibited at levels  of one yg/liter and complete-
    ly prevented by two lag/liter.  In the same study all yellow perch (Per-
    oa flavescens) were killed by ten yg/liter of methoxychlor, and their
    growth was retarded by as little as 0.625 yg/liter (Merna and Eisele
    1973).
    Birds—Methoxychlor is of low avian toxicity.  The acute oral LD,.,. for
    young mallards was 2,000 mg/kg, while the LC^ was 5,000 ppm when birds
    were fed treated feed for five days followed by clean feed for three
    days.  The LC   for pheasants, bobwhites, and coturnix quail was greater
    than 5,000 ppm (Pimentel 1971).
    In hens and chicks fed methoxychlor for 85 and 56 days, respectively,
    fat and skin storage was observed at all  levels of methoxychlor treat-
    ment (i.e., 2,4,8,10,100 and 1,000 ppm) while the higher levels of
    treatment also caused organ storage of methoxychlor.  Sixty-three days
    after the end of methoxychlor feeding, 0.05 ppm remained in the skin
    and fat.  After three weeks of feeding chickens methoxychlor, egg resi-
    due levels were 0.4 percent of the dietary levels, decreasing to less
    than 0.5 ppm within three weeks after methoxychlor was removed from the
    diet.  Carcass residues were six to eight times as high as egg residues
    (Lillie et^ al. 1973).  Low levels (one to ten ppm) were not estrogenic
    in six week old chicks (Foster 1973).  No adverse effects on growth, food
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    -------
    utilization, weight, or mortality were noted at any level  (Olney et^ al.
    1962).
    Chicks from eggs injected with up to 500 ppm of methoxychlor were no
    more affected by post-hatching starvation than untreated chicks, nor
    was the hatching rate lower in methoxychlor-treated chicks  (Dunachie
    and Fletcher 1969).
    Mammals—The acute oral LDcQ of methoxychlor in rats is 6,000 mg/kg
    (Martin 1968).  In dogs, levels of 2,000 to 4,000 mg/kg/day induced con-
    vulsions after five to eight weeks (Tegeris et al. 1966) .  Kunze et^ al.
    (1950) reported growth retardation in rats feed 500 ppm/day of methoxy-
    chlor, apparently due to the unpalatability of the diet.   Storage of
    methoxychlor in the fat of the rats was moderate at 500 ppm, slight at
    100 ppm, and not detectable at 25 ppm; moreover, all detectable resi-
    dues disappeared from the fat within two weeks  after feeding of meth-
    oxychlor was stopped (Kunze et_ aJ^. op. ait.).
    Methoxychlor has some estrogenic activity at high levels (Welch et al.
    1969, Nelson 1974, Harris et_ a±. 1974), and 1,000 ppm methoxychlor in
    rams' feed increased the number of dead or tailless sperm  somewhat
    (Jackson et^ al. 1969) .
    Methoxychlor was not carcinogenic when mice were injected with a single
    dose of ten mg or treated weekly with 0.1 mg on the skin, but the auth-
    ors considered the test insufficient (Hodge et al. 1966).  Radomski et
    al. (1965) considered methoxychlor a carcinogen which caused liver tu-
    mors at 2,000 ppm in mice.  No conclusive data on the carcinogenicity
    of methoxychlor were available (Vettorazzi 1975).
                                       267
    

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    CYCLODIENE INSECTICIDES
    Aldrin, Dieldrin, and Endrin
    Aldrin is the common name for l,2,3,4,lO,10-hexachloro-l,4,4a,5,8,8a£^
    hexahydro-en-5,8-dimethanonaphthalene, a nonsystemic insecti-
    cide used primarily against soil insects.  In the U.S., the name aldrin
    refers to a technical product of at least 95 percent purity; in Canada,
    to the pure compound.  In Britain the pure compound is known, as HHDN.
    Produced by the Shell Oil Company, in 1948, aldrin is a white crystal-
    line, odorless solid; stable to heat, alkali and metals with a melting
    point of 104 to 140.5 C, a vapor pressure of 2.31 x 10  mm mercury at
    20°C, and a water solubility of 0.027 ppm.  It is readily soluble in
    organic solvents such as ethanol, (50 mg/ml), carbon tetrachloride
    (3,030 mg/ml) and turpentine (1270 mg/ml).  It is produced by condensing
    the dehydrochlorinated Diels-Adler adduct of cyclopentadiene and vinyl
    chloride, bicyclo(2,2,l)-2,5-heptadiene, with hexachlorocyclopentadiene
    (Martin 1968).
    Aldrin may be oxidized (commercially) with peracetic or perbenzoic acid
    to yield dieldrin:  l,2,3,4,10,10-hexachloro-6,7-epoxy-l,4,4a,5,6,7,8,8a:
    octahydro-l,4~enc?o-ea;c>-5,8-dimethano-naphthalene, a nonsystemic insecti-
    cide of high contact and stomach activity to most insects.  In the U.S.,
    the term dieldrin refers to a technical compound of at least 85 percent
    purity.  In Canada, dieldrin is the pure chemical, which in Britain is
    designated HEOD.
    Dieldrin is stable to alkali, mild acid, and Light, and gives no reac-
    tion with a Grignard reagent (Martin 1968).  It forms white, odorless
    crystals with a melting point of 175 to 176 C, has a vapor pressure of
             -7                o
    1.78 x 10  mm mercury at 20 C, and a water solubility of 0.186 ppm
    (Wurster 1971).  Its solubility is 40,000 ppm in ethanol, 480,000 ppm
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    in carbon tetrachloride and 170,000 ppm in turpentine.
    Endrin is the common name for l,2,3,4,10,10-hexachloro-6,7-epoxy-l,4,4a,
    5,6,7,8,8a-octahydro-en&>-l,b-endo-5,8-dimethano-naphthalene.  It is
    made by the epoxidation of isodrin with peracetic or perbenzoic acid.
    Isodrin (1,3,4,5,6,7,8,8-octachloro-l,3,3a,4,7,7a-hexahydro-4,7-methano-
    isobenzofuran) is made by the slow reaction of cyclopentadiene with the
    condensation product of vinyl chloride and hexachlorocyclopentadiene,
    as described by Brooks (1974, vol. 1).  Under the trade name Telodrin,
    isodrin was at one time marketed as an insecticide in its own right.
    Endrin, a nonsystemic insecticide, is a white, crystalline solid which
    melts with decomposition above 200 C, has a vapor pressure of 2 x 10
    mm mercury at 25 C.  Its solubility in ethanol is 30,000 ppm, in carbon
    tetrachloride 510,000 ppm, and in turpentine 210,000 ppm.
    Aldrin, dieldrin, and endrin are related in that endrin is isomeric
    with dieldrin, and dieldrin is the epoxide of aldrin.  Isodrin, an in-
    termediate in the formation of endrin, is isomeric with aldrin, and
    endrin is its epoxide.
    Degradation-
    Biological—Some degradation of cyclodiene insecticides by soil micro-
    organisms is well documented, particularly the conversion of aldrin to
    dieldrin (Gannon and Bigger 1958, Tu et^ aJ^. 1968, Decker and Bigger
    1965).  Experiments on degradation of cyclodienes in the laboratory are
    summarized in Table 46.  It is noteworthy that only in one case was it
    claimed that one organism, Trishoderma koningii3  converted even three
    percent of the dieldrin to carbon dioxide (Bixby et al. 1971).  Of
    twenty cultures which were successful in partially degrading dieldrin,
    all were able to degrade endrin to keto-endrin, but only thirteen were
    able to degrade aldrin to dieldrin (Patil and Matsumura 1970).  In a
    series of 150 soil cultures, twenty-five could convert endrin to keto-
    endrin (Matsumura et^ al^. 1971); even more strikingly, only 'a few' of
                                      269
    

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                  Table 46.  DEGRADATION OF ALDRIN, DIELDRIN,
                     AND ENDRIN UNDER LABORATORY CONDITIONS
       Parameter
        Product
        Reference
    Aldrin
      Chlovella pyrenoidosa     *
      Pen'Lo'ill'iwn           dieldrin keto-aldrin
        funiaulosum
      92 cultures           dieldrin; ? metabolites
      13/20 dieldrin-
        degrading organisms 6,7-dihydroxy-aldrin
                              Eisner .et al. 1972
                              Murado-Garcia and
                                Baluja-Marcus 1973
                              Tu et al. 1968
    
                              Patil and Matsumura 1970
    Dieldrin
      microbial cultures
      Tp-iahoderma vir-ide
      6 Pseudomonas; 2
        Triohoderma viride
      soil, HO, cow rumen,
        rat gut
    photodieldrin; traces
    unidentified
    photodieldrin
      Triahoderma koningii  CO
      Pseudomonas sp.           **
      sewage lagoon             0
    Vockel and Korte 1974
    Matsumura and Boush 1968
    
    Matsumura and Boush 1967
    
    Matsumura. _et al. 1970
    Bixby _et _al. 1971
    Matsumura et al. 1968
    Halvorson et al. 1971
    Endrin
      20/150                ketoendrin
      20/20 dieldrin degrad-
        ing cultures        ketoendrin
                              Matsumura 1971
                              Patil and Matsumura  1970
     * Compound  (1)  in  Figure  7
     ** Compounds  (2,3,4,5,6) in  Figure  7
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    500 cultures from heavily contaminated soil taken from the manufacturing
    site were able to degrade dieldrin; six of the successful cultures were
    Pseudomonas and two were Trichoderma  (Matsumura and Boush 1967) .  For
    aldrin, the conversion to dieldrin is reportedly more effectively car-
    ried out by fungi and actinomycetes than by bacilli; after three weeks
    some further degradation, presumably of dieldrin, was observed  in mixed
    cultures, but no metabolites were identified  (Tu e_t_ al_. 1968).  Vockel
    and Korte (1974) reported photodieldrin as the only major metabolite
    of dieldrin, but recorded traces of unidentified metabolites also.
    Photodieldrin  was also the predominant degradative product when diel-
    drin was incubated with soil, or with microorganisms from Lake Michigan
    water, from rat intestines, or from bovine rumens (Matsumura et al.
    1970).  Degradation products of aldrin and dieldrin are illustrated in
    Figure 8; those of isodrin and endrin in Figure 9.
    Despite the limited success of cyclodiene conversion in the laboratory,
    extrapolation to field conditions is difficult (Cowley and Lichtenstein
    1970).  No degradation of dieldrin in sewage  lagoon sediment was obser-
    ved (Halvorson et al. 1971).  In simulated flooded and upland soil con-
    ditions, Castro and Yoshida (1971) found that aldrin disappeared more
    rapidly under flooded-soil conditions, but dieldrin proved persistent
    in both environments.  When one hundred samples of estuarine and ocean-
    ic surface films, marine plankton, and algae were incubated with cyclo-
    dienes, only 35 of 100 estuarine cultures were able to degrade  aldrin,
    dieldrin and endrin to ferans-aldrindiol, photodieldrin, and keto-endrin,
    respectively, but none of the water samples from open ocean were even
    that active (Matsumura and Boush 1972).  Moreover, sea bottom sediment
    was ineffective in degrading dieldrin, aldrin or endrin; algae were
    necessary for activity (Patil et_ al^. 1972).
    Most recently, microbial degradation of dieldrin in waste composting
    was attempted, with singular lack of success.  At least 97.3 percent of
    the dieldrin remained unaltered after three weeks (Mueller and Korte
    1975).  When dieldrin was exposed to microbes from soil heavily contam-
                                       271
    

    -------
             1 = mammals
             2 = insects
    CL
                                                         aldrin
        METABOLIC PATHWAYS OF ALDRIN AND DIELDRIN
                           Figure 8
                                272
    

    -------
                                      1 = RAT    4 = PLANT
                                      2 = INSECT  5 = PWNT
                                      3 = SOIL   6 = ANIMAL
    METABOLIC PATHWAYS OF ISODRIN AND ENDRIN
                       Figure  9
                           213
    

    -------
    inated with pesticides, no degradation was observed, and aldrin degra-
    dation extended no further than the production of dihydroaldrintmns-
    diol and dihydrochlordene-l,3-dicarboxylic acid, plus traces of 4-keto-
    aldrin (Vockel and Korte 1974).  Photodieldrin was also recalcitrant to
    degradation by algae (Reddy and Khan 1975) .
    Although readily stored and heavily accumulated in mammalian fat, with
    sixteen hundred-fold accumulations reported in man  (Zatz 1972), cyclo-
    diene insecticides are excreted and, to some extent, metabolized by
    mammals.  An acute dose of endrin has a half-life of one to two days
    in rats if the dose was 16 yg/kg or 64 yg/kg, but a half-life of six
    days if 128 yg/kg were administered (Korte et a.l_. 1970) .  In the same
                                               14"
    article, it was reported that if 200 yg of   C-endrin were injected as
    a split dose, the radioactivity was excreted in the form of metabolites,
    not of endrin.  Male rats retained 5.2 percent of the radioactivity
    after 24 hours; females retained 12.1 percent.  This sex difference
    persisted on a chronic dose of 0.4 ppm; steady state storage was achiev-
    ed in both sexes after six days, but females stored twice as much en-
    drin as males.  Datta and co-workers (1965) reported more efficient ex-
    cretion of dieldrin by male rats, with unidentified polar compounds be-
    ing excreted in the urine; the males were again approximately twice as
    effective in eliminating the cyclodiene as were the females.  In rabbits,
    dieldrin was metabolized-to trans-6,7-dihydroxy-dehydro-aldrin, with a
    toxicity one-half to one-sixteenth that of dieldrin (Korte and Arent
    1965).
    Muller and co-workers (1975) observed that rats and primates oxidized
    dieldrin directly, producing 12-hydroxy~dieldrin; mice and rabbits
    opened the epoxide ring to give aldrin-4,5-trcmS-dihydrodiol.  Since
    the mouse metabolized dieldrin more rapidly than either rats or rabbits,
    the authors speculated that this might be correlated with the hepatomas
    observed primarily in this species.  Conversion of  the aldrin and diel-
    drin metabolite to dihydrochlordene-dicarboxylic acid was quite rapid
                                       274
    

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                                               14
    in rats and 44 percent of the administered   C was eliminated as meta-
    bolites within one week with dechlorination as the major pathway (Lay
    _et_ al. 1975) .  The photoisonierization product of dieldrin, fed to rats
    at 10 to 30 ppm for 13 weeks, resulted in the identical urinary meta-
    bolites as dieldrin (Baldwin and Robinson 1975).
    Photolytic—After one month's exposure to sunlight on glass, aldrin
    residues consisted of 2.6 percent aldrin, 4.6 percent dieldrin, and 93
    percent of other photoproducts, of which two were highly insecticidal
    (Rosen and Southerland 1967) .  Through the nathways of photoisomeriza-
    tion and photooxidation, dieldrin was converted to photodieldrin; which
    is resistant to further transformation (Crosby and Moilanan 1974).  In
    ultraviolet light, the conversion of dieldrin to photodieldrin was 50
    percent completed in one hour and two unidentified compounds were also
    formed (Benson 1971).  On silica gel chromatography plates, the photo-
    isomerization of aldrin, dieldrin, and endrin was accelerated by many
    compounds with high triplet-energy values although no direct correlation
    was found between specific triplet-energy values and photosensitizing
    activity (Ivie and Casida 1971).
    Ultraviolet light of greater than 230 nm was found to further degrade
    the aldrin metabolite, dihydrochloroindene-dicarboxylic acid, which is
    formed in rat intestines; and Gaeb and his co-workers (1974a) suggested
    that the degradation should also proceed in sunlight.  Degradation of
    solid aldrin, dieldrin, and endrin occurred in a current of oxygen (Gaeb
    et al. 1974b).  Endrin isomerized completely in seventeen days in hot
    sun (southern California in June) with formation of pentacyclic ketone,
    but no dechlorination occurred (Burton and Pollard 1971).  Spontaneous
    degradation of endrin without dechlorination in the dark was reported by
    Barlow (1966).  Gaeb and co-workers  (1974c, 1975b) observed that aldrin
    adsorbed on silica gel surfaces was  converted to different photoproducts
    than solid aldrin on glass.  They suggested that the adsorption monolay-
    er on silica gel permits greater access of oxygen to the pesticide and
                                       275
    

    -------
    that decomposition on glass is a less realistic model than decomposition
    from adsorption, at least for soil insecticides.  Photodieldrin was de-
    graded to carbon dioxide and hydrogen chloride by ultraviolet light in
    the refrigerator, photodieldrin was converted to two unidentified meta-
    bolites, but in the freezer, it was stable for 45 days (Reddy and Khan
    1975).  Hartley (1968) suggested that volatilization of pesticides
    might result in their degradation in the highly photochemically active
    ionosphere, if the chemical had escaped to 50 meters and then escaped
    upward by eddy currents.
    Chemical and physical—Dieldrin and heptachlor were not degraded by
    Grignard reagents of LiAlH,, nor in a mixutre of melted potassium hy-
    droxide and potassium nitrate at 230 C, nor in alkaline medium at high
    pressures: but some degradation—albeit without dechlorination—occurred
    in methanol and benzene at 13 KBar pressure and 140 C with an acid cata-
    lyst (Roemer-Maehler et _al_. 1973) .  Dieldrin was partially decomposed
    in 30 percent H.O^, but not by ethanolamine (Kennedy et^ aJU 1972b) and
    complete degradation was achieved by metallic sodium or lithium in liq-
    uid ammonia (Kennedy et al. 1972a).  Endrin was partially degraded by
    alkali, but not by chlorine gas or potassium permanganate (Leigh 1969).
    Heating dieldrin to 230 C caused partial dechlorination and resulted in
    residues of chlorinated benzoic and phthalic acids (Stojanovic et aJ.
    1972b).  Heating to 900 C in the presence of air decomposed dieldrin to
    CO, CO , C19, and HC1, with unidentified compounds accounting for only
    9.4 percent of the gases (Kennedy et_ aJU 1972b) .  The authors had demon-
    strated earlier that incineration of pesticides at 900 to 1000 C results
    in more nearly complete degradation of a large variety of herbicides
    and insecticides than does chemical degradation (Kennedy &t_ al. 1969) .
    Thus, even though data on the incineration of endrin and aldrin were
    not given, it is very plausible that their thermal degradation at 900 C
    also would be feasible and complete.
                                       276
    

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    Photodieldrin was degraded to a number of unidentified products by y^
    irradiation, but the authors did not consider the technique, which re-
    quired seven megarads, to be a technologically feasible mode of degrad-
    ing residues of these pesticides (Vollner and Korte 1974).  Irradiation
    of aldrin, dieldrin, and heptachlor with 0.5 to 2.5 megarads of   Co-C
    y-radiation and/or 10 to 20 megarads of 6-radiation produced numerous
    unidentified residues which, it was speculated, might be  easily biode-
    gradable  (Ceurvels et al_. 1974).
    Transport-
    Within soil—Chlorinated hydrocarbon pesticides are considered to be
    immobile on a subirrigated column system (Harris 1969).   Dieldrin was
    found to exhibit 'minimal' leaching when several soils were placed in
    columns or sloping troughs; this minimal leaching was, however, affect-
    ed by soil type (Thompson et al. 1970).  In irrigated fields in the
    United Arab Republic, light soils such as sandy and calcareous sandy
    loams were found to release pesticides more readily than  clay or clay
    loams (Gawaad et al. 1971) .  Isodrin was distributed more evenly than
    aldrin, dieldrin, toxaphene or chlordane after application of 73 of
    146 kg/ha in Congaree sandy loam (Nash and Woolson 1968).  In a sloping
    field of sandy loam soil, residues decreased most rapidly at high points;
    the buildup followed plow lines, suggesting washoff rather than leaching,
    and was more striking for aldrin (dieldrin) than for heptachlor (Peach
    et^ ai_. 1973).  In hot, dry soil, lateral movement did not exceed 15 cm,
    and the data were not consistent with diffusion of dieldrin in water
    (Cliath and Spencer 1971).
                                                                    14 —.
    In soil boxes 60 cm x 60 cm, filled with loam soil, leaching of   C-C
    aldrin could be detected after several weeks, although only about ten
    percent of the radioactive compounds had migrated vertically after
    three years (Moza et_ al_. 1972).  Of this, ten percent, or one percent of
    the total radioactivity, moved laterally and even upward  in adjacent
    boxes (Kohli et al. 1973).  Application of aldrin was equivalent to
                                       277
    

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                                       14
    2.9 kg/ha, or a total of 103 mg of   C-aldriri per box.  One metabolite
    was identified as dihydrochloroindene-dicarboxylic acid (Moza et al.
    1972).  It was later established that this compound could be further
    degraded by UV light (Gaeb et_ al_. 1974) .
    When aldrin was incorporated four to six inches into the soil at a rate
    of 20 and 200 Ibs/A (22.4 and 224 kg/ha), up to twice as much pesticide
    was recovered in the lower as in the uppt.r half of the plot, which
    sloped from 5 to 15 degrees (Lichtenstein 1958).  At 1.5 and 2.5 Ibs/A
    (1.68 and 2.80 kg/ha), soil-incorporated aldrin remained mostly in the
    top three inches of soil:  90 percent at one year and 72 to 80 percent
    after three years, with no residues detected in the six to nine inch
    layer (Lichtenstein et_ al_. 1962).  Cultivation resulted in a 76 to 82
    percent decrease in residues recovered a:"ter seven to eleven years
    (Lichtenstein et_ _al_. I971b) ; moreover, pesticides penetrated without:
    cultivation (Harris and Sans 1969).  Leaching to 60 cm in light sandy
    soil was reported by Voerman and Besemer (1970).  In mineral soil, 14
    percent of the pesticides were found at this depth (Harris and Sans
    1969).  Carter and Stringer (1970b) reported that aldrin, dieldrin,
    gamma-chlordane, and heptachlor penetrated to the same extent when ap-
    plied as emulsified concentrates; penetration was greater in sandy soils
    than in clay soils, with the latter retaining 70 percent of the pesti-
    cides in the upper layer regardless of moisture content.  Nash and Wool-
    son (1968) reported that the relative mobilities of a series of chlori-
    nated hydrocarbons in sandy soam were BHC (lindane) > isodrin > hepta-
    chlor > endrin > toxaphene > dieldrin > aldrin > dilan > chlordane.
    Eighty-five percent of the aldrin and dieldrjn, but not of the isodrin,
    remained in the upper 23 cm of soil, with the; greatest concentration
    from 7 to 23 cm.  McLand (1967) stated that 90 percent of the residues
    recovered from 200 Ibs/A (224 kg/ha) of soil-applied aldrin or dieldrin
    were in the top three inches (7.5 cm) of soil 17 months later.  The sum
    of these data makes it clear that, despite their relative immobility,
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    considerable movement of the cyclodiene insecticides  eventually  occurs
    under field conditions because of their unusually great persistence.
    Between soil and water—When 22 to 45 kg/ha were applied  to  soil  in
    strips not less than 3.6 meters from a pond, 0.3 ppm  dieldrin was  re-
    covered from the bottom mud of the pond only if the dieldrin was  not
    incorporated into the soil and vertical motion resulted in residues of
    no more than 1.1 ppm below 15 cm in the soil after 81 weeks  (Edwards et
    al. 1970).  Endrin was found in runoff at no more than 3  ppb, and  was
    reported to reach ground water only if drought led to soil cracking and
    rain then carried endrin-carrying soil particles into the fissures; an
    interval of 72 hours was reported to halve the amount of  endrin  so trans-
    ported, compared to rain 24 hours after endrin application (Willis and
    Hamilton 1973).  Over a 41 month period little loss of dieldrin  from
    soil was attributed to runoff (0.07 percent) or washoff (2.2 percent);
    volatilization accounted for 2.9 percent even though  the  highest  levels
    of volatilization undoubtedly occurred before measurements were made
    (Caro and Taylor 1971) .  Barlow and Hadaway (1958) concluded that  diel-
    drin did not evaporate until it had diffused evenly through  soil  blocks
    and had been adsorbed to the soil.
    Despite their extremely low levels of movement into water, cyclodienes
    are measurable contaminants of canals (Bevenue et_ al^. 1972:  dieldrin),
    rivers (Young and Nicholson 1951: endrin; Lauer e_t^ _al_. 1966: endrin;
    Morris and Johnson 1971, Johnson and Mortis 1971: dieldrin)  and  aquifers
    (Wells et_ al_, 1970: dieldrin).  Even  jhen water contained no measurable
    amounts of cyclodienes, bottom sediment and bottom dwelling  organisms
    often contained measurable residues (Moubry _et_ aL^. 1968;  Leland  et al.
    1973).  Because of the hydrophobic nature of the cyclodienes, they were
    found to enter water adsorbed to soil, especially when organic matter
    was present (Goerlitz and Law 1974).  Aldrin can be so thoroughly  ad-
    sorbed to loam that no toxicity is observed in bioassays  (Lichtenstein
    et al. 1967).  Bevenue and co-workers (1972) found dieldrin  to accumu-
                                       279
    

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    late 4,000-fold in algae, 9,000 fold in sediment and 32,000-fold in fish
    as compared to water levels in canals.  The water residues were in the
    range of parts per trillion, and fish contained about one ppm of diel-
    drin.  A similar conclusion was reached by Reinert (1970).  Persistence
    of pesticides in bottled river water subjected to natural and artifi-
    cial light for eight weeks was found to be 20 percent for aldrin as al-
    drin, with the remaining 80 percent recovered as dieldrin; 100 percent
    for endrin, dieldrin, and DDT.  In contrast, methyl parathion, para-
    thion, malathion, and carbaryl had totally decomposed (Eichelberger and
    Lichtenberg 1971).
    In lakes, aldrin was removed from water by flocculent bacteria such as
    bacilli, flavobacteria, and protaminobacter, which adsorbed and concen-
    trated particulates; the fate of the sedimented aldrin is not known
    (Pfister 1971, Leshniowsky et_ al_. 1970).  Adsorption by inorganic mat-
    ter was found to be slow, with equilibrium on kaolinite or montmoril-
    lonite reached only after one month (Weil et_ a^. 1972) .  On natural
    aquifer sands, adsorption of dieldrin and lindane was in the nanogram
    per liter range, was unaffected by temperature or pH, and was reversible
    (Boucher and Lee 1972).  On montmorillonite, however, increasing the
    pH from six to ten decreased adsorption; changes of temperature between
    10  and 30 C had no effect, and the addition of sodium chloride gave
    inconclusive results (Huang 1971).  A single large scale marine contam-
    ination was reported after the sinking of a dieldrin-carrying ship.
    Waters near the wreck initially contained 40 ppb which decreased to less
    than 0.0005 ppb within five months.  Mollusks were found to contain 13
    parts per billion, fish 0.9 to 23 parts per million of dieldrin and no
    information on the routes of dispersal or the contamination of the sed-
    iment was given  (Simal et al. 1971).
    After application of approximately one ppb of dieldrin to a small
    slough in Canada, residues were undetectable in mud and water after ten
    months, but persisted in some vegetation and in aquatic invertebrates
                                      280
    

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    for almost two years.  Final concentrations in invertebrates ranged
    from 1.8 to 44.6 ppb and concentration in successive trophic levels was
    not seen (Rosenberg 1975).  In a terrestrial-aquatic ecosystem, aldrin
    was almost completely converted to dieldrin during the thirty-three day
    cycle; in Gcaribusia, only 0.5 percent of the   C was stored as aldrin.
    Three minor degradation products were found in the fish, namely, 9£
    hydroxydieldrin, 9-ketodieldrin, and an unknown thought to be trans-^
    dihydroxydihydroaldrin; these compounds were also found when dieldrin
    was examined.  Aldrin was found to have a Biodegradability Index (BI)
    of 0.00014 in Ganibusia and of 0.0017 in the snail (Metcalf et_ al^.  1973).
    Results for dieldrin were very similar to those for aldrin, with a BI
    of 0.0018 in fish and 0.009 in snails.  The Ecological Magnification
    (EM) was 5,957 and 11,149 for dieldrin in fish and in snails, respec-
    tively; the EM for aldrin was 3,140 for fish and 44,600 for snails (Met-
    calf et^ al_. 1973, Metcalf and Sanborn 1975).  The extreme resistance of
    dieldrin to degradation was apparent in the high degree of extractable
    radioactivity (Ave. 91 percent for the organisms) and the total amount
    of unchanged dieldrin in the organisms (88 percent of extractable  radio-
    activity) after 33 days.  In the water, dieldrin was present at concen-
    trations of 0.002 ppm, accounting for 25 to 28 percent of the radioac-
    tivity (Sanborn and Yu 1973, Sanborn 1974).
    Endrin in terrestrial-aquatic model ecosystem studies was found to be
    extremely toxic to the salt marsh caterpillar, and killed the Daphnia
    and mosquito larvae repeatedly after the water levels reached 0.06 ppm.
    Gambus'ia died within hours of being added to the aquarium when intro-
    duced on the 30th day of the experiment.  The toxicity persisted for
    more than sixty days, delaying the termination of the experiment to
    sixty-six days, rather than the usual thirty-three days.  This toxicity
    paralleled the endrin-induced fish kills in the Mississippi reported by
    Breidenbach et^ al. (1967) and Barthel ejt a!L. (1969).  Endrin was,  how-
    ever, slightly less persistent than dieldrin; its BI was 0.009 in  fish
                                      281
    

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    and 0.0124 in snails, and the EM values were 1335 in fish and 49,218  in
    snails (Metcalf et_ al. 1973).
    In Lake Poinsect, a shallow, eutrophic lake in South Dakota, the levels
    of aldrin increased more rapidly in the higher trophic levels than did
    dieldrin levels (Hannon et_ al_, 1970).  In the alga, Ankistrodesmus omal-
    lo-ides, adsorption of aldrin was greater than that of photodieldrin
    (Neudorf and Khan 1975) .  A clear case of increasing accumulation at
    higher trophic levels was observed when homogenated clams (Rangia cun-
    eata} were fed to crabs (Callinectus sapidus) which had been exposed
    to dieldrin.  The clams contained 193 Pg/kg (0.193 ppm) dieldrin and  the
    crabs which ate the clams concentrated the dieLdrin 3.9-fold in five
    days, and 4.7 to 6.8-fold in ten days (Pe'croceLli e^ al_. 1975).
    The substance of these data is that aquatic systems are no more efficient
    in the degradation of cyclodiene insecticides than is soil, and removal
    from water is into sediments or organisms, where accumulation rather
    than degradation can occur.  More data are available for dieldrin than
    for endrin, although the latter has been responsible for fish kills
    (Young and Nicholson 1951, Lauer g!t_ _a]L. 1966, Breidenbach et .al. 1967).
    Volatilization—The global transport of chlorinated hydrocarbons is
    well established (Risebrough et^ a^. 1968, Wheatley 1973, Bidleman 1974),
    as is the global contamination by these compounds (Wheatley and Hardman
    1965, Tarrant and Tatton 1968, Tatton and Ruzicka 1967).  Estimates of
    the amount of pesticide volatilized from treated fields were 2.8 per-
    cent for dieldrin and 3.9 percent for heptachlor, as measured by fiber-
    glass filters suspended over the field (Caro 
    -------
    When ten ppm of dieldrin were applied to untreated, sprinkled and flood-
    ed soils, volatilization was seven percent, 18 percent and two percent
    respectively in five months  (Willis e_t_ al_. 1972) which led the authors
    to conclude that their data were inconsistent with the theory of codis-
    tillation of Acree _et_ al.  (1963).  In the laboratory, dieldrin covered
    with soil volatilized more rapidly as the overlying soil bulk decreased,
    and volatilization increased with time as the dieldrin diffusion into
    the overlying soil neared  the steady state.  Volatility was proportion-
    al to the initial concentration of dieldrin in the soil and was limited
    by diffusion (i-'ariner e_t al. 1973).  Dieldrin moved to the surface of the
    soil during periods of low moisture and relative humidity and then vo-
    latilized rapidly when the soil was remoistened (Spencer and McCliath
    1973).  Maximum volatilization of di-.ldrin occurred when tne relative
    humidity was 100 percent (and soil water loss was zero), with the rate
    dependent on the dieldrin  concentration.  When the relative humidity
    was less than 100 percent, volatilization decreased with decreasing
    soil moisture, but was independent of the rate of water loss (Igue et
    al. 1972).  Relative humidity did not, however, affect the volatiliza-
    tion of dieldrin or of aldrin from glass surfaces (Phillips 1971) .  The
    rate of volatilization of dieldrin from Gila silt loam at 20  or 30 C
    was estimated to be five kg/ha/year, compared with 202 kg/ha/year for
    lindane and 22 kg/ha/year for DDT,  The rate of volatilization increas-
    ed witn increasing temperature and decreased witn decreasing soil con-
    centrations of dieldrin (Farmer et ajU 1972).
    Into organisms—Organochlorine insecticides are considered weakly sys-
    temic in plants, since uptake is measurable but not sufficiently great
    to be insecticidal (Finlayson and McCarthy 1973).  In several soils
    known to be heavily contaminated with pesticides, traces of aldrin,
    dieldrin, and endrin were found to be absorbed in the order:  carrots
    > radishes > turnips > onions (Harris and Sans 1967) .  Recovery of al-
    drin was less common than recovery of dieldrin or endrin, which were
                                       283
    

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    absorbed in the order:  sugar beets > carrots > potatoes > sugar beet
    tops > corn, oats, and alfalfa (Harris and Sans 1969).  Soybeans, grown
    fifteen years after pesticides were applied to Congaree sandy loam, con-
    tained residues of dieldrin, endrin, heptachlor epoxide, endrin trans-
    formation products, and pentachlorocyclohexanes but aldrin, isodrin,
    heptachlor, BHC, toxaphene and dilan were not identified (Nash and Har-
    ris 1973).  Beall and Nash (1969) found the degree of translocation in-
    to crop seedlings to be:  DDT < endrin < heptachlor, with endrin and
    heptachlor accumulating to some degree.  In this study, uptake was not
    correlated with soil pE, cation exchange capacity, or clay content.
    Harris and Sans (1972) found that insecticidal activity and absorption
    by plants were positively correlated with organic content of the soil
    rather than with the applied concentration of dieldrin.  Lichtenstein
    (1959) found that plant uptake of these pesticides from soils was in
    the order:  sandy loam > silt loam > muck.  Carbon added to the soil
    reduced the uptake of aldrin, dieldrin, and heptachlor by pea roots in
    sand and in loam (Lichtenstein et_ al. 1968).   Inhibition of uptake of
    pesticides by carrots and potatoes was greater than 50 percent and per-
    sisted for four seasons when 2,000 ppm (0.2 percent) carbon was added
                                                             14
    to soil (Lichtenstein et al. 1971c).  Radioactivity from   C-dieldrin
    was recovered from plants as dieldrin, photodieldrin, and hydrophilic
    metabolites (Kohli et^ al. 1973).
    Microorganisms have been found to be effective accumulators of cyclo-
    diene pesticides (Ko and Lockwood 1968a) and adsorption by dead fungi
    as well as by live fungi, streptomycetes and bacteria has been report-
    ed (Chacko and Lockwood 1967).  Dead yeasts were found to adsorb more
    dieldrin than live yeasts (Voermean and Tammes 1969).  Such adsorption
    by soil microorganisms is a logical consequence of the low water solu-
    bility and high lipid partitioning coefficient of the cyclodienes
    (Rosenberg 1975).
    Dieldrin, aldrin, endrin, heptachlor and heptachlor epoxide are known
    to be taken up by higher plants from the soil, and in some cases to
                                      284
    

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    accumulate, particularly in root crops (Morley and Chiba 1965, Elgar
    1966, Young 1969, Saha and Lee 1970, Popov and Donev 1970, Camoni et al.
    1971).  Aldrin is converted to dieldrin in or on plants (Gannon and
    Decker 1958).  The translocation of isodrin, and of its conversion pro-
    ducts endrin and keto-endrin, into the soil after leaf application has
    been documented for cabbage (Klein et^ al^. 1972), but not for forage
    crops (Wheeler et al. 1967).
         14
    When   C-aldrin was applied to soil on which potatoes were grown, 60
    percent of the radioactivity was recovered as metabolites, chiefly
                                  14
    dieldrin and dihydrochlordene-  C-dicarboxylic acid, (1,2,3,4,7,8-hexa-
    chloro-1,4,4a,6,7,7a-hexahydro-l,4-encfo-methylene-indene-5,7-dicarboxy-
    lic acid).  Aldrin was recovered in the potato peel and pulp and photo-
    dieldrin was in the potato haulm when potatoes were grown in England,
    but not when they were grown in Germany.   Water which leached from the
    plots contained dihydrochlordene-dicarboxylic acid (Klein e.t_ _al_. 1973).
                                       14
    Subsequent analysis of the fate of   C-aldrin in corn, wheat, and soils
    produced similar results in that the conversion products in plants and
    soils were qualitatively the same as in potatoes and soil.  Aldrin re-
    sidues decreased with increasing soil depth, and decreased, in corn, in
    the order roots, leaves, stems, cobs.  Less than ten percent of aldrin
    or dieldrin leached below 40 cm in the most permeable soil and harvest
    residues in the grain did not exceed 0.01 ppm (Weisgerber et_ al. 1974b).
    Persistence-
    The extreme functional persistence of the cyclodiene insecticides is
    due to their highly stable ring structures and to the toxicity of the
    few transformation products that are formed.  Thus the major terminal
    residues of aldrin is dieldrin (Gannon and Bigger 1958) which has ap-
    proximately the same mammalian toxicity (Pimentel 1971) and approximately
    half the insecticidal activity (Mulla 1960a) of aldrin; the photolytic
    product of dieldrin, photodieldrin, is two to three times as toxic to
    insects, but almost five times as toxic to mammals as dieldrin (Brooks
                                       285
    

    -------
    1974, vol. 1).  After five annual applications of aldrin, 95 percent
    of the aldrin had 'disappeared' in one year when measured as aldrin, but
    assays of aldrin and dieldrin combined showed no significant reduction
    in residues after six years (Korschgen 1971).
    Persistence was found to be greater in truck than in loamy soil (Lichten-
    stein et_ a^. 1960), and in brown forest soils than in loess-sandy soils
    (Homonnay-Csehi 1971).  Dieldrin did not decompose during six months'
    exposure in percolated and standing moist soil (Yule et al. 1967) and
    was considered stable in hot climates (Atabaev et_ al. 1970).  A summary
    of the data on the persistence of aldrin, dieldrin, endrin, and isodrin
    is given in Table 47.  Freeman and co-workers (1975) analyzed the dis-
    appearance of soil-incorporated dieldrin and concluded that four years
    was too short a period to determine the kinetics of dieldrin disappear-
    ance.  Linear regression led to a "best estimate" of 12.9 years for 95
    percent dissipation, with an 80 percent probability that the true value
    lay between 10.0 and 20.5 years.  The authors stressed that a ten year
    disappearance time is a minimum estimate and would have to be revised
    upwards sharply if first-order kinetics proved to be valid for dieldrin
    disappearance.
    The extremely variable residue levels which were found are due to the
    multiplicity of factors which affect persistence; e.g., soil type, pH,
    moisture, temperature, organic matter content, clay content, mode of
    application and rate of application.
    Under conditions predisposing to maximum persistence (thorough soil in-
    corporation, minimum tillage, and up to 448 kg/ha) Nash and Woolson
    (1967) found residues of 31 percent technical dieldrin fifteen years
    after dieldrin application and 40 percent of the applied aldrin as al-
    drin and dieldrin.  In comparing tilled to untilled fields, it was found
    that almost six times as much aldrin and dieldrin was recovered from
    the latter as from the former  (Lichtenstein et al. 1971).
                                      286
    

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        Table 47.  RESIDUES AND RATE OF DEGRADATION OF ALDRIN, DIELDRIN,
        ISODRIN, AND ENDRIN UNDER FIELD CONDITIONS.  ALDRIN WAS MEASURED
    	AS DIELDRIN, AND ISQDRIN AS ENDRIN	
       %     # of  Loss/year
    Residue  Years	%	Conditions	Reference	
    Aldrin and Dieldrin
       10     21      4.3  incorp. as termiticide
       23     16      4.8  sandy loam
       31     15      4.6  for max. persistence
        5.8   15      6.3  silt loam
        5.0   13      7.3  soil incorporated
       11.2    8     11.1  bioassay
       50     13      3.8  dieldrin
      "all"    6       -   bioactivity; loam soil
       50      6      8.3  aldrin applied
        5      1     95    aldrin residue only
      3-19     4.5   19.8  various soils
      8-10     4.5   18.2  turf
    
       40      3     20    isotope—labeled
      ^40      3     20    sugar plantation
    
      ^33      2     33o5  sugar plantation
       55      2     22.5  incorporated granules
       15      2     42.5  surface granules
       40      2     30    incorporated emulsion
        6.5    2     46.8  surface emulsion
       65      1     35    incorporated granules
       16      1     84    surface granules
       45      1     55    incorporated emulsion
        8      1     92    surface emulsion
       25      1.7   42.9  northern Tanzania
       50      1     50    Texas
    Isodrin and Endrin
       16     16      5.2  Isodrin applied
       39     16	3.8  Endrin applied	
    Bennet et al. 1974
    Nash and Harris 1973
    Nash and Woolson 1967
    Lichtenstein £t al. 1971a
    Freeman £t ad. 1975
    Wingo 1966
    Hermanson et^ al. 1971
    Korschgen 1971
    Hermanson et al. 1971
    Ibid.
    Lichtenstein et al. 1960
    Lichtenstein and Polivka
      1959
    Czaplicki 1969
    Stickley and Hitchcock
      1972
    Ibid.
    Lichtenstein et aj.. 1964
    Ibid.
    Ibid.
    Ibid.
    Ibid.
    Ibid.
    Ibid.
    Ibid.
    Park and McKone 1966
    Randolph _et al. 1960
    
