-------
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
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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.
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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
-------
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
-------
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
-------
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
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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
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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
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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
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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
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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
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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
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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
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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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207
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208
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209
-------
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210
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211
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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
-------
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
-------
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
-------
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
-------
/ \ \
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
-------
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
-------
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
-------
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
-------
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
-------
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
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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
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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
-------
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
263
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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
266
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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
268
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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
270
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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
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1 = mammals
2 = insects
CL
aldrin
METABOLIC PATHWAYS OF ALDRIN AND DIELDRIN
Figure 8
272
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1 = RAT 4 = PLANT
2 = INSECT 5 = PWNT
3 = SOIL 6 = ANIMAL
METABOLIC PATHWAYS OF ISODRIN AND ENDRIN
Figure 9
213
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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
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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,
278
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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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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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290
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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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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
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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
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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
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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
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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
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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
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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
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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
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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
-------
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
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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
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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
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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
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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
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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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415
-------
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
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P-NITROPHENOL
ANIMAL
HO.
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T
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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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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 <27?raz-irradiation of 0.1 to 5.0 megarads decomposed
71 percent of malathion in hexane (Lippold et_ al. 1969). The heat pro-
duced by infrared light also decomposed malathion (Mosher and Kadoum
1972). Stojanovic e_t al. (1972b) identified the degradation products
of malathion heated to 300 C to be the diethyl esters of succinic, mal-
eic, and/or fumaric acids. Pure malathion was 25 percent decomposed
by heating to 663 C, but formulated malathion was 25 percent decomposed
only at 715 C (Kennedy et^ al_. 1969). At 900°C, malathion decomposed
to form carbon monoxide, carbon dioxide, sulfur dioxide, hydrogen sul-
fide, and oxygen (Kennedy et_ a!U 1972b) .
Transport-
Within soil—At relative humidity greater than 40 percent, malathion
penetrated into montmorillonite (Bowman et_ al_. 1970). Between 4.2 and
5.3, the pH of the clays did not affect adsorption, but calcium and
magnesium clays adsorbed less malathion than potassium clays. Malathion
adsorption was positively correlated with organic matter content, hu-
mic acid content, and cation exchange capacity (MacNamara and Toth
1970). On pond sediments and watershed soils, malathion was more rea-
dily adsorbed than either phorate or carbaryl (Meyers et al^. 1970). No
data were abailable on the movement of malathion through soil, and
little significance can be attached to the effects of such movements
since malathion is ordinarily degraded rapidly. But the absence of
degradation of adsorbed malathion (Bowman et al. 1970) suggests that
movement of malathion with soil, as on washoff, is possible. No data
were available on the transport of malathion metabolites and no data
were available on the movement of malathion or its metabolites between
soil and water or between water and sediment.
Into organisms—No malathion residues were found in milk after treat-
ment of cows with ultra-low-volume sprays for horn fly control (Oehler
452
-------
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.
The effects of malathion on aquatic microorganisms are summarized in
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
decreased the nitrogen content of the clover (Salem et al. 1971).
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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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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484
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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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532
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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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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
-------
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
-------
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
-------
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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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605
-------
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35
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14
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35
Ratte. 3. Mitt: Ausscheidung Verteilung und Abbau von S-markier-
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Seiler, J. P.; 1973. Survey on the mutagenicity of various pesticides.
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79:1088c, 1973).
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607
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Somers, E., D. V. Richmond and J. A. Pickard; 1967. Carbonyl sulfide
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608
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609
-------
in Everglades peat. Plant Disease Reptr. 42:807-810.
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polychlorodibenzo-p-dioxin content in selected pesticides. J. Agr.
Food Chem. 20:351-354.
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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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