EPA 660/2-74-011
APRIL 1974
                        Environmental Protection Technology Series
   A  Demonstration of Thermal  Water
   Utilization in Agriculture
                                 Office of Research and Development

                                 U.S. Environmental Protection Agency
                                 Washington, O.C. 20460

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                    RESEARCH REPORTING SERIES
Research reports of the Office of Research and Development,
U.S. Environmental Protection Agency, have been grouped into
five series.  These five broad categories were established to
facilitate further development and application of environmental
technology.  Elimination of traditional grouping was consciously
planned to foster technology transfer and a maximum interface
in related fields.  The five series are:

     1.   Environmental Health Effects Research
     2.   Environmental Protection Technology
     3.   Ecological Research
     4.   Environmental Monitoring
     5.   Socioeconomic Environmental Studies

This report has been assigned to the ENVIRONMENTAL PROTECTION
TECHNOLOGY STUDIES series.  This series describes research performed
to develop and demonstrate instrumentation, equipment and methodology
to repair or prevent environmental degradation from point and
non-point sources of pollution.  This work provides the new or
improved technology required for the control and treatment of
pollution sources to meet environmental quality standards.
                        EPA REVIEW NOTICE

This report has been reviewed by the Office of Research and
Development, U.S. Environmental Protection Agency, and approved
for publication.  Approval does not signify that the contents
necessarily reflect the views and policies of the U.S. Environmental
Protection Agency, nor does mention of trade names or commerical
products constitute endorsement or recommendation for use.

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                                                       EPA-660/2-74-011
                                                       April  1974
                    A DEMONSTRATION OF

                 THERMAL WATER UTILIZATION

                      IN AGRICULTURE
                             by
                      James W.  Berry
                   Herman H. Miller, Jr.
                       Grant S802032
                   Program  Element 1BB392


                      Project Officer

                    AT den Christiansen
                  Thermal Pollution Branch
      Pacific Northwest Environmental Research Laboratory
          National Environmental  Research Center
                  Corvallis,  Oregon  97330
                       Prepared for

             OFFICE OF RESEARCH AND DEVELOPMENT
            U.S. ENVIRONMENTAL  PROTECTION AGENCY
                  WASHINGTON, D.C.   20460
For sale by the Superintendent of Documents, U.S. Government Printing Office, Washington, D.C. 20402 - Price $2.80

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                           ABSTRACT
The five-year thermal water demonstration project described in
this report was designed to determine benefits and uncover any
harmful effects related to thermal  water's application in agri-
culture.  The water's temperature approximated that which would
be expected from fossil or nuclear power stations and other in-
dustrial plants.  Benefits were explored in the following areas:
frost protection, undersoil heating, greenhouse applications,
double cropping, plant cooling, and humidity control.

Benefits to agriculture of the water's heat content are described;
no detrimental effects were uncovered.

This report is submitted in fulfillment of Grant S802032 by Eugene
Water & Electric Board under the partial sponsorship of the En-
vironmental Protection Agency.  Work was completed as of May 31,
1973.
                              m

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                           TABLE OF CONTENTS
                                                                Page
Abstract                                                         iii
Table of Contents                                                  v
List of Figures                                                   ix
List of Tables                                                    xv
Acknowledgments                                                  xix
Consultants                                        '              xxi
Conclusions                                                    xxiii
Economics                                                       xxix
Recommendati ons                                               xxxi i i
Section I.  Introduction                                           1
     Background                                                    1
     Early Evolution of the Project                                3
     Early Siting Plans                                            5
     Objectives                                                    7
     The Project's Organization                                    8
     The Irrigation System                                         8
     Irrigation Scheduling                                        10
     Monitoring Equipment                                         10
Section II.  Thermal Water Conditions                             17
     Thermal Water Temperature                                    17
Section III.  Frost Protection                                    21
     Introduction                                                 21
     Frost Protection Objectives                                  22
     Procedure                                                    22

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                                                              Page

     Results 1969                                               25

             1970                                               30
             1971                                               35