    Nash and Harris 1973
    Ibid.
                                       287
    

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    Data concerning the persistence of endrin are few.  Mulla (1960b) found
    no loss of activity after nine months in soil.  On air-dried soils at
    pH < 7, seven of ten endrin samples had isomerized after 48 hours; a
    ten to 80 percent loss had occurred within the first twelve hours
                                       14
    (Asai et_ al. 1969).  At pH of 6.4,   C-labeled endrin was transformed
    to a cfeZta-ketone, an aldehyde, and an alcohol; the alcohol was not
    produced in moist soil at pH of 4.2, and none of the transformations
    took place in dry soil at pH of 4.2 (Nash je_t al. 1972).  Endrin was
    found to be stable in alkali, and its transformation products were
    stable in all treatments (ibid.).
    Lichtenstein and his co-workers (1964) applied aldrin as an emulsion
    and as granules, and each formulation was both surface applied and in-
    corporated into the soil.  The most persistent application was of gran-
    ules incorporated into the soil, but formulation was of less importance
    than soil incorporation.  After two years, soil incorporation resulted
    in residues of 55 percent for granules and 40 percent for emulsions,
    but surface application resulted in residues of only 15 percent and 6.5
    percent for emulsions and granules respectively.
    The type of soil affected both the biological activity and the persis-
    tence of cyclodienes in soil.  In one study, it was found that the tox-
    icity of dieldrin decreased linearly with increasing organic content in
    moist soil or with increasing clay content in dry soil; in mineral soil,
    toxicity increased with increasing moisture, but in muck soil, toxicity
    decreased with increasing moisture (Harris 1972).  Lichtenstein and
    Schulz (1960) reported that the epoxidation of aldrin to dieldrin was
    more rapid in loam than in muck, with conversion 50 percent complete af-
    ter three months in the laboratory at 39 C, and after 16 months in the
    field; moist soil resulted in more rapid epoxidation than did either
    dry soil, autoclaved soil, or sand.  Increased organic matter was re-
    ported to decrease dissipation of dieldrin (Harris and Sans 1972) .  Re-
    covery in chernozoic soil was reported to increase with increasing mois-
                                       288
    

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    ture  (Head and McKercher 1971) .  It was postulated that the hydrophobia
    cyclodienes were adsorbed by soil particles in the absence of moisture,
    but competed for available adsorption sites in moist soils which, in
    the latter case, would result  in increased toxicity and/or mobility
    (Harris 1964).  It has been reported that dieldrin adsorbed almost in-
    stantaneously on kaolinite and illite surfaces, while it gradually
    diffused into the interlamellar spaces on the expanding montmorillonite
    clays; the adsorptive capacities of the clays for dieldrin were not
    correlated with either the ion exchange capacity or the specific sur-
    face areas of the clays (Ju-Chang and Liao 1970).  Wiese (1964) found
    progressive biological inhibition as the clay content increased when
    organic matter content was held constant.  Bollen and co-workers (1958)
    did not find any correlation between recovery rates of aldrin or diel-
    drin and either buffer capacity, ammonium binding capacity, cation ex-
    change capacity, or pH.  In another study, it was found that the nature
    of the clay minerals did not affect the amount of aldrin adsorbed, but
    the mechanical composition and organic content of the clays did.  Or-
    ganic matter added to the clays decreased the adsorption of aldrin (Ya-
    ron et al. 1967).  Clays were also found to catalyze the decomposition
    of insecticides because acid diluents in the clay resulted in breakage
    of the epoxide rings of dieldrin and endrin, with formation of ketoen-
    drin  (Fowkes et_ al_. 1960).  Lower pH, higher temperatures, and lower
    levels of organic bases were found to increase the reaction rates.
    Temperature also affected the amount and kind of terminal residues.  It
    was reported that the epoxidation of aldrin to dieldrin did not occur
    at 7 C in loam (Lichtenstein and Schulz 1959a); dissipation from the
    soil in 56 days was found to be 16-27 percent at 6 C, but 86-98 percent
    at 46 C (Lichtenstein and Schulz 1959b) .  Effects of temperature on al-
    drin in soil are shown in Figure 10 (Lichtenstein and Schulz 1959b).
    Finally, level of application was also found to affect the rate of loss
    of aldrin and dieldrin, with higher levels being conducive to slower
                                      289
    

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    dissipation (Nash and Woolson 1967, Wingo 1966).  Data are shown for
    several chlorinated hydrocarbons in Figure  7  (Lichtenstein and Schulz
    1959b).
    Effects on Non-Target Species-
    Microorganisms—The effects of aldrin, dieldrin, and endrin on soil
    microorganisms are summarized in Tables 48, 49 and 50.  The variability
    of results, while possibly due to variations in treatment levels, meth-
    odology, and laboratory environments, probably also argues for great
    diversity of response by microorganisms.  It has been shown that dif-
    ferent marine phytoplankton genera may differ by 1,000-fold in their
    sensitivity to pesticides (Menzel et al. 1970); the same might be ex-
    pected of soil organisms.  Soils, moisture, and temperature variations
    between experiments may also have complicated comparisons, if only by
    affecting solubility or vapor pressure (Richardson and Miller 1960).
    The discordant effects shown in Tables 48, 49 and 50 augur well for soil
    response to even extremely high pesticide concentrations.  Nevertheless,
    as Parr (1974) emphasized, the existence of even slight effects due to
    chlorinated hydrocarbons is serious because of their extreme persistence.
    Jones (1956) found that 0.01 percent of aldrin might reduce ammonifica-
    tion for more than three years; in paddy culture, insecticides were
    found to affect the availability of nitrogen, but not of phosphorus or
    potassium, for more than three months.  The studies were usually of
    shorter duration, typically one to two months, and significant effects
    required the application of extremely large doses of pesticides.
    Invertebrates—The effects of pesticides on soil invertebrates have been
    exhaustively reviewed (Edwards and Thompson 1973) and need not be de-
    tailed here.  The authors concluded that the relationship between dose
    and effect tends to be logarithmic, minimizing chances of killing a
    large portion of the soil fauna; nevertheless, these pesticides common-
    ly result in decreased species diversity and changes in predator-prey
    relationships, with previously harmless species occasionally increasing
                                       291
    

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    294
    

    -------
    sufficiently to become pests.  Subsequent literature has not changed
    these conclusions.  Similar decreases in species diversity were reported
    for aquatic invertebrates (Wallace and Brady 1971) .  In a detailed as-
    sessment of the effects of 20 Ibs/A of ten percent aldrin granules
    (2.24 kg/ha) applied to an Illinois stream in November of 1960, Moye
    and Luckman (1964) observed increases in caddis flies (Tvio'hop'beTa) and
    midges (Chironomidae) through the summer following the aldrin treatment;
    mayflies (Ephemoptera) were reduced severely by the treatment and beetles
    (Elmidae") were apparently unaffected.  The authors concluded that the
    effects were largely nullified by the second summer, at which time the
    numbers of caddis flies and midges had decreased to normal levels.
    Davis and Hidu (1969) assessed the effects of aldrin, dieldrin and en-
    drin on clams or oysters, and on the survival and growth of their lar-
    vae.  Survival of oyster (Crassostrea Virginia) larvae was decreased
    by 0.025 ppm endrin or dieldrin; eggs developed normally at less than
    0.1 ppm endrin and 0.05 ppm dieldrin.  For clams (Mercenaria meroenar-
    •ia), larval survival was decreased by 0.25 ppm aldrin, but eggs develop-
    ed normally in 0.5 ppm.
    Phytotoxicity—In plants, high levels of aldrin were reported to inhi-
    bit the growth of beans and tomatoes while stimulating cucumbers, car-
    rots, and parsnips, but the effects were limited to potted plants and
    virtually disappeared in the field (Dennis and Edwards 1969).  At agri-
    cultural levels, aldrin, dieldrin, toxaphene and chlordane were report-
    ed to inhibit the growth of corn, soybeans, beans and cotton potted in
    clay loam (Diaz-Mena 1954).  Shaw and Robinson (1960) found tomatoes to
    be uninhibited by 10 to 100 Ibs/A aldrin (11.2-112 kg/ha), but inhibi-
    tion occurred at 150 Ibs/A (168 kg/ha) of aldrin or 200 Ibs/A (224 kg/
    ha) dieldrin.  V-Lci-a faba was reportedly not inhibited by 25 mg/kg diel-
    drin in clay soil, but 500 mg/kg caused some stunting (Selim et al.
    1970).  In general, phytotoxic reactions were more likely to occur in
    poor than in rich soils, and crop quality often deteriorated before
    either growth or yield were affected (Boswell 1955) .
                                       295
    

    -------
    Fish and amphibians—The 24-hour LC   of aldrin ranged from 0.036 ppm
    in rainbow trout (Salmo gairdnerii-) to 0.096 ppm in bluegills  (Lepomis
    macrooh-irus}.  The96-hour LC^- in bluegills was only 0.013 ppm.  The
    24-hour LC,._ of dieldrin for rainbow trout was 0.05 ppm, for bluegills
    0.0055 ppm; for endrin, the levels were 0.0018 ppm in rainbow  trout and
    0.0003 ppm in bluegills.  The 96-hour LC - of dieldrin in bluegills was
    0.008 ppm; of endrin, 0.0006 ppm (Pimentel 1971).  The margin  between
    safety and lethality in juvenile spot fish (Leiostomus xanthupus) was
    less than 0.1 ppb:   fish exposed to 0.05 ppb were not noticeably af-
    fected after three weeks while fish exposed to 0.15 ppb died (Pimentel
    1971).  Endrin contamination of river basins was strongly correlated
    with major fish kills between 1963 and 1964, and the fish kills stopped
    when the endrin levels fell (Breidenbach et^ al.. 1967).
    Application of 0.1 to 0.5 Ib/A (0.11-0. 56 kg/ha) aldrin, endrin, diel-
    drin, or heptachlor exterminated frogs and toads (Mulla 1962).  Toler-
    ance in anurans from heavily treated cotton fields has been reported
    (Ferguson and Gilbert 1967) and freshwater invertebrates were  also ob-
    served to develop tolerance (Naqvi and Ferguson 1968).  Bioaccumulation
    in fish has been reported repeatedly (Reinert 1970, Morris and Johnson
    1971, Ettinger and Mount 1967) and a twenty-thousand-fold concentration
    over aqueous levels was induced in shiners under laboratory conditions
    (Reed 1969).
    Birds—In birds, toxicity is often expressed by reproductive failure;
    these data are reviewed by Stickel (1973), Edwards (1973), and Menzie
    (1972).  Direct toxicity in wild birds has been reviewed by Tucker and
    Crabtree (1970), Stickel et_ al_. (1969), and Heath et_ a^. (1972), among
    others.  Acute toxicity in chickens ranged from an LDrn of 2.7 mg/kg
    for isodrin to 43 mg/kg for dieldrin (Sherman and Rosenberg 1953) with
    a 90 percent mortality after 42 days at 12 ppm dietary endrin  or isodrin
    (Sherman and Rosenberg 1954).
    Mammals—The acute toxicity of the cyclodiene insecticides to  mammals
                                       296
    

    -------
    is sufficiently great to warrant their use in vole extermination pro-
    grams (Schindler et al. 1966) and field mouse control  (Lang and Cruger
    1960).  Their relative toxicity in mammals is:  endrin, isodrin > al-
    drin, dieldrin.
    The acute oral LD   of aldrin and dieldrin was between 20 and 70 mg/kg
    in twelve species (Hodge et al. 1967); isodrin and endrin had an LD_A
                             	                                     JU
    of three to 20 mg/kg in rats (Jones et_ al. 1968, Servintuna 1964) and
    were more toxic dermally and by inhalation than aldrin or dieldrin
    (Spynu 1964).  The acute dermal toxicities in rats were estimated at
    35 mg/kg for isodrin, 98 mg/kg for aldrin, and 90 mg/kg for dieldrin
    (Servintuna 1963).  Dermal toxicity of heptachlor was 195 mg/kg, and of
    chlordane 840 mg/kg, in the same study.  The acute dermal toxicity of
    endrin was given as 60-120 mg/kg (Jones et al. 1968) .  Age affected ca-
    nine sensitivity to aldrin and dieldrin (Cleveland 1966), and sex af-
    fected metabolism and excretion of dieldrin in rats  (Klevay 1970).  In
    humans occupationally exposed to aldrin, dieldrin, and endrin, blood
    levels of up to 0.2 yg/ml for dieldrin and 0.05 to 0.1 yg/ml endrin were
    said to have no persistent adverse effects on health; symptoms of in-
    toxication, if not fatal, were said to be reversible in a maximum of
    weeks (Jager 1970, 1971).  The general applicability of these data is
    suspect, however, since all workers with symptoms of organochlorine
    poisoning were promptly removed from exposure, and all workers with
    conditions which might predispose to irreversible effects were removed
    from the areas of exposure.  Finally, any workers who were even concern-
    ed about possible consequences were removed from the set of exposed
    workers (Jager 1970, 1971).  Thus, the final sample consisted of those
    workers who were selected for minimum susceptibility to organochlorine
    poisoning.
    The toxicity of cyclodiene insecticides was altered by the presence of
    other chlorinated hydrocarbon pesticides (Keplinger and Deichmann 1967),
    organophosphate insecticides (Triolo and Coon 1966) and carbamate in-
                                       297
    

    -------
    secticides (Williams et^ jil. 1967).  DDT and dieldrin interacted to in-
    crease DDT storage in rats (Street and Chadwick 1967) but decreased DDT
    storage in guinea pigs (Wagstaff and Street 1971).  Aldrin was reported
    to synergize with other agents in the induction of cardiovascular path-
    ologies (Kagan et al. 1974).  Dieldrin at ten ppm also decreased the
    levels of vitamin A in both the maternal and fetal livers of rats (Phil-
    lips and Hatina 1972).  One ppm of dieldrin reportedly caused an in-
    crease in liver weight in female rats after two years (Walker et_ al.
    1969), a level which assumes some significance when it is recalled that
    the ordinary human carries 9.7 to 27 ppm dieldrin in his body fat (Deich-
    mann and MacDonald 1971).  Other effects of low levels of dieldrin in
    experimental animals included irritability in rats fed ten ppm for
    eight weeks (Walker et al. 1969).  In a survey of terminal hospital
    patients, dieldrin levels were significantly eilevated in patients with
    hypertension (Radomski et_ al_. 1968).
    Aldrin, dieldrin, and endrin were teratogenic in mice and in hamsters;
    in hamsters, a considerable embryonic mortality was also seen (Otto-
    lenghi £t_ al. 1974).  At considerably lower levels, Chernoff et al.
    (1975) did not observe and gross malformations in mice, but noted that
    ossification was retarded and the frequency of extra ribs increased.
    Endrin was found to be teratogenic in rats and in mice (Noda et al.
    1972), and endrin and dieldrin adversely affect murine reproduction
    (Good and Ware 1969).  Dieldrin at 0.5 to 2.0 Ibs/A  (0.56-2.2 kg/ha)
    had no significant effects on reproduction in penned cottontails  (Ma-
    lecki et_ aL_. 1974), but was transported into both blastocysts and im-
    planted fetuses in rabbits (Hathaway £tL JLL- 1967).  Aldrin at 0.15 to
    0.3 rag/day for fourteen months adversely affected estrus, pregnancy,
    livebirths, and milk production in females, as well as libido in male
    beagles, although neither parental illness ncr teratogenesis were ob-
    served (Deichmann et al. 1971).
    Aldrin and dieldrin increased the incidence of liver tumors in mice
    (Davis and Fitzhugh 1962), rats, and dogs  (Fitzhugh ot_ al^. 1964).  The
                                       298
    

    -------
    significance of these data were initially disputed  (Terracini 1967,
    Barnes 1966, Deichmann ejj^ a^. 1970).  More recent data, however, have
    confirmed the carcinogenicity of dieldrin (Walker et_ aJ^. 1969, 1973;
    Thorpe and Walker 1973, Vettorazzi 1975).
    Mutagenic effects have been suggested for the cyclodiene insecticides
    in general (Rossival 1970), and chromosome abberations have been induced
    by endrin in barley (Wuu and Grant 1966).  Dean, Doak, and Somerville
    (1975) reported, however, that HEOD, the pure form  of dieldrin was not
    mutagenic in the host-mediated assay in mice, the dominant lethal test
    in mice, or in chromosome analyses of hamster cells.
                                       299
    

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    Chlordecone and Mirex
    Chlordecone is the common name for l,la,3,3a,4,5,5,5a,5b,6-decachloro-
    octahydro-1,3,4-methano-2H-cyclobuta(cd)pentalen-2-one, introduced by
    Allied Chemical Corp. in 1958 as an insecticide and possible fungicide.
    It is synthesized by the condensation of two molecules of hexachloro-
    cyclopentadiene in the presence of sulfur trioxide to form mirex, fol-
    lowed by hydrolysis to the ketone, Chlordecone.  It is a stable tan to
    white solid of the cyclodiene group of insecticides which sublimes with
    some decomposition around 350 C.  Its water solubility is 0.4 percent
    (4,000 ppm) at 100 C, but it is readily soluble in strongly alkaline so-
    lutions at room temperature and readily forms hydrates at ordinary tem-
    peratures and humidity.  The technical product is of greater than 90
    percent purity.
    Mirex, the common name for 1,la,2,2,3,3a,4,5,5,5a,5b,6-dodecachloroocta-
    hydro-l,3,4-metheno-lH-cyclobuta(c,d)pentalene, is a white crystalline
    solid with a melting point of 485 C which is insoluble in water and un-
    affected by nitric, sulfuric or hydrochloric acids.  Introduced by
    Allied Chemical Corp. in 1958, mirex is a stomach poison with little
    contact toxicity, used primarily in baits against fire ants.  It is
    produced by the dimerization of hexachlorocyclopentadiene in the pres-
    ence of aluminum chloride, but can also be made by reacting chlordecone
    with phosphorus pentachloride.
    Degradation-
    Biological—The single report of the degradation of mirex by sewage
    sludge organisms identified neither the organisms nor the metabolites.
    The degradation proceeded under anaerobic conditions and was not light-
    mediated (Andrade and Wheeler 1974).  In estuarine environments, mirex
    was converted to chlordecone and reduced chlordecone (Brown et al. 1975).
    Essentially no metabolism of mirex was observed in plants.  The stability
                                       300
    

    -------
       14
    of   C-mirex was so great that its recycling after the death of plants
    was postulated  (Mehendale et_ aJ^. 1972).  In rats, mirex was poorly ab-
                                                14
    sorbed from the gut, and over 50 percent of   C-mirex was excreted fe-
    cally within 38 hours.  Only 0.69 percent of the radioactivity was el-
    iminated as urinary metabolites in the first week, and of the mirex
    absorbed from the gut, half remained in the tissues after 100 days
    (Mehendale et_ al_. 1972).  In another study, an oral dose of 0.2 mg/kg
    mirex was excreted unchanged in the feces or stored in the fat in rats.
    Fecal excretion was 85 percent complete after 48 hours, but after seven
    days fat levels of mirex were 0.9 ppm, and this level remained constant
    for at least three weeks.  A mirex-photoproduct was equally stable (Gib-
    son et_ al. 1972) .
    Chlordecone has not been shown to be degraded by plants, animals, or
    microorganisms.  It is, however, a metabolite of the insecticide Kele-
    van (decachlorooctahydro-2-hydroxy-l,3,4-metheno-2H-cyclobuta-(cd) £^
    pentalen-2-levulinic acid ethyl ester) in soil and in potato weeds
    (Sandrock et_ al_. 1974).
    Photolysis—Knoevenagel and Himmelreich (1973) reported that photolysis
    of chlordecone or Kelevan in the presence of oxygen resulted in the for-
    mation of carbon dioxide and hydrogen chloride.  Data on the conditions
    or rates of the reactions were not available.  Kelevan was converted to
    mirex by ultraviolet light; it was suggested that the conversion invol-
    ved splitting of the chlordecone ring to form two half-mirex rings, with
    subsequent fusion (Begum et al. 1973).  Photoproducts of chlordecone hy-
    drate were identical with a mirex photoproduct (Alley and Layton 1974,
    Alley et_ al^. 1974) .
    A solution of 0.4 M mirex in 350 ml cyclohexane or isooctane was 95
    percent dissipated by ultraviolet light in 48 hours (Alley et al. 1973).
    On silica gel chromatography plates, mirex in the presence of sun or
    ultraviolet light decomposed extremely slowly to chlordecone hydrate
    (Ivie et al. 1974).
                                       301
    

    -------
    Physical or chemical—No data were available on the physical or chemi-
    cal degradation of mirex or chlordecone, except that mirex is unchanged
    after treatment with nitric, sulfuric and hydrochloric acidis.  However,
    chlordecone appears to decompose somewhat as it sublimes at 350 C
    (Brooks 1974).
    Transport-
    In an estuarine environment, 95 percent of the mirex was adsorbed to
    organic matter, kaolinite, or montmorillonite (Brown et^ a^. 1975).  In
    soil cylinders 80 cm deep, 1.2 percent of the chlordecone leached
    through clay loam, 17.2 percent leached through clay, 17.4 percent
    through sandy clay loam, 28.1 percent leached through sandy loam, and
    36.8 percent leached through sandy clay loam (Gawaad et_ al_. 1971).
    Following a single aerial application of mirex as a fire-ant bait, pond
    sediments contained 0.7 to 1.1 ppb, while soils contained up to 2.5 ppb.
    Pond water contained 0.2 to 0.53 ppb immediately after treatment, and
    all residues had disappeared from the water within three months.  Bahia
    grass in the same pond contained mirex residues in roots and blades
    (Spence and Markin 1974).  Mangrove seedlings (Rh-izophora mangle) con-
    tained mirex after the soil was treated with 11.2 kg/ha (Walsh et al.
    1974) and apples retained 0.3 ppm chlordecone three months after a
    spraying resulted in initial residues of 1.4 ppm (Brewerton and Slade
    1964).
    Four applications of 1.25 Ibs/A mirex bait, equalling 1.7 g/A (0.04
    kg/ha) of the active ingredient, resulted in residues of 0.65 ppm in
    catfish after six months, apparently due to uptake during normal feed-
    ing rather than by direct ingestion of the bait (Collins et al. 1973).
    In a survey of woodcocks (Phitohela minor) in. southern states, residues
    of mirex were found in four of ten birds fron Mississippi, one of which
    contained 26.7 ppm.  In Louisiana one of ten birds contained mirex as
    did one of five from Maryland; two of five from Alabama, and two of five
    from Tennessee (Clark and McLane 1974).
                                       302
    

    -------
    While these data are sparse, it is apparent that mirex and chlordecone,
    like all the chlorinated hydrocarbon insecticides examined, are trans-
    ported into all phases of the environment.  No data are available for
    chlordecone in the aquatic-terrestrial model ecosystem, but mirex was
    among the least degradable compounds tested, with over 97 percent of
    the extractable radioactivity in the organisms (snail, mosquitos, algae,
    and fish) being undegraded mirex.  Data were also cited on the presence
    of mirex in fish from Lake Ontario and of up to 20 ppm in wild rodents
    (Metcalf and Sanborn 1975).
    Persistence-
    No estimates of the persistence of mirex or chlordecone in soil, and
    no description of their probable fate in soil, were available.  The
    absolute lack of data on their degradation by microorganisms suggests
    that mirex and chlordecone may exceed even dieldrin in environmental
    stability.
    Effects on Non-Target Species-
    Microorganisms—The effects of chlordecone on microorganisms and soil
    processes in Egyptian soils were not considered severe.  Levels of ten
    kg/ha did not significantly depress fungi at any time, and even in-
    creased their numbers after 45 days; bacterial levels increased for no
    more than 30 days.  Treatment with 22 kg/ha led to inhibition of vir-
    tually all soil processes at some time during the two month observation
    period; actinomycetes were also inhibited (Gawaad et_ al_. 1972a, 1972b,
    1973a, 1973b).  These data are summarized in Table 51, as are the even
    more sparse data for mirex.
    Invertebrates—Use of mirex in baits against imported fire ants did not
    harm bee colonies near or within treated areas (Glancey et al. 1970) .
    The LC   of mirex for red crayfish (PpocccnibaTus claf'ki') was greater
    than 0.1 ppm (Muncy and Oliver 1963).  Mortality from water levels of
    one ppm was delayed, but ingestion of one or two grains of bait caused
                                      303
    

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    55.5 percent and 100 percent mortality, respectively, within four days
    (Ludke et^ a]^. 1971).  If bait was present in the water but inaccessible,
    crayfish accumulated 1.45 ppm  (Ludke et^ a^. op. oit.).  Nonetheless,
    Markin et al. (1972) concluded that the fire ant program posed no haz-
    ards to the Louisiana crayfish industry.  No data were available for
    chlordecone.
    Fish and amphibians—Mirex at five ppm, but not at one or three ppm,
    significantly reduced the growth of bluegills, Lepomis macroo'hirus
    (Pimentel et al. 1971).  No mortality and no malformations were obser-
    ved in caged channel catfish exposed to 1.7 g/A (0.04 kg/ha) of mirex
    which had been applied as bait at 1.25 Ib/A (Collins et^ al_. 1973).
    Chlordecone inhibited oxygen uptake by bluegill liver mitochondria in
    vitro (Hiltibran 1974) and inhibited ATPase activity in channel cat-
    fish (Desaiah and Koch 1973).
    Birds—The acute oral LD   of mirex in mallards was greater than  2,400
    mg/kg (Tucker and Crabtree 1970).  The LC5Q for pheasants was  1,400  to
    1600 ppm; for coturnix quail, over 10,000 ppm, when birds were fed
    treated feed for five days followed by clean feed for three days (Pim-
    entel 1971).  Feeding 440 ppm chlordecone was lethal to adult male
    quail within seven to 15 days  (McFarland and Lacy 1969).  The toxicity
    of mirex to immature quail, but not to adult quail, increased if the
    photoperiod was shortened (Eroschenko and Wilson 1974).  Also in quail,
    chlordecone induced fatty liver degeneration (Atwal 1973), increased
    the weight of the adrenal glands, and exerted an estrogenic effect, on
    both sexes (Eroschenko and Wilson 1974, McFarland and Lacy 1969, Fos-
    ter 1974) .  Chlordecone also increased the thickness of eggshells path-
    ologically in wild birds (Erben 1972) and was teratogenic in pheasants
    and quail (Foster 1974).  Mirex at 500 ppm was not estrogenic in quail,
    pheasants, mallards, or chickens (Foster 1974).
    Mammals—The acute oral LDrn °f mirex to female rats was 365 mg/kg,
    with 95 percent confidence limits of 281 to 475 mg/kg (Gaines and Kim-
                                       305
    

    -------
    brough 1970).   The acute oral LD   of chlordecone for rats was 114 to
    140 mg/kg (Jones et_ al_. 1968); Gaines (1969) cited 125 mg/kg, with 95
    percent confidence limits of 115 to 136 mg/kg.  Mirex was far more tox-
    ic as a five percent solution in corn oil than as a 20 percent corn
    oil suspension (Gaines 1969).
    A chronic intake of five ppm mirex increased parental mortality and de-
    creased litter size in inbred Balb/c mice; in CFW mice, parental mor-
    tality was not increased, but litter size decreased (Good e_t a\^. 1965,
    Ware and Good 1967).  When Balb/c mice were fed ten ppm chlordecone,
    litter size as well as the number of litters produced decreased and
    at 40 ppm, females produced no litters.  Reproduction resumed seven
    weeks after chlordecone was removed from the diet, but the first sub-
    sequent litters were small, even if treated males were mated with un-
    treated females; if treated females were mated to untreated males, the
    second litters were also small (Huber 1965).  Mirex reduced litter size
    in rats at 25 ppm but not at five ppm.  Mortality of pups born to and
    nursing on treated dams was higher than if pups nursed on untreated fe-
    males (Gaines and Kimbrough 1970).  Neither mirex nor chlordecone has
    been proved teratogenic in mammals (Nishimura 1973) but mirex caused
    cataracts in pups born to and nursing on females fed 25 ppm (Gaines and
    Kimbrough 1970).
                                      306
    

    -------
    Chlordane
    Chlordane is the common name for 1,2 ,4,5,6,7,8,8-octachloro-2,3,3a,4,7,
    7a-hexahydro-4,7-methanoindene, introduced as a non-systemic contact
    insecticide by the Velsicol Corporation in 1945 as Octachlor.  Two iso-
    mers of chlordane have been isolated:  alpha-chlordane, the endo-O'is
    isomer, and beta-chlordane, the endo-trans isomer.  The aZp/za-isomer is
    more readily dehydrochlorinated and is the chief constituent of the com-
    mercial product called ^omma-chlordane.  The melting point of both the
    alpha and the beta isomers is between 103 and 105 C.
    Chlordane is manufactured by chlorinating cyclopentadiene to give hexa-
    chlorocyclopentadiene and condensing the latter with cyclopentadiene to
    produce chlordene.  Chlordene is further chlorinated to chlordane.
    Chlordane is formulated as 50 and 70 percent emulsifiable concentrates,
    two and 20 percent kerosene solutions, or five and ten percent dusts and
    granules.  A high purity chlordane, consisting of 95 percent alpha and
    beta chlordane, is marketed under the name HCS 3260.  It has a water
    solubility of 56 ppb.
    Technical chlordane is a viscous amber liquid (75 to 120 centistokes at
    130 F) which is almost insoluble in water but soluble in most organic
    solvents including petroleum oils.  The refined product has a vapor
    pressure of 1 x 10   mm mercury at 25 C.  Technical chlordane consists
    of 60 to 75 percent isomers of chlordane and 25 to 40 percent of re-
    lated compounds, including two heptachlor isomers.
    Heptachlor is the common name for 1,4,5,6,7,8,8-heptachloro-3a,4,7,7a-$
    tetrahydro-4,7-methanoindene.  It was initially isolated from technical
    chlordane and was introduced as an insecticide by Velsicol in 1948 as
    Heptagran, a non-systemic stomach and contact insecticide with some
    fumigant action.  It is a white crystalline solid with a mild camphor
    odor, which has a water solubility of 56 ppb and a vapor pressure of
                                      307
    

    -------
    3 x 10  mm mercury at 25°C, and a melting point of 95° to 96°C.  The
    technical product, consisting of approximately 72 percent heptachlor
    and 28 percent related products, is a soft waxy solid which melts be-
    tween 46 and 74 C and has a viscosity of 50 to 75 centipoises at 90°C.
    It is stable to light, air, moisture, and moderate heat, but susceptible
    to epoxidation.  Heptachlor is formulated as an emulsifiable concen-
    trate, a wettable powder, a dust, and a granule.  It is synthesized by
    the action of sulfuryl chloride in chlordene in the presence of benzoyl
    peroxide, or by the chlorination of chlordene in the dark in the pre-
    sence of fullers' earth (Martin 1968).
    Degradation-
    Biological—The few data on microbial degradation of heptachlor and
    chlordane are shown in Table 52.  The degradation pathways of chlordane
    and heptachlor are shown in Figures 11 and 12, respectively.  In one
                                 14
    study (Bourquin et al. 1972)   C00 was recovered from ring-labeled
                    *~|(" ~ T             2.
    heptachlor and labeling in the cells suggested that additional degra-
    dation to CCL was masked by incorporation into cellular products.
    Bourquin and co-workers considered the C-8 of the cyclohexane moiety
    to be the site of ring cleavage.  The most likely compound to be so
    cleaved was 1-hydroxychlordene, but other substrates were not ruled
    out.  Chlordene, heptachlor epoxide, and l-hydroxy-2,3-epoxychlordene
    were also recovered.  Castro and Yoshida (1971) reported the total de-
    gradation of heptachlor, without formation of heptachlor epoxide, in
    two months in flooded soils in the laboratory, but no products were
    identified.  Chlordane was metabolized little, if at all, in either
    flooded or upland soils (Castro and Yoshida 1971).  Heptachlor was re-
    ported to degrade slowly but steadily in a sewage lagoon but no meta-
    bolite characterization was reported (Halvorson ejt al. 1971).
    Heptachlor was epoxidized by 35 of 47 species of fungi and by 26 of 45
    species of bacteria and actinomycetes.  Heptachlor was metabolized to
    chlordene, chlordene epoxide and l-hydroxy-2,3-epoxychlordene via !•£
    hydroxychlordene (Miles et_ aJU 1969).  In sandy loam, the conversion of
                                      308
    

    -------
    1-HYDROXYCHLORDANE
                            CL,
                            OXYCHLORDANE    L2-DICHLOROCHLOPDENE
                                    PHOTOCHLORDANE
            1-HYDROXYCHU)RDENE   l-HYDROXY-Z^EPOXY
                                       CHLORDENE
    PRODUCTS OF CHLORDANE AND CHLORDENE (AFTER MENZIE, 1974)
                               Figure 11
                                      309
    

    -------
             ci_6,
            PHOTOHEPTACHLOR    PHOTOHEPTACHLDR "EPOXIDE"
    HEPTACHLOR
      HEPTACHLOR EPOXIDE
          "DIOL1
    CHLORDENE
    1-HYDROXYCHLORDENE
                                  CL
    l-HYDROXY-2, 3-EPOXY
      / CHLORDENE
         CHLORDENE EPOXIDE
              "KETO" CHLORDANE
                      PRODUCTS OF HEPTACHLOR
                       (AFTER MENZIE, 1974)
                           Figure 12
                                310
    

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    heptachlor epoxide to the less toxic 1-exohydroxychlordene was only one
    percent completed in 12 weeks (Miles et^ al^ 1971).
    On cabbage leaves, heptachlor was epoxidized with subsequent formation
    of other metabolites which included hydroxychlordene and prillic acid.
    Methoxychlordane and hydroxydihydroheptachlor were found in the soil
    (Weisgerber et al. 1974).  Kaul et_ al_. (1972) identified the major met-
    abolite of trans-chlordane on cabbage as 2,4,5,6,7,8,8-heptachloroC
    2,3,3a,4,7,7a-hexahydro-4,7-methano-lH-inden-lol ten weeks after appli-
    cation of chlordane.  Peanuts grown on soil treated with heptachlor
    contained heptachlor epoxide (Morgan et_ a^. 1967).  The green alga,
    Chlorella pyvenoidosa3 metabolized heptachlor to heptachlor epoxide and
    4,5,6,7,8,8-hexachloro-2,o-epoxy-4,7-methano-3a,4,7,7a-tetrahydroindan£^
    1-one with heptachlor epoxide representing 68 percent of the algal as-
    sociated radioactivity (Eisner et^ al. 1972).
    Heptachlor is metabolized to heptachlor epoxide in rats, dogs, rabbits
    (Brooks 1969), and cows (Davidow eit al_. 1953, Gannon and Decker 1960).
    Mizyukova and Kurchatov (1970) injected rats intraperitoneally with
    120 mg/kg of heptachlor, and noted that heptachlor was present in liver,
    fat, and blood in one hour and heptachlor epoxide was present in the
                                                   14
    same tissues within four hours.  When 25 yg of   C-heptachlor were in-
    jected intravenously, most of the radioactivity was excreted in the
    feces, partly as heptachlor epoxide and partly as an unidentified uri-
    nary compound which, in rabbits, was tentatively identified as hydroxy-
    chlordene epoxide (Brooks 1969).  Female rats epoxidized heptachlor
    more slowly than did males, and were able to accumulate more heptachlor
    epoxide with less toxicity than were males (Radomski and Davidow 1953).
    When Z?e£a-hydroxyheptachlor was injected intravenously into rats, 36
    percent of the radioactivity was excreted within 48 hours  (Korte et al.
    1970).
    Barnett and Dorough (1974) analyzed chlordane metabolism in rats.  When
    a single oral dose of radioactive chlordane was given, more than 90 per-
                                      312
    

    -------
    cent was eliminated within one week.  C'is-chlordane was eliminated some-
    what more quickly than trans-chlordane (70 versus 60 percent in 24 hours)
    Of the total radioactivity eliminated in the first 24 hours, 15 percent
    was eliminated as unmetabolized chlordane, primarily in the feces.  If
    chronic levels of one, five, or 25 ppm were fed, fat storage after 56
    days was equal to three times the dietary intake, and oxychlordane was
    the major and most persistent tissue residue.  Oxychlordane was elimi-
    nated in the feces if fed directly, but was not found as a fecal meta-
    bolite of either eis- or tmns-chlordane.  The excretion of chlordane
    decreased when feeding ended.
    Photolytic-
    Numerous photoproducts of heptachlor and chlordane have been identified
    (Ivie et_ a^. 1972, Knox at al^. 1973, Parlar and Korte 1973, Onuska and
    Comba 1975, Gaeb et_ al_. 1975).  Oxychlordane, an oxidative product of
    chlordane, was shown to isomerize in the presence of xanthene photosen-
    sitizers to form a keto-product of considerable murine toxicity, and an
    epoxy-intact isomer of low toxicity (Ivie 1973).  At wave lengths of
    254 nm deposits of solid cyclodienes formed bridged photoisomers (Fisch-
    ler and Korte 1969) while trans-chlordane and nonachlor, both consti-
    tuents of technical chlordane, formed bridged isomers mostly at wave-
    lengths greater than 300 nm  (Vollner et al. 1971).  Some dechlorination
    also occurred for chlordane at wavelengths of more than 300 nm.  In
    direct sunlight, chlordane dissipated faster than either DDT or diel-
    drin with decomposition presumed but not established (Ginsburg 1953).
    Decomposition of volatilized cyclodienes is given support both by the
    numbers of photoproducts found (see above) and by the data of Stanly
    et al. (1971), who found neither heptachlor epoxide nor chlordane in
    any of 880 composite atmospheric samples.
    Chemical and physical—Vollner and Korte (1974) reported 70 percent de-
    composition of c^s-chlordane by 54 Mrad of   Co gamma-±rrad±at±on when
    five to ten mg/ml of chlordane were dissolved in hexane, and 0.29 Mrad
                                        313
    

    -------
    were delivered per hour.  When dissolved in hexane at 0.2 ppm, heptachlor
    was degraded by 0.5 to 2.5 Mrads of   Co ^otfraz-radiation or by 20 Mrads
    of beta-radiation, but no metabolites were identified (Ceurvels et al.
    1974).
    Chemically, heptachlor dissolved in butanol was degraded to hydroxychlor-
    dene by 16 Kbar pressure at 110 C in the presence of sodium hydroxide.
    The reaction was 60 percent complete is six hours (Roemer-Maehler et al.
    1973).  Kaneda and co-workers (1974) reported degradation of heptachlor
    by aqueous saturated solutions of calcium hypochlorite.   The only meta-
    bolite identified was 1-hydroxychlordene, but further degradation oc-
    curred.  Heptachlor was 80 percent destroyed by five hours exposure to
    KMnO,, but not by exposure to chlorine gas or alkali (Leigh 1969).
    When river water was contaminated with heptachlor, heptachlor epoxide,
    alpha chlordane and gamma chlordane, only heptachlor epoxide remained
    unaffected after eight weeks.  Eighty-five percent of the chlordane re-
    mained, and no conversion products were identified.   Heptachlor was con-
    verted to 1-hydroxychlordene and heptachlor epoxide, with an equilibrium
    ratio of 2:3 achieved in four weeks (Eichelberger and Lichtenberg 1971).
    The authors considered chemical rather than biological degradation to
    have effected the changes, but the water was not sterile so that it is
    impossible to rule out biological degradation.  During storage, three
    percent of a heptachlor dust formulation decomposed in 42 months with
    no product characterization reported (Raman and Krishnamoorthy 1973).
    Transport-
    Within soil—Heptachlor applied to soil at one, two or three Ibs/A
    (1.12, 2.24 or 3.36 kg/ha) was found mostly (90 percent) in the top
    three inches of soil after one year and after three years over 70 per-
    cent of the recovered residues were still found in the top three inches
    of soil (Lichtenstein et_ al. 1962b).  When heptachlor was applied at
    five Ibs/A (5.60 kg/ha) for five years, or once at 25 Ibs/A (28.0 kg/ha),
    residues decreased by 76 to 82 percent if the soil was cultivated.  Of
                                       314
    

    -------
    the residues recovered,  26  percent  were  in the  top two in.,  52 percent
    were between two and  four inches, and  6.5  percent  were in the six to
    nine inch la>er of  soil  (Lichtenstein  et_ al_.  I971b) .   Residues of hep-
    tachlor in a sloping  field  decreased most  at  high  points, and buildup
    at low points followed plow line, suggesting  washoff  rather  than leach-
    ing as the mechanism  of  transport  (Peach e_t al.  1973).  High levels of
    organic matter in the soil  decreased degradation,  leaching,  and vola-
    tilization of heptachlor  (Bowman e_t_ al_.  1965).   When  applied as a ter-
    r?i:" ,iJe, heptachlor  exhibited  little  lateral or vertical movement af-
    ter 15 ye.-ir-  'ctewart anc Chisholm  1971) or 21  years  (Bennett _et_ a_l.
    1974).  After I'.M*"  rnentns during the growing  season,  heptachlor which
    had been disked /.., cm into the so'l was found  to  have migrated to a
    depth of 30 cm, a-.thougn 68 percent of the residue had remained i-n s-Ltu
    (Caro 1971).  CheKal  and Yurovska/r  (1967)  concluded  that hepcachlor
    had a mobility of 21  cm  per growing season and  was therefore a poten-
    tial contaminant of water supplies.  Granular heptachlor was more mo-
    bile in soil than diazinon,  parathion  or phorate but  mobility depended
    on the type of soil and  level of insecticide  used,  since bioassays were
    used (Burkhardt and Fairchild 1967),
    Between soil and water—In  a newJy  developed  Great Plains irrigation
    district, when heptachlor was applied  in such a way that soil residues
    of the epoxide 1.5  to 2.5 months later were 0,16 to 1."^ r»-"n, reservoir
    water was found to  contain  one  ppt  of  heptachlur and  0.006 ppb of its
    epoxide (Knutson e_t_ al_.  1971b).  In West Virginia,  35 ponds  examined
    were all contaminated with  heptachlor.  Water levels  ranged  from less
    than one ppb to 291 ppb and levels  in  mud  ranged from less than one ppb
    to 59.9 ppb which were in all cases lower  than  soil levels in the sur-
    rounding watershed.  Detectible residues persisted for 25 months.   The
    uneven distribution of residues in  the different ponds was found to be
    correlated with distance from treated  areas rather than with types of
    soil (Weatherholtz  et_ _al_. 1967) .  Among  the mechanisms for removal of
    heptachlor and chlordane from water into sediment  are bacterial floes
                                      315
    