             1972                                               37

             1973                                               47

     Discussion                                                 47

Section IV.  Thermal Water Irrigation and Plant Cooling         53

     Thermal Water Irrigation                                   53

        Introduction                                            53
        Procedure                                               56
        Results                                                 63

     Plant Cooling                   •                           77

        Procedure                                               79
        Results                                                 80

Section V.  Undersoil Heating                                   89

     Design Information and Assumptions                         89
        Selection of Pipe Material                               91
        Heat Transfer                                           93
        Soil Heating Literature Survey                         102
     General Procedure                                         104

     Recorded Soil Temperatures                                107

     The Influence of Soil Heat on  Selected Plants             110

        Tomatoes                                               116
        Sweet Corn                                             118
        Asparagus Crown Planting                               124
        Asparagus Nursery                                      130
        Rhododendrons                                          134
        Cantaloupes                                            137
        Squash                                                 143

Section VI.  Soil Heated Greenhouse                            147

     Greenhouse Air Temperatures                               147

     Greenhouse Soil Temperatures                              149

     Greenhouse Crop Production                                155

        Leaf Lettuce                                           155
        Tomatoes                                               161
        Japanese Salad and European Cucumber                   168
                                VI

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Section VII.  Mold Count, Bacteria, and Mycotoxin Study        175

Section VIII.  Soil Heat/Irrigation                            181

     Plot Description                                          181

     Procedure                                                 181

        Cucumbers                                              186
        Snap Beans                                             186
        Cabbage                                                187
        Peppers                                                187
        Tomatoes                                               187
        Lima Beans                                             187
        Onions                                                 187

     Tabular Data:  Soil Heat/Irrigation                       188

Section IX.  References                                        197

Section X.  Appendices                                         203
                                vii

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                          LIST OF FIGURES
Frontispiece:  The Thermal  Water Project on
               the McKenzie River                            xxxv

No.
 la    Willamette basin map                                     6

 1     Weyerhaeuser pumping pit                                 9

 2     Thermal water system exhaust                            11

 3     Weekly mean temperature of thermal  water as it          18
       leaves cooling condenser of Weyerhaeuser's elec-
       trical generating plant (pumping pit),  enters  the
       soil heat grid (inlet)  about 2.7 miles  from pump-
       ing pit, exits from soil heat grid  (outlet), and
       collects in pool surrounding spray  exhaust (ex-
       haust pool) before it filters through gravel back
       to the river

 4     Mean daily ambient air temperatures averaged by          19
       weeks from January 1972 to March 1973 and long
       term weekly mean temperatures, 1931-1965

 5     Exposed open-bulb minimum thermometer                   24

 6     Influence of thermal water (85°F) applied through       26
       undertree sprinklers (at .22 in/hr) on  air
       temperatures 1 ft above the ground  on March 23,
       1973 (dew point was 24° to 26°F outside orchard)

 7     Influence of thermal water (85°F) applied through       27
       undertree sprinklers (at .22 in/hr) on  air temp-
       eratures 5 ft above the ground on March 23, 1973
       (dew point was 24° to 26°F outside  orchard)

 8     Influence of thermal water (85°F) applied through       28
       undertree sprinklers (at .22 in/hr) on  air temp-
       eratures 10 ft above the ground on  March 23, 1973
       (dew point was 24° to 26°F outside  orchard)

 9     Influence of thermal water (85°F) applied through       29
       undertree sprinklers (at .22 in/hr) on  air temp-
       eratures 20 ft above the ground on  March 23, 1973
       (dew point was 24° to 26°F outside  orchard)

                                 ix

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No.                                                           Page

10     Air temperature modification at the 5 ft level          33
       under thermal water applied through sprinklers
       on 15 ft risers (March, April  1970)

11     Air temperature modification at the 1 ft level          34
       under thermal water using 18 in. risers

12     Ice load in peach and apple orchard                     36

13     Air temperature at 5 ft height in a sour cherry         39
       orchard frost protected with overtree, sprinkler
       applied, thermal water and in an open area
       adjacent to orchard:  wind speed recorded about
       800 ft north of orchard