    -------
    (Speidel et al. 1972) and adsorption by suspended particles  (Weil et_
    al. 1972).
    Volatilization—Both heptachlor and chlordane have a higher vapor pres-
    sure than DDT and are correspondingly more volatile on inert surfaces.
    In the absence of wind, rain, or direct sunlight, heptachlor toxicity
    was reduced by 41.9 percent in 24 hours (Mistric. and Gaines 1953).
    Over a treated field, 3.9 percent of the applied heptachlor accumulated
    on fiberglass filters (Caro et^ a^. 1971).  Conversely, dissipation of
    heptachlor and chlordane from alfalfa was 95 percent complete in three
    weeks, with 60 percent (0.6 ppm from two Ibs/A) present in the soil
    (Dorough et_ al. 1972).
    Bidleman and Olney (1974) concluded that most chlorinated hydrocarbons
    are airborne as vapor rather than adsorbed to particles.  They recorded
                                 2
    chlordane levels of 0.25 ng/m  over Providence, Rhode Island.  Over
    Oahu (Hawaii), rainwater contained 1-3 ppt chlordane (Bevenue et al.
    1972).  The purified chlordane, Velsicol HCS-3260, was less volatile
    than technical chlordane and was highly persistent in soil (Harris 1973).
    Into organisms—It has long been known that cows fed heptachlor excreted
    heptachlor epoxide in their milk (Davidow et^ al. 1953, Bruce et_ al_. 1966,
    Dorough and Hemken 1973).  Hogs foraging on corn stover in fields pre-
    viously treated with heptachlor accumulated heptachlor epoxide in their
    fat (Dobson et al. 1972) and chickens fed 10-15 ppm of chlordane for
    five days accumulated 10-13.3 ppm in their fat  (McCaskey et^ al_. 1968).
    Indirect contamination of mammals has been observed in the arctic, where
    polar bears, seals, porpoises, and foxes all contained measurable resi-
    dues of heptachlor epoxide.  Arctic sheep were  free from residues of
    heptachlor epoxide (Clausen et^ al^. 1974).
    Hannon e_t al. (1970) observed a higher ratio of heptachlor to hepta-
    chlor epoxide at higher trophic levels in Lake  Poinsett, South Dakata;
    Gish (1970) found gamma-chlordane residues in most heptachlor-treated
    soils.  Both studies noted increasing levels of organochlorine contami-
                                       316
    

    -------
    nation  (including DDT and several cyclodienes) at higher trophic levels.
    Gish considered the organochlorine content of some earthworms  (13.8 ppm)
    to be high enough to cause acute poisoning in birds.   In Louisiana,
    spraying of heptachlor between 1956 and 1962 against fire ants resul-
    ted in woodcocks contaminated with 2.4 ppm heptachlor  epoxide in 1962,
    but only 0.42 ppm in 1965 (McLane £t_ al^. 1971).
    The uptake of heptachlor by plants has been reported frequently  (King
    e£ al. 1966, Waldron e* al. 1968, Lichtenstein and Schulz 1965, Bruce
    and Decker 1966).  In potato fields, soil applications of 1.25 to 2.5
    kg/ha of heptachlor resulted in tuber residues which exceeded the per-
    missible levels for three years; the structurally similar insecticides
    aldrin and dieldrin were also taken up (Polizu et al.  1972).  Applica-
    tions of one or two kg/ha heptachlor at planting resulted in residues
    of 0.04 mg/kg in potato skin and 0.01 mg/kg in their pulp (Sazonov and
    Chikhacheva 1972).
          ®
    Popov and Donev (1970) reported heptachlor uptake into wheat, beans,
    sugar beets, and oat vetch; Catnoni et^ al^. (1971) found residues of 0.03
    ppm heptachlor and 0.005 ppm heptachlor epoxide in beet roots when soil
    levels were 0.017 ppm and 0.024 ppm, respectively (Van Steyvoort 1968).
    In soybeans, heptachlor residues were concentrated somewhat over soil
    levels  (Beall and Nash 1969).  Soybeans planted 15 years after the ap-
    plication of heptachlor still contained detectible residues of hepta-
    chlor epoxide (Nash and Harris 1973).  Heptachlor is taken up by corn
    plants less readily than either aldrin or dieldrin, but is translocated
    more readily within the plant (Polizu e_t^ al. 1971) .
    The heptachlor residues of corn, oats, soybeans, and peanuts were cor-
    related with their fat content (Bruce et^ al. 1966) .  Applications of
    two to four Ibs/A (2.24 to 4.48 kg/ha) of chlordane to corn fields at
    planting resulted in no detectible residues (< 0.008 ppm) in corn or
    cobs, and only traces in stalks, at harvest.  Silage plants harvested
    102 days after planting contained 0.03 to 0.04 ppm of  chlordane  (Dorough
                                       317
    

    -------
    and Pass 1972).
    In a sandy Nova Scotia loam soil, chlordane was taken up into parsnips,
    beets, carrots, potatoes, and rutabagas with carrots containing the
    highest residues (0.26 ppm).  At harvest, 16 months after chlordane
    treatment, potatoes were found to contair 0.15 ppm, parsnips 0.12 ppm,
    carrots 0.07 ppm, and rutabagas and beetf*, 0.01 ppm chlordane residues.
    The composition of the plant-absorbed residues; was similar to the com-
    position of the applied chlordane (Stewart 19"75) .  The high purity chlor-
    dane, Velsicol HCS-3260, was taken up by plants in the order:  radish
    > potatoes > carrots > beans.  In alfalfa, the residues consisted of
    alpha- and gamma chlordane, photo-aZpTw-ehlordane, and oxychlordane
    (Wilson and Oloffs 1974).
    A 61-81 percent reduction in crop residues of heptachlor, heptachlor
    epoxide, and. chlordane resulted from the application of carbon at the
    rate of 2,000 ppm to contaminated soil.  The protective effect lasted
    at least four seasons (Lichtenstein et^ a^. 1968, 1971c) .  Increasing
    the interval between treating and planting fields decreased plant up-
    take of organochlorine insecticides, which included chlordane and hep-
    tachlor.  Soil differences also affected plant uptake (Koula 1970).
    When the fate of heptachlor was investigated in a terrestrial-aquatic
    model ecosystem, it was found that heptachlor behaved somewhat like al-
    drin (q.v.)» being readily converted to its epoxide.  Once formed, hep-
    tachlor epoxide was approximately as stable as dieldrin (q.v.).  An
    additional degradative pathway was the conversion of heptachlor to !-£
    hydroxychlordene, mostly by chemical hydrolysis, resulting in a signi-
    ficant reduction of toxicity and an increase in water solubility.  The
    authors considered heptachlor epoxide to be highly bioaccuinulative, but
    1-hydroxychlordene and its epoxide were considered not to be truly bio-
    accumulative.  Heptachlor was not converted to chlordene under the con-
    ditions of the model ecosystem (Lu ej^ aj^. 1975).
                                       318
    

    -------
    When the fate of HCS chlordane was investigated in a model terrestrial-
                                         14
    aquatic ecosystem, algae accumulated   C-chlordane 98,386-fold over the
    concentration found in the water.  Magnification by snail, mosquito,
    and fish was 132,613-fold, 6,132-fold, and 8,258-fold greater than the
                    14
    water levels of   C-chlordane (Sanborn et al. 1976).  While not showing
    increased uptake of chlordane with increasing trophic level, these data
    demonstrate the extreme affinity of chlordane for lipid and the insuf-
    ficiency of water levels of chlordane as a measure of chlordane con-
    tamination.
    Persistence-
    Data on the persistence of chlordane and heptachlor in soils under var-
    ious conditions are summarized in Tables 53 and 54.  In Table 54, hep-
    tachlor residues include or are identical with heptachlor epoxide resi-
    dues.
    Wingo (1966) argued that accumulation of high concentrations of hepta-
    chlor in soil was unlikely at normal agricultural levels, but his data
    showed that persistence increased with level of application.  Figure 13
    (after Hermanson et al. 1971), shows the effect of repeated applications
    of chlordane to soil.  Baluja-Marcos and Serrano-Gonzalvez (1970) esti-
    mated the time required for elimination of both heptachlor and chlordane
    from Spanish agricultural soils to be between three and five years
    which compares well with the data of Hermanson et al. (1971) who esti-
    mated the so-called persistence-half-life for both compounds to be four
    years.  No change was observed in the levels of heptachlor or untreated
    soil, autoclaved soil, or either of these ammended with five ppm of
    urea, in 11 months following application of heptachlor (Kiigemagi et al.
    1958).  Chlordane was not noticeably degraded under aerobic or anaerobic
    conditions in various Phillipine soils (Castro and Yoshida 1971).  Chlor-
    dane and heptachlor retained their termiticidal capacity for up to 21
    years, but residue levels were not given (Johnston et^ al^. 1971).  When
    heptachlor was applied at ten Ibs/A/yr (11.2 kg/ha) for three years the
                                       319
    

    -------
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                       YEARS
    
    VARIATIONS IN THE TOTAL ORGANICALLY BOUND
    CHLORIDE CONTENT OF SOIL SAMPLES, EX-
    PRESSED AS PERSISTENCE CURVES
    
         (HERMANSON EL AL. 1971)
                     Figure 13
                        322
    

    -------
    residues decreased to two ppm heptachlor, 0.8 ppm heptachlor epoxide,
    and 2.1 ppm gamma-chlordane six years after the first application from
    a total application of 15 ppm (Stewart and Chisholm 1965) .
    The insect toxicity of chlordane applied to soil at ten to 15 Ibs/A
    (11.2 to 16.8 kg/ha) was undiminished after three years (Wolcott 1954).
    Harris (1964a, 1964b, 1967, 1972b) and Harris and Sans (1972) found that
    the toxicity of chlordane and heptachlor was affected by  soil type and
    soil moisture.  The biological activity of heptachlor was in some cases
    correlated more closely with the organic content of the soil than with
    the concentrations of pesticide.  Field-moist soil (12.1  percent mois-
    ture) increased the insecticidal activity of heptachlor more than 12-
    fold over oven-dried soil (1964b).  Heptachlor epoxide was more toxic
    in moist soil due to fumigant action, and more persistent in mineral
    soil than heptachlor itself (Harris and Sans 1972).  Carbon amendment
    of soil prevented the extraction of heptachlor from sandy or loamy soil
    and decreased its toxicity.  Binding of heptachlor to carbon increased
    with time, and was more striking under laboratory conditions than in
    the field (Lichtenstein et^ a^. 1968).  Heptachlor also adsorbed to
    clays, both on surfaces and into the intralamellar spaces of montmoril-
    lonite (Ju-Chang and Liao 1970).  Sorption onto kaolinite or montmoril-
    lonite in water was slow and required one month to reach  equilibrium
    (Weil e± al. 1972).
    In discussing the persistence of chlordane and heptachlor, it is neces-
    sary to include their conversion products.  Few data are  available on
    the products of chlordane in soils, but the longer persistence and high
    insecticidal activity of heptachlor epoxide has been known for years
    (Gannon and Bigger 1958).  In Queensland soils, the conversion of hep-
    tachlor to its epoxide is essentially completed within 43 months (Stick-
    ley 1972).  Chopra (1966) found that heptachlor epoxide was not formed
    in sandy loam, but was formed in silt loam.  Carter and Stringer (1970)
    found that up to 60 percent of the heptachlor residues in an Oregon
                                      323
    

    -------
    loamy fine sand consisted of 1-hydroxychlordene, and heptachlor epoxide
    formed only a small part of the residues in most soils.  Further analy-
    sis of the heptachlor residues in Oregon soils identified the major
    residues of technical heptachlor as:  heptachlor, 1-hydroxychlordene,
    ^OTwna-chlordane and aZp/za-chlordane, nonachlor, and heptachlor epoxide.
    One to two years later, 1-hydroxychlordene had essentially been replaced
    by its epoxide, l-hydroxy-2,3-epoxychlordene with soil type affecting
    the relative levels of the various residues (Carter et al. 1971).
    Lichtenstein et_ al. (1970) pointed out that applications of 25 Ibs/A
    (28.0 kg/ha) of technical heptachlor included 6.25 to 7.5 Ibs of garrma-
    chlordane and 1.0-2.5 Ibs of nonachlor.  Ten years later, relatively
    more ^omwa-chlordane than heptachlor/heptachlor epoxide remained in the
    soil and residues were claimed to be eight percent of the total techni-
    cal heptachlor, but no reference was made to hydroxychlordene or its
    epoxide.  These data make it apparent that residues are defined in dif-
    ferent ways, adding to the variability imposed by soil, temperature and
    other climatic variables.
    The persistence of heptachlor and chlordane can be gauged, if only in-
    directly, by the observations that in Ontario all tested soil which had
    histories of heptachlor administration contained gamma-chlordane (Harris
    et^ al_. 1966); of 20 fields in northern Saskatchewan, ten contained hep-
    tachlor/heptachlor epoxide residues (Soho et al. 1968) .  In a later
    study, 17 of 41 soils contained chlordane, and 24 of 41 contained hep-
    tachlor or its epoxide, even though samples were not selected by their
    history of pesticide contamination (Saha and Sumner 1971).  Yule, Chiba
    and Morley (1967) observed no decomposition of soil-incorporated hepta-
    chlor in 11 months.
    Effects on Non-Target Species-
    Microorganisms—Richardson and Miller (1960) observed that chlordane
    and heptachlor inhibited mycelial growth in culture.  In flask culture,
    chlordane and heptachlor inhibited nitrification (Winely and San Clemente
                                        324
    

    -------
    1970).  As shown in Tables 55, 56 and 57, however, neither chlordane nor
    heptachlor is excessively destructive of the overall fungal and bac-
    terial populations of soils.
    Heptachlor, but not chlordane, enhanced ammonification in soil (Peri
    1952, Jones 1956, Gordienko 1964).  Both heptachlor and chlordane pro-
    bably enhance nitrification at least temporarily, even though Peri
    (1952) found no significant effects on the numbers of nitrifying bac-
    teria when chlordane was applied at agricultural levels.  Heptachlor
    had no effect on ammonifying bacteria in alluvial meadow soil (Rankov
    and Khristova 1971) , but did inhibit nitrifying bacteria in pot culture
    (Gawaad .et^ al^. 1973).  Preplanting applications of 0.6 kg/ha in the
    row, or 0.5 kg/ha seed treatment with heptachlor, reportedly increased
    the numbers of azotabacteria and fungi during the growing season (Kha-
    lidov et_ al. 1968).
    Gordienko (1964) suggested that the observed stimulatory effects of
    heptachlor on available nitrate were due to death and decomposition of
    microorganisms.  This hypothesis is supported by Shamiyeh and Johnson
    (1973) who found that 100 ing/liter (100 ppm) of heptachlor inhibited
    89 percent of bacterial cultures, 81 percent of actinomycetes, and 50
    percent of fungal cultures on agar.  Contamination of agar with 25 mg/
    liter (25 ppm) of heptachlor killed 63 percent of bacteria transferred
    onto the plates.  Bacterial resistance could be selected for at these
    levels.  Shamiyeh and Johnson further determined that, in soil, total
    numbers of bacteria increased, with the greatest increase occurring
    six to nine months after the application of 55 kg/ha.  Total numbers of
    fungi showed an initial decrease.  Chlordane was toxic to several path-
    ogenic soil fungi in the laboratory, and sufficiently toxic to Oph-io~
    bolus (Take-all, on wheat) to be of significance under field conditions.
    Pythiwn, on the other hand, was stimulated by chlordane (Grossman and
    Steckhan 1960).
                                       325
    

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    These data, and the species examined for chlordane susceptibility by
    Trudgill et_ al. (1971) as listed in Table 55 argue that heptachlor and
    chlordane are toxic to some but not all microorganisms, so that major
    changes in the composition of soil microbial populations must be ex-
    pected in the presence of these compounds, even if overall numbers of
    microorganisms remain constant.
    Plants—Stitt and Evanson (1949) reported that: 34.8 Ibs/A (38.9 kg/ha)
    of chlordane adversely affected cucumbers, bush beans, and turnips.
    Boswell (1955) noted that phytotoxicity was more likely in poor soils
    than rich, presumably because the latter have greater adsorptive capa-
    city.  In quartz sand chosen for its lack of adsorptive capacity, chlor-
    dane significantly reduced the growth of corn roots, but not: of pea
    roots while heptachlor increased root growth of both corn and pea roots,
    the latter significantly (Lichtenstein et^ al. 1962).  Shaw and Robinson
    (1960) found that 200 Ibs/A of chlordane (224 kg/ha) or 120 Ibs/A of
    heptachlor (134.4 kg/ha) were required to inhibit the growth of tomatos
    or sudan grass.
    These data suggest that, except under conditions of extreme soil pover-
    ty and gross contamination, neither heptachlor nor chlordane is likely
    to exert direct toxic effects on plants.  Even in the absence of pests,
    heptachlor reportedly increased yields of several crops (sugar beets,
    winter rye, spring wheat, barley, oats, potatoes) for two years after
    a single application.  The crop improvement was synergistic with min-
    eral fertilizers (Persin 1961).
    Invertebrates—The effects of heptachlor and chlordane on soil fauna
    were reviewed by Edwards and Thompson (1973) who concluded that chlor-
    dane and heptachlor drastically decrease the numbers of earthworms;
    considerably decrease the numbers of Co11embc1a> paurapods and soil
    mites.  They may also kill some terrestrial molluscs, but do not much
    affect springtails or symphelids.  Heptachlor was reported to decrease
    the numbers of Aoari-nae and increase the numbers of Collembola when
                                       330
    

    -------
    applied to a beet field at 0.6 kg/ha (Khalidov et^ al_. 1968).
    Freshwater invertebrates from areas contaminated by chlordane were more
    resistant to the pesticide than those from uncontaminated areas  (Naqvi
    and Ferguson 1968).  Chlordane at 0.01 ppm reduced shell growth and
    shell movement in oysters (Butler et al. 1960).
    Fish—The LC,.,. for various fish to chlordane ranged from 0.01 ppm in
    48 hours for rainbow trout to 0.082 ppm for goldfish after 96 hours
    (Pimentel 1971).  For heptachlor, the LC _ was 0.25 ppm after 24 hours,
    but 0.009 ppm after 96 hours in rainbow trout while goldfish had a 96
    hour LC5Q of 0.23 ppm (Pimentel 1971).
    In mummichogs (Fundulus heteroelitus) heptachlor toxicity was greater
    after 24 hours than after 96 hours, either as a result of bioaccumulation
    or because of the toxicity of heptachlor epoxide (Eisler 1970a).  Never-
    theless, heptachlor was among the least toxic organochlorines (Table
    36).  Khan and co-workers (1973) determined the relative toxicities of
    chlordane and heptachlor in fish to be less than those of chlordane and
    photoheptachlor, respectively.
    Amphibians—Heptachlor, but not chlordane, was toxic to toads (Bufo
    boreas) and frogs (Saaphiopus hammondii) at 0.1 to 0.5 Ibs/A (0.11 to
    0.56 kg/ha) (Mulla 1962).  The 24 hour LC5Q of heptachlor for Fowler's
    toad was 0.85 ppm (Pimentel 1971).
    Birds—Tucker and Crabtree (1970) listed the acute oral LD Q of chlor-
    dane and heptachlor to mallards as 1,200 mg/kg and more than 2,000 mg/
    kg, respectively.  Coturnix quail which were fed 0.05 to 0.1 mg hepta-
    chlor per day for 18 to 32 days produced normal numbers of eggs of the
    normal weight.  Prehatching mortality among the chicks was also normal,
    but deaths among newly-hatched chicks were higher for the first week
    after hatching.  Survivors xjere normal with respect to survival, age of
    sexual maturity, and fecundity.  Egg residues of heptachlor ranged from
    one to 17 ppm (Grolleau and Froux 1973).  When applied to fields at
                                       331
    

    -------
    agricultural levels, heptachlor has repeatedly been shown to reduce bird
    populations as reviewed by Pimentel (1971).
    When chlordane in acetone was injected into hens' eggs, no increase in
    mortality occurred at levels up to 500 ppm.  Heptachlor at 400 ppm and
    500 ppm killed 20 and 47 percent of the chick embryos, respectively
    (Dunachie and Fletcher 1969).  When 0.1 ml of one percent: heptachlor
    was injected into the yolk sacs of fertile hens' eggs before, incubation,
    the number of eggs which hatched was reduced to 65 percent of control
    levels (Mclaughlin et_ al. 1962).
    Mammals—Estimates for the acute oral LD,-,-. of chlordane in rats include
    283 mg/kg (Jones £t al. 1968) and 335 mg/kg in males, 430 mg/kg in fe-
    males (Gaines 1969) and 500 mg/kg (Spynu 1964, Martin 1968).  In mice,
    Spynu (1969) calculated the acute oral LD  _ to be 220 + 34 mg/kg.  Hep-
    tachlor was calculated to have an acute oral LD   of approximately 100
    mg/kg in rats (Martin 1968, Gaines 1969);  female rats were less sensi-
    tive, with an LD,.n of 162 mg/kg reported by Gaines.  Jones et al. (1968)
                    jU
    estimated the oral LD _ of heptachlor in rats to be 40 mg/kg, and the
    dermal LD ... to be between 200 and 250 mg/kg, as opposed to a dermal
    LD,.,, of more then 1,600 mg/kg for chlordane.  Spynu (1964) reported an
    acute oral LD n of 210 + 5 mg/kg for heptachlor in mice.  Heptachlor
                 jU
    and chlordane were in the minority of pesticides which were more toxic
    to male than to female rats (Gaines 1969) .
    Chlordane decreased the toxicity of subsequent parathion treatments,
    apparently by increasing the levels of serum aliesterases (Williams et
    al. 1967).  Chapman and Leibman (1971) pointed out, however, that
    whereas both DDT and chlordane stimulated  the metabolism of parathion
    to paraoxon and to diethylhydrogen phosphorothionate, only chlordane
    protected against parathion toxicity.  They concluded that factors
    other than enhanced metabolism must account for the chlordane-parathion
    interaction.
                                       332
    

    -------
    At levels of two to five mg/kg/day given intraperitoneally for 7 days,
    chlordane inhibited the uterogenic activity of estrone and decreased the
    uterine content of estrogen in rats and mice, and at 10-50 mg/kg/day,
    estrone metabolism was also decreased.  Chlordane also increased the
    levels of estradiol 178, testosterone, progesterone, and deoxycorticos-
    terone, while heptachlor increased estrone metabolism (Welch et^ al.
    1969, 1971).  The number of pregnant mice decreased when females were
    treated intraperitoneally with 25 mg/kg chlordane per week (Welch et_
    al. 1971) .  Mestitsova (1967) found that heptachlor resulted in decreased
    litter size within and between generations, a decrease in the survival
    of suckling rats, especially between 24 and 48 hours after birth, and
    cataracts in survivors.  No clinical toxicity was observed when hepta-
    chlor levels of six mg/kg were fed for 18 months.  In another study,
    Green (1970) found a decrease in the number of pups born when rats were
    fed heptachlor levels equal to the maximum food allowances although no
    increase in the number of abnormal pups was found.  In cell culture of
    human Chang-strain liver cells, chlordane inhibited the replication of
    both vaccinia and polio virus (Gabliks 1967).
    Terracini (1967) observed heptachlor to be weakly carcinogenic in rats,
    mice, and dogs.  In contrast, no effect of long-term feeding of hepta-
    chlor was found by Cabral and co-workers (1972) and a tumorstatic effect
    was claimed for chlordane when urethane was used as the carcinogen
    (Yamamoto et al. 1971) .  More recent studies demonstrated that mice fed
    25 or 50 ppm chlordane had significantly more carcinomas than control
    mice (Carter 1974, Train 1975).  Markaryan (1972) considered several
    organochlorines, including heptachlor, to be mutagenic with the levels
    of induced mutations lower than with alkylating agents or irradiation,
    and consisting mostly of chromatid aberrations.  The World Health Or-
    ganization characterized chlordane as carcinogenic in one species and
    heptachlor as uncertainly carcinogenic (Vettorazzi 1975).
                                       333
    

    -------
    In summary, these data demonstrate that heptachlor and chlordane exert
    considerable influence on enzymic and hormonal levels, even at dosages
    which are not overtly toxic.  Although gross congenital abnormalities
    do not seem a common consequence, chlordane and heptachlor obviously
    affect reproduction at all-stages.  Heptachlor and chlordane are car-
    cinogenic, and some evidence for mammalian mutagenicity also exists.
                                      334
    

    -------
    Endosulfan
    Endosulfan is the common name for 6,7,8,9,10,10-hexachloro-l,5,5a,6,9,
    9a-hexahydro-6,9-methano-2,4,3-benzodioxathiepin-3-oxide, a non-system-
    ic stomach and contact insecticide introduced by Farbwerke Hoechst AG
    in 1956 under the name Thiodan.  For its manufacture, the Diels-Alder
    adduct of hexachlorocyclopentadiene and cis-l,4-diacetoxybutene is
    hydrolyzed to the diol which is then reacted with thionyl chloride.
    Endosulfan is a mixture of two isomers, the alpha isomer having a mel-
    ting point of 108  to 110 C, and the beta isomer having a melting point
    of 208  to 210 C.  The technical product is a brownish crystalline so-
    lid with an odor of sulfur dioxide and a melting point of 70  to 100 C.
    It has no measurable vapor pressure at 75 C, has a water solubility
    less than one ppm, and is moderately soluble in most organic solvents.
    Degradation-
    Biological—Bacteria and green algae decomposed endosulfan to endosul-
    fan-alcohol (Gorbach and Knauf 1971).  Martens (1972) identified the
    major metabolic products of microbial endosulfan degradation as the
    sulfate and the endodiol.  In soil with natural microbial populations,
                                    14                              14
    a maximum of 5.4 percent of the   C-endosulfan was converted to   C0_
    in fifteen weeks; 30 to 60 percent was converted to endosulfan sulfate
    (Martens 1972).  In water, microbial degradation was favored by neut-
    ral, aerobic conditions (Greve and Wit 1971).  Under aerobic conditions
    unidentified soil bacteria converted aZ-pfcz-endosulfan as well as beta-
    endosulfan to their respective alcohols, but the ether was obtained
    only from Jeta-endosulfan (Perscheid et al. 1973) .
             14
    In mice,   C-endosulfan was converted to its sulfate prior to tissue
    storage while fecal excretion included endosulfan itself, endosulfan
    diol, and endosulfan sulfate.  Compounds other than the sulfate were
                                      335
    

    -------
    apparently restricted to the liver and kidneys (Deema e_t_ al_. 1966).
    In rats and mice, the alpha isomer was more rapidly excreted than  the
    beta isomer.  Five metabolites of endosulfan were detected, including
    the hydroxyether and the gamma-lactone; nevertheless most endosulfan
    was recovered unaltered (Schuphan et al. 1968).  When two ewes were fed
                 14
    0.3 mg/kg of   C-endosulfan, the radioactivity was almost totally  el-
    iminated within 22 days; fifty percent was eliminated in the feces, 41
    percent in the urine, and one percent was excreted in the milk.  Milk
    residues fell to two ppb by the twenty-second day, and to no more  than
    0.03 ppb after 40 days.  Urinary metabolites included 1,4,5,6,7,7-hex-
    achloro-2,3-bis-(hydroxymethyl)-bicyclo-2,2,l-heptene-5(endosulfan al-
    cohol) and l-alpha-hyd-roxy endosulfan  (Gorbach et al. 1968) .
    The data on biological degradation of endosulfan are summarized in
    Table 58 and Figure 14.
    Chemical and physical—In neutral solution, the alpha and beta isomers
    each decomposed to two unidentified but not identical compounds, while
    in alkaline solution both isomers formed the diol, which was then  open
    to further degradation (Schuphan and Ballschmiter 1972) .
    Photolytic—When endosulfan was irradiated by UV light at wavelengths
    approximating sunlight, the alpha isomer was dechlorinated  in hexane
    solution.  The beta isomer was stable to UV light in hexane, but lost
    one chlorine if in dioxan-water solution (Schumacher et^ a^. 1971,  1973).
    Archer and co-workers (1972) obtained endosulfandiol as the major  pro-
    duct of UV irradiation.  Other photoproducts included the a1pha-hydroxy-
    ether, a lactone, an ether, and some minor unidentified products,  but
    no endosulfan sulfate.  No degradation occurred in the dark (Archer et
    al. 1972).  Under laboratory and greenhouse conditions, endosulfan sul-
    fate and endosulfan ether were reported to be the major metabolites
    (Beard and Ware 1969).
                                      336
    

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    Transport-
    Within soil—Of 6.7 kg/ha soil-applied endosulfan, 90 percent of the
    residues were recovered from the top 15 cm of soil, and nine percent
    from the 15 to 30 cm layer  (Stewart and Cairns 1974) .  When endosulfan
    was applied to a broad spectrum of soils in columns, water percolation
    of the soils permitted recovery of 64 percent of the endosulfan from
    Lakeland sand, but no more  than seven percent from sandy clays.  Loam
    recoveries were intermediate (Bowman et al. 1965).
    Between soil and water—Endosulfan was found as a pollutant of the
    Main, Rhine, and Regnitz rivers in Germany (Herzel 1972), with levels
    of up to 0.70 ppb in the Rhine (Greve and Wit 1971).  Richardson and
    Epstein (1971) concluded that flocculation would not significantly de-
    crease water levels of endosulfan.  Greve and Wit (1971) found that
    endosulfan readily adsorbed to river silt, and that 85 percent could
    be removed by filtration.
    Into organisms—When potato foliage was sprayed eight times with 0.6
    kg/ha of endosulfan, both potato peel and pulp contained 0.01 ppm endo-
    sulfan (Stewart and Cairns  1974).  Rate of penetration of endosulfan
    and its metabolites into beet and bean plants was of the order:  beta
    isomer > sulfate > ether > aZp/za isomer > diol.  Only the diol was not
    transferred to the roots in detectible amounts.
    The common mussel, Mytilus edulis, reportedly took up alpha and beta-
    endosulfan differentially, although the same study suggested that en-
    dosulfan was not absorbed directly from seawater by the mussel, but
    rather was taken up with suspended particles to which it was adsorbed
    (Roberts 1975).  When pigs were fed an acute oral dose of 2 ppm, organ
    residues after 27, 54, and 81 days were reportedly insignificant com-
    pared to organ residues of DDT in pigs fed seven ppm of the latter.
    Exact residues were not available, however (Maier-Bode 1966).
                                      339
    

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    Volatilization-
    Endosulfan volatilized more readily from glass than from leaf surfaces,
    and more readily from sugar beet foliage than from bean foliage.  Under
    controlled laboratory conditions, endosulfan isomers and metabolites
    volatilized from glass in the order:  alpha isomer > ether > beta isomer
    > sulfate > diol but at the higher temperatures of the greenhouse, the
    order was:  alpha isomer > ether > beta isomer > diol > sulfate (Beard
    and Ware 1969).
    Persistence-
    Endosulfan is an infrequently found residue in agricultural soils of
    southern Ontario (Harris ^ al.  1966).  Stevens et^ al. (1970) found
    endosulfan residues in one third of soils with a history of regular
    pesticide usage (vegetable, cotton, forest), and in nine percent of
    soils with a history of little or no pesticide use (root vegetables,
    grains).  Residues in vegetable/cotton soils were as high as 1.22 ppm;
    in forests as high as 4.63 ppm;  in grain/root crop soils as high as
    0.92 ppm.  Mullins et^ a^. (1971) found endosulfan in only one of fifty
    randomly selected Colorado soils, even though forty-one of the soils
    contained pesticide residues.
    When soil was treated with 6.7 kg/ha of endosulfan, 50 percent of the
    alpha isomer was converted to endosulfan sulfate within 60 days.  The
    beta isomer required 800 days for 50 percent conversion to endosulfan
    sulfate  (Stewart and Cairns 1974) .  The sulfate was characterized by
    the authors as being equally toxic to insects and "relatively stable",
    but no persistence times for it were given.  Residues of endosulfan
    sulfate, (0.3 ppm), fceta-endosulfan  (0.06 ppm) and aIpha-endosulfan
    (0.01 ppm) were found in potato peels, and 0.03 ppm endosulfan sulfate
    in the potato pulp.  The authors concluded that conversion to endosul-
    fan sulfate occurred in the potato (Stewart and Cairns 1974) .
    When one Ib/A (0.89 kg/ha) of granular endosulfan was applied to Ber-
    muda grass, 13.7 percent remained after 96 days, during which two crops
                                      340
    

    -------
    of hay were cut and 16.5 inches of rain fell  (Byers £t^ a^. 1965).  In
    flooded rice fields of east Java, agricultural levels of endosulfan
    (1.4 liter of Thiodan 35 EC in 750 liters of water per hectare) resulted
    in elevated endosulfan levels for no more than five days.  Maximum le-
    vels in mud were 1.9 ppm (Gorbach et_al. 1971).  Greve and Verschuuren
    (1971) reported endosulfan residues of up to 0.07 ppb in river water,
    and up to 0.01 ppb in drinking water.  Greve and Wit  (1971) estimated
    a half-life of five weeks for endosulfan in water at pH 7, but of five
    months at pH 5.
    Effects on Non-Target Species-
    Microorganisms—Gorbach and Knauf (1971) did not find any inhibition
    of bacterial action by endosulfan under field conditions.  Knauf and
    Schulze (1973), however, noted that the aquatic microorganism CTzZoreZZa
    Vulgaris responded to 0.2 ppm of endosulfan by reducing its rate of re-
    production.
    Invertebrates—Luedemann and Neumann (1962) studied the effects of en-
    dosulfan on ten aquatic invertebrates.  Mussels (Dvei-ssend) were unaf-
    fected by less than ten ppm and killed by 100 ppm endosulfan while the
    American river crab (Cambarus affinis) was affected by 0.1 ppm and kil-
    led by one ppm.  Most sensitive was the flea crab (Cayinogrammarus).
    which was killed by 0.005 ppm, with toxic effects noted at 0.001 ppm.
    Fish and amphibians—Endosulfan is highly toxic to fish.  Gorbach and
    Knauf (1971) considered the lethal levels to be between 0.001 and 0.01
    ppm, depending on the species.  Toor et al. (1973) found 0.007 ppm to
    be the threshold level of endosulfan toxicity in carp, while 0.005 ppm
    was the maximum sublethal dose.  Rainbow trout fry were adversely af-
    fected by 0.006 ppm and pike by 0.001 ppm endosulfan, while the lethal
    levels were 0.01 ppm and 0.005 ppm for the two species, respectively
    (Leudemann and Neumann 1962).  Greve and Wit  (1971) considered one ppb
    to be a sufficiently great concentration of endosulfan to cause large
    fish kills under unfavorable conditions.  Schoettger  (1970) reported
                                      341
    

    -------
    TL,./, levels of endosulfan to be as low as 0.3 ppb in trout, but noted
    that trout eggs could tolerate 50 ppm for two hours.  Endosulfan at
    one Ib/A (1.12 kg/ha) was toxic to the toad Bufo boreas  (Mulla et al.
    1963).
    Birds—The LD_Q of endosulfan for starlings was 35 mg/kg  (Schafer 1972):
    for mallards, 200 to 705 mg/kg, and for ring-necked pheasants, 620 to
    1000 mg/kg (Martin 1968).  In tests on chicken and quail  embryos, nei-
    ther immersion of the eggs nor injection of the embryos with endosul-
    fan caused birth defects, but sterility occurred in both  males and fe-
    males so treated (Lutz-Ostertag and Kantelip 1971).
    Mammals—The LD ~ of endosulfan to rats was 100 mg/kg (Schafer 1972).
    In mice, the acute oral LD   was estimated at 15 mg/kg in highly inbred
    (Balb/c) mice; chronic dietary intake of ten ppm was sublethal (Deema
    et al. 1966).  Diet was found to affect tolerance to endosulfan in
    rats, which had an acute oral LD,.., of 5.1 + 1.4 mg/kg endosulfan if  fed
    a protein-deficient diet; when casein constituted 81 percent of the
    diet, the LDC_ rose to 98 + 7 mg/kg endosulfan (Eldon et  al. 1970).
                _>u            —                           	
    Endosulfan was the only chlorinated hydrocarbon insecticide found not
    to be accumulated in mammals (Vettorazzi 1975).
                                      342
    

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    Toxaphene
    Toxaphene is the name for a mixture of chlorinated camphene compounds
    of uncertain identity, with a chlorine content of 67 to 69 percent by
    weight.  It was introduced by Hercules Powder, Inc. in 1948 and is
    used heavily on cotton, formerly with DDT and now with methyl para-
    thion or parathion.  Other names for toxaphene include polychlorocam-
    phene (USSR), chlorinated camphene, and octachlorocamphene.  It is
    similar in composition and origin to several other chlorinated terpenes,
    such as strobane.  Toxaphene is the most widely used chlorinated hy-
    drocarbon insecticide (Matsumura et al. 1975).
    Toxaphene is a yellow waxy solid with a mild terpene odor which softens
    between 70  and 90 C.  It is noncorrosive in the absence of moisture,
    and its solubility in water is 0.4 ppm (La Fleur 1974, Metcalf and San-
    born 1975).  It is readily soluble in organic solvents, including pet-
    roleum oils, and can be dehydrochlorinated by heat, strong sunlight,
    and by certain catalysts such as iron (Martin 1968) .
    Bevenue and Beckman (1966) considered gas chromatography to be an un-
    reliable method of identifying toxaphene if other pesticides were pre-
    sent.  The alternatives, total chloride determination and bioassay, are
    hardly specific to toxaphene, and so are limited to situations in which
    the history of contamination is known (Guyer et al. 1971) .  Kawano e_t_
    al. (1969) reported that a mixture of sulfuric-fuming nitric acid can
    be used to remove parathion and DDT from samples before analyses for
    toxaphene.
    Despite prolonged and heavy use, relatively little is known of the ac-
    tion or fate of toxaphene in the environment, since the complexity of
    its composition makes residue analyses tedious and uncertain (Guyer et
    al. 1971).  Nelson and Matsumura (1975) circumvented the analytical
                                      343
    

    -------
    difficulties by constructing a simplified toxaphene, consisting of a
    few toxaphene components, but this approach is restricted to laboratory
    experiments.  Isolation of some major components of toxaphene was a-
    chieved recently by Matsumura et al. (1975) who elucidated the struc-
    ture of two toxaphene components which were said to account for up to
    56 percent of the mixture's toxicity to mammals.  Casida and his co-
    workers established that toxaphene consists of at least 175 polychlor-
    inated derivatives of camphene, one of which was identified as 2,2,5-
    end^o, 6-exOj8,9,10-heptachlorobornane, shown in Figure 16 (Casida et al.
    1974,  Holmstead et_ al. 1974, Palmer et_ al. 1975).  An octachloronor-
    bornane constituting six percent of the mixture was isolated and was
    found to be fourteen times as toxic to mammals as toxaphene (Khalifa
    e_t_ ai^. 1974).  Anagnostopoulos, Parlar, and Korte (1974) also isolated
    several toxaphene components, of which three are shown in Figure 15.
    Together these constituted five to eight percent of technical toxaphene.
    Degradation-
    Biological—rats fed 20 mg/kg   Cl-toxaphene excreted about 37 percent
    of the radioactivity unchanged in the feces, but 15 percent was excre-
    ted in the urine, mostly as ionic chloride.  Repeated doses led to de-
    creases in the fecal, or unmetabolized, fraction (Crowder and Dindal
    1974).  Ohsawa et al. (1975) found half the radioactivity in the urine
    as chlorides, and concluded that biodegradability was characteristic
    of all toxaphene fractions, but that relatively few of the fractions
    were toxic to the rat.
    In dairy cattle, lactating cows fed up to 20 ppm toxaphene for 77 days
    excreted it in their milk for only fourteen days, after the end of the
    treatment, but a single cow who was nearly dry excreted toxaphene in
    her milk for longer periods.  The authors concluded that excretion in
    milk was a major route of toxaphene elimination in cattle (Zweig et al.
    1963).  There were no data available on the degradation of toxaphene
    by microorganisms, plants or invertebrates.
                                       344
    

    -------
    2,2.,5-ENDO, 6-EXO, 8, 9,10-HEPTA-
    CHLOROBORNANE~TTASIDA ET AL.  1974)
    (ANAGNOSTOPOULOS  ET AL. 1974)
             CLCH2
                        CL
    
     (ANAGNOSTOPOULOS ET AL,  1974)
                                                CL
      (ANAGNOSTOPOULOS  ET AL, 1974)
                        STRUCTURES  OF  TOXAPHEME  COMPONENTS
                               Figure 15
                                      345
    

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    Chemical and physical—Clay-catalyzed decomposition of toxaphene is
    purportedly mediated by acidic diluents of the clays and increasing
    temperature as well as increasing acidity speeded the degradation (Fow-
    ker et al. 1960).  Physical degradation of toxaphene has not been re-
    ported on.  Inasmuch as toxaphene consists of mixed chlorinated cam-
    phenes, it seem plausible that degradative methods safe for DDT and cy-
    clodiene insecticides would be safe for use with toxaphene.  Iron is
    known to catalyze dehydrochlorination of toxaphene (Martin 1968) .
    Transport-
    Studies on transport are difficult because of the complexity of the
    mixture and the difficulty of identifying small quantities of the mul-
    titudinous components.  Bradley and co-workers (1972) recovered less
    than one percent of the toxaphene applied to cotton plots in the sur-
    face runoff water; of the toxaphene lost to water flow, 75 percent was
    associated with sediment.  After ten years, up to 95 percent of the
    toxaphene residues remaining in Houston black clay were in the top 12
    inches of soil (Swoboda e_t_ al. 1971) .  Toxaphene applied to Dunbar soil
    in a South Carolina field plot was found in ground water within two
    months however.  The half-life in soil was estimated to be 120 days,
    but groundwater contamination persisted for the entire year of obser-
    vation (La Fleur et al. 1972).  Toxaphene is also a contaminant of the
    lower Mississippi and its tributaries (Barthel et al. 1969) .  Further-
    more, traces of two heptachloronorbornenes which could be degradation
    products of toxaphene have been found in New Orleans drinking water at
    levels of 0.04 to 0.06 ppb (ANON. 1974).  Klein and Link (1967) found
    that when toxaphene was sprayed on kale, most of the pesticide disap-
    peared within three days, even in the absence of rain: after seven days
    and two inches of rain, only eight percent remained on the leaves and
    after 28 days, only traces were found.
    Weith and Lee (1971) observed that toxaphene residues in the top five
    centimeters of lake sediment increased for 190 days following treatment,
                                      346
    

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    and then decreased by a factor of two every 120 days, apparently by
    transport to deeper strata; a rate of movement of 0.4 to 1.1 centime-
    ters per day was estimated.  Toxaphene was not, however, detected be-
    low 20 centimeters.  Lake water did not leach toxaphene out of sediment
    under laboratory conditions.
    When a toxaphene-contaminated stream was dredged, toxaphene residues
    increased in estuarine fauna and flora.  Oysters  (Crassostrea
    ca) contained two to five ppm, but mummichogs (Fundulus
    contained more than 200 ppm toxaphene.  Even marsh grass (Spart~ina al-
    termiflora} contained 7.5 ppm toxaphene, providing a rare example of
    transport of toxapbene from soil into plants.  The authors postulated
    that uptake by the marsh grass was facilitated by the species' ability
    to transport and accumulate salt (Reimold and Durant 1974).  Adsorption
    on charcoal decreased the toxicity of toxaphene to goldfish (Barren
    1969).
    When toxaphene was studied in an aquatic terrestrial ecosystem (Metcalf
    et_ _al_. 1971), algae, snails, and mosquitofish were found to contain
                                                         14
    6902-fold, 9600-fold, 890-fold and 4247-fold as much   C-toxaphene,
    respectively, as was found in the water, indicating that toxaphene is
    highly accumulative in aquatic food chains (Sanborn and Metcalf 1975).
    Persistence-
    After 16 years, residues of toxaphene in Congaree sandy loam were es-
    timated at 49 percent (Nash and Harris 1973).  After 14 years under
    conditions predisposing to maximum persistence, 45 percent remained in
    the soil (Nash and Woolson 1967).  Randolph ett_ al_. (1960), however, ob-
    served a loss of 50 percent of toxaphene in one year in Texas soils.
    The data in these studies included DDT residues similar to those re-
    ported for toxaphene.
    When toxaphene was applied for five years to a California soil, the
    total application reached 103.6 Ibs/A (116 kg/ha), with soil residues
                                      347
    

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    of ten to 15 ppm after the fifth application.  Four years later, four
    to six ppm remained, a loss of approximately 60 percent over four years
    (Hermanson et al. 1971) .
    Persistence of toxaphene in lakes was found to depend heavily on the
    nature of the lake:  shallow eutrophic lakes were successfully restock-
    ed with fish after one year, whereas deep, oligotrophic lakes were
    still toxic after five years (Terriere et_ al. 1966).  Levels of toxa-
    phene were 88 ppb in treatment of the shallow lake:  one year later,
    water levels had fallen to one ppb, but aquatic plants contained 500
    ppb, aquatic animals (other than fish) 1,000 to 2,000 ppb, and trout
    contained up to 20,000 ppb.  Similar levels were observed in trout from
    the deep lake with sparse biota (Terriere et al. 1966).  Similar re-
    sults were obtained by Johnson et al. (1966), who concluded that sorp-
    tion rather than degradation of toxaphene was responsible for the
    detoxification of toxaphene in eight Wisconsis lakes.
    Effects on Non-Target Species-
    Microorganisms—When pure cultures of marine phytoplankton were grown
    in the presence of pesticides, toxaphene at 0.15 ppm was absolutely
    toxic, preventing growth in all species tested.  Even 0.01 ppm depres-
    sed growth in all species except the rather resistant Protocooous;
    0.00015 ppm prevented all growth of Monoerysis lutheri,, the most sen-
    sitive species in the group and 0.000015 ppm toxaphene still caused
    78 percent growth inhibition in this species (Ukeles 1962).  At high
    agricultural levels of application, toxaphene x^as reported to have sig-
    nificant effect on the numbers of bacteria or fungi in soil within ten
    months of five annual applications (Martin et al. 1959).  Smith and
    Wenzel (1947) had reported stimulation of fungi and bacteria which
    were able to use toxaphene for growth.
    Plants—Cullinan (1949) observed degradation of toxaphene during tests
    of phytotoxicity and soil effects.  Diaz-Mena (1954) also observed phy-
    totoxicity with toxaphene, as with all chlorinated hydrocarbons, under
                                      348
    

    -------
    his experimental conditions.  Toxaphene reportedly inhibited photosyn-
    thesis in alfalfa unless rain occurred within six days.  Increasing
    temperature decreased the degree of inhibition  (Kralovic 1974) .
    Invertebrates—Oysters  (Cras so street virgin-Lea)  exposed to one  ppb/liter
    each of DDT, toxaphene, and parathion gained less wieght and were more
    subject to mycelial fungal infections than control oysters, while other
    single pesticides at one ppb did not have any discernible effect  (Lowe
    et_ al. 1970).  Hard shell clams (Meroenaria meroena.ria) and oysters
    (Cras so street. viTginiaa) were more affected by toxaphene during the em-
    bryonic than larval stage (Davis and Hidu 1969).
    Fish and amphibians—Toxaphene is among the most toxic of pesticides
    to fish; with only rotenone and endrin acknowledged to be more toxic
    (Adlung 1957).  Little  species difference was observed in the  relative
    sensitivities of fish families to toxaphene:  comparisons were made be-
    tween Ictaluridae3 Cyprinidae3 Centrarchidae, and Salmonidae (Macek and
    McAllister 1970).  Toxaphene was more toxic to  mosquitofish in static
    than in flowing solutions (Burke and Ferguson 1969) .  Toxaphene accu-
    mulation was found in bluegills (Lepomis macrochirus) after treating
    lakes for rough fish control even though the restocked bluegills grew
    well (Hughes and Lee 1973).
    In fathead minnows (Pimephales promelas), water levels of 55 to 1,230
    ng/liter (0.055 ppb to  1.23 ppb) resulted in growth disturbance after
    90 and within 150 days; the minnows' collagen content was shown to de-
    crease, both absolutely and in relation to calcium content, and the in-
    creased mineralization was expressed by increased fragility.   Under
    stress, toxaphene-treated minnows' backbones fractured (ITehrle and
    Mayer 1975a).  Brook trout (Salvelinus fontinalis) were exposed to to-
    xaphene from 22 days before to ninety days after hatching.  Although
    hatching itself was not affected, growth was significantly decreased
    by 139 and 288 ng/liter (0.137 to 0.288 ppb) within 30 days, and by
    39 ng/liter (0.039 ppb) within ninety days after hatching.  Whole-body
                                      349
    

    -------
    collagen was decreased within 15 days of hatching, and calcium and
    phosphorus content increased (Mehrle and Mayer 1975b) .
    Toxaphene was less toxic to anuran amphibians than were endrin, aldrin,
    or dieldrin, and had approximately the same toxicity as DDT  (Ferguson
    and Gilbert 1967).  Tolerance of up to 200-fold was found in amphibians
    near insecticide treated cotton fields (ibid).
    Birds—The !!)_„ of toxaphene in seven-day old mallard ducklings was
    30.8 mg/kg, with 95 percent confidence limits of 23.3 to 40.6 mg/kg
    (Tucker and Crabtree 1970).  Mallards were less sensitive at three to
    five months of age, with an LD,-^ of 70.7 mg/kg and 95 percent confidence
    limits of 37.6 to 133 mg/kg.  Mature sharp-tailed grouse had an W)rn of
    10-2C mg/kg.  Symptoms were seen within 20 minutes in some species, but
    mortality generally occurred between two and fourteen days (Tucker and
    Crabtree 1970).
    Limited tests with young chickens suggested that toxaphene, in contrast
    to Ojp'-DDT and p^p'-DDE, decreased sleeping time (Stickel 1973).  Tox-
    aphene increased the thyroid growth of bobwhite quail when birds were
    treated with 50 ppm for three or four months while liver weights did
    not increase even after 500 ppm were fed for the same length of time
    (Hurst e^ al. 1974).
    Mammals—The acute oral LD,.- of toxaphene in rats is g€;nerally consid-
    ered to be 90 mg/kg in males and 80 mg/kg in females  (Servintuna 1963,
    Guyer et_ al_. 1971) although Jones et_ al_. (1968) claimed an LD5Q of 283
    mg/kg.  The dermal LD . was slightly over 1,000 mg/kg (Servintuna 1963,
    Jones et al. 1968).  Schindler  (1956) found that toxaphene controlled
    voles when applied at two kg/ha, and Lange and Crueger (1960) found
    that four liters/ha of a 50 percent toxaphene solution resulted in a
    thorough kill of field mice.
    In rats, less than additive effects were reported for the combination
    of carbofenthion, diazinon, or parathion with toxaphene, but carbaryl
                                      350
    

    -------
    or malathion interacted additively (Keplinger and Deichman 1967).   The
    mode of action of toxaphene poisoning is not understood, but it is
    thought to be pharmacologically similar to that of the cyclodienes,
    since cyclodiene resistance invariably confers toxaphene resistance in
    insects (Brooks 1974, Vol. 2).  No effects of toxaphene on rat repro-
    duction were found during a multigeneration study (Kennedy et_ al.  1973)
                                      351
    

    -------
    Conclusions
    Although data on organochlorine insecticides are by no means complete,
    it is apparent that, in less than forty years, they have become almost
    universal contaminants of land, water, and living things.  Of the 12
    compounds for which a literature search was carried out, only methoxy-
    chlor is biodegradable.  With respect to the other compounds, it must
    be assumed:
         1.  that, over the period of their persistence, all will move
             through soil, into water, into the atmosphere, and into
             living organisms;
         2.  that there are no efficient biological pathways for their
             degradation to naturally occurring substances;
         3.  that the effects of some, and perhaps all, of these com-
             pounds on microorganisms, fish, birds, and even man may
             eventually prove as disastrous as they seemed benign or-
             iginally.
    Accordingly, it is recommended that waste chlorinated hydrocarbon insec-
    ticides be burned or chemically degraded, with suitable precautions for
    disposal of chlorine and other toxic gases.  Disposal in soil, whether
    in shallow pits or deep wells, is considered utterly undesirable, since
    the available evidence is that dispersal would precede any significant
    degradation.  The sole exception to these conclusions is methoxychlor,
    which might be disposed of in flooded soil or in sequestered ponds,
    provided adequate precautions were taken against contaminating natural
    waters.  Endosulfan is not excepted from the conclusion against soil
    or water disposal, since the few available data suggest that its major
    terminal residue endosulfan sulfate, which shares most of the toxic
    properties of endosulfan itself, is very persistent in soil.
                                       352
    

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    -------
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                                      415
    

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    ORGANOPHOSPHORUS INSECTICIDES
    Methyl Parathion and Parathion
    Methyl parathion is the common name for 030-d±methyl C>-p-nitrophenyl
    phosphorothioate, known as parathion-methyl in western Europe and as
    metaphos in the USSR.  Introduced in 1949 by Farbenfabriken Bayer as
    "Dalf" or "Folidol-M1, methyl parathion is a nonsystemic contact and
    stomach insecticide.  When pure, it is a white crystalline powder with
    a melting point of 35  to 36 C and a vapor pressure of 0.97 x 10  mm
    mercury at 20 C.  At 25 C its solubility in water is 55 to 60 ppm; it
    is slightly soluble in light petroleum and mineral oils and soluble in
    most other organic solvents.  The technical product is a light to dark
    tan liquid of about 80 percent purity (Martin 1968).
    Parathion is the common name for (9,£>-diethyl 0-p-nitrophenyl phosphoro-
    thioate, also a nonsystemic contact and stomach insecticide.  Known as
    thiophos in the USSR, parathion is a pale yellow liquid with a boiling
    point of 157 C at 0.6 mm mercury, and a vapor pressure of 3.78 x 10  mm
    mercury at 20 C.  Its solubility in water is 24 ppm at 2.5 C, and it is
    slightly soluble in petroleum oils.  It is miscible with most organic
    solvents.  Parathion can be hydrolyzed in alkaline media, but only one
    percent is hydrolyzed in 62 days at pH five or six (Martin 1968) .
    Parathion is synthesized by condensing diethyl phosphorochloridothioate
    with sodium p-nitrophenate, while methyl parathion requires dimethyl
    phosphorochlorodithioate.
    Degradation-
    Biological—Biological pathways of parathion degradation are shown in
    Figure 16; pathways for methyl parathion are analogous.  The metabolic
    products of microbial degradation of methyl parathion are listed in
    Table 59, as are data representative of mammalian degradation/metabolism.
                                       416
    

    -------
                                HO-
    
                                    P—OH
                              C2H50
               NO 2
    
    
    P-NITROPHENOL
                                ANIMAL
                                                  HO.
                                               C2H50
                                                                  MO-
                                          —OH
                                                             T
                                                             ANIMAL
    (C2H50)2P-0  Q
     (C2H50)2P-0/Q
                                                             NO,
                                                          PARAOXON
              PARATHIOH
    
                   r~
                FISH
              MICROBES
                                                            FISH
    
                                                          MICROPES
    (C2H50)2P-0/Q
    
    
    
       AMINOPARATHION
    (r.2H5o)2  o- I
                                                     0
                                                     II
                                             (C,HcO),D_ OH
                                                             MH,
                                                      CONJUPATE
             DEGRADATION  PATHWAYS FOR PARATHION (MODIFIED
    
              HAQUE  AND FREED 1075),  DEGRADATION °ATHWAYS FOR
    
                      METHYL PARATHION ARE ANALOGOUS,
                            Figure 16
                                 417
    

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    The microbial degradation of parathion has been documented repeatedly
    (Singh 1974, Boush and Matsumura 1967, Griffiths and Walker 1970, Get-
    zin and Rosefield 1968) .  Table 60 lists specific organisms and the
    products of their degradation.
    Naumann (1959) observed that methyl parathion was 99.9 percent degra-
    ded in three weeks if 0.5 to one percent (5,000 to 10,000 ppm) were
    added to the soil.  Sterilized soil had first to be recolonized before
    degradation took place.  Sethunathan  (1973a, 1973b) and Sethunathan and
    Yoshida (1973a, 1973b) found that parathion was degraded more rapidly
    in flooded soil or under anaerobic conditions than under aerobic con-
    ditions.  If flooded soil was additionally inoculated with Flavohac-
    teTium,, the half-life of parathion was approximately 0.76 days, com-
    pared to 3.5 days in uninoculated soil.  Aminoparathion was the pri-
    mary anaerobic metabolite, with p-nitrophenol as the terminal residue.
    Baci-llus species were found which were capable of degrading p-nitro-
    phenol to carbon dioxide.  Maximum initial degradation of parathion
    occurred in acid sulfate soil under anaerobic conditions and repeated
    applications enhanced the degradation in alluvial soils.  Ring clea-
    vage and CO- production, however, occurred only under aerobic condi-
    tions .
    Penicillium waksmani degraded up to 1000 mg/ml (1000 ppm) parathion on
    agar, but was inhibited at higher levels of parathion.  After 15 days,
    61 percent of the parathion had been degraded, with aminoparathion as
    the major product (Rao and Sethunathan 1974).  The addition of organic
    natter shifted degradation from the hydrolytic pathways typical of
    aerobic unflooded soils to reductive pathways, increasing production
    of aminoparathion (Rajaram and Sethunathan 1975) .  A mixed bacterial
    culture degraded a parathion-xylene formulation in aqueous medium at a
    maximum rate of 50 mg/liter/hour, or with an optimum parathion concen-
    tration of 5000 mg/liter (5°00 ppm) in batch cultures.  Both the xylene
    diluent and the parathion were metabolized,  the latter preferentially
                                      419
    

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                                          420
    

    -------
    at slightly alkaline pH.  Complete air saturation, a pH between 7.0
    and 7.5, a temperature of 37 C were optimal.  Five of six pseudomo-
    nads isolated from the mixed culture used an ortho ring fission system
    for p-nitrophenol metabolism while the sixth did not grow on p-nitro-
    phenol  (Munnecke and Hsieh 1975).
    Naumann (1967) found a Pseudomonas species which was able to dissolve
    crystalline methyl parathion from the medium in four to eight weeks.
    Siddaramappa et al. (1973) found that Pseudomonas could degrade para-
    thion (formulated as Folidol) in a 1,000 ppm aqueous solution with 20
    grams of alluvial soil and 24 ml water; two weeks were required for the
    degradation.  In sewage lagoons, parathion was degraded less rapidly
    than malathion but more rapidly than diazinon (Halvorson et al. 1971),
    and both parathion and methyl parathion were inactivated within days
    by polluted stream water (Yasuno et al. 1966).  Bacillus subtilis was
    highly effective in converting parathion to aminoparathion and methyl
    parathion to methylaminoparathion (ibid).
    In summary, both parathion and methyl parathion appear to be eminently
    degradable compounds in that microorganisms capable of degrading them
    exist.  Since both compounds appear to serve as energy sources for the
    degrading microorganisms, selection for more efficient degradation is
    plausible, in contrast to the situation found for cometabolism by or-
    ganochlorine-degrading microorganisms (Alexander 1972).
    On plants, evaporation and photolysis predominated as modes of para-
    thion removal (Popov and Khol'kin 1958).  Paraoxon decomposed more
    rapidly than parathion on citrus foliage (Spear et al. 1975).  The ma-
    jor metabolites of methyl parathion in rice grains were thiophosphoric
    acid and 0,0-dimethyl thiophosphoric acid (Tomizawa et al. 1962).
    Parathion is rapidly metabolized in mammals.  In rabbits, the maximum
    blood levels were found twenty minutes after intravenous injection of
    six to ten mg/kg parathion, and removal from the blood occurred in 30
                                     421
    

    -------
    to 60 minutes.  A second injection was cleared less rapidly (Gar et al.
                                       32
    1955).  In rats, maximum levels of   P were found in liver, brain,
    lungs, and kidneys within two hours after ingestion; bone levels of
    32
      P increased for only seventy-two hours (Kortus et al. 1968).
    Hollingworth et^ al_. (1967a, 1967b) compared the metabolism of methyl
    parathion with the less toxic fenitrothion 0,0-dimethyl 0-(3-methyl-
    4-nitrophenyl) phosphorothioate.  Analysis of urinary and fecal meta-
    bolites of the two compounds in mice demonstrated that direct excre-
    tion of their oxygen analogs was a significant detoxification mecha-
    nism.  The parent compounds were not, however, excreted directly.  Nei-
    ther ring hydroxylation nor reduction of the nitro group to the amino
    group were significant in mice.  As dosage increased, the excretion of
    dimethyl phosphoric acid did not rise proportionally, whereas the lev-
    els of desmethyl phosphorothionate increased from a secondary metabo-
    lite to the major urinary metabolite.  It was concluded that, whereas
    hydrolytic removal of dimethyl phosphoric acid was the primary murine
    detoxification mechanism, desmethylation was a secondary route availa-
    ble when levels of the toxicants became too high and the hydrolyzing
    enzyme systems were overwhelmed.
    In rat liver slices, parathion activation to paraoxon was associated
    with the microsomal or mitochondrial fraction (Nakatsugawa and Dahm
    1967, Fukami and Shishido 1963).  In female rats, 4.4 percent of the
    LD-,. dose was converted to paraoxon within one hour, with 64 percent
    of the conversion occurring in the liver (Kubistova 1959) .  In dairy
    cows, 14 ppm for 61 days produced no detectable parathion in milk,
    blood, or urine of the cattle; conjugation with a p-aminoglucuronide
    prior to urinary excretion was postulated (Pankaskie et al. 1952).
    Gyrisco and his co-workers (1959) found no residues in the milk of four
    dary cows fed ten ppm of parathion for three years.  In sheep, how-
    ever, 0.10 to 0.15 percent of a daily ingested dose of 2.0 to 5.5 mg/kg
    was excreted in the milk; four to five mg/kg parathion also decreased
    the volume of milk produced (Alamanni and Cossedu 1969) .
                                      422
    

    -------
                                                          o
    Photolytic—Ultraviolet light between 1,850 and 4,000 A  converts para-
    thion to paraoxon  (Payton 1953).  On leaf surfaces and glass, sunlight
    catalyzed the conversion of parathion to paraoxon  (about one percent)
    and to p-nitrophenol  (El-Refai and Hopkins 1966).  Parathion in ethanol
    is photolyzed to C^S-triethyl thiophosphate as a major product, and
    paraoxon and 030S(9-triethyl phosphate as minor products (Grunwell and
    Erickson 1973).  Koivistoinen and Meilainen (1962a, 1962b) claimed that
    paraoxon was not affected by ultraviolet light.  Baker and Applegate
    (1970) examined the effects of temperature and ultraviolet light on
    methyl parathion and  found that UV radiation increased removal of methyl
    paration from soils by ten to 14 percent at 30 C and by 14 to 17 per-
    cent at 50°C.
    Chemical and physical—Parathion is most readily degraded by hydrolysis,
    which is easily catalyzed by peroxidases or by ferrous iron and EDTA
    (ethylenediaminetetraacetic acid) (Knaak et al. 1962).  In natural a-
    queous medium approximately 70 percent of the parathion was hydrolyzed
    in four weeks and 72  percent in six weeks.  In another study, 74 per-
    cent of the methyl parathion was hydrolyzed in six weeks (Cowart et al.
    1971).  Hydrolytic degradation eventually proceeded to the terminal
    residue p-nitrophenol, itself toxic.
    Hydrolysis of parathion proceeded more rapidly in calcareous sediment
    than in slightly acid sediments; aminoparathion was the major metabo-
    lite (Graetz et_ a!L. 1970).  At a pH of 7.4 at 20°C, parathion was es-
    timated to have a half-life of 108 days if chemical hydrolysis were the
    means of degradation; under the same conditions, paraoxon had a half-
    life of 114 days (Faust and Gomaa 1972).  In bottled river water both
    methyl parathion and  parathion were completely degraded within eight
    weeks (Eichelberger and Lichtenberg 1971).  Menzie (1972)  considered
    parathion to be nonpersistent in water.
    Under shelf storage,  less than four percent of a 50 percent methyl
    parathion emulsion decomposed in sixteen months (Raman and Krishna-
                                       423
    

    -------
    moorthy 1973).  Dust formulations of methyl parathion decomposed to
    give i9,0-dimethylphosphate, its ^-methyl isomer, (9-methyl 5-methyl
    0-p-nitrophenylthiophosphate and p-nitrophenol  (Gota et_ al. 1960).
    Parathion could be removed from noncombustible containers by washing,
    and disappeared from 50 percent ethanol washes within five hours.  So-
    dium hydroxide and sodium hypochlorite were less effective (Hsieh jet
    al. 1974).
    Parathion can be converted to paraoxon by seven percent chlorination
    of water or by one to two ppm of ozone, but potassium permanganate at
    ten to 40 ppm was not effective (Robeck &t_ al. 1965).  The toxic de-
    gradation product p-nitrophenol, if present to one part per hundred in
    water, could be removed by the addition of 40 kilograms of sodium hy-
    droxide plus 50 kilograms of bleaching powder for each 200 liters of
    water:  after two to three hours at 100 C, all organic compounds were
    removed from the water and 320 grams of inorganic salts were produced
    per liter of water (Mel'nikov et al. 1958).
    Radiolysis was successfully used to degrade parathion:  0.1 to 5.0 Mrads
    resulted in 27 percent degradation of parathion in hexane solution
    (Lippold et al. 1969) and 10,000 rads of jyomma-radiation from a   Co
    source resulted in better than 80 percent destruction of sufficiently
    dilute aqueous solutions (Sunada 1967).  Sufficiently dilute was de-
    fined as concentrations measured in parts per trillion.
    Transport-
    Within soil—McCarty and King (1966) stated that methyl parathion and
    parathion migrated rapidly in soil-water systems, but were also de-
    graded rapidly.  Lichtenstein et_ al. (1967) found, on the contrary,
    that parathion moved through soil less rapidly than aldrin.  Some para-
    thion entered water through sorption to loam and transport with loam
    particles, and one ppm of parathion in the presence of percolating
    water resulted in small water residues of the pesticide.  In soil col-
    umns of Nacodoches clay subsoil, parathion leached to 60 inches when
                                       424
    

    -------
    230 inches of rainfall were simulated, while in Houston black clay,
    1,725 inches of simulated rain were required to produce leaching to
    60 inches (Swoboda and Thomas 1968).  Adsorption was found to be the
    main factor retarding mobility, and Swoboda and Thomas (1968) consid-
    ered parathion to be dissolving as a liquid phase in an organic frac-
    tion of the soil.  Parathion applied at 0.1 pounds per acre, followed
    by flooding and a subsequent application of 0.2 pounds per acre, was
    degraded before reaching drainage tiles six feet below the soil sur-
    face (Johnson et al. 1967).
    Stewart &t_ al. (1971) reported that little leaching occurred in six-
    teen years after four annual applications of 31.4 pounds of parathion,
    despite 42 inches of precipitation per year.  Wolfe et al. (1973) re-
    ported that very little parathion was found below the nine inch level
    six years after 30,000 to 95,000 ppm of parathion were applied to soil.
    In a 15 year study of pesticide residues in light sandy soil, Voerman
    and Besemer found that dieldrin and DDT, but not lindane or parathion,
    leached to 60 centimeters; parathion was not found below 20 centime-
    ters.  Mol et^ sil_. (1972) did not find parathion much below 2.5 centi-
    meters even with 220 mm of rain during the eight month persistence of
    parathion under their experimental conditions.  Burkhardt and Fairchild
    (1967) applied parathion (formulated as Niran) in several sandy soils,
    and observed increased mobility at higher levels of moisture.  Sacher
    and co-workers (1972) observed little movement of parathion in char-
    coal or kaolinite formulations.  Parathion contamination of a farm
    pond and its sediment was correlated with the degree of erosion, sug-
    gesting that parathion moved with soil particles rather than by leach-
    ing (Nicholson et_ al. 1962) .
    No mention is made in these studies of the fate or mobility of the de-
    gradation products of parathion or methyl parathion.
    Between soil and water—When soil was added to parathion in water, 63
    percent of the parathion was adsorbed by the soil from a low volume of
                                      425
    

    -------
    water (100 ml), but only 38 percent was adsorbed from a larger volume
    (250 ml).  The carrier, the depth of the water, its agitation, and the
    rate of parathion application all affected the rate of loss of para-
    thion to soil (Weidhass et_ al. 1961).  King et_ al. (1969) tested the
    ability of several adsorbents to remove parathion from water, and
    found that soil with a high clay content was more effective than sandy
    soil; coal was 2.5 times as effective as soil, and algal systems were
    ten times as effective as soil.  Activated charcoal had 1,000 times the
    sorptive capacity of soil.  Movement of parathion into water from soil
    appeared to occur by erosion rather than by leaching (Nicholson et_ al.
    1962).
    Into organisms—The high toxicity of parathion and methyl parathion in
    most animals makes bioaccumulation unlikely, nor has evidence for it
    been found in cattle (Pankaskie et_ al^. 1952, Gyrisco et_ al_. 1959),
    sheep (Alamanni and Cossedu 1969) or rabbits (Kortus et al. 1968).
    Methyl parathion was taken up by carrots from soil and retained for up
    to four weeks (Engst et_ al_. 1966a, 1966b) .  No methyl paraoxon was
    found, suggesting very slow metabolism (1966a) but five phosphorus-^
    containing degradation products were found, including monomethyl phos-
    phate and dimethyl phosphate  (1966b).  El-Refai and Hopkins (1966)
    documented the transfer of ten percent of foliar applications of para-
    thion into the bean plant.  Smith (1950) said that only minute amounts
    of the parathion absorbed from foliar applications was translocated
    within the plant, and Zuckerman et_ al. (1966) did not find any trans-
    fer to roots or soil from foliar applications, but near-insecticidal
    levels of parathion were transported from soil to leaves.
    Bean plants grown in soil containing parathion contained parathion met-
    abolites if and only if microorganisms capable of metabolizing para-
    thion were present in the soil; in sterile root cultures, bean plants
    translocated only unaltered parathion (Mackiewicz et al. 1969).
                                      426
    

    -------
    Studies of parathion movement in a model cranberry bog demonstrated
    that both fish and microorganisms are capable of accumulating parathion;
    fish metabolized the compound better than did mussels, and dead fish
    accumulated 80-fold the water concentrations of parathion (Miller et
    al. 1966).
    In the terrestrial-aquatic model ecosystem only fish contained para-
    thion (0.1006 ppm) at the end of the 38 day experiment and none of the
    ecosystem organisms contained paraoxon.  Most of the organisms con-
    tained radioactivity; 68 percent of the radioactivity in the algae,
    Daphniaj snails, and mosquito larvae was unextractable; in the fish,
    only 19.7 percent was unextractable, although only 31.5 percent of the
    unextractable material (6.21 percent of the total piscine radioactivity)
    was parathion (Yu and Sanborn 1975).  Parathion, paraoxon, and p-nitro-
    phenol were found in the water at 0.3, 0.47, and 1.4 ppb, respectively.
    Parathion was estimated to have a half-life of 15 to 16 days in water,
    and no evidence was found for bioaccumulation in any of the organisms
    (Yu and Sanborn 1975, Metcalf and Sanborn 1975).
    Volatilization-
    On petri dishes, parathion in ethanol solution at 35 C was 62 percent
    volatilized in 90 days (Allessandri and Amormino 1954) while 94 per-
    cent of parathion sprayed on peach leaves was lost within one week
    (Brunson and Koblitsky 1952).  Mistric and Gaines (1953) found that
    wind, sun, and rain, and/or high temperatures significantly increased
    the volatilization of methyl parathion and parathion, which, if pro-
    tected from these elements, retained their full insecticidal power for
    more than 24 hours, and for more than 48 hours, respectively.  After
    one pound per acre of methyl parathion or parathion was sprayed on
    cotton in Arizona, immediate residues were 106 ppm of methyl parathion
    and 117 ppm of parathion; after 96 hours, residues had fallen to 3.9
    and 5.5 ppm, respectively (Ware et_ al^. 1972).
                                      427
    

    -------
    Polizu and Floru (1967) observed maximum volatilization of parathion
    at a relative humidity of 40 percent and a temperature between 20 and
    50 C; the precise emulsifiers present did not seem to affect the rate
    of volatilization.  Quinby and co-workers (1958) estimated a half-life
    of less than 0.5 hours for methyl parathion on cotton in Mississippi,
    where these conditions for maximum volatilization probably held.  Para-
    thion was also lost more rapidly at high temperatures (Mistric and Mar-
    tin 1956).  Encapsulated parathion persisted for up to 70 days on peach
    foliage, however (Winterlin e_t_ Q. 1975).
    Although the studies cited did not distinguish between volatilization
    and photolysis, the importance of volatilization or of dust-borne
    transport is emphasized by the presence of organophosphate pesticides
    in the atmosphere above the southeastern United States (Stanly et^ ajU
    1971).
    Persistence-
    Data on the persistence of parathion, methyl parathion and parathion
    metabolites are summarized in Tables 61 and 62 for those studies in
    which the percent of residue remaining after a specified time could be
    ascertained.  At ordinary levels of application, either to soil or to
    foliage, both compounds are degraded within weeks if microbial degra-
    dation can occur (Lichtenstein et_ al. 1968), and accumulation even of
    repeated doses is unlikely (Goldsworthy and Foster 1950).  Under con-
    ditions of excessive application or incorporation to the soil, however,
    the ordinary modes of degradation do not appear to function.  Simula-
    ted spills of concentrated parathion resulted in 15 percent residues
    after five years (Wolfe e_t_ al_. 1973) and 0.1 percent after 16 years
    (Stewart et_ al. 1971).  The residue levels of 13,800 ppm reported by
    Wolfe e_t^ al. (1973) were considered high enough to be lethal and were
    considered a plausible contamination arising from normal methods of
    transferring parathion.  Microorganisms in the area of the simulated
    spill did not show adaptation in degrading parathion or enhanced re-
                                      428
    

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    sistance to parathion and the number of bacterial colonies in the vi-
    cinity was reduced.  A similar observation was made by Kasting and
    Woodward (1951) who observed that 2 lb/A (2.24 kg/ha) of soil-applied
    parathion disappeared within 16 days, whereas 100 Ibs/A (112 kg/ha)
    persisted for over 165 days.
    Methyl parathion was also said to be retained longer in the soil if the
    initial concentration was substantial (Naishtein et^ al. 1973); the
    authors did not consider soil microorganisms to be the primary means of
    degradation.  Stobwasser (1963) observed that the second year's appli-
    cation of parathion produced lower residues in carrots, even though
    higher levels were applied, than did the first year's treatment.
    Persistence of parathion and methyl parathion were found to depend on
    the type of soil and the rate of application (Burkhardt and Fairchild
    1967).  In the laboratory, at 30 C and 40 percent soil moisture, three
    ppm of parathion remained in Windy loam eight months after 20 ppm had
    been incorporated.  Under the same conditions, Mocho silt loam, Linne
    clay, and Madera sandy loam retained one to two ppm after 30 days, and
    Laveen loamy sand retained only 0.2 ppm after 30 days.  Changing the
    moisture resulted in persistence of up to 1.5 ppm in silt loam after
    eight months instead of after one month.  Both microbial and hydrolytic
    degradation were considered to contribute to the dissipation of the
    parathion (Iwata et al. 1973).
    Harris and Mazurek (1966) compared the activity of pesticides in dry
    mineral soil, moist mineral soil and muck.  Both parathion and methyl
    parathion were most effective in moist mineral soil and least effec-
    tive in dry sand or clay, but more effective in moist muck (Harris
    1966).  When clay was added to sandy loam, the effectiveness of para-
    thion decreased (Harris 1967).  Liang and Lichtenstein (1974) compared
    the toxicity of parathion to fruit flies on sand and on silt loam and
    observed greater toxicity on sand; parathion toxicity synergized with
    atrazine if the latter was present at levels of at least 19 ppm.  In
                                      432
    

    -------
    sandy loam, parathion lost its effectiveness within four weeks (Harris
    1969).  The addition of detergents increased the two month persistence
    level of parathion thirteen-fold and the detergents also synergized the
    toxicity of the pesticide against fruit flies (Lichtenstein 1966).
    Leenheer and Ahlrichs (1971) analyzed the kinetics of parathion adsorp-
    tion on soil organic matter and determined that the initial rate of
    adsorption was limited by the diffusion of the pesticide onto the ad-
    sorptive sites on the outer surfaces of the adsorbent; after about ten
    minutes, the limiting factor became the diffusion of parathion into
    the interior of the adsorbent.  The fast, reversible adsorption, with
    low heats of adsorption and high adsorptive capacity on hydrophobic
    surfaces which was characteristic of parathion was considered indica-
    tive of physical adsorption, with Van der Waals bonds between parathion
    and the adsorbent surfaces (Leenheer and Ahlrichs 1971).  Yaron and
    Saltzman (1972) suggested that parathion cannot displace the strongly
    adsorbed water molecules in partially hydrated systems, so adsorption
    occurs mainly on water-free surfaces.  In consequence, parathion toxi-
    city in clay or organic soil increases, and its persistence decreases,
    as increasing soil moisture prevents its adsorption (Naumann 1959,
    Harris 1964a, Harris 1964b, Lichtenstein and Schulz 1964, Harris and
    Mazurek 1966, Harris 1967, Chopra and Khullar 1971).  Increasing a-
    mounts of clay or organic matter also provided more hydrophobic sites
    on which parathion could be adsorbed (Chopra et^ al. 1970, Saltzman et_
    al. 1972).
    Parathion was more readily adsorbed on organic than on mineral surfaces
    from aqueous solution, and bonding to organic matter was stronger.  De-
    sorption from mineral surfaces was rapid and essentially complete, but
    only small amounts of parathion were released from organic matter
    (Saltzman et_ al_. 1972, Kliger and Yaron 1975).  Hot only did organic
    matter adsorb more parathion than did clays, but sodium montmorillon-
    ite was a better adsorbent than was kaolinite (Saltzman and Yaron 1972).
                                      433
    

    -------
    Additltion of organic matter was also found to alter the route of para-
    thion degradation from hydrolysis to nitroreducation, with aminopara-
    thion as the product (Sethunathan 1973).
    The persistence of parathion was said to be increased by increasing
    the pH (Carlo et al. 1952) or decreasing the temperature (Chopra and
    Khullar 1971, Yaron and Saltzman 1972, Baker and Applegate 1970).
    Methyl parathion added to sandy-clayey soil at 20 mg/kg decomposed in
    seven days at 20 to 25 C when the soil moisture was 6.5 to 10 percent,
    but in ten to eleven days when the soil moisture was reduced to 1.7
    to 3.4 percent (Obuchowska 1967).  Emendation of soil with different
    ions altered adsorption and the relative magnitude of adsorption in
                                    _i_     I  I     i I      _i_
    the presence of the ions was:  H  > Ca   > Mg   > Na  (Chopra et al.
    1970).
    The persistence of methyl parathion was twice as great in ultra-low-
    volume sprays as in emulsifiable concentrations when sprayed on fol-
    iage in normal agricultural usage (Saini et^ al_.  1970).  In dusts, in-
    creasing the mean particle size of the carrier from 11.8 microns to
    23.2 microns speeded degradation by about five percent (Takehara et aj^
    1967a).  Methyl parathion was more rapidly degraded from a Zeeklite
    formulation than from clay L; the rate of degradation varied directly
    with the total iron content, the amorphous mineral content, and the
    base exchange capacity of the formulation (Takehara et al_. 1967b).
    Effects on Non-Target Species-
    Microorganisms—The effect of parathion and methyl parathion on soil
    microorganisms are summarized in Tables 63 and 64 and Table 65, re-
    spectively.  The few data on analogs and metabolites are also included
    in Table 65.
    Capriotti and Martini (1959) found parathion to inhibit the growth of
    microflora at normal levels of application, but Somer (1970) observed
    no such inhibition.  Cowley and Lichtenstein (1970) observed fungal
                                       434
    

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    inhibition at levels approximating field applications of parathion and
    of the seventeen fungi tested, none was able to use parathion as a
    source of carbon or phosphorus.  Since the data were obtained under
    laboratory conditions, the authors warned against extrapolation to
    field conditions.  Parathion was tested for mutagenicity in Esaher'ic'h.'ia
    Goli K-12 and was not mutagenic (Mohn 1973), but did inhibit aflatoxin
    synthesis by Aspergillus (Hsieh 1973).
    The effects of methyl parathion on soil microorganisms have been thor-
    oughly investigated by Naumann (1970a, 1970b, 1970c, 1970d, 1971), as
    summarized in Table 65.  Naumann noted that nitrogen-fixing bacteria
    were most affected by methyl parathion (formulated as Wofatox), where-
    as denitrifying bacteria and soil algae tended to remain unaffected.
    Bacterial populations tended to increase and fungal populations to de-
    crease (1970b).  When soil respiration was measured in a Warburg appa-
    ratus, 500 ppm or less of methyl parathion resulted in a decrease in
    soil respiration, followed several hours later by an increase; three
    separate additions of 5,000 ppm ended the respiratory stimulation after
    12 weeks.  The effects were similar in clay, sand, or compost, but were
    least marked in clay.  Formulated methyl parathion, in contrast to the
    pure compound, depressed actinomycetes, nitrogen-fixing bacteria, cell-
    ulolytic bacteria, denitrifying bacteria, and soil algae (I970d).  The
    data make it very clear that methyl parathion served as a substrate for
    soil microorganisms (1970c).  Mohn (1973) considered methyl parathion
    a probable mutagen after testing it in E. soli.
    Despite the melange of techniques, it would appear that parathion and
    methyl parathion stimulated the soil microflora, particularly bacteria.
    The source of such stimulation is those organisms which, using para-
    thion or methyl parathion as energy sources, multiply in their presence.
    Since only a small proportion of the total soil microflora, and even
    of the species known to degrade these pesticides, could be expected to
    have the actual capability of using parathion as an energy source, the
                                      438
    

    -------
    inhibition of pure cultures by parathion is not inconsistent with over-
    all stimulation of soil respiration.
    When algae (Anaoystus nidulans, Scenedesmus obliquus) and protozoa  (Eu-
    glena gracilis, Pavcaneciwn bwpsaria, Paramecizm rnultimicronucleatim)
    were exposed to parathion at one ppm for seven days, neither adverse
    effects nor any metabolites were found, although parathion was concen-
    trated from 50 to 116-fold (Gregory £t_ sd. 1969).  Cabejszek and Mal-
    eszevska (1970) found that 0.16 to 0.80 mg/liter (0.16 to 0.80 ppm)
    of methyl parathion decreased oxygen consumption by aquatic organisms
    within 30 minutes, but Luczak and Maleszevska (1966) observed no in-
    hibitory effect from methyl parathion formulated as Wofatox at ten
    mg/liter (10 ppm), and observed stimulation of nitrate-reducing bac-
    teria at 250 mg/liter (250 ppm).
    Plants—Parathion and methyl parathion are not considered to be phyto-
    toxic (Martin 1968).  At two Ibs/A (2.24 kg/ha), however, parathion
    decreased the stands of cucumbers, bush beans, and turnips, and reduced
    the quality of peas, cauliflower, and Swiss chard (Stitt and Evanson
    1949).  Sprays were less damaging than root drenches (Dennis and Ed-
    wards 1963).  In quartz sand at 30 ppm (equivalent to 16.8 kg/ha) para-
    thion increased the respiration of corn root tips (Lichtenstein et al.
    1962) .  Leaf damage to sorghum was reported from both parathion and
    methyl parathion  (Meisch et^ al_. 1970).  Parathion did not, however,
    accumulate in carrots under conditions producing residues of diazinon
    and other organophosphates (Bro-Rasmussen et al. 1969) .  Anaphase in-
    hibition was caused by 0.0001 to 0.05 percent solutions of parathion
    in the onion, Alli-im aepa; c-mitoses, chromosome and chromatid breaks,
    micronuclei and anaphase bridges were also observed (Ravindran 1971).
    Invertebrates—Methyl parathion at ten ppt killed 80 percent of Louis-
    iana red crayfish (Procambarus clarkii) within five days in the labor-
    atory, but 100 ppb had no effect in the field (Hendrick et_ al_. 1966).
                                       439
    

    -------
    Aquatic invertebrates were killed by levels of parathion ranging from
    0.004 ppm in the caddis fly (Aratopsyahe gvandis) to 0.032 ppm in the
    stone fly (Pteromareys ealifornicd); only endrin was consistently more
    toxic (Gauf in et^ ^. 1961, 1965).  Luedemann and Neumann (1962) point-
    ed out that, although the organophosphates were less toxic to fish
    than the organochlorines, both classes were equally toxic to piscine
    food organisms.
    The effects of organophosphates on soil invertebrates have been treated
    in the excellent review of Edwards (1973) who concluded that, although
    not as toxic to mites as many organochlorines, organophosphates are
    particularly toxic to predatory mites.  Effects on other soil inverte-
    brates were not well defined.  Parathion has long been considered high-
    ly dangerous to bees (Eckert 1948) , but was acutely less toxic to hon-
    eybees in the laboratory than dieldrin, azinphosmethyl, carbaryl, phor-
    ate, or DDT (Johansen 1961).  Dusts were twice as toxic to bees as
    sprays (Johansen et_ aL^. 1957).
    Fish and amphibians—The toxicity of parathion to fish varies from a
    96 hour TL  (median tolerance limit) of 0.055 ppm in guppies (Lebistes
    reticulatus) to 2.7 ppm in goldfish (Carassium awcatus)3 with bluegills
    (Lepomts maeroahirus) and fatheads (Pimephales promelas") intermediate
    (Pickering _e_t al. 1962) .  Leudemann and Neumann (1961) found three mg/
    liter (3 ppm) of parathion to be lethal to all rainbow trout (Salmo
    iyideus') and pike fry (Esox luci-us') which were exposed while the no-
    effect levels were 0.8 rag/liter (0.8 ppm) for trout and 1.0 mg/liter
    (one ppm) for pike.  Spermatogenesis in guppies was decreased by ex-
    posure to 0.1 to one ppm or parathion for more than six days; ten ppm
    were lethal within hours (Billard et al. 1970).
    Eisler (1970b) found that methyl parathion was less toxic to several
    species of fish than were the organochlorines, Phosdrin, malathion, or
    DDVP.  The 96 hour toxicity level of parathion was 5,200 to 75,800 ppb
    in piscine species including the American eel (Angiulla PO strata"), blue-
                                       440
    

    -------
    heads (Thalasoma bifasaiatum'), striped killif ish  (Fundulus majalis"),
    and striped mullet (Mugil cephalus').  Mulla and co-workers (1963)
    found methyl parathion, at levels used in controlling mosquito larvae,
    to be nontoxic to mosquitofish.  Parathion applied to ponds at 0.1  Ib/A
    (0.11 kg/ha) killed 22 percent of the mosquitofish (Gambusia affinis)
    added 30 hours after treatment (Mulla and Isaak 1961).  The toxicity
    was greater over a period of  240 than over 96 hours in the estuarine
    mummichog, Fundulus heteroclitus (Eisler 1970a).  Toxicity was in-
    creased by increasing water temperature from 10   to 30 C, increasing
    salinity, or decreasing the pH.  While the latter alterations in tox-
    icity might be due to nonspecific stress effects, the increased toxi-
    city after 45 minutes was undoubtedly due to paraoxon formation; great-
    er toxicity of longer time periods  suggests cumulative action either
    due to accumulation of toxicants, as with organochlorines, or progres-
    sive toxicity, as in the neurotoxicity evoked by  some organophosphate
    compounds.
    Lee and Buzzell (1969) induced respiratory changes in goldfish with
    0.56 mg/liter (0.56 ppm) of methyl  parathion although it took 3.20
    mg/liter (3.2 ppm) for 65 days to kill the fish.  Burke and Ferguson
    (1969) found that parathion was less toxic in flowing than static
    solutions, presumably because of the accumulation of paraoxon under the
    latter conditions.  DDT, toxaphene  and endrin, which do not require
    activation, were more toxic in flowing solutions.  Mount and Boyle
    (1969) hypothesized that more resistant species of fish might well ac-
    cumulate parathion to some extent,  although the catfish they studied
    (letalurus nebulosus") did not.
    Parathion caused nerve cell injury  in both carp (Cyprinus aarpio L.)
    and river crabs (Cambarus affinis Say) in a study by Kayser ert_ al.
    (1962).   No data on piscine carcinogenesis, mutagenesis, or teratogen-
    esis were found.  Resistance  to chlorinated hydrocarbon insecticides
    did not confer parathion resistance on sunfish or shiners (Minchew and
    Ferguson 1969).
                                      441
    

    -------
    Amphibians were found to be relatively resistant to organophosphates
    (Mulla 1962).  In the toad, Bufo viridis, a lethal injection into the
    dorsal lymph sac required 967 mg/kg of parathion or 188 trig/kg of para-
    oxon (Edery and Schatzberg-Porath 1960).
    Birds—The acute oral LD Q of methyl parathion is 6.12 to 16.3 mg/kg in
    mallards and 5.7 to 11.9 mg/kg in pheasants (Tucker and Crabtree 1970).
    Parathion has an acute oral LD   of 0.125 to 0.250 mg/kg in fulvous
    tree ducks, 1.37 to 2.96 mg/kg in mallards, and 12.4 mg/kg in pheasants
    (Tucker and Crabtree 1970).  Keith and Mulla (1966) found no definite
    toxicity when mallards were fed five ppm parathion daily for five to
    nine weeks, but 25 ppm were essentially lethal.  Heath and co-workers
    (1972) calculated the LC   for five days of treated feed followed by
    three days of clean feed to be 90 ppm of methyl parathion in bobwhites,
    682 ppm for mallards, 46 ppm for Japanese quail, and 116 ppm for phea-
    sants.  For parathion, the corresponding LC   was 44 ppm in Japanese
    quail, 364 ppm in pheasants, with bobwhites and mallards intermediate.
    Methyl mercury (Morsdren) was found to potentiate the action of para-
    thion in coturnix quail (Dieter and Ludke 1975) .
    Parathion was teratogenic in chickens if injected into the eggs (Up-
    shall et_ al. 1968, Roger et al. 1969, Yamada 1972, Reis et_ _aJL_. 1971,
    Dunachie and Fletcher 1969, Meiniel 1974) and in Japanese quail when
    eggs were dipped into a ten percent solution (Meiniel et al. 1970,
    Meiniel 1973).  Sterilization and feminization of treated offspring
    were also observed (Lutz-Ostertag et al. 1970).
    Mammals—Methyl paraoxon and paraoxon inhibit acetylcholinesterase in
    mammals, and poisoning is due to the resulting potentiation of neural
    synaptic transmission by acetylcholine.  Since the active agent in
    cholinesterase inhibition is not the phosphorothionate itself, species
    differences in sensitivity to parathion and methyl parathion may be
    due to differing rates of conversion to the analogs (paraoxon and methyl
    paraoxon), differing sensitivities of the cholinesterases to inhibi-
                                      442
    

    -------
    tion, or differing rates of metabolism of the oxygen analog (Murphy et
    al. 1968).  A succinct review of the mechanisms of action and toxicity
    of the organophosphates is presented by Fest and Schmidt (1973).
    Both parathion and methyl parathion are readily absorbed through the
    lungs or skin as well as by ingestion.  The minimum toxic level for a
    human adult is estimated at 7.5 mg per day for parathion and somewhat
    over 19 mg per day for methyl parathion (Rider et al. 1969).  Faerman
    et al. (1969) found hematological abnormalities in workers producing
    organophosphates:  iron-deficiency anemia, lower hemoglobin content,
    and erythrocyte degeneration were observed.  The acute toxicity of
    parathion in man is sufficiently great to warrant the conclusion that,
    regardless of the expected degree of occupational exposure, almost any
    person who works with parathion is in danger of being poisoned if he
    is careless (Arterberry et al. 1961).
    The acute oral LD   of parathion is 13 mg/kg in male and 3.6 mg/kg in
    female rats; that of methyl parathion, 14 mg/kg in male and 24 mg/kg
    in female rats (Martin 1968, Gaines 1969).  The acute oral LD   of pa-
    rathion was 11 mg/kg in mice (Klimmer and Plaff 1955), 22-24 mg/kg in
    mule deer and 28 to 56 mg/kg in domestic goats (Tucker and Crabtree
    1970).  The acute dermal LD   of parathion in rats is 21 mg/kg in males
    and 6.8 mg/kg in females (Martin 1968).
    In tissue culture of normal cells (human skin fibroblasts) and malig-
    nant cells (HeLa), it was observed that the direct cellular toxicity
    of parathion was greater than that of paraoxon.  The direct cellular
    toxicity of p-nitrophenol, the major terminal residue of parathion,
    was as great as that of parathion itself (Litterst and Lichtenstein
    1971).
    Aldrin, chlordane, and DDT were found to protect somewhat against or-
    ganophosphate poisoning (Triolo and Coon 1966, Williams et_ a^. 1967,
    Chapman and Leibman 1971).  Triolo, Mata and Coon (1970) hypothesized
    that rat serum aliesterases bind paraoxon, and thus the well established
                                      443
    

    -------
    enhancement of serum esterases by organochlorine insecticides mediated
    paraoxon detoxification.  Parathion inhibits the metabolism of benzo-
    (a)pyrene in rats (Weber et al. 1974) .
    Parathion is embryotoxic in all species studied.  When female rats
    were given methyl parathion three days  before parturition, methyl para-
    oxon was found in all fetal tissues within twenty minutes (Ackermann
    1974, Ackermann and Engst 1970).  Rat fetuses treated to day 17 were,
    however, found to have normal levels of acetylcholinesterases, sugges-
    ting that younger fetuses cannot convert parathion to paraoxon (Talens
    and Wooley 1973).  Tanimura et al. (1967) reported normal litters from
    rats treated on day 12 of pregnancy.  Leibovich (1973) reported de-
    creased numbers of neonates and decreased survival among rats born to
    dams who were fed parathion (0.1 to ten mg/kg) throughout pregnancy.
    Embryotoxicity, but not teratogenesis,  was reported in offspring of
    female rats fed 1.4 mg/kg/day of parathion for one week following mat-
    ing (Noda et_ al. 1972).  Implantations  decreased and resorptions in-
    creased.  Kimbrough and Gaines (1968) found parathion to be teratogenic
    as well as embryotoxic in rats only if  maternal toxicity occurred.  In
    mice, methyl parathion induced cleft palate (Tanimura e_t_ aJK 1967).
    Rats were reportedly more sensitive to  parathion treatment in early
    pregnancy than were hamsters (Lauro et  al. 1969) .  Data on other spec-
    ies of laboratory mammals were not available.
    The sum of these data is that parathion is acutely toxic and exerts
    considerable stress on the maternal organism; direct effects on the
    embryo have not been ruled out, but have not been seen in the rat.
    There are no data available suggesting that parathion and methyl para-
    thion are either carcinogenic or mutagenic.  Data to the contrary were
    also not available.
    Conclusions-
    The major hazard of parathion and methyl parathion in ordinary usage
    is clearly in their acute toxicity to mammals, birds, beneficial ar-
                                      444
    

    -------
    thropods and fish.  When applied at reasonable levels in the natural
    environment, parathion and methyl parathion are degraded within weeks.
    In the interim, transport can occur from soil into water and from
    water into sediment.  Volatilization inevitably occurs from soil fur-
    faces and from foliage, and quantifiable residues are taken up by food
    plants.  Nevertheless, the relatively rapid detoxification of these
    compounds by microbial degradation and by hydrolysis assures dissipa-
    tion.
    Under conditions of bulk disposal, however, degradation is significantly
    retarded (Naishtein et al. 1973) even when the massive treatments are
    soil-mixed, as would occur in spills.  If 31 pounds per acre are ap-
    plied, residues are found for sixteen years (Stewart et_ a^. 1971),
    while potentially lethal residues are found in the top inch of soil for
    five years after the equivalent of 190,000 Ibs/A were applied.  These
    data argue strongly against bulk disposal of parathion in the soil.
    Moreover, there are too few data available on the persistence, soil
    toxicity, and motility of p-nitrophenol and other metabolites of para-
    thion to permit evaluation of their effects on the environment.
    Nonbiological degradation of parathion production wastes is feasible,
    but requires extensive cleanup procedures (Stutz 1966).  More plausible
    would be controlled microbial degradation, preferably in a two-phase
    process which permits anaerobic detoxification followed by aerobic
    ring-cleavage as described by Sethunathan (1973a, 1973b) and by Sethu-
    nathan and Yoshida (1973a, 1973b).  No data are available on the feas-
    ibility of such a process on a large scale.
                                      445
    

    -------
    Malathion
    Malathion is the common name for  5-1,2-bis-(ethoxycarbonyl)ethyl  0,0-^,
    dimethyl phosphorodithioate, introduced by the American Cyanimid Com-
    pany in 1950 as Malaphos.  Its common name in West Germany and South
    Africa is mercaptothion; 5.n the USSR, carbofos.  Malathion is prepared
    by the addition of 030-dimethyl phosphorodithioic acid to diethyl mal-
    eate in the presence of hydroquinone (Martin 1968).  It is yellow to
    dark brown liquid with a melting point of 2.85 C, a boiling point of
    156  to 157 C at 0.7 mm mercury, and a vapor pressure of 4 x 10   mm
    mercury at 30 C.  Its solubility in water is 145 ppm at room tempera-
    ture and light petroleum oils are soluble to about 35 percent malathion.
    It is formulated as emulsifiable concentrates, dusts, and atomizing
    concentrates for use as a nonsystemic insecticide and acaricide.
    Degradation-
    Walker and Stojanovic (1973) analyzed the relative contributions of
    chemical and biological reactions to the degradation of malathion in
    soil.  They concluded that microbial degradation predominated, but
    that increasing pH or soil organic matter increased the importance of
    hydrolysis.  The relative contributions of chemical and biological
    reactions in three soils are shown in Table 66, and data on biological
    degradation are summarized in Table 67.
    Biological—Neither Trichoderma wivi-de nor Pseudomonas converted mala-
    thion to malaoxon, although both degraded malathion (Matsumura and
    Boush 1966).  Soil fungi (Pennicilium notation, Aspergillus niger) were
    able to degrade three mg malathion per 100 ml nutrient solution  (30
    ppm), but Ehizocton-ia solani was inactivated at this level, although
    active at two mg malathion per 100 ml nutrient solution (20 ppm) (Mos-
    tafa et al. 1972b) .  Rhizobiwn tvifo1i.-i degraded 95.5 percent of mala-
                                      446
    

    -------
         Table 66.  DEGRADATION OF MALATHION IN THREE SOILS
         OVER A 10 DAY PERIOD (WALKER AND STOJANOVIC 1973).
                          Total%%
    	Degradation (%)    Chemical	Biological
    Loam                   100              9            91
    Sand                    99              5            95
    Clay                   100             23            77
    Loam-water              85             40            60
    Sand-water              29              3            97
    Clay-water              75             47            53
                                447
    

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    thion within one week with only 0.5 percent being converted to malaoxon
    (Mostafa et_ al^. 1972a) .  Getzin and Rosefield  (1968) reported a stable,
    cell-free soil enzyme which converted malathion to its monoacid; the
    enzyme was resistant to heat, dessication, and microbial destruction.
    Sethunathan and Yoshida (1973a) identified a Flaoobaateviwn which de-
    graded parathion and diazinon but not malathion.  In alkaline soils,
    adsorption reportedly preceded degradation (Konrad et ajl. 1969).
    Malathion was readily degraded by sewage lagoon microorganisms  (Halvor-
    son £t_ al_. 1971).  In activated-sludge sewage  systems, the volume of
    organic matter was better correlated with the degree of degradation
    than was the volume of water.  A ratio of  malathion:microorganism  ::
    1:5  or less inhibited microbial degradation (Randall et^ SL^. 1967).  In
    surface water the rate of malathion degradation by natural and sewage
    microorganisms increased for five days, presumably reflecting changes
    in microbial populations (Jirik &t_ al. 1971) .
    Malathion sufficed as the sole source of carbon for a heterogeneous
    collection of bacteria from aquatic culture, but degradation proceeded
    only to the malathion-beta monoacid, which remained stable for at least
    4.5 months (Paris et^ aJ^. 1975).  An aquatic fungus, Aspergillus oryzae,
    also converted malathion to its monoacid, producing ethanol as a by-
    product, which served as a carbon source for the fungi.  Fungal trans-
    formation was, however, much slower than the bacterial transformation
    (Lewis et al. 1975).  In a microbial salt-marsh ecosystem, malathion
    was rapidly decomposed by indigenous bacteria, with a relatively insig-
    nificant contribution by those bacteria which use malathion as their
    sole source of carbon.  The major agents of degradation were carboxy-
    esterases and some phosphatases (Bourquin 1975).
    Paraoxon residues on plants inhibited malathion dissipation from plums,
    tomatoes, and string beans after harvest; neither parathion nor mala-
    thion itself was inhibitory (Koivistoinen et al. 1964).  Aldrin pre-
                                       449
    

    -------
    treatment, in contrast, increased malaoxon degradation (Cohen and Mur-
    phy 1974).  Wheat seed-coat enzymes converted malathion to its thio-
    late and phosphate (Rowlands 1966), and in rice grains malathion is
    converted to thiophosphoric acid (Tomizawa et al. 1962).
    Malaoxon is produced from malathion by mouse liver (O'Brien 1957),
    where its inactivation depends on an esterase highly sensitive to oth-
    er organophosphates.  Therefore, the toxicity of malathion can be
    sharply increased by the presence of other organophosphates (Cook et
    ail. 1957, 1958).  A lactating cow which was fed 63 ppm malathion for
    three days excreted 77 percent within one week; the remainder had not
    been excreted after three weeks (O'Brien et_ al_. 1961).
    In an aquatic-terrestrial ecosystem, malathion was exceptionally de-
    gradable:  no traces of the parent compound were found in any of the
    organisms.  The fish, snails, and mosquito contained several uncharac-
    terized metabolites, which were also found in water (Metcalf and San-
    born 1975).
    Photolytic—Mosher and Kadoum (1972) analyzed the dissipation of mala-
    thion from surfaces under the influence of light.  Themmost rapid de-
    gradation was observed with infra-red light and was due to the heat
    generated (119 C).  Far ultraviolet was a more effective light source
    for degrading malathion, than near ultraviolet light.  Decomposition
    products included malaoxon, malathion monoacid, malathion diacid, 0,0-
    dimethyl phosphorothioic acid, dimethyl phosphate, phosphoric acid,
    and unidentified products.  Malathion disappeared most rapidly from
    glass beads, and least rapidly from wheat grains.  Sorghum grains were
    intermediate (Mosher and Kadoum 1972).
    Anthraquinone accelerated the photodecomposition of malathion on silica
    gel chromatographic plates (Ivie and Casida 1971).  After 16 hours of
    exposure to ultraviolet light at 37 C, 66 percent of the malathion had
    disappeared from ladino clover (Archer 1971).  Wolfe and co-workers  (1975),
    using wave lengths above 290 nm, estimated the photolytic half-
                                        450
    

    -------
    life of malathion to be 990 hours (41.25 days) in water at pH 6, but
    only 16 hours in Suwannee river water which contained large amounts of
    colored material.
    Chemical—Malathion was more rapidly degraded in clay loam in which
    heat-labile substances had been destroyed than in the original soil
    (Getzin and Rosefield 1968).  In water at pH 10, malathion decomposed
    to the dimethyl phosphate and succinic or thiosuccinic esters (Shev-
    chenko et al. 1974).  Degradation is extremely rapid at high pH (Paris
    and Lewis 1973) but proceeds quite slowly at low pH, and Wolfe et al.
    (1975) reported that malathion persisted for up to two weeks in oxygen-
    saturated acidic water.  Spiller (1961) could not detect degradation
    after 12 days at pH 5.0 to 7.0, and similar results were obtained for
    pH 2.0, 4.0, and 6.0 (Konrad et al. 1969).  In neutral solution, mala-
    thion was 70 percent hydrolyzed in one week (Cowert et al. 1971).
    Of malathion formulated in Zeeklite (a quartz cristobalite) 8.4 to 9.2
    percent had decomposed after 30 days at 40 C, while 36.9 percent of
    the malathion formulated on clay L had decomposed in the same period
    (Takehara et al. 1967b).  The decomposition of dusts was not affected
    by moisture but was catalyzed by copper, lead, mercury or tin (in de-
    creasing order of efficacy) while the decomposition of emulsions in-
    creased with increasing moisture (Yamauchi et al. 1959).  When mala-
    thion was applied to a calcareous (alkaline) West Point loam at the
    equivalent of 11,227 kg/ha (five tons per acre), carbon dioxide evo-
    lution decreased if analytical grade malathion was used, but increased
    when formulated malathion was used, presumably due to degradation of
    the carrier (Stojanovic et^ al. 1972a).
    Malathion was completely degraded by treatment with liquid ammonia and
    metallic sodium or lithium (Kennedy et_ auL. 1972a).  Treatment with 8N
    sodium hydroxide decomposed malathion to inorganic phosphate, while
    I5N ammonium hydroxide partially decomposed it (Kennedy et_ al_. 1972b).
    Ozone treatment of malathion-contaminated water reportedly decreased
                                     451
    

    -------
    the toxicity of the water (Gabovich and Kurennoi 1966).
    Physical—Cobalt-60 
    -------
    et_ al_. 1969), but when malathion was  used  to  disinfect  stables,  0.08
    to 0.28 ppm were detected  in  the milk for  up  to  three months  (Milhaud
    et^a^. 1971).
    Carp exposed to 2.5 mg/liter  of malathion  (2.5 ppm)  for four  days  ac-
    cumulated 7.91 + 2.27 mg/kg in their  livers  (Bender  1969).  In a salt
    marsh in northwestern Florida, 0.42 kg/ha  were applied  in  three  fog-
    gings at two week intervals and blue  crabs (Callineetus sopi-dus} ,  grass
    shrimp (Palaemonetis vulgaris, Palaemonet-Ls pugio),  pink shrimp  (Pen-
    aeus duoramon) and sheepshead minnows (Cypr-inodon varietgatus) confined
    in the treated area contained no measurable residues of malathion, nor
    did snails (Littorina irrorarata'), but plants (Juncus sp.)  contained
    0.05 to 0.10 ppm malathion for up to  14 days.  Water retained traces
    of malathion for one day  (Tagatz et al. 1974).
    Volatilization-
    Ethanol solutions of malathion were evaporated to dryness  on  watch
    glasses and kept at 35 C for  90 days.  Not more  than 7.5 percent of the
    malathion volatilized in the  first fifteen days; 41  to  49  percent had
    volatilized after 90 days; and the lower levels  of volatility were ob-
    served with malathion of greater purity (Alessandrini and  Amormino
    1954).
    Persistence-
    The persistence of malathion  in soil, in water,  and  on  organisms is
    summarized in Table 68.  Malathion residues were found  in  43  percent
    of the soils sampled in five  west Alabama  counties (Albright  et  al.
    1974).  Malathion was more persistent in muck than in soil  with  low
    organic matter content and soil residues of malathion after eight days
    were said to be three percent (Lichtenstein 1965).   Krishnan  and co-
    workers (1958) claimed five week residual  effectiveness  for water-dis-
    persible malathion powders.   Chopra and Girdhar  (1971)  found  persis-
    tence to increase with increasing pH, decreasing relative humidity,
                                      453
    

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    increasing concentration, and decreasing exposure to ultraviolet light.
    On plants, ultralow volume sprays were approximately twice as persis-
    tent as emulsified concentrations (Saini et al. 1970).
    In water, malathion is hydrolyzed almost instantly at pH 12, but not
    at all at pH 5 to pH 7 (Spiller 1961) .  Paris and Lewis (1973) sugges-
    ted that malathion may be relatively persistent in aquatic systems be-
    cause it is not rapidly destroyed at neutral pH but in samples of riv-
    er water ranging from pH 7.3 to 8.0, malathion residues after seven
    days were 25 percent of the original level and after four weeks no
    malathion was detectable (Eichelberger and Lichtenberg 1971).  Menzie
    (1972) characterized the persistence of malathion in water as "variable",
    but noted that it persisted less than one day in fish.  In cattle, 2.7
               32
    percent of   P-malathion remained in the hide after two weeks (March
    et al. 1956).
    Very little has been published on the fate of non-insecticidal metabo-
    lites of malathion.  Lenon and co-workers (1972) reported the presence
    of an unidentified metabolite of malathion in all of 49 cisterns tested
    on the Virgin Island while malathion itself was present in only two of
    the cisterns, at levels of 0.01 ppb and 0.14 ppb.  Paris et_ a\^. (1975)
    reported that both ieta-malathion monoacid and malathion diacid were
    stable for 4.5 months in aquatic cultures.
    Effects on Non-Target Species-
    Microorganisms—Malathion was not mutagenic in Eschepi-ehia eoli under
    conditions in which a number of organophosphates were mutagenic (Mohn
    1973).  Yurovskaya and Zhulinskaya (1974) claimed that any effects of
    malathion on soil microorganisms were only temperary.
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    Table 69.  Algae were considered less sensitive to malathion than either
    protozoa or rotifers (Ranke-Rybicka and Stanislawska 1972); DaSilva and
    co-workers (1975) reported that malathion at a level of 100 ppm initially
                                       455
    

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    inhibited algal growth and subsequently stimulated it.  One species
    among nine algae tested, (Cylindpospermum musoiaola) was already ex-
    ceeding control growth after one hour; one species (Nostoc derived
    from Collematenax) never reached the control levels of growth.  The
    other seven species (See Table 69) were below control levels after one
    hour, and well above after 28 days.  In sewage disposal lagoons, levels
    of malathion as low as one ppm caused 0.83 percent mortality (Steelman
    et al. 1967).
    The effects of malathion on soil processes and soil microorganisms are
    summarized in Table 70.  At 10 pg/ml (10 ppm) malathion completely in-
    hibited Nitrosomonas europaea, but 1000 yg/ml (1000 ppm) were required
    to inhibit Nitrobaater agilis (Garretson and San Clemente 1968).  In an
    upland Novalickes clay loam, malathion decreased the total nitrogen
    concentration of the soil, and first decreased, but then increased,
    soil levels of phosphorus and calcium (Vicario 1972).  Gram-positive
    bacteria were more sensitive to malathion than gram-negative bacteria
    (Nestor 1972) and malathion was toxic both to entomogenous fungi and
    to pathogenic fungi (Hulea and Piticas 1973).  Aflatoxin synthesis in
    Aspergillus was inhibited by malathion (Hsieh 1973).
    At five tons per acre  (11,227 kg/ha), formulated malathion strongly in-
    hibited bacteria and streptomyces, and slightly inhibited fungal growth.
    Malathion itself inhibited bacterial growth  slightly, and stimulated
    streptomyces (Stojanovic et^ a^. 1972a).
    Invertebrates—Malathion applied to white clover (Trifolium repens") at
    1.25 Ibs/A (1.39 kg/ha) of wettable powder or emulsifiable concentrate
    was not residually toxic to honeybees (Clinch 1969), but 0.50 to 0.75
    Ibs/A (0.61 to 0.84 kg/ha) was toxic to all  bees in the field (Ander-
    son and Atkins 1958).  A 48 hour exposure to malathion reportedly in-
    creased tolerance of copepods in the contaminated areas to malathion
    (Naqvi and Ferguson 1968, 1969).  In treated and control areas  of a
    pine hardwood forest, microarthropod populations did not differ one
                                       457
    

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    year after treatment of podzol soil with  2  Ibs/A  (2.24 kg/ha)  of raala-
    thion (Hartenstein 1960), but MacPhee and Sanford  (1956)  described  the
    effects of raalathion on beneficial arthropods in Nova Scotia apple  or-
    chards as drastic.
    The knock-out level of malathion for Dctphnia magna was ten ppm for  19
    minutes (Klimmer and Plaff 1955), while the median tolerance limits
    for freshwater shrimp (.Gcamarus locustTis) was 0.00162 mg/1  (0.00162
    ppm) (Gaufin et^ al. 1965).
    Fish and amphibians—Malathion is less toxic to fish than endrin or
    endosulfan (Toor et al. 1973).  All rainbow trout  (Salmo  ir-ideus) died
    when exposed to one mg/liter  (one ppm); the 96 hour LC    was 0.17 ppm
    (Pimentel 1971).  In ponds, 0.5 Ib/A (0.56 kg/ha) of malathion killed
    48 percent of the mosquitofish (Gambus-uz  aff^nis) which were placed in
    the water after 24 hours, and 70 percent  of those placed  in the water
    48 hours after malathion treatment (Mulla and Isaak 1961).  Emulsifiable
    concentrates were more toxic than technical grade malathion to four
    species of warm-water fish, but the difference was slight (Pickering
    et_al. 1962).
    Birds—The acute oral LDsn for young mallards was 1485 mg/kg,  and the
    LC,.-. was over 5000 ppm when two week old  birds were fed treated feed
    for five days followed by clean feed for  three days (Pimentel  1971).
    Feeding of 0.1 ppm malathion decreased egg production in  hens  (Sauter
    and Steele 1972).  Transient paralysis lasting for four to 14  days
    was observed in chickens given 100 mg/kg  of malathion (Gaines  1969).
    In tissue culture, the ID(-0 (the dose causing 50 percent  growth inhi-
    bition) of malathion on embryonic chick muscle was between ten and
    100 ppm (Wilson et al. 1973).  Malathion  caused hypoglycemia and in-
    creased histogenesis of the islets of Langerhans in chicken embryos
    (Arsenault and Gibson 1974).
    Injection of malathion into the yolks of  hens' eggs caused malforma-
    tions of legs and beaks (Walker 1971; Greenberg and LaHam 1969, 1970;
                                       459
    

    -------
    Mclaughlin et^ sd. 1963; Dunachie and Fletcher 1969; Roger et^ a^. 1969).
    Levels as low as 15 yM were effective, and cholinesterase inhibition
    was not the basis for teratogensis, which could be prevented by nico-
    tinamide (Walker 1971).  Quinolinic acid, nicotinic acid, glycine, and
    tryptophan also decreased the incidence of malformations but only tryp-
    tophan prevented growth retardation (Greenberg and LaHam 1970).
    Mammals—The inhibition of cholinesterase by malaoxon is minimal in
    mammals because of the rapid hydrolysis of malaoxon (Cook et_ al. 1958,
    Murphy et al. 1968, Dauterman and Main 1966).  The acute oral LD_. of
                                                                    50
    malathion in rats is 1,000 mg/kg in females and 1,375 mg/kg in males
    (Gaines 1969):  Jones £t a^. (1968) cited 1,400 and 1,900 mg/kg.
    Among the reported effects of sublethal doses of malathion are hyper-
    glycemia in rats given a subclinical dose of two to 2.5 mg/kg subcut-
    aneously (Ramu and Drexler 1973) and decreased nidation and increased
    early resorption in rats given malathion four to eight days after in-
    semination (Lauro £t_ aL. 1969).  In tissue culture, malathion at 200
    to 400 pg/ml (200-400 ppm) inhibited mitoses (Huang 1973); growth of
    Chang liver cells could be inhibited by 15 yg/ml (15 ppm) (Gabliks and
    Friedman 1965).  Malathion also inhibited the in vitro replication of
    vaccinia and poliomyelitis viruses (Gabliks 1967).  In rats treated
    with 4,000 mg/kg (4,000 ppm) for two generations, the only adverse ef-
    fect reported was an increase in ringtail disease in the second gener-
    ation (Kalow and Marton 1961).
    In humans, malathion is a moderately potent allergen, with allergies
    occurring under field conditions (Milby and Epstein 1964).  Danilov
    (1968) recommended a distance of 1,000 meters between areas of malathion
    production and human or animal habitations, because of the hazards of
    byproducts and waste products.
    Conclusions-
    The rapid degradation of malathion makes it eminently suitable for soil
    disposal because of its short persistence and minimal effects on soil
    processes.
                                       460
    

    -------
    Diazinon
    Diazinon is the coiranon name for 0,0-diethyl £>-6-methyl-2-(l-methyl-
    ethyl)-4-pyrimidinyl phosphorodithioate, introduced by the Geigy Chem-
    ical Company in 1952 as Basudin.  It is a nonsystemic insecticide with
    some acaricidal activity.  Diazinon is prepared by the condensation of
    diethyl phosphorochloridothionate with 2-isopropyl-4-methyl pyrimidin-6-ol,
    which was in turn prepared by the condensation of isobiityramidine and
    ethyl acetoacetate (Martin 1968).  It is a colorless oil with a boiling
    point of 83° to 84°C at 0.002 mm Hg and a vapor pressure of 1.4 x 10
    mm Hg at 20 C.  Its solubility in water is 40 ppm at room temperature
    and it is readily miscible with ethanol, acetone, and xylene.  It is
    also soluble in petroleum oils.  Technical diazinon is a dark brown
    liquid of approximately 95 percent purity.
    Degradation-
    Biological—Diazinon is degraded in soil by a combination of microbial
    and chemical reactions.  The initial step is the hydrolysis of the het-
    erocyclic P-0 bond, resulting in formation of diethylthiophosphoric
    acid and 2-isopropyl-4-methyl-6-hydroxyprimidine (Getzin 1967, Lich-
    tenstein ejt al. 1968, Bartsch 1973).  The latter product is resistant
    to further degradation under anaerobic conditions, (Sethunathan 1972a,
    Sethunathan and Yoshida 1969, 1973a).  Sethunathan and MacRae (1969)
    considered chemical hydrolysis to precede microbial action, but Seth-
    unathan (1972a) subsequently reported greater persistence of diazinon
    in sterilized than in normal soil, and also noted increased hydrolysis
    of diazinon after repeated applications (Sethunathan 1972a, 1972b).
    Microbial degradation of diazinon is summarized in Table 71.
    Tetraethylpyrophosphate was cited as one product of microbial diazinon
    degradation (Paris and Lewis 1973).  A Flavobacteriwn species isolated
                                        461
    

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                                                       14
    from paddy water was able to convert 30 percent of   C-labeled diazi-
    non to carbon dioxide, with intermediate formation of 2-isopropyl-6£
    methyl-4-hydroxyprimidine; diazinon itself was 95 percent depleted
    within 72 hours  (Sethunathan and Yoshida~1973a).  Diazinon was more
    rapidly degraded in sand than in loam, and more rapidly in moist  than
    in dry soil; steam-treating the soil affected persistence more than
    soil type, moisture levels, or concentration  (Bro-Rasmussen et al.
    1968).  Decreased diazinon degradation due to destruction of heat-
    labile soil substances was not observed by Getzin and Rosefield  (1968).
    However, hydrolysis of diazinon to diethylthiophosphoric acid and 2-£.
    isopropyl-4-methyl-6-hydroxypyrimidine occurred readily in the presence
    of sodium azide  (Lichtenstein et al. 1968).
    When diazinon was applied to the surface of paddy soil, emulsions were
    more rapidly degraded than granules (Masuda and Fukada 1970).  In a
    New York State muck soil, addition of marl (a finely powdered mixture
    of calcium carbonate and clay) speeded diazinon degradation in unster-
    ilized soil, but retarded it in autoclaved soil (Kageyama et^ a^.  1972).
    Nasim and co-workers (1972) reported that the degradation of diazinon
    in Dacca paddy field soil was carried out by unidentified, heat-labile
    substances; degradation reportedly proceeded for 24 hours and then
    stopped.
    Among the specific organisms which have been found to degrade diazinon
    are Arthrobaeter and Streptomyees acting together (Gunner and Zucker-
    mann 1968); Streptomyces alone in the presence of glucose (Sethunathan
    and MacRae 1969); TT-Ldhoderma vivide (Matsumura and Boush 1968) and
    FlavobaoteTium (Sethunathan and Yoshida 1972a, 1973a).  The latter also
    degraded parathion, but not malathion (Sethunathan and Yoshida 1973a).
    Two of eight microbial colonies tested by Hirakoso (1969) were able  to
    degrade diazinon.  Microorganisms from sewage lagoons degraded diazi-
    non less readily than either malathion or parathion (Halvorson et al.
    1971).  In mosquito-breeding polluted x^ater, diazinon remained unaltered
                                      463
    

    -------
    for days if the medium was alkaline (Hirakoso 1968).  Diazinon was re-
    moved from culture by all planktonic algae tested, but no estimates of
    degradation were made (Butler et^ al. 1975).
    Pseudomonas melophthora} the intestinal symbiote of the apple maggot,
    degraded diazinon to some extent, with 71 percent of the diazinon re-
    maining unmetabolized, 26.7 percent converted to water-soluble sub-
    stances, and 2.4 percent to solvent-soluble substances (Boush and Mat-
    sumura 1967).
    In plants, metabolism was primarily due to hydrolysis of the pyrimi-
    dinylphosphorus ester bond with foliage the main site of hydrolysis.
    Accumulation of 2-isopropyl-4-methylpyrimidin-6-ol, and possibly of
    conjugated metabolites, occurred in the leaves (Kansouh and Hopkins
    1968).
    Rat liver microsomes were capable of degrading diazinon in vitro to
    diethylphosphorothioic acid and diethyl phosphoric acid (Yang et^ al.
    1969); in vivo, rats excreted 50 percent of the radioactivity from
    14
      C-diazinon labeled at the pyrimidine and ethoxy moieties.  No pyri-
    midine ring cleavage was detected (Muecke et^ al. 1970).  Rats hydrolyzed
    the alkyl-P bond of diazinon to form diethylphosphoric acid at high
    levels of diazinon treatment.  At lower levels, hydrolysis of the
    aryl-P bond was the primary degradative pathway (Plapp and Casida 1958).
    Sheep treated with diazinon excreted hydroxy-diazinon and its isomer,
    diethyl-6-hydroxymethyl-2-isopropyl-4-pyrimidinyl phosphorodithionate,
    in their urine (Machin et al. 1972) .  Dogs excreted 50 percent of the
                           14
    total radioactivity of   C-labeled diazinon in their urine within 24
    hours; 16 percent as diethylphosphoric acid and 45 percent as diethyl-
    thiophosphoric acid (Iverson e_t^ al. 1975).
    Chemical and physical—Hydrolysis of diazinon in soil was considered
    to be adsorption-catalyzed rather than acid-catalyzed, was more rapid
    in soil than in water, and was extremely rapid at pH 2, but slow at
    pH 6.  Degradation was most rapid in Poygan sand (11 percent per day)
                                      464
    

    -------
    and least rapid in Ella sediments  (six percent per day); Kewaunee dolo-
    mitic till was intermediate.  Hydrolysis was considered more signifi-
    cant than bacterial action in the degradation of the parent compound
    (Konrad et^ al_. 1967).  In water between pH 3.1 and pH 10.4, diazinon
    was hydrolyzed to 2-isopropyl-4-methyl-6-hydroxypyrimidine at differ-
    ent rates although first-order kinetics applied to all pH tested.
    Diazinon persisted for less than 145 hours at pH 10.4, over 3200 hours
    at pH 9.0, and over 4435 hours at pH 7.4 (Gomaa et_ al^. 1969).   It was
    reported that formulated diazinon degraded during storage to form tet-
    raethylmonothiopyrophosphate (Mello et al. 1972).
    Photolytic—Ultraviolet irradiation of diazinon results in formation
    of hydroxydiazinon (Paris and Lewis 1973).  Photolytic degradation of
    diazinon was catalyzed by anthroquinone and to a lesser extent  by pen-
    tachlorophenol (Ivie and Casida 1971).
    Transport-
    Within soil—The biological activity of diazinon in soil depends both
    on soil type and on the soil moisture.  Diazinon is more toxic  in min-
    eral soil than in muck (Harris and Mazurek 1966a).  It is more  toxic
    in moist than in dry clay or sand  (Harris 1966b) but the effect is more
    pronounced in sand; diazinon is somewhat more toxic in dry muck than
    wet muck (Harris 1964a, 1964b).
    Diazinon was more mobile in brown forest soil than in either degraded
    chernozem or marsh soil, and was more mobile in soil than either phor-
    ate or lindane (Ostojic et_ al. 1972).  The diffusion coefficient of
    diazinon in a silt loam was calculated to be 0.63 mm  per day at 27 C,
    and increased with increasing temperature, decreasing soil bulk density;
    and, to a lesser extent, with increasing moisture (Ritter et^ al^. 1973).
    In 17.8 cm soil columns, diazinon was more mobile than triazine herbi-
    cides, chlorinated hydrocarbon insecticides, phorate, or disulfoton
    (Harris 1969a).
                                      465
    

    -------
    Between soil and water—Diazinon was completely eliminated from a model
    cranberry bog seven days after application (corresponding to six days
    after the bog was flooded); microflora were considered the main agents
    of degradation, but both fish and mussels accumulated diazinon.  After
    144 hours (six days), diazinon had been completely removed from the
    water (Miller et_ al_. 1966).  On a small agricultural watershed, the
    loss of diazinon in surface runoff or sediment was considered insigni-
    ficant (Ritter et^ a^. 1974).
    Volatilization—Volatilization accounted for the loss of 86 percent of
    the diazinon on watch glasses over a 90 day period at 35 C.  Loss of
    77.5 percent occurred within the first 15 days (Alessandrini and Amor-
    mino 1954).
    Into organisms—Diazinon was taken up by the roots of bean plants and
    translocated within plants.  If the roots were subsequently rinsed and
    placed in nutrient solution, diazinon migrated from the roots into the
    nutrient solution (Kansouh and Hopkins 1968).  Cabbages watered with
    two ppm of diazinon contained 0.01 ppm after 30 to 40 days, and tobac-
    co contained 0.02 ppm after 56 days (Miles et^ al_. 1967).
    In spinach, diazinon accumulated at more than one ppm in the leaves,
    and at up to 60 ppm in the roots, when the soil was treated with 10 ppm;
    residues in strawberries remained below 0.1 ppm, and no diazinon resi-
    dues were detected in onions even when soil levels were 100 ppm (Kono
    1974).  In rice paddies, diazinon applied to the water was absorbed by
    the leaf sheath of the plants whereas soil-applied diazinon was absor-
    bed through the roots; in the latter case, none of the radioactivity
    was released into the water (Hirano and Yashima 1969).  The maximum
    residues of diazinon in rice plants occurred five days after treatment
    (Sethunathan et_ al. 1971) .
               32
    Emulsified   P-diazinon was more rapidly taken up into rice leaves from
    paddy soil than were granules.  Residues of the former reached their
                                      466
    

    -------
    highest levels in leaves within one day of treatment, while leaf resi-
    dues after granule treatment rose continuously for 16 days after treat-
    ment (Masuda and Fukada 1970).  The major metabolites in rice leaves
    were (C2H50>2P(0))H, 50.4 percent;  (C2H50)2P(S)OH, 31.1 percent; H3P04
    and P(S)OH«, 7.2 percent.  In rice ears, the major metabolite (85.9
    percent) was (C_H 0)P(0)OH (Masuda and Fukada 1970).
    Persistence-
    Sterilizing soil by steam treatment reportedly increased the persis-
    tence of diazinon more than altering the type of soil, its moisture,
    or the level of diazinon applied (Bro-Rasmussen et al. 1968).  Sethu-
    nathan (1972a) and Sethunathan and MacRae (1969) reported that steri-
    lization increased the persistence of diazinon in all soils except
    acid clays (pH 4.7).
    Decreasing the temperature of the soil from 35  to 15 C increased the
    persistence of diazinon by a factor of eight (Getzin 1968); in another
    study,  reducing the soil temperature from 24  to 13 C lengthened the
    period of bioactivity of diazinon against a test insect (Folsonria oan-
    dida) from less than six weeks to 16 weeks (Thompson 1973).  Decreas-
    ing the soil moisture from 30 percent to 2 percent of field capacity
    increased the soil "half-life" of diazinon from six weeks to 16 weeks
    (Getzin 1968).  The effects of soil type, temperature, moisture, and
    sterilization all interact in determining the persistence of diazinon
    (Ero-Rasmussen et^ al. 1968).  At 90°F and 55-5 percent relative hu-
    midity, bioactivity of diazinon reportedly persisted for 29 days (Kal-
    kat e^ al. 1961).
    Kageyama et al. (1972) reported that the addition of marl (a finely
    powdered mixture of calcium carbonate and clay) halved the persistence
    of diazinon in ordinary muck soil, but enhanced its persistence in
    sterilized muck soil.  After seven months in sandy loam soil, one per-
    cent of two kg/ha diazinon remained, but ten percent remained in peaty
    loam (Suett 1971).  Diazinon residues of 13 percent remained in hen-
                                     467
    

    -------
    house litter after four weeks, (Galley 1972) and 4.6 percent remained
    in neutral aqueous medium after five weeks  (Cowert et al. 1971).
    Under ordinary agricultural conditions, the biological persistence of
    diazinon ranges between two and four weeks  (Krishnan et_ al_. 1968, Get-
    zin and Rosefield 1966, Bro-Rasmussen et^ al_. 1968, Harris 1969b, Harris
    and Hitchon 1970).  Read (1969) reported that the effectiveness of
    diazinon in mineral soil decreased steadily for one month and then re-
    mained nearly unchanged for during the second and third month.  In a
    newly developed irrigation district, foliar sprays of diazinon left
    initial residues of up to 3.34 ppm in the soil, which decreased to
    0.02-0.05 ppm within 1.5 to 2.5 months (Knutson et^ al. 1971).  When
    two to four times the normal agricultural levels of diazinon were ap-
    plied to a carrot field, less than 0.3 ppm remained in the soil 42 days
    later (Stobwasser 1963), and when 400 g/A (about 0.45 ppm) were sprayed
    on field-grown lettuce, somewhat less than 0.1 ppm (22 percent) were
    detectable after ten days (Coffin and McKinley 1964).
    In rice, diazinon was detected at 0.004 ppm 53 days after treatment
    with 2.5 kg/ha (Masuda and Kanazawa 1972).  When soil was treated with
    6 ppm, diazinon residues in the plant Impatiens batsami were detectable
    for 63 days (Augustinsson and Johnsson 1957).
    Data on the persistence of diazinon are summarized in Table 72 for those
    studies in which the residue remaining after a specific length of time
    could be calculated.  In summary, diazinon is most persistent if in-
    corporated at high levels into a cold, dry, alkaline soil which has
    never before been exposed to diazinon or parathion.  It is least per-
    sistent if sprayed at low levels onto a warm, moist, acid soil which
    has been repeatedly treated with diazinon.  Under the former conditions,
    diazinon might be expected to persist well over three months, while
    under the latter conditions it would be dissipated, if not degraded,
    within two to three weeks.
                                      468
    

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    Effects on Non-Target Species-
    Microorganisms—Diazinon was not mutagenic in Esaherichia ooli- under
    conditions in which several organophosphorus compounds were mutagenic
    (Mohn 1973).  Diazinon, but not its metabolites diazinon-oxon, diethyl-
    phosphorothioate, and 2-isopropyl-4-methyl-6-hydroxyprimidine, markedly
    inhibited the growth of heterotrophic aerobic bacteria (Robson and
    Gunner 1970).  At 40 to 120 kg/ha, diazinon formulated as Basudin in-
    hibited nodule formation in red clover  (Trifolium pvatense) grown on
    sandy soil.  Nodule formation was also  inhibited in alfalfa (Medioago
    sativa) grown on chernozem.  If applied at 80 to 120 kg/ha, diazinon
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    At 100 yg/g  (100 ppm), diazinon stimulated fungal growth for one week.
    Ammonification increased and nitrification decreased, but overall soil
    respiration was not affected (Tu 1970).  At high levels, diazinon in-
    hibited mycelial growth in the fungus Aspergillus (Eder 1963), but
    neither the growth nor the carbon-14 assimilation of the freshwater
    alga Scenedesmus quadriaaudatus was affected by diazinon in the culture
    medium (Stadnyk -ifoliwn repens) at
    1/8 pound per acre (0.14 kg/ha) of a 40 percent wettable powder caused
    28 percent mortality to bees present on the clover: residual toxicity
    after three hours was 78 to 92 percent mortality if 1/4 pound per acre
    (0.28 kg/ha) was sprayed (Clinch 1969).  In soil, diazinon decreased
    the numbers of parasitic mites and of paurapods; the numbers of spring-
    tails increased (Edwards et al. 1969).  Increases in the numbers of
    springtails were secondary to decreases in the numbers of predatory
                                     471
    

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    mites  (Edwards and Thompson 1973).  In an old-field ecosystem,  species
    diversity and density increased in the year following  treatment with
    14 Ibs/A (15.7 kg/ha) of diazinon (Malone et_ al. 1967).
    Plants—Diazinon at 14 Ibs/A  (15.7 kg/ha) increased root growth and de-
    creased shoot growth in an old-field ecosystem; the number and density
    of plant species increased for up to one year after treatment  (Malone
    et^al. 1967).
    High levels of diazinon reportedly inhibited both shoot and root growth
    in higher plants (Eder 1963), but Dennis and Edwards  (1963) did not
    consider diazinon phytotoxic.
    Fish and amphibians—Diazinon was not toxic to young rainbow trout
    (Salmo i-vldeus} at 0.1 mg/liter (100 ppm), caused some deaths at 0.4
    mg/liter (400 ppm), and killed all the trout at 0.5 mg/liter (500 ppm).
    Pike (Esox luci-us) were somewhat less sensitive, with  the first deaths
    occurring at 0.5 mg/liter  (500 ppm) and all the pike killed at two mg/
    liter  (2000 ppm) (Luedemann and Neumann 1961).  The 48 hour EC - (ef-
    fective median concentration) of diazinon was 170 ppb  in rainbow trout
    and 86 ppb in bluegills at 24°C (Pimentel 1971).  The  LD__ for bull-
    frogs was over 2000 mg/kg  (Tucker and Crabtree 1970).
    Birds—The oral LD   of diazinon was 3.5 mg/kg in young mallards and
    4.3 mg/kg in pheasants (Tucker and Crabtree 1970).  For redwinged black-
    birds and starlings, the acute oral LD^_ was 110 mg/kg and 2.0 mg/kg
    respectively (Schafer 1972).  The five day dietary LC,.- in bobwhites,
    pheasants, Japanese quail, and mallards was 245 ppm, 244 ppm, 47 ppm,
    and 191 ppm, respectively  (Heath et al. 1972).  Diazinon was terato-
    genic in chicks (Green 1970) and reduced hatchability  at levels of one
    ppm (Sauter and Steel 1972):  egg production declined  at 180 ppm (Von-
    dell 1958).
    Mammals—The acute oral LD_n of diazinon in rats is variously given as
    75 mg/kg in females and 108 mg/kg in males (Gaines 1968, Pimentel 1971):
    150 to 220 mg/kg (Schafer 1972) or even 300 to 600 mg/kg (Jones et al.
                                      473
    

    -------
    1968).  Formulated diazinon which had decomposed during storage was 30
    times as toxic to humans and to cattle as freshly formulated diazinon
    because of the formation of tetraethylmonothiopyrophosphate (Mello et
    all. 1972).  Like all organophosphates, the oxon of diazinon is a chol-
    inesterase inhibitor; its toxicology was described by Gysin and Margot
    (1958) and the toxicology of organophosphates including diazinon has
    been reviewed recently (Eto 1974).
    At 100 to 200 mg/kg, diazinon was both toxic to pregnant rats and ter-
    atogenic to their fetuses (Kimbrough and Gaines 1968).  Seven mg/kg
    and 30 mg/kg of diazinon did not produce congenital malformations in
    rabbits, and 0.125 and 0.25 mg/kg were not teratogenic in hamsters
    (Robens 1969).  A mutagenic effect  of diazinon on human peripheral
    leukocytes in culture has been reported (Tsoneva-Maneva et_ al. 1969) .
    Conclusions-
    Neither the persistence of diazinon itself nor its effects on soil pro-
    cesses and soil microorganisms is extreme.  Nevertheless, there is no
    conclusive evidence for the decomposition of diazinon to naturally
    occurring substances, and data are  lacking on the persistence, trans-
    port and effects of 2-isopropyl-4-methyl-6-hydroxypyrimidine in soil.
    Therefore, large-scale soil disposal of diazinon in the absence of
    further information is not recommended.
                                      474
    

    -------
    Disulfoton and Phorate
    Disulfoton is the common name for 0, (9-diethyl S'-2-(ethylthio)ethylphos-
    phorodithioate, introduced by Farbenfabriken Bayer AG in 1956 under
    the trade names Di-Syston and Dithio-Systox as a systemic insecticide
    and acaricide.  It is made by the interaction of the sodium salt of
    030-diethyl hydrogen phosphorodithioate with 3-chloroethyl thioethyl
    ether (Martin 1968) .  The pure compound is a colorless oil with a char-
    acteristic odor, a vapor pressure of 1.8 mm mercury at 20 C, and a
    water solubility of 25 ppm at 20°C.  Its boiling point is 62°C at 0.01
    mm mercury, and it is readily soluble in most organic solvents.  The
    technical product is a dark yellow oil.  Formulations include granules
    and impregnation on activated carbon.
    Phorate is the common name for G^O-diethyl £'-(ethylthio)methyl phos-
    phorodithioate, introduced by the American Cyanamid Company as Thimet
    in 195A.  It is a systemic insecticide used primarily to protect seed-
    lings from sap-feeding insects.  Phorate is made by the reaction of
    0,0-diethyl hydrogen phosphorodithioate with formaldehyde, followed by
    the addition of ethyl mercaptan.  It is a clear liquid with a boiling
    point of 118 to 120 C at 0.8 mm mercury, a freezing point below -15 C,
                                    -4                o
    and a vapor pressure of 8.4 x 10  mm mercury at 20 C.  Its solubility
    in water is 50 ppm at room temperature and it is readily miscible with
    vegetable oils and xylene, as well as with carbon tetrachloride and
    dioxane.  It is formulated as an emulsifiable concentrate, dusts and
    granules.
    Degradation-
    Biological—Data on metabolic products of disulfoton and phorate are
    summarized in Table 74.  The primary degradative pathways of disulfo-
    ton and phorate proceed via their sulfoxides to their sulfones, lead-
    ing to an increase in the anticholinesterase activity (Metcalf et al.
                                      475
    

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    476
    

    -------
    1957, Fukuto and Metcalf 1969).  Getzin and Shanks  (1970) analyzed the
    degradation of phorate and its oxygen analog in soil, and noted that
    phorate is converted to phorate sulfoxide and then  to its sulfone; in
    Sultan silt loam, conversion of phorate sulfoxide to phorate was also
    observed.  In a plant-soil model ecosystem, corn plants contained only
    metabolites of phorate even though the soil still contained unaltered
    phorate.  Corn roots as well as soil contained phorate sulfone and phor-
    ate  sulfoxide, while the leaves of the plants contained phoratoxon
    sulfoxide and phoratoxon sulfone (Lichtenstein et al. 1974).  When
    phorate was applied to soil in granular bands under field conditions,
    the major metabolite was phorate sulfone when the level of treatment
    was five Ibs/A (5.60 kg/ha), but phorate sulfoxide when the level of
    treatment was one Ib/A (1.12 kg/ha).  The oxygen analog of phorate was
    not found in submerged soils (Kawamori et_ al. 1971b) .
    Almost no degradation of either phorate or disulfoton occurred in soil
    in a 60 day period in summer, and degradation was significantly greater
    between October and April than in the summer; temperature played a
    greater role in determining the rate of degradation than did soil type.
    In the winter, disulfoton was degraded more rapidly than phorate; in
    summer, too little degradation took place to distinguish differences.
    The soil type and temperature effects interacted, with degradation be-
    ing more rapid in loamy sand in the winter and in silt loam in the sum-
    mer (Menzer et al. 1970).  Takase and co-workers (1972) examined the
    degradation of disulfoton in several soils.  Metabolism was more rapid
    in all soils under flooded (anaerobic) than under upland (aerobic) con-
    ditions, microbial oxidation was considered the major route of degra-
    dation, and little breakdown occurred in sterile soil.  A later study
    of the breakdown of disulfoton in sterile and glucose-amended soil was
    considered to provide evidence against microbial oxidation (Takase and
    Nakamura 1974).
    Whether the most rapid route of degradation in the field is chemical or
    biological has never been proven, but disulfoton is readily degraded by
                                     477
    

    -------
    microorganisms, at least under laboratory conditions:  most fungi
    (among twenty isolates tested) were able to use disulfoton as their
    sole source of carbon, as were most of the ten cultures of Streptomy-
    cetes tested.  Aspevgi,t1us f1avwny Ee1mint'kospovi.wn3 and two StTepto-
    myaes species were able to grow with disulfoton as their only source
    of carbon (Bhaskaran et al. 1973),
    In rats, the excreted metabolites of disulfoton were diethylphosphoro-
    thioic acid, diethyl phosphoric acid, and two unknown compounds, while
    phosphoric acid and traces of diethylphosphorodithioic acid were found
    in the rats' urine.  Intermediates in the rats' livers, 30 minutes
    after intraperitoneal injection of 10.5 mg/kg of disulfoton, included
    disulfoton sulfoxide and sulfone  (Bull 1965).
    Chemical and physical—Di-Syston applied to fertilizer, particularly
    superphosphates, decomposes as a result of catalytic oxidation  (Ibra-
    him et al. 1969).  When disulfoton and phorate were exposed to one to
    four Mrad of cobalt-60 gamma-irradiation, the corresponding sulfoxides
    and sulfones were found in most samples; the sulfoxide of the oxygen
    analog and the sulfone of the oxygen analog were found only after treat-
    ment with the full four Mrad dose.  Irradiation increased the inhibi-
    tion of beef liver carboxylesterases by the pesticides, suggesting
    that the radiation-induced degradation consisted mostly of activation
    (Grant et al. 1969) .
    Transport-
    Within soil—Phorate was less mobile than diazinon, and less mobile in
    degraded chernozem and in black marsh soil than in brown forest soil
    (Ostojic _e_^ al_. 1972).  McCarty and King (1966) considered disulfoton
    to move rapidly in soil-water systems.  Harris (1969b) compared the mo-
    bility of pesticides in 17.8 cm soil columns and found phorate and di-
    sulfoton to be only slightly mobile, albeit more mobile than the chlor-
    inated hydrocarbon insecticides.  No data were available on the trans-
    port of the metabolites of disulfoton or phorate within soil.
                                       478
    

    -------
    Between soil and water—In addition to transport through soil into
    water, transport on soil particles (washoff) can be a means of pesti-
    cide transport into streams and lakes.  Kawamori and co-workers  (1971a)
    noted that disulfoton adsorbs more readily to silty clay loam than to
    clay loam, and least readily to alluvial loamy sand.  They concluded
    that the high rate of recovery was due to adsorption on the organic
    rather than on the clay fraction.  Both compounds were most readily ad-
    sorbed to mineral soils (Harris and Hitchon 1970) and to silty loam
    and clay soils (Bhirud and Pitre 1972) when the soils were dry.  Soil-C
    adsorbed disulfoton could not be desorbed if soil had dried in the in-
    terim (Graham-Bryce 1967) .  Transport of newly desorbed disulfoton or
    phorate in runoff remains a possibility, but no data are available to
    assess its plausibility.
    Volatilization—Burns (1971) considered the 41 percent loss of phorate
    from sandy soil within the first three days after application to be
    due largely to volatilization.  Losses from clays and loams were much
    smaller.
    Into organisms—Both phorate and disulfoton are systemic insecticides,
    readily taken up by plants.  Soil treated with two pounds per acre (2.24
    kg/ha) of either phorate or disulfoton resulted in excessively high
    levels in spinach after 5.5 months; both parent compounds, their sul-
    foxides, their sulfones, and the sulfoxides of their oxygen analogs
    were found in the spinach (Menzer and Ditman 1968) .  When soil was
    treated with 30 kg/ha of five percent disulfoton granules (Solvirex)
    17 days after potatoes were planted, potato tubers contained 0.04 to
    0.11 ppm at harvest time (Trojanowski et_ al^. 1967).  Masuda and Kana-
    zawa (1972) detected 0.18 ppm disulfoton in unpolished rice 53 days
    after soil was treated with 2.5 kg/ha.  The residual levels of disul-
    foton in vegetables grown on treated soil were greatest in carrots,
    intermediate in Chinese cabbage, and lowest in turnips.  Carrots, rice,
    and soil contained relatively more disulfoton sulfone than disulfoton
    sulfoxide (Masuda and Kanazawa 1972).
                                       479
    

    -------
    When phorate was applied to soil or sand, only metabolites were found
    in the corn grown on the soil; oxidation appeared to occur in the plant,
    not in the soil.  Root residues were 2.5 to five times as great in
    plants grown on sand as in plants grown on agricultural soils, but leaf
    residues were the same regardless of the soil type (Lichtenstein et al.
    1974) .  Sorghum retained no residues of disulfoton 85 days after soil
    treatment (Singh et_ al_. 1972), but carrots contained phorate sulfone
    even in the second growing season after soil treatment (Lichtenstein
    et al. 1973).  Potatoes contained residues only in the growing season
    during which soil had been treated (Batora et al. 1967).
    Persistence-
    The available data on persistence of disulfoton and phorate in soil
    are summarized in Tables 75 and 76.  Persistence differs widely not
    only because of differing test conditions between experiments, but also
    because different assays were used.  Bioassays dominate the literature
    on phorate and disulfoton; the data are therefore skewed to include
    insecticidal metabolites of the applied insecticides.  Persistent but
    non-insecticidal metabolites have not been considered to any great ex-
    tent in studies available to date.  Among the possible factors decreas-
    ing the measured persistence of phorate and disulfoton are losses due
    to volatilization of sprayed insecticides and adsorption to soil.  The
    latter almost certainly serves to prolong soil retention even while
    decreasing persistence as measured by bioassays.
    Effects on Non-Target Species-
    Microorganisms—The effects of phorate and disulfoton on soil micro-
    organisms and soil invertebrates are summarized in Tables 77 and 78.
    Cowley and Lichtenstein (1970) observed inhibition in 13 of 17 fungal
    cultures treated with 40 yg/ml (40 ppm) of phorate, but in a fescue
    meadow treated with agricultural levels of phorate, both bacteria and
    fungi were stimulated for most of one year (Malone and Reichle 1973) .
                                       480
    

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    -------
    The latter report suggests that phorate decreased the populations of
    soil arthropods, with secondary increases in bacteria and fungi.
    Sreenivasula and Rangaswami  (1973) reported the stimulation of almost
    all soil microorganisms by phorate and disulfoton, but noted that, as
    the incubation progressed, gram-positive bacteria were displaced by
    gram-negative bacteria.  Laygo and Schulz (1963) reported recovery of
    soil microfaunal populations within nine days of phorate application
    even though the compound itself persisted more than 23 days.
    Invertebrates—Phorate decreased populations of Collembola and of soil
    arthropods other than mites  (Malone and Reichle 1973), and decreased
    total numbers of mites for more than nine months if applied at 4.5 kg/
    ha (Edwards and Thompson 1973).  Organophosphorus insecticides reduced
    the number and biomass of soil invertebrates less than did aldrin or
    dieldrin, but phorate and disulfoton significantly decreased populations
    of parasitic mites and paurapods, and increased populations of trombi-
    diform mites, oribatid mites, and springtails.  Phorate, but not disul-
    foton, significantly decreased earthworm populations (Edwards et al.
    1969, Edwards and Thompson 1973).
    The LD__ of phorate to bees was 0.004 percent (40 ppm) (Johansen 1961).
    The nectar of fuchsia and nasturtiums watered with 25 mg phorate was
    not toxic to honeybees and the acute oral LD,.- of disulfoton and phor-
    ate to honeybees was reported as greater than 20 yg/bee and 0.44 yg/bee,
    respectively (Lord et^ al. 1968).
    Disulfoton was toxic to aquatic insects at levels between 0.0082 mg/
    liter (stone fly, AoTonewcia paaifioa) and 0.24 mg/liter (freshwater
    shrimp, Gcamarus loeustr-is)  (Gaufin et^ al. 1965).  Disulfoton decreased
    survival and affected development of the eggs of both oysters (Crasso-
    strea. virginiaa) and clams (MevaencafLa meraenai"ia) at levels of one ppm
    or more (Davis and Hidu 1969).
                                      485
    

    -------
    Plants—At 60 kg/ha, disulfoton caused an initial delay in plant growth,
    followed by enhanced growth after 30 days (Kobayashi and Katsura 1968).
    A.t ten ppm, soil-incorporated disulfoton stimulated growth of bean and
    corn plants for six weeks, but at 100 ppm, growth inhibition occurred.
    Disulfoton at 100 ppm also increased the levels of nitrogen, phosphorus,
    potassium, calcium, and magnesium; and decreased levels of iron, cop-
    per, aluminum and zinc in the treated plants  (Cole et^ _al. 1968).  Di-
    sulfoton inhibited the metabolism of linuron and dicamba in leafy tis-
    sues (Chang et al. 1971).  Phytotoxicity between dalapon and either di-
    sulfoton or phorate was additive, indicating no interaction between
    the herbicide and either insecticide (Nash 1967).
    Fish and amphibians—Phorate at agricultural levels was toxic to carp
    (Lilly et_ al. 1969) .  The 96 hour median tolerance limit (TO for di-
    sulfoton was 0.063 ppm in bluegills (Lepomis maerochirus'), 0.25 ppm in
    guppies (Lebi-stes reti-culatus), 3.7 ppm in fathead minnows (Pi-mephales
    promelas), and 6.5 ppm in goldfish (Carassius auratus)  (Pickering et
    al. 1962).
    Birds—The acute oral LD   of disulfoton was greater than 32 mg/kg in
    starlings, and was 3.2 mg/kg in redwinged blackbirds; for phorate, the
    LD,-0 was 7.5 mg/kg in starlings and 1.0 mg/kg in redwinged blackbirds
    (Schafer 1972).  The dietary LC_n of disulfoton when birds were fed
    treated feed for three days was 333 ppm in Japanese quail (Cotumix
    ooturnix) , 715 ppm in bobwhite (Colinus wi-rg-inianus) , 634 ppm in phea-
    sants, and 510 ppm in mallards (Anas platyrhynchos) (Heath et_ al_. 1972).
    Phorate (as Thimet) injected into hens' eggs at two ppm on the 10th day
    of incubation decreased the hatchability from 89.7 to 27.5 percent,
    increased the thyroid size of the chicks, and was teratogenic (Richert
    and Prahlad 1972).
    Mammals—The acute oral LD   of phorate in rats was reported to be two
    to three mg/kg (Jones et al. 1968); for disulfoton, an LDcn of 12.5
                          	       '                      ju
                                       486
    

    -------
    mg/kg is cited by Pimentel  (1971), while Jones et al.  (1968) cited
    4 mg/kg.  Both compounds were toxic when applied to rats' skins, with
    a dermal I&c.n °f 7® to 300 rag/kg cited for phorate and 50 mg/kg for di-
    sulfoton (Jones et al. 1968).
    Conclusions-
    Most of the data on the persistence of phorate and disulfoton in soil
    are based on persistence of bioactivity, rather than on chemical per-
    sistence.  Moreover, essentially no data on the transport of either
    compound in soil, into water, or into air are available.  Therefore,
    no conclusions on the feasibility of soil disposal of either phorate
    or disulfoton can be drawn.
                                      487
    

    -------
    Az Inpho sme t hy 1
    Azinphosmethyl is the common name for 0, 0-dimethyl  £-(4-0X0-1,2,3-
    benzo-triazin-3(4H)-61)methyl  phosphorodithioate.  It is made by the
    interaction of ^-chloromethylbenzazimide with Ot 0-dimethyl hydrogen
    phosphorodithioate in the presence of a base.  A non-systemic insecti-
    cide and acaricide, azinphosmethyl was introduced by Farbenfabriken
    Bayer AG in 1953 and is known under the trade names Guthion and Gusa-
    thion.  Azinphosmethyl forms white crystals with a melting point of
    73 to 74°C.  It is very slightly soluble in water (3.3 ppm at 25°C)
    and is soluble in most organic solvents.  It is unstable above 200°C.
    Degradation-
    Biological — Microbial degradation of azinphosmethyl was presumed to ac-
    count for the faster loss of azinphosmethyl from natural than from
    sterilized soil, but non-biological factors appeared to predominate
    (Yaron e_t^ al_. 1974a, see below).  In mice, the microsomal and soluble
    fractions of liver cells were most active in converting azinphosmethyl
    to its oxygen analog, and also in degrading it to dimethyl phosphoric
    acid and dimethyl phosphorothioic acid (Motoyama 1972) .
    Chemical — Yaron and co-workers (1974a) analyzed the kinetics of
    phosmethyl loss from soil and concluded that both biological and chem-
    ical mechanisms contributed to its degradation.  A lag phase was obser-
    ved in all soils; subsequent degradation essentially corresponded to
    first-order kinetics.  Degradation was most rapid, and the lag phase
    least pronounced, in moist, unsterilized soil at warm temperatures.
    Table 79 shows the length of time required for the loss of 50 percent
    of the azinphosmethyl applied to a silty, loamy, loessial sierozem.
    Moisture affected the rate of degradation more than did microbial acti-
    vity, and temperature was extremely important in determining the half-
    life of azinphosmethyl within each soil/moisture combination.
                                     488
    

    -------
    Table 79.  NUMBER OF DAYS REQUIRED FOR 50% LOSS OF AZINPHOSMETHYL
        FROM SOIL AT THREE TEMPERATURES AND TWO LEVELS OF MOISTURE
                       (AFTER YARON ET_ AL. 1974a)
    
     ~~Sterile soilNatural soil
     Temperature       	            	
        (°C)	Dry	Wet	Dry	Wet
          6            484            88            484            64
         25            135            29             88            13
         40             36             6             32             5
                                    489
    

    -------
                                          o
    Photolytic—Ultraviolet light at 2537 A  decomposed azinphosmethyl la-
    beled at the carboxyl carbon.  The degradation products were:  benza-
    zimide, anthranilic acid, methyl benzazimide sulfide, ff-methyl benzazi-
    mide, and an unidentified water-soluble compound.  None of the products
    was insecticidal.  Degradation proceeded only in the light, and was
    more rapid in water at high pH than on glass.  In water at pH 10, 18
    percent of the metabolites were water-soluble, while at pH 11, 97 per-
    cent were water-soluble.  Azinphosmethyl was stable in water between
    pH 6 and pH 9 (Liang and Lichtenstein 1972).
    Transport-
    Through soil—Eight years after an undiluted (18.1 percent) emulsibiable
    concentrate of azinphosmethyl was applied to soil, no residues were de-
    tected below 37.5 cm in sandy loam soil (Staiff et_ a!U 1975).  Yaron et_
    al. (1974b) concluded that azinphosmethyl did not leach deeply into
    soil, and also that its leaching was unaffected by the amount of irri-
    gation.
    Volatilization—Azinphosmethyl was less readily volatilized from leaves
    or from soil than were diazinon, parathion, and several organochlorine
    insecticides (Lichtenstein and Schulz 1970).  Its volatilization from
    leaves was reportedly not affected by high temperatures (Hightower and
    Martin 1958).
    Into organisms—Azinphosmethyl applied to an irrigated field at normal
    agricultural levels resulted in residues in potato peels (Yaron et al.
    1974b) .
    Persistence-
    Staiff and co-workers (1975) assessed the persistence of several for-
    mulations and several levels of azinphosmethyl in sandy loam soil over
    an eight year period.  The soil pH ranged from 6.6 to 7.8, and rainfall
    averaged 25 cm per year.  Their data are summarized in Table 80.  They
    concluded that soil contamination by undiluted azinphosmethyl remained
                                       490
    

    -------
    Table 80.  RESIDUES OF AZINPHOSMETHYL IN SOIL AFTER CONTAMINATION
          WITH UNDILUTED  (18.1%) AND DILUTED (0.045%) EMULSIFIED
           CONCENTRATE SOLUTIONS AND DILUTED SOLUTIONS (0.045%)
                            OF WETTABLE POWDER.
    Contaminant;
    soil stratum
    EC-7: 18.1%;
    0-2.5 cm
    2.5-7.5 cm
    EC-7: 0.045%
    0-2.5 cm
    2.5-7.5
    WP-7: 0.045%
    0-2.5 cm
    2.5-7.5 cm
    Time
    1 day
    
    49,946 ppm
    30,488 ppm
    
    354 ppm
    23 ppm
    
    276.8 ppm
    107.0 ppm
    after application
    4 years
    
    6,075 ppm
    7,662 ppm
    
    1 . 5 ppm
    1 . 3 ppm
    
    2.0 ppm
    2 . 2 ppm
    
    8 years
    
    850 ppm
    967 ppm
    
    Nl£7
    Nl£7
    
    ND
    ND
    aj Emulsifiable concentrate
    W Not detected
    cj Wet table powder
                                    491
    

    -------
    a significant hazard for at least four years.
    The soil residues in the top 7.5 centimeters four years after the soil
    was contaminated with diluted azinphosmethyl at 0.045 percent (450 ppm)
    represented 1.6 percent of the initial residues, or a loss of 24.6 per-
    cent per year while the undiluted emulsibiable concentrate left resi-
    dues representing 2.5 percent of the initial residues after eight years,
    corresponding to a loss of 12.2 percent per year.  It was suggested
    that high concentrations of azinphosmethyl strongly inhibit soil micro-
    organisms, resulting in slower degradation of the pesticide.
    Soil-applied azinphosmethyl decomposed rapidly in Georgia cotton-grow-
    ing soil, but traces could be detected to the end of the third year
    (Roberts et_ al. 1962).  At agricultural levels in an irrigated field,
    azinphosmethyl reportedly disappeared within thirty days regardless of
    the amount of irrigation (Yaron et_ al. 1974).  Ruhr et_ al. (1974) also
    reported that three Ibs/A (3.36 kg/ha or 6 ppm) of azinphosmethyl de-
    creased to 1.6 ppm within thirty days in one orchard; essentially com-
    plete dissipation occurred within sixty days in a second orchard.
    In water, azinphosmethyl has a half-life of about thirty days at pH 9.0,
    but of less than seven days at pH 9.5, when the temperature is at 25 C;
    at 45 C and pH 9.5, the half-life decreased to less than one day (Heuer
    et_ al. 1974).  In comparing the persistence of water emulsion sprays
    with that of low-volume sprays on oat plants, Dorough and Randolph (1967)
    found that azinphosmethyl persisted longer as a low-volume spray (21
    days) than as a water emulsion spray (Seven days).
    Effects on Non-Target Species-
    Microorganisms—Azinphosmethyl reportedly had no effect on yeast res-
    piration of fermentation at concentrations ranging between 2 x 10   M
    and 2 x 10~3M (Eder 1963) .  Staif f et_ al^. (1975) considered it proba-
    ble that azinphosmethyl at high levels partially sterilized the soil,
    hindering its own degradation.
                                       492
    

    -------
    Plants—No reports of phytotoxicity were found for azinphosmethyl, but
    it has been reported to inhibit photosynthesis in the leaves of Red
    Delicious apples  (Heinicke and Foot 1966).
    Invertebrates—Azinphosmethyl is more highly toxic to earthworms  (Eis-
    enia sp.) than malathion or the organochlorines BHC, chlordane, hepta-
    chlor, aldrin and dieldrin (Hopkins and Kirk 1957).  It is highly toxic
    to honeybees (Anderson and Atkins 1958, Anonymous 1974).  When ladybird
    beetles were immersed in azinphosmethyl at concentrations of 0.5 lb/100
    gallons, 35 to 65 percent survived (Colburn and Asquith 1973).
    Fish and amphibians—The 96 hour TL.. of young salmonids to azinphos-
    methyl was 0.58 ppb (0.0006 ppm) for rainbow trout, 4.2 ppb (0.0042
    ppm) for coho salmon, and 4.3 ppb (0.0043 ppm) for chinook salmon
    (Katz 1961).  Only 13 percent of carp embryos exposed to one part per
    million survived to hatch; 0.1 ppm did not increase embryonic mortali-
    ty, but resulted in 100 percent mortality of all fry within 48 hours
    after eclosion (Malone and Blaylock 1970).  The toxicity of azinphos-
    methyl to bluegills and to rainbow trout increased with increasing tem-
    peratures (Macek et^ al. 1969).  At levels used for controlling mosquito
    larvae, azinphosmethyl was reportedly not toxic to the mosquitofish
    (Gambus-La) or to pollywogs (Mulla et al. 1963).
    Birds—The acute oral LDcn of azinphosmethyl was 125 to 150 mg/kg in
    mallards (Keith and Mulla 1966) and 277.2 mg/kg in 10 to 12 day old
    chickens (Sherman et al. 1967) .  The LC   of azinphosmethyl to baby
    chicks was 1197 ppm, but levels above 300 ppm decreased growth rates
    within one week (Steve £t_ a.l_. 1961).  Injection of one mg azinphosmethyl
    into chicken eggs was teratogenic (Upshall et al. 1968).  Chickens fed
    40 mg/kg azinphosmethyl developed leg weakness (Gaines 1969).
    Mammals—The acute oral LD5Q of azinphosmethyl in rats is 15 mg/kg (Eto
    1974).  No data were available on the carcinogenicity, mutagenicity,
    teratogenicity, or other reproductive effects of azinphosmethyl.
                                       493
    

    -------
    Conclusions-
    Despite its apparently rapid dissipation in soil, and its consequently
    minimal leaching, the feasibility of disposing of azinphosmethyl in
    soil is not demonstrated by the data.  Staiff and co-workers (1975)
    have indicated a tendency for higher levels of soil contamination to
    resist degradation; no contrary data are available.  There is plenti-
    ful evidence, however, that temperature and moisture exert a strong
    effect on the rate of azinphosmethyl degradation.  Therefore, the
    least objectionable site for soil disposal of azinphosmethyl wastes
    would be a moist, semitropical soil.  Since wettable powders appear to
    degrade more quickly, but leach more readily than emulsifiable concen-
    trates, no conclusions concerning relative risks of different formula-
    tions can be drawn.
                                      494
    

    -------
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    -------
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                                      528
    

    -------
    Tomizawa, C., T. Sato, H. Yamashita and H. Fukuda; 1962.  Decomposition
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                                       529
    

    -------
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                                      530
    

    -------
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                                      531
    

    -------
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      Biodegradation of parathion.  Plant Soil 33:273-281.
                                      532
    

    -------
    CARBAMATE INSECTICIDES
    Carbaryl
    Carbaryl is the common name for 1-naphthyl W-methyl carbamate, intro-
    duced by the Union Carbide Corporation in 1956 as Sevin.  A contact
    insecticide with slight systemic properties, carbaryl is made by reac-
    tion of 1-naphthol and methyl isocyanate or by reacting 1-naphthol with
    phosgene and then methylamine.  It is a white crystalline solid with
    a melting point of 142 C, a vapor pressure of 0.005 mm mercury at 26 C,
    and a water solubility of less than 0.1 percent (1,000 ppm) at room
    temperature.  It is soluble in most polar organic solvents such as di-
    methyl sulfoxide.
    Degradation-
    Biological—The degradation of carbaryl by microorganisms is summarized
    in Tables 81 and 82 and the pathways are shown in Figure 17.  The de-
    gradation to 1-naphthol proceeds by hydrolysis, hydroxylation and pos-
    sibly also by conjugation (Mehendale and Dorough 1972).  Bollag and
    Liu (1971) noted that 1-naphthol is both more toxic and more persis-
    tent than carbaryl itself.  Degradation of carbaryl to CO  and coumarin
    has been reported for Pseudomonas (Kazano e£ j|l.. 1972).  Bollag and
    Liu (1971) reported that Fusarium solani degraded 1-naphthol more rea-
    dily than carbaryl, and that filamentous fungi were more effective than
    bacteria.  Of 11 microorganisms tested, three were completely unable
    to degrade carbaryl (Sikka et al. 1975).  Trichoderma vivide decomposed
                    3
    11.3 percent of  H-carbaryl, but only 2.1 percent of the label was
    water-soluble (Matsumura and Boush 1968) .  Aspevgillus terr>eus degraded
    carbaryl when it was present at 50 to 100 ppm, but was completely in-
    hibited by 200 to 500 ppm.  The pyrethrin-synergizing methylenedioxy-
    phenyl compounds, Sesamex and Sesamol, also decreased the rate of car-
                                      533
    

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    -------
    1,2-DIHYROXYNAPHTHALENE
    
    
                 \*
    -------
    baryl degradation by Aspergillus  (Bollag and Liu 1974).  An Aehromo-
    baoter species converted carbaryl to 1-naphthol, hydroquinone and cate-
    chol pyruvate in the absence of other sources of carbon (Sud et al.
    1972).  Pseudomonas melophthora, a symbiote of the apple maggot, con-
                          3
    verted 6.4 percent of  H-carbaryl to water-soluble metabolites and 45.5
    percent to solvent-soluble metabolites (Boush and Matsumura 1967) while
    another symbiote, Bacillus cereus, reportedly also degraded carbaryl
    (Singh 1974).
         14
    When   C-1-naphthol was added to cultures of bacteria in river water,
                                                  14
    44 percent of the 1-naphthol was converted to   C-carbon dioxide with-
    in 60 hours.  Seventeen percent of the radioactivity remained in the
    growth medium, and 22 percent was associated with the bacteria.  The
    major residue was 4-hydroxy-l-tetralone, and bacterial growth was com-
    pletely inhibited by more than 100 ppm of 1-naphthol (Bollag et al.
    1975).
    Metabolism of carbaryl in plants may consist of little more than in-
    activation; alternatively, oxidation or hydroxylation of the ff-methyl
    group may be followed by ring degradation (Kuhr 1968).
    In fish (Cyprinus earpio"), Ishii and Hashimoto (1970) reported com-
    plete degradation of carbaryl, with no 1-naphthol detectable after 24
    hours.  In cows, 1-naphthol and conjugated metabolites of carbaryl
    were excreted in the urine and feces, but not in milk, when cows were
    fed 450 ppm of technical carbaryl for fourteen days.  Urinary excretion
    ended within four days of the last exposure to carbaryl, and even in-
    gestion of 12 ppm of 1-naphthol did not result in tainted milk (White-
    hurst et al. 1963).  Rat intestines converted carbaryl to napthyl glu-
    curonide in vitro (Pekas 1971).
    In human embryonic lung cells in culture, carbaryl was almost completely
    metabolized within 72 hours.  The major metabolites were 1-naphthol,
    4-hydroxycarbaryl, 5-hydroxycarbaryl, and 5,6-dihydroxycarbaryl.  Un-
    known compounds and conjugates were also produced (Lin et al. 1975).
                                       537
    

    -------
    In mice, both 4-hydroxycarbaryl and 5-hydroxycarbaryl are rapidly con-
    jugated to form 2>e£a-D-glucosides, which are significantly less toxic
    to the animals (Cardona and Borough 1975).
    Chemical and physical—Treatment with liquid ammonia and metallic so-
    dium or lithium destroyed 92.8 and 93.5 percent of analytical grade
    carbaryl, respectively, but the decomposition products were not iden-
    tified (Kennedy et^ al.  1972a).  Treatment with I6N nitric acid resulted
    in formation of nitrobenzene; 15 N ammonium hydroxide only resulted in
    conversion to 1-naphthol (Kennedy et_ a]^. 1972b) .  In soil, nonbiologi-
    cal hydrolysis of carbaryl to 1-naphthol has been shown to occur (Ka-
    zano et_ al. 1972) .
    Thermal degradation of  carbaryl in commercial formulation was 88.7 per-
    cent effective at 600 C, and 89.5 percent effective in a dry combustion
    furnace at 1,000°C (Kennedy et_ a^. 1969).  Volatile products of car-
    baryl combustion at 900 C included carbon monoxide, carbon dioxide,
    hydrochloric acid,  ammonia, and oxygen, as well as unidentified pro-
    ducts (Kennedy et_ al. 1972a, 1972b) .
    Photolytic—Ultraviolet light decomposed carbaryl primarily by cleav-
    age of the ester bond (Aly and El-Dib 1971, Fedorova and Karchik 1970).
    Further photolytic studies demonstrated that some degradation products
    were also cholinesterase inhibitors and that the nature of the degra-
    dation depended on formulation (Crosby et al. 1965).  Moisture (Fedor-
    ova and Karchik 1970) and high pH (Aly and El-Dib 1971) accelerated
    photolysis of carbaryl.
    Transport-
    Within soil—Carbaryl was less readily adsorbed to pond sediments and
    watershed soils than either malathion or phorate (Meyers et al. 1970).
    After 1,000 liters/ha of three percent Sevin were applied to soil, 51.5
    to 58.1 percent of the original level of carbaryl was detected between
    zero and five centimeters after five days; residues were detected at
                                       538
    

    -------
    depths of 50 to 60 centimeters for 15 to 20 days (Nalbandyan 1974).
    Adsorption of carbaryl to soil organic matter surfaces is probably
    physical rather than chemical, depends on the saturating cation and in-
    creases with increasing temperature between 5  and 40 C (Leenheer and
    Ahlrichs 1971).
    Between soil and water—No data were available on the transport of
    carbaryl or its major metabolite, 1-naphthol, through or with soil
    into water, or from water into sediments.
    Into air—Loss of carbaryl from petri dishes after 12 days exposure to
    a constant air flow of ten cubic feet per hour was 1.6 mg at a relative
    humidity of three to 13 percent, and 6.2 mg at a relative humidity of
    75 to 85 percent, but the amounts originally exposed were not given
    (Lyon and Davidson 1965) .
    Into organisms—Carrots contained less carbaryl than either parathion
    or diazinon after fields were treated with two or three times the nor-
    mal agricultural levels of each chemical (Stobwasser 1963) .
    In the subarctic, residues of carbaryl one month after application of
    five kg/ha (2.2 ppm) were 0.1 ppm in soil, 0.5 ppm in lichens, 0.6 ppm
    in arctic birds, 1.4 ppm in lemming livers, 1.5 ppm in woodcock livers,
    and ten ppm in the testes of small mammals (Shilova et al_. 1973).  Kurtz
    and Studholme (1974), however, found little uptake of carbaryl in song-
    birds after forests were sprayed for gypsy moths, and no carbaryl resi-
    dues were present in cattle after seven days, although milk excretion
    persisted for over 60 hours (Hurwood 1967).  Organ retention of carba-
    ryl in mice lasted two days after doses of 50 mg/kg; in rabbits, six
    days after doses of 400 mg/kg; and in chickens, five days after 1,500
    mg/kg (Ryamushkin and Yakub 1971).
    Persistence-
    Carbaryl applied as a termiticide retained 60 to 100 percent of its
    effectiveness for four years (Beal and Smith 1972).  Ivanova and
                                      539
    

    -------
    Molozhanova (1974) postulated an exponential decrease in soil levels
    of carbaryl with time; empirically, the rate of loss was:
                        1/k = 16.9 x + 15.3 pH - 46.24
    where x is equal to the humus content of the soil.
    In river water exposed to natural and artificial light in jars, 95 per-
    cent of ten g/liter (10,000 ppm) of carbaryl decomposed x^ithin one
    week, and no carbaryl was detected after two weeks  (Eichelberger and
    Lichtenberg 1971).  In laboratory aquaria, the "half-life" of carbaryl
    in seawater without mud was 38 days at 8 C, but at  20 C, 43 percent
    was converted to 1-naphthol in 17 days.  When mud was included in the
    aquaria, less than ten percent of the carbaryl was  converted to 1-naph-
    thol after ten days.  In a natural mud flat, carbaryl persisted for
    42 days, 1-naphthol for only one day (Karinen et_ aJU 1967).
    Soil residues one month after five kg/ha were applied to soil in the
    subarctic were 0.1 mg/kg (0.1 ppm)  (Shilova et^ al_. 1973).  Kazano et_
    al. (1972) noted that 1-naphthol was chemically bonded to the humus in
    soil and was stable to alkali.
    Effect on Non-Target Species-
    Microorganisms—In the laboratory, while 20 yg/ml (20 ppm) inhibited
    growth of Fusariwn oxysporum, the effects could be  prevented by yeast
    extracts, asparagine, ammonium nitrate, or ammonium sulfamate, but not
    by vitamins.  None of the 17 fungi tested was able  to grow with carba-
    ryl as the sole source of carbon (Cowley and Lichtenstein 1970).  Jaku-
    bowska and Novak (1973) reported significant inhibition of fungal
    growth by carbaryl, but in another study carbaryl stimulated fungal
    growth (Askerov 1969).  Algae and bacteria varied in their response, as
    summarized in Tables 83 and 84.  Carbaryl in sandy  soil produced a
    greater effect on microorganisms than in either chernozem or peat
    (Brantsevich et_ al_. 1973).
    Invertebrates—The acute LPrn of carbaryl to honeybees was 0.02 per-
    cent, or 200 ppm, under laboratory conditions.  Under the experimental
                                      540
    

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    -------
    conditions used, carbaryl was less toxic to bees than parathion, diel-
    drin, or azinphosmethyl, but more toxic than phorate or DDT  (Johansen
    1961).  In pasture, carbaryl reduced the biomass of earthworms by as
    much as 60 percent, and their numbers by as much as 68 percent (Thomp-
    son 1970); straw decomposition was delayed by 6.5 to 17.6 percent be-
    cause of carbaryl toxicity to the earthworms AlloZophoTba caliginosa
    (Atlavinyte e_t al. 1974).
    At 2.3 and 4.6 kg/ha on intertidal mud flats, carbaryl decreased the
    numbers of juvenile clams (Tresus oapax, Macoma masuta, Callianassa
    aaliforniensis'), but did not appear to reduce the numbers of polychaete
    or nemertean worms (Armstrong and Milleman 1974).  The harvest of
    Louisiana red crawfish, Procambarus olarkii3 was unaffected by carba-
    ryl at agricultural levels (Hendrick et al. 1966) .
    In an aquatic ecosystem (Kanazawa et al. 1975), carbaryl was character-
    ized as relatively persistent when it was applied to air-dried soil,
    after which water and aquatic organisms were added.  Most of the car-
    baryl (68 percent) remained in the soil: 0.11 to 1.59 percent was
    taken up by the catfish, crawfish, daphnids, algae, and duckweed.  No
    toxicity was associated with the soil-bound carbaryl, 45 percent of
    which was not extractable by solvents or methanol (Kanazawa et al.
    1975).
    In an aquatic-terrestrial model ecosystem  (Metcalf et al. 1971) , no
    carbaryl residues were found in any of the organisms, and the water
    contained only degradation products.  Sanborn (1974) and Metcalf and
    Sanborn (1975) concluded that carbaryl would not accumulate in aquatic
    food chains.
    Plants—Carbaryl increased the herbicidal persistence of CIPC (iso-
    propyl m-chlorocarbanilate)  regardless of soil pF or soil type (Kauf-
    man et al. 1970).  Propanil inhibited interconversion of carbaryl met-
    abolites on leaves (Chang e_t al. 1971b) , and carbaryl inhibited the
                                      543
    

    -------
    metabolism of propanil in leaf tissue (Chang et al. 1971a) and in soil
    (Kaufman et al. 1971) .  Chlorpropham and malathion stimulated the de-
    gradation of carbaryl on leaves, but linuron inhibited it (Chang et_ al.
    1971b).
    On grain sorghum, agricultural levels of carbaryl were not phytotoxic
    (Meisch _et_ al. 1970) .  Soaking cotton seeds (Gossypiim barbadense) in
    carbaryl for one to  three days decreased seed germination, but weekly
    sprays of a 50 percent saturated solution increased both abscission
    and cotton yields per plant (Hammouda et al. 1966) .
    At 1,500 ppm, carbaryl decreased the germination of barley (Eordeym
    Vulgare) by 52 percent, and induced chromosome aberrations in root tip
    cells (Wuu and Grant 1966) .  Chromosome aberrations were induced in
    beans (V-Ceia faba) by spraying plants with carbaryl daily for eight
    days.  Pollen sterility was not induced, but the chromosome damage was
    dose-dependent (Amer and Farah 1968) .
    Fish — The 24-hour LC^ of carbaryl to fish ranged from 1.75 ppm for
    longnose killifish  (Fundulus similis) to 6.7 ppm for three-spine stick-
    lebacks (Gasierosteus aculeatus) , while the 96-hour LC   ranged from
    0.76 ppm in coho salmon (Oncorhynehus kisuteh) to 20 ppm in black bull-
    heads, (Ictalurus melas) .  Some data suggest that sub-clinical levels
    of carbaryl lowered the natural resistance of fish to parasites (Pim-
    entel 1971).
    Birds — The acute oral LD,.- of carbaryl in Japanese quail (Cotuvn-ix ao-
           japoniaa) was 2,290 mg/kg and in mallards (Anas platyrh-inohos)
    more than 2,179 mg/kg (Tucker and Crabtree 1970).  In 39 day old Japan-
    ese quail, liver levels of vitamin A were decreased in females but not
    in males  (Cecil et al. 1974).  The acute oral LDC_ in male chicks was
                    — —                           jU
    197 mg/kg, with 95 percent confidence limits ranging from 154 mg/kg to
    250 mg/kg (Sherman and Ross 1961) , but Zhavoronkov &t_ a^ . (1973) claim-
    ed that after feeding one percent of the LD   to hens for ten days,
    development of their chicks was impaired.
                                      544
    

    -------
    When 3.44 rag/embryo of carbaryl was  injected into  the allantoic  cavity,
    50 percent of chick embryos died, but the survivors exhibited no his-
    topathologic changes, even when 6.75 mg/embryo were injected  (Tos-Luty
    et al. 1973).  Olefir and Vinogradova (1968) reported numerous malfor-
    mations in chick embryos after 0.064 mg/kg carbaryl were  injected  into
    the yolk sac.  Dunachie and Fletcher (1969) observed malformations,
    mainly of the feathers, in chicks treated with 50  ppm carbaryl injected
    into the yolk.
    Mammals—The acute oral LD   of carbaryl in rats is between 40 mg/kg
    (Jones et_ al.. 1968) and 540 mg/kg (Metcalf et_ al.  1962) .  Yakin  (1967)
    cited an acute oral LD,-_ of 721 mg/kg for rats and 150 mg/kg  for cats.
    Since rats survived daily injection  of five percent of  the LD^  for at
    least six months, Yakin (1967) considered carbaryl no more than mildly
    cumulative.  Pretreatment with DDT decreased the toxicity of  carbaryl
    to mice (Meksongsee et_ al. 1967) .
    Numerous reports suggest that carbaryl exerts a considerable  effect on
    cellular enzymes (Khaikina 1970, Orlova 1970, Kagan e_t al. 1970, Kuz'-
    minskaya and Yakushko 1970, Kuz'minskaya 1971), on the  immune response
    (Olefir 1971), and causes cardiovascular disturbances (Orzel  and Weiss
    1966, Kagan et_ _a2L. 1970, 1973, 1974; Lukaneva and  Rodionov 1973).  In
    tissue culture, carbaryl was more toxic than its metabolite 1-naphthol
    (Litterst and Lichtenstein 1971).  Lower concentrations of carbaryl
    stimulated the growth of HeLa cells, but at higher concentrations  growth
    was inhibited (Blevins and Dunn 1975).  Two percent of  the LD  » given
    daily for thirty days, altered the exocrine activity of the pancreas
    (Urbanowicz et al. 1973) .
    Reproductive disturbances in rats have been reported at chronic  treat-
    ment with no more than 50 mg/kg/day  (Shtenberg et  al. 1970, Shtenberg
    and Ozhovan 1971, Przezdziecki et^ a!U 1974, Trifonova et_  &L_.  1970).  Em-
    bryotoxic effects were also reported by several authors (Shtenberg et
    al. 1973, Tos-Luty et_ al. 1974, Torchinskii 1974).  In a  three-genera-
                                       545
    

    -------
    tion study, chronic feeding of 2,000 ppm decreased the reproductive
    fitness of both rats and gerbils (Collins et^ al_. 1971).  In mice, no
    significant effects on reproduction were observed when ten mg/kg of
    carbaryl were fed for three generations, and even 500 mg/kg produced
    no significant effects except an increase in pre-weaning mortality.
    Administration of 100 mg/kg by intubation before mating did, however,
    reduce fertility (Weil et_ aJL. 1972).
    Carbaryl was not teratogenic in guinea pigs at 300 mg/kg, in hamsters
    at 250 mg/kg, or in rabbits at 200 mg/kg (Robens 1969).  Carbaryl is
    not teratogenic in rats (Shtenberg and Torchinskii 1972, Weil et al.
    1973).  In beagle dogs, Smalley and co-workers (1968) observed malfor-
    mations at carbaryl levels of 50 mg/kg, but no dose-response relation-
    ship was evident.  There was no evidence of chromosome damage in mice
    injected intraperitoneally with 20 mg/kg of carbaryl (Jordan et al.
    1975) and no increase in resistance to carbaryl after 12 to 14 genera-
    tions of selection (Guthrie et al. 1971).
    Makovskaya and co-workers (1965) reported fatty necrotic areas in the
    livers and spleens of mice treated with 60 mg/kg carbaryl for six
    months; no tumors were found even after 20 months.  Zabezhinski (1970)
    claimed that beta-Sev±n caused "cancerous tumors" when given orally
    or intravenously, but no dosage level was reported.  Carbaryl can also
    serve as a precursor to the potent bacterial mutagen, nitrosocarbaryl
    (Elespuru et^ al_. 1974, Siebert and Eisenbrand 1974) which could plaus-
    ibly be formed within the human digestive system (Uchiyama et al. 1975) .
    Mild, permanent, and increasing functional deviation was observed in
    the nervous system of maze-trained rats treated with subacute levels
    of carbaryl (Desi et^ al. 1974).
    Conclusions-
    Inasmuch as both carbaryl and its major metabolite 1-naphthol are rea-
    dily decomposed by microorganisms, soil disposal of carbaryl is feasible.
                                       546
    

    -------
    Metalkamate
    Metalkamate, more commonly referred to as Bux, is a mixture of three
    parts 777- (l-methylbutyl)-phenyl /7-methylcarbamate and one part of
    m-(l-ethylpropyl)-phenyl /^-methylcarbamate, introduced by Chevron
    Chemical Company in 1966 under the trade names of Ortho 5353 and Bux.
    Metalkamate is a colorless solid with a melting point of 45 to 50 C.
    It is soluble in water to less than 50 ppm, but readily soluble in
    xylene and methanol.  Bux is formulated as ten percent clay granules,
    and is used primarily against corn rootworm larvae (Tucker 1973).
    Degradation-
    Tucker and Pack (1972) analyzed the degradation of metalkamate in soil
    under laboratory conditions and concluded that microbial degradation
    predominated, since degradation was more rapid in unsterilized than in
    sterile soil.  In unsterilized soil, 50 percent of the metalkamate was
    degraded within one week and in sterilized soil, five to fifteen per-
                                            14                   14
    cent was degraded in the same time with   C0« evolution from   C-car-
    bonyl-labeled metalkamate.  In additional studies on the major compo-
    nent, m-(l-methylbutyl)-phenyl ff-methylcarbamate, the major metabolite
    was m-(l-hydroxy-l-methylbutyl)-phenyl A7-methylcarbamate.
    Metalkamate is stable in neutral or acidic media, but under alkaline
    conditions it is hydrolyzed to the respective phenols, carbon dioxide,
    and methylamine (Tucker 1973).  No data were available on the photo-
    lysis or physical degradation of metalkamate.
    Transport-
    No data were available on the movement of metalkamate in soil, between
    soil and water, or on losses due to volatilization.
    In an aquatic-terrestrial model ecosystem, metalkamate did not show
    any tendency to accumulate in the higher members of the trophic web.
                                      547
    

    -------
    The alga and Elodea contained residues of 0.98 ppm and 0.24 ppm, res-
    pectively, of the parent compound; and the crab, which died seven days
    after the addition of metalkamate, contained 0.05 ppm.  The other or-
                                               14
    ganisms contained no detectible amounts of   C.  Yu et_ al. (1974) and
    Metcalf and Sanborn (1975) concluded that metalkamate would not lead
    to environmental problems of accumulations in the food chain.
    Persistence-
    Harris (1973) considered metalkamate to be a moderately persistent
    soil insecticide which lost its insecticidal activity within 16 weeks.
    Metalkamate was less toxic to crickets when soil-applied than as a
    direct contact insecticide, but the inactivation was only moderate in
    moist sand.  In muck, activity against crickets was reduced by a fac-
    tor of fifty in comparison to direct toxicity (Harris, 1973).  Degra-
    dation of metalkamate in solution was 50 percent complete in silt or
    silt loam soil in one week under laboratory conditions.  The authors
    concluded that slower degradation would occur under field conditions
    since Bux is applied as granules (Tucker and Pack 1972).
    Effects on Non-Target Species-
    No data were available on the effects of metalkamate on soil processes
    or soil microorganisms.  Apple (1971) considered Bux sufficiently phy-
    totoxic that in-row application at the rate of one pound per acre might
    injure corn with damage depending on climatic conditions in the days
    following planting.  Bux applied at one pound per acre reduced the num-
    bers of earthworms in pasture severely (Thompson 1970), but recovery
    occurred within one year (Thompson and Sans 1974).  The acute oral LD
    of Bux is 87 mg/kg in rats, and the acute dermal LD,._ is 500 mg/kg
    (Anonymous 1974).
    Conclusions-
    Metalkamate is toxic to earthworms in pasture (Thompson 1970, Thompson
    and Sans 1974), is phytotoxic to corn at approximately 2 ppm, or 1 Ib/A
                                      548
    

    -------
    (Apple 1971), and appears to be highly toxic to crabs (Metcalf and San-
    born 1975).
    In the absence of data on its transport within soil and from soil to
    water, soil disposal of metalkamate wastes is not recommended.  Prior
    treatment by chemical hydrolysis to the phenols before soil disposal
    might greatly enhance the degradation, but the consequences are merely
    speculative.
                                      549
    

    -------
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      microbial method.  Bull. Environ. Contain. Toxicol. 14:389-394.
    Ukeles, R.; 1962.  Growth of pure cultures of marine phytoplankton in
      the presence of toxicants.   Appl. Microbiol. 10:532-537.
    Urbanowicz, M., J. Gawecki and B. Bonk; 1973.  Effect of some carba-
      mate pesticides on the organism of the rat and in particular on the
      exocrine function of  the pancreatic gland.  Bromatol. Chem. Toksykol.
      6:413-418. (Chem. Abstr. 81:10297p, 1974).
    Weil, C, S., M. D. Woodside,  C. P. Carpenter and H. F. Smyth, Jr;
      1972.  Current status of tests of carbaryl for reproductive and ter-
      atogenic effect.  Toxicol.  Appl. Pharmacol. 21:390-404.
    Weil, C. S., M. D. Woodside,  J. B. Bernard, N. I. Condra, J. M. King
      and C. P. Carpenter;  1973.   Comparative effect of carbaryl on rat
      reproduction and guinea pig teratology when fed either in the diet
      or by stomach intubation.  Toxicol. Appl. Pharmacol,, 26:621-638.
    Whitehurst, W.  E. , E. T., Bishop and F. E. Critchfield; 1963.  The meta-
      bolism of Sevin in dairy cows.  J. Agr. Food Chem. 11:167-169.
                                      560
    

    -------
    Wuu, K. D. and W. F. Grant; 1966.  Morphological and somatic chromo-
      somal aberrations induced by pesticides in barley (Hordeum vulgare).
      Can. J. Genet. Cytol. 8:481-501.
    Yakim, V. S.; 1967.  Data for substantiating the maximum permissable
      concentration of Sevin in the air.  Gig. Sanit. 32:29-33.
    Yu, C., G. M. Booth, D. J. Hansen and J. R. Larsen; 1974.  Fate of Bux
      insecticide in a model ecosystem.  Environ. Entomol. 3:975-977.
    Zabezhinskii, M. A.; 1970.  Possible carcinogenic effect of 3-Sevin.
      Vop. Onkol. 16:106-107. (Chem. Abstr. 75:32870y, 1971).
    Zhavoronkov, N. I., A. V. Akulov, S. D. Antsiferov, A. P. Verkhovskii
      and S. M. Evdokimov; 1973.  Effect of carbamates on hens.  Veteri-
      nariya  (Moscow) 114-116.  (Chem. Abstr. 79:122422r, 1973).
    Zinchenko, V. A. and T. V. Osinskaya; 1969.  Change in the biological
      activity of soil during composting with herbicides.   Agrokhimiya
      1969:94-101. (Chem. Abstr. 72:2381k, 1970).
                                     561
    

    -------
                                   SECTION V
                            FUNGICIDES AND FUMIGANTS
    Captan
    Captan is the common name for 3a,4,7,7a-tetrahydro-2-(trichloromethyl)
    thio-lH-isoindole, a fungicide used mainly for foliage protection which
    was introduced by Standard Oil in 1949 under the name Orthocide.  Cap-
    tan forms white crystals with a melting point of 178 C and a vapor pres-
    sure of less than 0.01 mm at 25 C.  It is insoluble in petroleum oils,
    and its water solubility at room temperature is less than 0.5 ppm.  It
    is soluble in xylene, chloroform, acetone, and isopropanol, and stable
    except under alkaline conditions.
    Captan is produced by the reaction of trichloromethylsulphenyl chloride
    on tetrahydrophthalimide.  The technical product is 93 to 95 percent
    pure captan and forms an amorphous yellow solid with a pungent odor.
    The melting point of technical captan is between 160  and 170 C.  It
    is formulated as 50 percent or 83 percent wettable powders, 5 percent
    dust, or as a 75 percent dust for seed treatment.
    Degradation-
    Biological—When 840 million Neurospora crassa spores were incubated
    with 375 yg captan, degradation of captan to carbonyl chloride occur-
    red in 20 minutes, with no formation of carbon disulfide (Somers et al.
    1967, Richmond and Pickard 1967).  Cell thiols were implicated in the
                                35
    degradation and most of the   S was eventually bound to oxidized gluta-
    thione and its derivatives (Richmond and Somers 1968).  Captan lost 50
    percent of its bioactivity against Khizoctonia solani after three weeks'
    incubation in humus-sandy forest soil  (Kluge 1969a).
             14                                              14
    Rats fed   C-labeled captan excreted 51.8 percent of the   C in their
    urine as thiazolidine-2-thione-4-carboxylic acid, a salt of dithiobis
    (methane sulfonic acid) and the disulfide monoxide of dithiobis(methane
    sulfonic acid).  Radioactive C0_ was exhaled, accounting for almost 23
    percent of the label, and 15.9 percent of the label was eliminated in
                                       562
    

    -------
    the feces.  Less than one percent of the label remained in the tissues
    (DeBaun et al. 1974).  Gastro-intestinal degradation was highly signi-
    ficant, since in rats which were injected intraperitoneally with cap-
    tan, 50 percent of the radioactive label was excreted in nine days, but
    administered orally the label from captan was 50 percent excreted with-
    in two hours (DeBaun et al. 1974).
         35
    When   S-labeled captan was fed to rats, 90 percent of the label was
    eliminated in 24 hours (Seidler et_ al. 1971).
    Chemical and physical—Captanrdecomposes between 200 C and 245 C leading
    to a 52 percent weight loss and formation of hexachlorodimethyl disul-
    fide and tetrahydrophthalimide (Pfeifer and Pfeifer 1970).  Captan de-
    gradation in soil was not affected by changes in pH between 3.6 and 7.4
    (Kluge 1969b).
                           «
    Transport-
    When the mobility of several fungicides was examined in soil columns
    with several types of soil, all were more mobile in sandy loam than in
    loam, and in dry than wet soil.  Peat moss greatly inhibited the mobi-
    lity of all compounds.  In general, suspended compounds were less mo-
    bile than dissolved compounds.  Captan as particles of 14.5 y was less
    mobile than when particles of 1.05 y were used (Munnecke 1961).
    Persistence-
    Captan was found to be degraded rapidly in most soils.  Bioassay with
    Myvofheoi-um ve?'Pueca"La indicated a 50 percent loss of activity after
    seven days in sandy soil, three to four days in moist soil, and less
    than one day in compost soil.  Under conditions of high local concen-
    trations, much longer persistence was noted (Griffith and Matthews
    1969).  Agnihotri (1970, 1971) and Burchfield (1959) also found that
    captan was persistent for less than one week in moist soil.
    In sharp contrast, Munnecke (1958) found persistence of diffusible ac-
    tivity for 65 days after captan was applied to a mix of sand and peat
                                       563
    

    -------
    while under the same conditions nabam was inactivated within hours.   If
    the mix was first sterilized, captan persisted for up to 150 days.  Ag-
    nihotri (1970), observing that Munnecke's data were atypical, suggested
    that the acidity of the peat moss was unfavorable for growth of captan-
    degrading bacteria.  The amount of organic matter, rather than clay,  in
    the soil determines the rate of captan release (Rersheim and Linn 1968).
    Fifty percent of the applied captan persisted for less than one hour  in
    water at 25 C, but for seven hours at 12 C (Hermanutz e_t_ al_. 1973).
    These data suggest that biodegradation of captan is rather rapid, which
    explains the nonpersistence of captan under field conditions.  No data
    on the degradation products of captan or their persistence in soil were
    available.
    Effects on Soil Microorganisms-
    As would be expected of a fungicide, captan sharply inhibited nontarget
    fungal growth in many studies (Wainwright and Pugh 1974, Naumann 1970,
    Domsch 1959) but after 28 days fungal populations had increased above
    pretreatment levels even if twice the usual agricultural levels of cap-
    tan were used.  Glioo1adiwn3 Penioil1ium3 and Tviohoderma predominated
    (Wainwright and Pugh 1974).  A decrease in fungal diversity was obser-
    ved by Naumann (1970).  When captan was applied to forest soil at 62.5,
    125, and 250 ppm, three pathogenic fungi were destroyed (Rhizoatoniaf
    Pythium), three saprophytic fungi were stimulated (Peni-Q-111-ium, Tricho-
    derma, Fusapiim) and actinomycetes and bacteria were stimulated for up
    to five weeks (Agnihotri 1970, 1971).  In laboratory cultures, agricul-
    tural levels of captan inhibited four microfungi (Hansenula, sattamus,
    MUOOT hi-emal'is, Penni-ai-lli-um stipitatwr and Trichoderma vir"ide) from
    cattail marsh, but in the field no effects on these fungi were observed
    (Tews 1971).
    Soeder et_ aK (1969) found captan almost as toxic to some algae as to
    Neupospora avassa:  37 or 40 ChloTella species were strongly inhibited
                                       564
    

    -------
    by as little as five rag/liter  (five ppm) captan in shake solution where-
    as Seenedesmus species were relatively resistant even at 50 rag/liter
    (50 ppm) of captan.  With respect to nontarget microorganisms and soil
    processes, captan generally stimulated ammonification and  inhibited ni-
    trification, while bacterial growth was sometimes stimulated and some-
    times inhibited.  These data are summarized in Tables 85 and 86.
    In addition to the considerable direct toxicity which it exerts on some
    microorganisms, captan induces DNA base changes (Kada et_ al_. 1974).   It
    is mutagenic in the bacteria Esohevlohla ooll (Legator et_  al^. 1969,
    Clark 1971, Bridges et al. 1972, 1973) and Salmonella (Seiler 1973),  in
    the fungus Altevnarla mall (Slifkin 1973), and induces mitotic gene con-
    version in the yeast Saodhapomyoes cerewis'iae (Siebert et  al. 1970).
    In the host-mediated assay in mice, captan was mutagenic in two species
    of Salmonella (Buselmaier et al. 1972).
    In summary, it is apparent that captan strongly affects soil microorgan-
    isms and soil processes and must be expected to alter the  soil complex
    profoundly whenever it is applied to soil, even if the precise changes
    cannot be predicted.
    Effect on Non-Target Species-
    Invertebrates—Captan is essentially nontoxic to insects under ordinary
    usage (Pimentel 1971, Beran and Neururer 1956).
    Plants—Captan was reported to stimulate plant growth (Kittleson 1963),
    but 1,000 ppm inhibited root growth of corn seedlings (Dugger et al.
    1958).  Levels of 100 and 200 ppm of a 50 percent wettable powder de-
    creased corn growth but stimulated growth of bean plants in soil con-
    sisting of silty clay loam, peat and fine sand in a 3:1:1  ratio (Cole
    et^al. 1968).
    Fish—Ninety percent of zebrafish larvae exposed to one ppm of captan
    died within 90 minutes (Abedi and McKinley 1967).  Lethal  concentrations
    were reported to be 29 ppm for brook trout (Salvellnus fontlnalls~), 64
                                      565
    

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    ppm for fathead minnows (Pimephales promelas"), and 72 ppm for bluegills
    (Lepomia macro shims') and the breakdown products of captan were not  tox-
    ic (Hermanutz et_ al. 1973).
    Birds—Captan is relatively nontoxic in birds with a five-day LC,... of
    2,000 ppm in bobwhite and over 5,000 ppm in mallards, pheasants, and
    coturnix quail (Pimentel 1971).  If captan is injected into hens' eggs
    it causes leg and wing malformations as well as significant mortality
    (Verrett et al. 1969).
    Mammals—The acute oral LD -. of captan is more than 8,000 mg/kg in rats
    (Jones et al. 1968), but 250 mg/kg caused poisoning in sheep  (Palmer
    and Radeleef 1964).  Chronic feeding of 0.05 to 0.4 ppm for six months
    did not affect two cows or five swine so fed (Johnson 1954), while 140
    days feeding with corn contaminated by 67 g/bushel apparently increased
    weight gain in steers (Dowe et^ aJ^. 1957).  In contrast, Grabarska (1972)
    reported serious dystrophic changes in many organs when rabbits were
    given 500 mg/kg for 14 days and similar damage was reported by Vasha-
    kidze et^ al.. (1973) when 265 mg/kg were given to rats for two months, or
    20 to 55 mg/kg were given for twelve months.  Treatment with 100 mg/kg/
    day of captan decreased the level of hepatic respiratory enzymes in
    guinea pigs (Krolikowska-Prasal 1973) .
    Since captan was observed to denature calf thymus in vi't-TO and cause al-
    kylations i/n vivo in mice it was considered carcinogenic by Anderson and
    Rosenkranz  (1974).  The teratogenicity of captan is theoretically at-
    tractive because it shares the phthalimide moiety with thalidomide but
    the data are inconclusive (Kennedy et_ aL_. 1968, 1975; Vondruska et al.
    1971, Shea 1972).  Even in the absence of teratogenicity, however, con-
    siderable embryotoxicity is often observed (Kennedy £jt al. 1975) .  The
    data on the long-term effects of captan and related fungicides have
    been critically reviewed by Bridges (1975) who concluded that captan
    was mutagenic in rats and bacteria, was teratogenic, and had been in-
    sufficiently tested for carcinogenesis.
                                      568
    

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    Conclusions-
    Captan is eminently suited to soil degradation if well dispersed, rather
    than massed, in the soil, but since captan is a microbial mutagen no
    form of unmonitored soil disposal can be recommended.  The low persis-
    tence of captan in water makes degradation in lagoons a possibility,
    subject always to the oaveat of mutagenesis.  There are no data avail-
    able on the feasibility of chemical or thermal destruction of captan,
    so no conclusions as to the relative merits of different modes of dis-
    posal are possible.
                                      569
    

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    Dodine
    Dodine is the common name for dodecylguanidine acetate, referred to as
    doquadine and taitrex in France and in the USSR, respectively, and in-
    troduced by American Cyanamid as Cyprex or Melprex in 1957.  Dodine is
    a white crystalline solid with a melting point of 136°C, soluble in
    water and ethanol, and insoluble in most organic solvents.  The free
    base is liberated by strong alkalies, but the acetate salt is stable
    in moderately alkaline as well as moderately acid solutions.  Dodine
    is used chiefly as a foliar fungicide, particularly against apple or
    pear scab and cherry leaf spot.  The usual formulations are 65 per-
    cent and 80 percent wettable powders, 75 percent dusts, or 20 percent
    liquid.
                                                                  *
    Degradation-
                                              *
    The major degradation product of dodine in plants is creatine (Kaufman
                                                                    •
    1974).  Dodine was adsorbed to the same extent by dead as by viable
    fungal spores; its rapid adsorption and Langmuir-type isotherm sugges-
    ted ionic bonding to Alternavia tenuis spores, while the relative ir-
    reversability of its adsorption to Neiipospora CTassa spores suggested
    covalent bonding.  The presence of calcium, magnesium, or uranil salts
    decreased dodine bonding to fungal spores (Somers and Pring 1966).
    Goldberg and Wershaw (1965) found Aahromobacter and Flavobacterium
    species could grow with dodine as the sole source of carbon.  When river
    mud from the Denver area was treated with dodine, five percent of the
    fungicide was degraded in 68 days whether or not the mud was precondi-
    tioned (Goldberg and Wershaw 1965).  There was no information on the
    chemical, physical or photolytic degradation of dodine.
                                       570
    

    -------
    Transport-
    There were no data available on the mobility of dodine in soil, water
    or air.
    Persistence-
    There was no data available on the persistence of dodine in soil.
    Effects on Non-Target Species-
    Dodine was not observed to induce mitotic gene conversion in the yeast
    Sacahapomyces cepevis'iae under conditions which resulted in gene con-
    version by both captan and folpet (Siebert j2t al_. 1970).
    Shaw (1959) found no difference in honey bee mortality between control
    and dodine-treated fields.  Some reduction in mirid predators was
    found when dodine was applied to orchards, but 500 ppm dodine in water
    did not affect adult female parasitic wasps (TvidhogTcctnma) after a 24-
    hour exposure (Pimentel 1971).
    No data on the effects of dodine on birds, amphibians, fish, or soil
    fauna were available.  The acute oral LD   of dodine was determined to
    be 566 mg/kg in rats by Jones et_ al_. (1968), and 1,000 mg/kg by Levin-
    skas et al. (1961).  The latter calculated a 24 hour dermal LD... of
         	                                                    DU
    2,000 mg/kg in rabbits.  Chronic feeding of dodine to rats resulted in
    a reduction in the weight gain of rats fed 3,200 ppm for 100 days or
    800 ppm for 2 years, but no effects on reproduction were observed after
    feeding 800 ppm for 2 years.  In dogs, levels of 200 or 800 ppm fed
    for one year resulted in slight thyroid stimulation.  No increase in
    pituitary chromatophobe adenomas was seen (Levinskas et al. 1961).
    Conclusions-
    Since no data were available on the persistence of dodine, its nonbio-
    logical degradation, or its transport in soil or water, no conclusions
    can be reliably drawn.  The relatively low mammalian toxicity of dodine
                                      571
    

    -------
    is reassuring, but its status as a fungicide militates against soil
    disposal in the absence of information about its toxicity to, and degra-
    dation by, soil organisms.
                                       572
    

    -------
    Maneb, Nabam, and Zineb
    Maneb is the common name for l,2-ethanediylbis(carbamodithioato)
    (2)-manganese, a protective foliar fungicide which was introduced in
    1950 by E. I. du Pont de Nemours and Co. as Manzate and by Rohm and
    Haas as Dithane M-22.  Pure maneb is a yellow crystalline solid which
    decomposes before melting, is slightly soluble in water and insoluble
    in most organic solvents.  Maneb is synthesized by reacting a water-
    soluble ethylenebis-dithiocarbamate with either manganous sulphate or
    manganous chloride.  The technical product is a light-colored solid.
    Exposure to either moisture or acids results in decomposition, with for-
    mation of polymeric ethylenethiuram monosulfide.  Maneb is formulated as
    a 70 percent wettable powder or in sprays which contain 1.5 to two Ibs.
    per gallon.
    Nabam, the common name for 1,2-ethanediylbis-carbamodithioic acid-disodium
    salt, was introduced in 1943 by E. I. du Pont de Nemours and Co. as
    Parzate, and by Rohm and Haas as Dithane D-14.  It is synthesized by the
    interaction of ethylenediamine and carbon disulfide in the presence of
    sodium hydroxide.  It forms colorless crystals of the hexahydrate which
    are soluble in water to about 20 percent (expressed as the anhydrous salt)
    at room temperature, forming a yellow solution.  Because the crystalline
    form is unstable, nabam is formulated as a 19 percent aqueous solution.
    Use of two quarts of this solution to one pound ZnSO. permits conversion
    to zineb.
    Zineb is the common name for l,2-ethanediylbis(carbamodithioato)
    (2)-zinc, was introduced in 1943 as an improvement on nabam and marketed
    as Dithane Z-78 by Rohm and Haas, and as Parzate-Zineb by E. I. du Pont
    de Nemours and Co.  Zineb is a light-colored powder made by precipitating
    nabam with soluble zinc salts.  It decomposes before melting, has a
                                       573
    

    -------
    negligible vapor pressure at room temperature and an aqueous solubility
    of about 10 ppm at 20 C.  It is soluble in pyridine and is somewhat
    unstable to light, heat, and moisture.  The polymer produced by precip-
    itating zineb from concentrated solution has a lower fungicidal activity.
    Zineb is usually formulated as a 65 percent wettable powder.
    Degradation-
    Few data on microbial degradation of the dithiocarbamate fungicides ex-
    ist, in part because of their rapid decomposition in the presence of
    moisture.  Asperg-illus niger degraded maneb more readily than zineb;
    almost no water-soluble compounds of the latter were observed (Engst
    and Schnaak 1967).  Figure 18 shows the degradative pathways of the
    dithiocarbamate fungicides.  Essentially identical degradation products
    are found for all three compounds:  ethylenebisthiuram disulfide, ethyl-
    enebisthiourea, ethylene diisothiocyanate, CS0, and H0S.  Munnecke et al.
                                                 z       z             	
    (1962) did not find H^S when nabam was degraded although Klisenko and
    Vekshtein (1971) reported elemental sulfur.  Engst and Schnaak (1970)
    included ethylenediamine and elemental sulfur among degradation pro-
    ducts; the former was reportedly the major fungitoxic product of nabam
                                               14
    (Cox et^ a.1^. 1951).  In rats, 55 percent of   C-maneb was excreted as
    ethylenediamine, ethylene bisthiuram monosulfide and ethylenethiourea
    (Seidler £t al. 1970).
    In the laboratory, zineb lost its efficacy in 16 days at 30  or 40 C.
    In the field, the fungitoxicity of zineb increased for four days, then
    declined with 50 percent of its bioactivity gone after 16 days (Grandi
    ^ al. 1958).  It is noteworthy that the degradative products of the
    dithiocarbamates are probably the active fungicides.  Rich and Horsfall
    (1950) observed that SO-, H-S, and ethylene thiourea accounted for only
    part of the fungitoxicity of nabam; Engst and Schnaak (1967) considered
    ethylenethiuram monosulfide to be the chief fungitoxin of the dithio-
    carbamate fungicides.  Engst (1970) noted the greater toxicity of some
    metabolites of these fungicides, and cited ethylenebis(thiouronium sul-
                                       574
    

    -------
                                    s-   -s
                                    \XH    \  M
                                     :/      rr
    
                                     \     /
                                      c	cv
                            ETHYLE!"Fn I 3D ITHI OCAP>BAM.ATE
                                       s—s
                                      \,H \,H
    
                                       •C   ,"
                                       .c— cv
                                      H '   ' H
                                      H H   H M
    ETHYLENETHI
                                         3A,"D
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            rr      N    + H2s
           1  H  H  "
    
    
    ETHYLEMETHIURAMMONOSULFIDE
                        H   /°\  ^H
                         NN       N
                           \	/       +  s
    
    
                          A   f/^"      +  CS2
    
                       ETHYLFNETHIOIREA
                    DEGRADATION OF ETHYLEMEBISDITHIOCARRAMATES
    
                                (AFTER  HYLIN  1073)
                              Figure 18
                                     575
    

    -------
    fide) as the major fungitoxin.  Viel and Chancogne (1966) tentatively
    identified the fungicidally active product of maneb as ethylenethiuram
    monosulfide.
    Zineb was more rapidly degraded in soil than in liquid cultures.  Ex-
    posure to sunlight for 19 months did not effect its degradation (Iley
    and Fiskell 1963).  Zineb was decomposed by temperatures of 200 C, with
    a weight loss of 34 percent and a change in color to brownish-black
    (Stojanovic et_ a^. 1972b) .  At 900 C, the volatile products of zineb
    decomposition were CO, CO , H S, and NH  (Kennedy e_t al. 1972b) .
    Chemically zineb could be degraded 99 percent or more by treatment with
    liquid NH,, plus metallic sodium or lithium, or with sodium biphenyl,
    while triethanolamine was not effective.  Treatment with 18/17 H_SO. re-
                                                                  2  4
    suited in formation of H^S and free zinc (Kennedy e_t_ al_. 1972a).  Nabam
    in soil was inactivated nonbiologically and very rapidly (Munnecke 1958).
    Transport-
    In soil columns, mobility was more affected by soil type for fungicides
    in suspension, such as zineb, than for those in solution, such as nabam.
    Dissolved fungicides were more mobile than suspended fungicides, and
    mobility of all fungicides was enhanced in wet rather than dry soil and
    in sandier and/or more porous soil.  Peat moss greatly decreased mobi-
    lity (Munnecke 1961).  No data were available on the transport of maneb,
    nabam, or zineb into or within water.  Ethylenethiourea was taken up by
    cucumbers (Vonk 1971).
    Persistence-
    As suggested by the ready decomposition of the dithiocarbamates by mois-
    ture, persistence in soil appears to be low.  Maneb persisted for three
    weeks when applied at one ppm, and more than 11 weeks but less than 12
    weeks when applied at 1,000 ppm (Chinn 1973).  No data were available
    on the persistence of the intermediate degradation products of the di-
    thiocarbamate fungicides in soil.  When beans and tomatos were treated
                                       576
    

    -------
    at seven day intervals with maneb with seven and eight treatments re-
    spectively, residues were present on the plants 14 days later  (Newsome
    et_a±. 1975).
    Effects on Soil and Soil Organisms-
    The effects of maneb, nabam, and zineb on soil processes and soil micro-
    organisms are summarized in Tables 87, 88 and 89.  It can be seen that,
    despite their economic status as fungicides, the dithiocarbamates are
    not uniformly or universally toxic to soil organisms.  Even relatively
    rapid recovery of fungal numbers (within 60 days) has been reported
    (Chandra and Bollen 1961) but after nabam treatment, soil fungal popu-
    lations consisted mostly of Tr-ichoderma and Penio-illvum (Corden and
    Young 1965).
    Dubey and Rodriguez (1970) analyzed the effects of nabam on nitrifica-
    tion and ammonification and found that nitrification was less  inhibited
    in rapidly nitrifying loam soil than in slowly nitrifying lateritic
    soil.  The ammonia-oxidizing bacteria were most strongly affected,
    while nitrite-oxidizing bacteria were not inhibited.  Maneb at 15 or 60
    ppm inhibited nitrification for eight weeks, while ammonification was
    inhibited only at 960 ppm.  Zineb applied to calcareous loam (pH 7.5)
    at 5,000 ppm reduced CO, evolution by 86 percent over a 56 day observa-
    tion period (Stojanovic et al. 1972a).  Mutagenesis was reported in
    Alternavia mali- by maneb, nabam and zineb (Slifkin 1973), and  in Sal-
    monella by maneb (Seiler 1973) but maneb was reportedly not mutagenic
    in Saccharomyces (Siebert et^ al. 1970).
    Effects on Non-Target Species-
    No evidence of mutagenesis by zineb was found in two studies on Droso-
    plntla melanogaster (Pilinskaya 1967, Ryazanov 1967).  Zineb was essen-
    tially nontoxic to honeybees at even the highest agricultural  levels
    of exposure (Nazarov 1966).
                                       577
    

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    -------
    In the amphibian Xenopus 1aevis3 nabam and maneb affected growth, mel-
    anogenesis, and notochordal development when eggs were exposed to 1-5
    ppm for 36-38 hours before hatching  (Bancroft and Prahlad 1973, Prahlad
    et al. 1974).  In hens, treatment with one percent of the LD^ of zineb
    — ~—~                                                       _)u
    decreased fertility, impaired egg development and caused degenerative
    changes in hens' livers, kidneys, and reproductive organs (Zhavoronkov
    et_ al. 1973).
    The oral LD,-n of dithiocarbamate fungicides to rats was calculated  to
    be between 1,000 and 8,000 mg/kg (Jones et_ a^. 1968).  Inhalation of
    zineb was observed to cause liver and kidney damage in albino rats
    (Ivanaova 1966).  A single dose of not more than 500 mg/kg or ten doses
    of 100 to 250 mg/kg of zineb did not cause poisoning in sheep (Palmer
    and Radeleef 1964).  Nabam pretreatment decreased the acute toxicity
    of methyl parathion in mice (Lange et_ al^. 1975).  Maneb and zineb,  if
    given at 250 mg/kg/day, reportedly increased blood coagulability in
    rabbits (Karpenko 1975).
    In cell culture, the carbamates zineb and carbaryl were found to accum-
    ulate more readily than the organochlorines HCH and DDT with lethal
    levels markedly lower in culture than in vivo (Shpirt 1973).  Zineb was
    considered to affect cell mitotic activity and cause chromosome damage
    (Rashev 1972); similar results were obtained when mice were injected
    with maneb or zineb (Kurinnyi and Kondratenko 1972) .
    Ethylene thiourea is a known thyroid carcinogen (Bontoyn and Looker
    1973, Hylin 1973) and it also caused lung tumors in rats (Rappoport et
    al. 1966) or orally (Didenko and Gupalovich 1975, Chernov and Khitsenko
    1969, Chernov 1972, Andrianova adn Alekseev 1970, Engst and Schnaak
    1974).  Maneb caused lung adenomas in mice (Chernov 1972) and in rats
    (Balin 1970).  Chepinoga et^ aJU (1970) administered 0.17 times the  LD--
    of zineb to rats, and classified the compound as blastemogenic and  em-
    bryotoxic while in the same study, maneb was found to be strongly em-
    bryotoxic and weakly mutagenic.  Zineb was not mutagenic and maneb  was
                                      581
    

    -------
    not tested for carcinogenicity.  Zineb was a transplacental carcinogen
    in mice (Kuitnitskaya and Kolesnichenko 1971).
    Ethylene thiourea, a degradation product of the thiocarbamate fungi-
    cides, was teratogenic and embryocidal in rats but only embryocidal in
    rabbits (Khera 1973).  Maneb was embryocidal in rats, and also caused
    reversible sterility of both males and females (Martsori 1969).  Maneb
    and zineb were teratogenic in rats only at levels greater than 2 g/kg,
    leading Petrova-Vergieva and Ivanova-Chemishanska (1971, 1973) to con-
    clude that human teratogenesis was unlikely.
    Conclusions-
    All methods of disposing of the dithiocarbamate fungicides maneb, nabam
    and zineb must take into account the carcinogenic metabolite ethylene
    thiourea.  If and only if this compound can be shown to be non-persis-
    tent in soil is soil disposal of these compounds feasible.  Either che-
    mical or thermal decomposition requires caution bacause of the release
    of H,jS, NH , and/or CO, but both are feasible for the dithiocarbamate
    fungicides.
                                      582
    

    -------
    Methyl Bromide
    Methyl bromide is the common name for bromomethane, a colorless gas
    with a boiling point of 4.5 C and a freezing point of -93 C.  The
    colorless liquid has an odor similar to that of chloroform.  Its solu-
    bility in water at 25 C is 13,400 ppm and it forms a voluminous crystal-
    line hydrate with ice water.  It is stable, neither corrosive nor in-
    flammable, and soluble in most organic solvents.  Methyl bromide is
    synthesized by the action of hydrobromic acid on methanol.  In the
    United States it is produced by American Potash, Dow Chemical Co.,
    Frontier Chemical Co., Great Lakes Chemical Co. and Michigan Chemical
    Co. for use as a soil fumigant against nematodes, fungi, and weeds.
    It is also used in the fumigation of storage areas and of stored pro-
    ducts.
    Degradation-
    Methyl bromide is decomposed by oxidative processes in soil and/or con-
    jugated with sulfhydryl-containing compounds, with concomitant debrom-
    ination (Goring et al. 1975) .  Shiroishi and co-workers (1964) used
    14
      C-methyl bromide to fumigate soil and found the residual radioacti-
    vity after one month to be heavily associated (44 percent) with pro-
    tein.  The same study demonstrated conjugation of methyl bromide with
    free amino acids.
    In the absence of oxygen, methyl bromide heated to 550 C decomposed to
    form methane (20 percent), hydrogen bromide (45 percent), considerable
    quantities of hydrogen, bromine, bromoethane, and CFL.  Other products
    included (CH Br) , anthracene and pyrene (Chaigneau et al. 1966).
                /   2.                                   	 	
    Photolysis of methyl bromide produced CH, when carried out in the pre-
    sence of silver, copper, or gold at temperatures between 50  and 250 C.
    Some C?Hfi was also recovered (McTigue and Buchanan 1959).  Photolysis
                                      583
    

    -------
    of methyl bromide at 1,850 A at 25 to 30 C in the presence of three
    percent bromine resulted in formation of methane (Kobrinsky and Martin
    1968).
    Transport-
    Methyl bromide is primarily lost into the air after soil fumigation.
    Some adsorbed methyl bromide might move with or through soil, but no
                                                     3
    data were available.  Soil fumigation with 73 g/m  of methyl bromide
    resulted in residues of up to 45 ppm in mature tomatoes, although the
    usual residues were considerable lower (Kempton and Maw 1973) .   Stored
    beans retained very high levels of methyl bromide for more than 17 days
    after treatment (Seefeld and Beitz 1968).  Aged methyl bromide was less
    readily taken up by plants than fresh, and plants accumulated more
    methyl bromide in roots and fruit than in leaves or stalks (Malkomes
    1972).
    Persistence-
    Methyl bromide is considered a nonpersistent pesticide inasmuch as more
    than 50 percent disappears from soil within one-half month (Goring et
    al. 1975).  Sorption of methyl bromide was greatest in peat, least in
    sand, and intermediate in clay soils; all soils adsorbed more methyl
    bromide when dry.  Moisture did not, however, increase the loss of
    methyl bromide from empty chambers (Chisholm and Koblitsky 1943) .  In
    sandy clay soil, eleven percent moisture affected little reduction of
    methyl bromide in a one-hour period (Fuhr et_ al. 1948).  The depth of
    soil penetration by methyl bromide depended on the dose applied (Mal-
    komes 1972).  Food residues of methyl bromide decreased with decreasing
    temperatures during fumigation (Dumas 1973) .
    Effects on Non-Target Species-
    The toxicity of methyl bromide to soil organisms can be gauged by its
    use as an herbicide, fungicide and nematocide (Martin 1968).  Essen-
    tially complete extermination of soil fauna in pine litter followed
                                       584
    

    -------
                         2
    treatment with 25 g/m   (250.4 kg/ha) of methyl bromide  (Heungens 1972),
    Among bacteria, spore forming organisms were more resistant than ni-
    trifying bacteria and fungi were more sensitive than actinomycetes.
    Methyl bromide was both less toxic and less selective in its toxicity
    than chloropicrin (Reber 1967).  Toxicity was greater in wet than in
    dry soils (McClellan et_ al. 1974) .
                                                 2
    In fine sand or fine loamy sand, 2 lbs/100 ft  (978 kg/ha) of methyl
    bromide decreased nitrification for 50 days, but overall bacterial
    activity increased above pretreatment levels after three weeks, and
    numbers of TT-ichoderma exceeded pretreatment levels after 30 weeks
    (Overman 1972) .  Winfree and Cox (1958) observed a two-month inhibi-
    tion of soil nitrification in Everglades peat after treatment with
                                  2
    methyl bromide at 2 lbs/100 ft  (978 kg/ha).
    Jenkinson and Powlson (1970) were able to detect effects of the elimi-
    nation of a section of the soil biomass by methyl bromide years later
    by stressing the soil organisms with formalin or radiation.  Second
    and subsequent fumigation resulted in less nitrogen mineralization re-
    gardless of the populations of pathogens present.  These data suggest
    permanent effects of methyl bromide on the complex of soil microorgan-
    isms even after the ordinary parameters of soil effects have returned
    to normal.
    In the host-mediated assay in mice, methyl bromide was mutagenic for
    Salmonella typh-imurium and Salmonella marcesoans (Buselmaier et_ al.
    1972).
    Conclusions-
    As a gas, methyl bromide would be totally unsuitable for soil disposal
    even if its toxicity to soil microorganisms were less profound or less
    long-lasting.  A reasonable method cf disposal is suggested by the
    ready anoxic decomposition of methyl bromide at 550 C.
                                      585
    

    -------
    Pentachlorophenol
    Pentachlorophenol is a white crystalline solid which is only slightly
    soluble in water (20 ppm at 30 C) but soluble in most organic solvents.
    It has a melting point of 190°C and a boiling point of 293°C, its va-
    por pressure increases from 0.00011 mm Hg at 20 C to 0.12 mm Hg at
    100 C, and it is volatile in steam.  Technical pentachlorophenol is a
    dark grey powder with a melting point between 187 and 189 C.
    Pentachlorophenol was introduced as a wood preservative in 1936 and is
    used as a fungicide, herbicide, defoliant and insecticide.  The sodium
    salt of pentachlorophenol is readily water soluble (300,000 ppm water
    at 25 C), but insoluble in petroleum oils.  It is used as a mollusci-
    cide and in other situations requiring aqueous solutions.  Pentachlor-
    ophenyl laurate, a nonfungicidal analog of pentachlorophenol, has been
    used as a mothproofing compound (Adema et_ al. 1967).
    Pentachlorophenol, produced by the catalytic chlorination of phenol,
    is manufactured by Dow Chemical Co. as Dowicide 7 and by Monsanto
    Chemical Co. as Santophen 20.  The corresponding sodium pentachloro-
    phenate products are Dowicide G and Santobrite.  The technical product
    is used directly or is formulated in oil.  Although pentachlorophenol
    is not deemed to need a trivial name, it is frequently referred to as
    PGP.
    Degradation-
    Biological—Pentachlorophenyl laurate was hydrolyzed to pentachlorophe-
    nol in the presence of soil, presumably by microbial action  (Allsopp
    et_ al. 1970) .  Degradation of pentachlorophenol by Tvic'hoderma virga-
    twn was observed, but no metabolites were identified (Cserjesi 1967a) .
    A single strain of Aphaloaseus fragrans was acclimatized to 0.2 per-
    cent (2,000 ppm) pentachlorophenol; all other species tested (Tvioho-
                                      586
    

    -------
    derma hapz-ianwrn, Tyiehoderma virgatum^ Tp-Lohoderma wirid-i3  Ceratoays-
    tis pil-ifeva3 Chaetom-ium globosum3 Graphium sp., Penieilliim  sp.) were
    inhibited by 0.04 percent  (400 ppm) pentachlorophenol  (Cserjesi  1967b) .
    Lyr (1963) reported detoxification of chlorinated phenols by  fungal
    oxidases, but no ring cleavage occurred, and the more  highly  chlorina-
    ted compounds were less susceptible even to detoxification.   In  paddy
    soil, pentachlorophenol decomposed to mono-, di-, tri-, and tetrachlor-
    ophenol.  Decomposition was more rapid in mature paddy soil than in
    immature soil with higher  levels of volcanic ash.  Since soil sterili-
    zation inhibited decomposition, microbial action was presumed (Ide et
    al. 1972).
    Suzuki and Nose (1970) analyzed decomposition of pentachlorophenol in
    farm soils, and observed that 90 percent was detoxified in  ten days
    when 100 ppm were applied  to the soil, but only ten percent detoxifi-
    cation of 1,000 ppm occurred in the same period.  Chloropicrin
    and C-H.HgO-acetate enhanced detoxification, whereas captan was inhi-
         o b
    bitory.  A gram-positive bacillus converted PCP to pentachloroanisole,
    with hydroquinone dimethyl ether as a minor product  (Suzuki and Nose
    1971) .  Chu and Kirsch  (1972) reported that a species of saprophytic
    coryneform bacteria was able to grow using pentachlorophenol as the
    sole source of carbon.  No other reports of ring cleavage were found.
    Vel-Muzquiz and Kaspar  (1974) considered microbial degradation to be
    relatively insignificant in the detoxification of pentachlorophenol,
    since they could not find evidence that microorganisms could grow with
    PCP as the sole source of carbon.
    Chicken-house litter treated with pentachlorophenol  imparted a musty
    taint to the chicken meat due to the microbial conversion of PCP to
    2,3,4,6-tetrachloroanisole (Curtis et^ a^. 1972).  In rats and mice,
    tetrachlorohydroquinone was the major, if not only, metabolite (Jakob-
    sen and Yllner 1971, Ahlborg and Lindgren 1974).
                                      587
    

    -------
    Photolytic—Sodium pentachlorophenate was inactivated by light of less
    than 330 nm when tested by bioassay against snail eggs (Hiatt et al.
    1960).  Pentachlorophenol itself was, in contrast, very stable to light
    (Crosby and Hamadmad 1971).  Among numerous compounds, including oxi-
    dized monomers and dimers, produced by the action of light on sodium
    pentachlorophenate were five products with greater toxicity to fish.
    Chloranilic acid was also produced, lending a purple color to the so-
    lution (Munakata and Kuwahara 1969).  Under field conditions, sodium
    pentachlorophenate was more rapidly degraded in clear, shallow water
    than in deep, turbid water, (Bevenue and Beckman 1969) suggesting that
    photolysis is a major degradative route.
    When sodium pentachlorophenate was exposed to sunlight, traces of oc-
    tachlorodibenzo-p-dioxin and other unidentified dioxins were found.
    The latter were unstable, but octachlorodibenzo-p-dioxin was stable to
    ultraviolet (Stehl et_ al. 1973, Plimmer 1973).
    In the presence of a large excess of oxygen, pentachlorophenol exposed
    to UV light of 230 nm or 290 nm was decomposed with 69 mg of the ini-
    tial 80 mg remaining after seven days.  In addition, 15 mg CO  and six
    mg HC1 were also recovered (Gaeb et al. 1975) .
    Chemical and physical—Pyrolysis of PCP at 300 C for 24 hours resulted
    in conversion to hexachlorobenzene, octachlorodiphenylene dioxide and
    other neutral polymeric products (Sanderman e_t_ al^. 1957).  Slow pyro-
    lysis at 200 C resulted in production of octachlorodibenzodioxin,
    while conversion of sodium pentachlorophenate to dioxins occurred at
    about 360 C (Langer e_t^ aJU 1973).  Nitric acid converts pentachloro-
    phenol to a mixture of tetrachloro-o-and p-quinones (Bevenue and Beck-
    man 1967) .
    Transport-
    Pentachlorophenol was relatively immobile in  acidic Hawaiian soil, but
    increasingly mobile as pH increased  (Green and Young 1971) .  In sandy
                                       588
    

    -------
    paddy soil, sodium pentachlorophenate leached more readily than PCP
    (Asa and Sakamoto 1963) .  PCP soil penetration was greater in xylenol
    emulsions than in oil emulsions (Sakagami et al. 1963).
    Transport of pentachlorophenol or its salts into water was demonstra-
    ted by the presence of 0.1 to 0.7 ppb of pentachlorophenol in the Wil-
    lamette River above Corvallis while the effluent from sewage treatment
    plants in three Oregon cities contained one to four parts per billion
    PCP in the water (Buhler et^ al. 1973).
    Persistence-
    The effectiveness of PCP decreased with decreasing pH between pH 3 and
    pH 8 and also decreased with increasing organic matter content of the
    soil and with increasing soil surface area (Su and Lin 1970).  Adsorp-
    tion to soil was positively correlated with soil organic matter, pH,
    and cation exchange capacity, and negatively correlated with clay con-
    tent and bioactivity (Tsunoda 1965).  Choi and Aomine  (1972) also noted
    that pentachlorophenol was less effective and more persistent in acid
    than in neutral soil, but there was no correlation in their study be-
    tween activity and the amount of clay, type of clay, or cation exchange
    capacity of the soil once the effects of pH and solubility were elimi-
    nated.  Low pH apparently decreased toxicity by decreasing the solubi-
    lity of pentachlorophenol.  Sodium pentachlorophenate was less soluble
    in humus-rich than in mineral soils, as would be expected of a lipid-
    immiscible compound.
    Treatment with 15 kg/ha of technical pentachlorophenol resulted in
    soil residues of 20.4 ppm of pentachlorophenol and 0.5 ppm of its im-
    purity, hexachlorobenzene.  The corresponding residues in lettuce were
    0.73 ppm and 0.01 ppm of PCP and hexachlorobenzene, respectively (Casa-
    nova and Dubroca 1973).  No degradation of either pentachlorophenol or
    sodium pentachlorophenate was observed after twelve months when these
    compounds were applied to warm, moist soil, but fixation to the clay
    fraction of the soil was not found (Harvey and Crafts 1952).  Penta-
                                      589
    

    -------
    chlorophenol applied to soil as a termiticide at an unspecified level
    persisted for more than five years (Hetrick 1952).
    Effects on Non-Target Species-
    Microorganisms—Data on the toxicity of pentachloropheriol to microor-
    ganisms are summarized in Table 90.  On soil derived from volcanic ash,
    pentachlorophenol was the strongest inhibitor of nitrification among
    eight herbicides tested.  In increasing order of toxicity, the compounds
    were:  Prometryne < lenacil < diphenamid < trifluralin < vernolate
    < MCPA < SWEP < pentachlorophenol.  Pentachlorophenol was the only com-
    pound to prevent oxidation of nitrite to nitrate as well as nitrite
    formation from ammonium ion (Noguchi and Nakazawa 1971).
    Invertebrates—Pentachlorophenol applied at 2.5 to 4 kg/ha decreased
    the number of earthworms (species not identified) in the top ten cen-
    timeters of soil by 50 percent (Kononova and Kazimirchuk 1970).  In
    sea urchin eggs (Ardbaa'ia), pentachlorophenol inhibited mitoses and
    disturbed the structure of the mitotic spindle (Sawada and Rebhun
    1969).  No embryos of clams (Mereenaria mevcenaria) or oysters (Cras-
    sostrea vipginicoC) exposed to 0.25 ppm sodium pentachlorophenate sur-
    vived, nor did eggs of either species hatch when exposed to 0.025 ppm
    sodium pentachlorophenate.  At the lower dose, 41 percent of oyster
    larvae survived (Davis and Hidu 1969).
    Vertebrates—The 24 hour LC,-^ of sodium pentachlorophenate for rain-
    bow trout (Salmo gairdnerii) was 0.26 ppm; for guchi fish (Naibea al-
    biflora), 0.09 ppm (Pimentel 1971).  Bevenue and Beckman (1967) re-
    viewed the toxicology of pentachlorophenol to fish.
    In birds, the LDcn for five days' treated feed followed by three days'
    clean feed was 4,000 to 5,000 mg/kg pentachlorophenol in pheasants,
    and 5,000 to 6,000 mg/kg in coturnix quail (Pimentel 1971).
    The acute oral LD   of pentachlorophenol was 27 to 80 mg/kg in rats,
    while that of sodium pentachlorophenate was 210 mg/kg  (Pimentel 1971).
                                       590
    

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    -------
    Tilemans and Dormal (1952) cited a human acute oral LD   of 275 mg/kg.
    Izeke and Iwao (1956)  calculated an acute oral LD-n of 199 mg/kg for
    mice.  Dermal toxicity is also well known (Bevenue and Beckman 1967).
    Pentachlorophenol was markedly less toxic in rabbits at 8 C than at
    36 C (Keplinger et al. 1959).   The biochemical basis of the toxicity
    of pentachlorophenol is its capacity to uncouple oxidative phosphory-
                               -6       -4              -4        -3
    lation at concentrations 10   to 10  M.  Between 10  M and 10  M, pen-
    tachlorophenol also inhibits mitochondrial ATPase, and at levels above
      _3
    10  M, PCP inhibits glycolytic phosphorylation, inactivates respira-
    tory enzymes, and causes gross damage to mitochondrial structures
    (Weinbach 1957).   No data pertaining to carcinogenesis, mutagenesis,
    or teratogenesis of PCP were available.
    Conclusions-
    Sufficiently little is known about the degradation of pentachlorophenol
    that any method of disposal is a gamble.  The few available data make
    it obvious, however, that biodegradation rarely includes ring cleavage.
    Soil disposal is therefore inadvisable unless the nature, toxicity,
    and persistence of the terminal residues are elucidated.  Similarly,
    in the absence of extensive data on the nature, quantity, toxicity,
    and persistence of the dioxins produced by pyrolysis of PCP over a
    wide range of temperatures, no conclusions can be drawn as to the feas-
    ibility of burning this compound.
                                      592
    

    -------
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                                     593
    

    -------
    Bancroft, R. and K. V. Prahlad; 1973.  Effect of ethylenebis(dithio-
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      (Chem. Abstr. 64:12546b, 1966).
    Petrova-Vergieva, T. and L. Ivanova-Chemishanska; 1971.  Teratogenic
      effect of zinc ethylenebis(dithiocarbamate) (zineb) in rats.  Eksp.
      Med. Morfol. 10:226-230. (Chem. Abstr. 76:149708p, 1971).
    Petrova-Vergieva, T. and L. Ivanova-Chemishanska; 1973.  Assessment of
      the teratogenic activity of dithiocarbamate fungicides.  Food Cos-
      met. Toxicol. 11:239-244.
    Pfeifer, F. T. and G. Pfeifer; 1970.  Thermal decomposition of fungi-
      cides of the phthalimide type.  Proc. Anal. Chem. Conf., 3rd.   2:
      371-377. (Chem. Abstr. 74:52423n, 1971).
    Picci, G.; 1956.  Effect of captan on soil microorganisms.  Agr. Ital.
      (Pisa) 56:376-382. (Chem. Abstr. 51:6926g, 1957).
    Pilinskaya, M. A.; 1967.  Mutagenic properties of zineb and ziram in
      Drosophila.  Gig. Toksikol. Pestits. Klin. Otravlenii 5:305-311.
      (Chem. Abstr. 71:122773r, 1969).
    Pilinskaya, M. A.; 1974.  Results of the cytogenic examination of per-
      sons occupationally in contact with the fungicide zineb.  Genetika
      10:140-146. (Chem. Abstr. 81:67966k, 1974).
    Pimentel, D. ; 1971.  Ecological effects of pesticides on non-target
      species.  Exec. Office of the President, Office of Science and Tech-
      nology, U.S. Gov't. Printing Office, Wash., D. C.
    Plimmer, J. R. ; 1973.  Technical pentachlorophenol, origin and analy-
      sis of base-insoluble contaminants.  Environ.  Health Perspect. 5:
      41-48.
    Pochon, J., J. Lajudie and 0. Coppier; 1951.  Action of certain anti-
      parasitic substances on the microflora of the soil.  Ann. Inst. Pas-
      teur. 80:517-519.
                                      605
    

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    Prahlad, K. V., R. Bancrot and L. Hanzely; 1974.  Ultrastructural
      changes induced by the fungicide ethylenebis(dithiocarbamic acid)
      disodium salt (nabam) in Xenopus laevis tissues during development.
      Cytobios 9:121-130. (Chem. Abstr. 81:59000a, 1974).
    Pugh, G. J. F.; 1973.  Effect of three fungicides on nitrification and
      ammonification in soil.  Soil Biol. Biochem. 5:577-584.
    Rappoport, M. B. , E. I. Makovskaya and R. P. Khaustova; 1966.  Pulmon-
      ary adenomas induced by a zinc dithiocarbamate (zineb).  Vrach, Delo.
      1966:100-104. (Chem. Abstr. 66:9344z, 1967).
    Rashev, Z.; 1972.  Cytopathic and cytotoxic action of pesticides on
      cell structures.  Eksp. Med. Morfol. 11:35-39. (Chem. Abstr. 77:
      97462c, 1972).
    Reber, H.; 1967.  Vergleichende Untersuchungen zur ToxizitSt und Selek-
      tivitat von Entseuchungsmitteln flir Bodenmikroorganismen.  Z. Pflan-
      zenkr. Pflanzenschutz. 74:414-426.
    Rich, S. and J. G. Horsfall; 1950.  Gaseous toxicants from organic sul-
      fur compounds.  Am. J. Botany 37:643-650.
    Richmond, D. V. and J. A. Pickard; 1967.  Carbonyl sulfide from the
      decomposition of captan.  Nature 215:214.
    Richmond, D. V. and E. Somers; 1968.  The fungitoxicity of captan. VI.
                       35
      Decomposition of   S-labeled captan by Neurospora orassa conidia.
      Ann. Appl. Biol. 62:35-43.
    Ryazanov, R. A.; 1967.  Effect of the fungicides ziram and zineb on the
      generative function of test animals.  Gig. Sanit. 32:23-30.  (Chem.
      Abstr. 66:85011q, 1967).
    Sakagami, Y., S. Suzuki, T. Ishino, Y. Sugihara and H. Hyuga; 1963.
      Translocation of pentachlorophenol in soil.  Meiji Daigaku Nogakubu
      Kenkyo HOkoku 15:41-46.  (Chem. Abstr. 60:6165b, 1964).
    Sanderman, W., K. Stockmann and R. Casten; 1957.  Uber die Pyrolyse
      des Pentachlorophenols.  Chem. Ber. 90:690-692.
    Sawada, N. and L. I. Rebhun; 1969.  Effect of dinitrophenol and other
      phosphorylation uncouplers on the firefringence of the mitotic appa-
      ratus of marine eggs.  Exp. Cell. Res. 55:33-38.
                                      606
    

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    Seefeld, F. and H. Beitz; 1968.  Dynamics of methyl bromide residue
      deposit in gassed products.  Nachrichtenbl. Deut. Pflanzenschutz-
      dienst. (Berlin) 22:248-252. (Chem. Abstr. 71:37549c, 1969).
    Seidler, H., M. Haertig, W. Schnaak and R. Engst; 1970.  Untersuchun-
      gen liber den Metabolismus einiger Insektizide und Fungizide in der
                                                14
      Ratte.  2. Mitt. Verteilung und Abbau von   C-markiertem Maneb.
      Nahrung 14:363-373.
    Seidler, H., H. Haertig, W. Schnaak and R. Engst; 1971.  Untersuchun-
      gen iiber den Metabolismus einiger Insektizide und Fungizide in der
                                                              35
      Ratte.  3. Mitt:  Ausscheidung Verteilung und Abbau von   S-markier-
      tem Captan.  Nahrung 15:177-185.
    Seiler, J. P.; 1973.  Survey on the mutagenicity of various pesticides.
      Experientia 29:622-623.
    Shaw, F. R.; 1959.  The effects of field applications of some of the
      newer pesticides on honeybees.   J. Econ. Entomol. 52:549-550.
    Shea, K. P.; 1972.  Captan and folpet.  Environment 14:22-24, 29-32.
    Shiroishi, M., A. Hayakowa, K. Okumura and K. Umeda; 1964.  Methyl
      Bromide.  Shokuryo Kenkyusho Kenkyu Hokoku 18:193-199. (Chem. Abstr.
      66:36639s, 1967).
    Shpirt, M. B.; 1973.  Toxicological evaluation of the action of DDT,
      hexachlorocyclohexane, tetramethylthiuram, Sevin, and zineb on human
      cell cultures.  Gig. Tr. Prof.  Zabol. (3) 1973:32-35. (Chem. Abstr.
      79:1088c, 1973).
    Siebert, D., F. K. Zimmermann and E. Lemperle; 1970.  Genetic effects
      of fungicides.  Mutat. Res. 10:533-543.
    Slifkin, M. K.; 1973.  Apparent induction of mutants and enhancement
      of conidial formation by fungicides in A.lter'nar'la malt.   Mycopathol.
      Mycol. Appl. 50:233-240.
    Boeder, C. J., R. Liersch and U.  Trueltzsch; 1969.  Unterschiedliche
      Wirkung von Captan auf das Wachstum einiger Stamme von Chlovella
      und Scenedesmus.  Arch. Mikorbial 67:166-172.
    Somers, E. and R. J. Pring; 1966.  Uptake and binding of dodine acetate
      by fungal spores.  Ann. Appl. Biol. 58:457-466.
                                     607
    

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    Somers, E., D. V. Richmond and J. A.  Pickard; 1967.   Carbonyl sulfide
      from the decomposition of captan.   Nature 215:214.
    Stehl, R. H.,  R. R. Papenfuss, R. A.  Bredeweg and R.  W.  Roberts; 1973.
      Stability of pentachlorophenol and  chlorinated dioxins to sunlight,
      heat, and combustion.  Advan. Chem. Ser.  120:119-125.
    Stojanovic, B. J., M. V. Kennedy and  F.  L.  Shuman, Jr.;  1972a.   Edaphic
      aspects of the disposal of unused pesticides,  pesticide wastes and
      pesticide containers.  J. Environ.  Qual.  1:54-62.
    Stojanovic, B. J., F. Hutto, M. V. Kennedy and F. L.  Shuman, Jr.; 1972b.
      Mild thermal degradation of pesticides.   J. Environ.  Qual. 1:397-401.
    Su, Y. and H.  Lin; 1970.  Influence of soil physiochemical character-
      istics on the efficacy of herbicide pentachlorophenol.  Chung. Kuo
      Nung Yeh Hua Hsueh Hui Chih 8:99-104.  (Chem. Abstr. 74:110707w, 1971).
    Suzuki, T. and K. Nose; 1970.  Decomposition of pentachlorophenol in
      farm soil.  I. Factors relating to  pentachlorophenol decomposition.
      Noyaku Seisan Gijutsu 22:27-30. (Chem. Abstr.  76:13140q, 1972).
    Suzuki, T. and K. Nose; 1971.  Decomposition of pentachlorophenol in
      farm soil.  II. PCP metabolism by a microorganism isolated from soil.
      Noyaku Seisan Gijutsu. 26:21-24. (Chem.  Abstr. 77:4204g, 1972).
    Tews, L. L.; 1971.  Effects of selected  fungicides and soil fumigants
      upon the microfungi of a cattail marsh.   Proc. Conf.  Gt. Lakes Res.,
      14th.  128-136. (Chem. Abstr. 77:110348s, 1972).
    Tilemans, E. and S. Dormal; 1952. Toxicite des produits phytopharm-
      ceutiques envers 1'homme et les animaux £ sang chaud.   Parasitica
      8:64-89.
    Tokunaga, S.;  1968.  Metabolism of pentachlorophenol in fish and mam-
      mals.  I. Distribution of pentachlorophenol in fish.   Kagaku Keisatsu
      Kenkyusho Hokoku. 21:126-130.  (Chem. Abstr. 69:84467t, 1968).
    Tsunoda, H.; 1965.  Pentachlorophenol (PCP) adsorption on soil.  I.
      Soil effect on PCP adsorption and  influence of PCP adsorption on the
      herbicidal efficiency of PCP.  Nippon Dojo-Hiryogaku Zasshi 36:187-
      190.  (Chem.  Abstr. 64:8860h, 1966).
                                       608
    

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    Ukeles, R.; 1962.  Growth of pure cultures of marine phytoplankton in
      the presence of toxicants.  Appl. Microbiol. 10:532-537.
    Vashakidze, V. I., R. N. Mandzhgaladze and V. S. Zhorzholiani; 1973.
      Toxicity of captan and its hygienic standardization in foods.  Gig.
      Sanit. 10:24-27. (Chem. Abstr. 80:34256e, 1974).
    Vel-Muzquiz, R. and P. Kasper; 1974.  Effect of pentachlorophenol on
      the microbial flora of selected soils.  Microbiol. Espan. 26:21-30.
      (Chem. Abstr. 80:8l467j, 1974).
    Verrett, M. J., M. K. Mutchler, W. F. Scott, E. F. Reynaldo and J. Mc-
      Laughlin; 1969.  Teratogenic effects of captan and related compounds
      in the developing chick embryo.  Ann. N.Y. Acad. Sci. 160:334-343.
    Viel, G. and M. Chancogne; 1966.  Maneb decomposition.  The action of
      water and oxygen.  Phytiat.-Phytopharm. 15:31-39. (Chem. Abstr. 66:
      18265n, 1967).
    Vinci, M.; 1953.  Action of methyl bromide in pregnancy.  Folia Med.
      36:899-907. (Chem.  Abstr. 48:6571d, 1954).
    Vondruska, J. F., 0.  E. Fancher and J. C. Calandra; 1971.  Investiga-
      tion into the teratogenic potential of captan, folpet, and Difolatan
      in nonhuman primates.  Toxicol. Appl. Pharmacol. 18:619-624.
    Vonk, J. W.; 1971.  Ethylenethiourea, a systemic decomposition product
      of nabam.  Meded. Fac. Landbouwwetensch., Rijksuniv. Gent. 36:109-
      112. (Chem. Abstr.  76:21724y, 1972).
    Wainwright, M. and G. J. F. Pugh; 1974.  Effects of fungicides on cer-
      tain chemical and microbial properties of soils.  Soil Biol. Biochem.
      6:263-267.
    Weinbach, E. C.; 1957.  Biochemical basis for the toxicity of penta-
      chlorophenol.  Proc. Natl. Acad. Sci. U.S. 43:393-397.
    Wilson, H. A.; 1954.   The effect of certain pesticides on nitrifica-
      tion in the soil.  W. Va. Agr. Expt. Sta., Bull. 366T, 14 pp.; Soils
      and Fertilizers.  17:502. (Chem. Abstr. 51:12415a, 1957).
    Winfree, J. P. and R. S. Cox; 1958.  Comparative effects of fumigation
      with chloropicrin and methyl bromide on mineralization of nitrogen
                                      609
    

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      in Everglades peat.  Plant Disease Reptr. 42:807-810.
    Woolson, E. A., R. F. Thomas and P. D. J. Ensor; 1972.  Survey of
      polychlorodibenzo-p-dioxin content in selected pesticides.  J. Agr.
      Food Chem. 20:351-354.
    Zhavoronkov, N. I., A. V. Akulov, S. D. Antsiferov, A. P. Verkhovskii
      and S. M. Evdokimov; 1973.  Effect of carbamates on hens.  Veteri-
      nariya 1973(8):114-116. (Chem. Abstr. 79:122422r, 1973).
                                      610
    

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                              SECTION VI SYNTHESIS
    Figures 19, 20 and 21 summarize the data available for the 45 pesticides
    reviewed in this report.  Persistence of both the original pesticide
    and of its metabolites or contaminants were characterized as low, mod-
    erate or high by the length of the bar on each graph, and the potential
    transport was similarly ranked.  These were considered the primary cri-
    teria for each pesticide's suitability for soil disposal.  Evaluation
    of toxicity is included in the figures for completeness, as is the con-
    clusion as to the feasibility of soil disposal, which is repeated from
    Table 1.
    The acute toxicity of a pesticide includes its effects on soil organisms,
    aquatic organisms, birds and mammals, while chronic toxicity includes
    reproductive effects and carcinogenesis.  The characterization of per-
    sistence, transport and toxicity is qualitative by necessity.  Where the
    available information is too incomplete even for qualitative conclusions,
    unshaded bars were used.
    Of forty-five pesticides, only ten are considered suitable for soil dis-
    posal in the light of presently available data.  For several of these,
    suitability is presumed despite very little information because of the
    absence of unfavorable information.  Several organophosphate compounds
    (methyl parathion, parathion, azinphosmethyl) are considered questiona-
    bly soil disposable because recent data suggest they do not decompose
    when massed in soil.  Therefore it must be stressed that the character-
    ization of pesticides as suitable for soil disposal is optimistic, and
    the number of such compounds will probably decrease as more data accu-
                                      611
    

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    mulate.  In contrast, there is a small but carefully established body
    of data on chemical and thermal disposal of certain pesticides.  Al-
    though incineration of pesticides requires many precautions, it seems
    more effective, and certainly more complete, than soil disposal.
    
    We therefore conclude that incineration is a more promising mode of
    pesticide disposal than is soil incorporation, and strongly recommend
    its continued assessment.
                                     615
    

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                                      APPENDIX
          The data cited in this report are cited in metric units both in the tables
    and in the text.  Where the data were originallly reported in other than metric
    units, the following conversions were employed:
    
    
          soil treatments:       1 Ib/A = 1.12 kg/ha
          soil concentrations:  0.5 ppm = 1.0 kg/ha
          solutions:            1.0% = 10,000 ppm
                                1 mg/ml = 1,000 ppm
                                          616
    

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                                        TECHNICAL REPORT DATA
                                (Please read Instructions on the reverse before completing)
    1. REPORT NO.
       EPA-600/9-77-022
                                  2.
                                                                3. RECIPIENT'S ACCESSION-NO.
    4. TITLE AND SUBTITLE
      The  Degradation of Selected Pesticides  in Soil:
      A Review of the Published Literature
                                          5. REPORT DATE
                                           August  1977 (Issuing Date)
                                          6. PERFORMING ORGANIZATION CODE
    7. AUTHOR(S)
      James  R.  Sanborn
      B. Magnus Francis
                                                                8. PERFORMING ORGANIZATION REPORT NO.
       Robert L. Metcalf
    9. PERFORMING ORGANIZATION NAME AND ADDRESS
      Illinois  Natural History  Survey
      University of Illinois
      Urbana,  Illinois  61801
                                          1O. PROGRAM ELEMENT NO.
                                          1DC618, SOS//4,  Task 04
                                          11. CONTRACT/GRANT NO.
                                            R-803591-01
    12. SPONSORING AGENCY NAME AND ADDRESS
      Municipal Environmental  Research Laboratory—Cin.,  OH
      Office  of Research  & Development
      U.S.  Environmental  Protection Agency
      Cincinnati,  Ohio  45268
                                                                 13. TYPE OF REPORT AND PERIOD COVERED
                                            2/23/75-5/1/76
                                          14. SPONSORING AGENCY CODE
    
                                            EPA/600/14
    15. SUPPLEMENTARY NOTES
        Project Officer:
    Richard  Games (513-684-7871)
    16. ABSTRACT
       This  report contains  a  literature summary on the degradation of forty-five
       pesticides in soil.   The point of beginning of each literature review  is  the year
       of  issue of the patent  for the particular pesticide.  After compilation of  the
       literature data for each pesticide, conclusions were formulated regarding the
       suitability of soil disposal of these pesticides.  On the basis of the data
       collected in this report it was suggested that ten pesticides are suitable  for
       soil  disposal, twenty-one are not suitable for disposal,  and the data  for
       fourteen are insufficient to formulate  any conclusions  regarding their suitability
       for soil disposal.
    17.
                                    KEY WORDS AND DOCUMENT ANALYSIS
                      DESCRIPTORS
                            b.IDENTIFIERS/OPEN ENDED TERMS  C.  COS AT I Field/Group
       ^Pesticides
       Degradation
       Disposal
       Research
                                                            13  B
                                                            6 F
    13. DISTRIBUTION STATEMENT
    
       RELEASE TO  PUBLIC
                            19. SECURITY CLASS {This Report)
                               TTnrl qggj
    21. NO. OF PAGES
         633
                                                   20 SECURITY CLASS (Thispage)
    
                                                     Unclassifiprl
                                                                              22. PRICE
    EPA Form 2220-1 (9-73)
                                                 617
                                                         , U S GOVERNMENT PRINTING OFFICE 1977-757-056/6507 Region No. 5-11
    

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