14     Air temperature at 10 ft height in a sour cherry        40
       orchard frost protected with overtree, sprinkler
       applied, thermal water and in an open area ad-
       jacent to orchard

15     Air temperature at 20 ft height in a sour cherry        41
       orchard frost protected with overtree, sprinkler
       applied, thermal water and in an open area adja-
       cent to orchard

16     Air temperature at 1 ft height in blocks of             43
       vegetable crops that were frost protected with
       sprinkler applied thermal and cold water and in
       non-irrigated area:  wind speed recorded about
       1200 ft east of vegetable plots

17     Air temperature at 5 ft height in blocks of vege-       44
       table crops that were frost protected with
       sprinkler applied thermal and cold water and in
       non-irrigated area:  wind speed recorded about
       1200 ft east of vegetable plots

18     Air temperature at 10 ft height in blocks of            45
       vegetable crops that were frost protected with
       sprinkler applied thermal and cold water and in
       non-irrigated area:  wind speed recorded about
       1200 ft east of vegetable plots

19     Air temperature at 20 ft height in blocks of            46
       vegetable crops that were frost protected with
       sprinkler applied thermal and cold water and in
       non-irrigated area:  wind speed recorded about
       1200 ft east of vegetable plots

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No.                                                           Page


20     Water temperature drop through sprinkler appli-         55
       cation (May 12, 1969)

21     Water temperature drop through sprinkler appli-         55
       cation (July 15, 1969)

22     Mean monthly temperature of McKenzie River in           57
       1971

23     Temperature sensor placement                            59

24     Effect of flood irrigating with 108°F water applied     61
       at rate of about 2 gpm on soil temperature

25     Soil moisture curve at one ft depth in sweet corn       65
       field

26     Soil moisture curve at 18 in. depth in filbert          65
       orchard

27     The effect of 60° and 88°F water applied in furrows     66
       on soil temperatures 6 in. beneath furrow and
       plant row

28     The effects of 60° and 88°F water applied in            67
       furrows on soil temperatures 12 in. beneath
       furrow and plant row

29     Comparison of non-heated soil temperature profile       69
       with temperatures of soil heated with thermal
       water circulated through 2 in. diameter PVC
 •'•'     pipes, 5 ft apart, buried 24-26 in. deep

30     Delmhorst meter readings in non-irrigated check         71
       block of filberts at three depths

31     Delmhorst meter readings in thermal water irri-         72
       gated block of filberts at three depths

32     Delmhorst meter readings in cold water irrigated        73
       block of filberts at three depths

33     Seasonal  curves of radial trunk growth of filbert       74
       trees (10-12 yrs old) grown on non-irrigated
       check plots and on thermal and cold water irri-
       gated plots

34     Plant growth rate as related to air temperature         78


                                 xi

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No.                                                           Page


35      (Upper) Temperatures 1 ft above the ground in cold      81
        and thermal water irrigated, and non-irrigated
        blocks

        (Lower) Wind speed recorded adjacent to irrigated
        blocks and relative humidity in irrigated and
        control blocks on September 15, 1972

36      Comparison of temperatures 5 ft above ground in         82
        cold water, thermal water, and non-irrigated
        blocks on September 15, 1972

37      Comparison of temperatures 10 ft above ground           83
        in cold water, thermal water, and non-irrigated
        blocks on September 15, 1972

38      Comparison of temperatures 20 ft above ground in        84
        cold water, thermal water, and non-irrigated
        blocks on September 15, 1972

39      Plant cooling with thermal water in pole bean           86
        field

40      Location plan                                           90

41      Temperature of pipe as related to working pressure      92

42      Undersoil pipe grid                                     95

43      Soil temperature vs. soil  depth                         96

44      Grid layout for soil heating study                      99

45      Installation of underground pipe grid system for       100
        soil warming study

46      Soil-air interface temperature variation—100°F        101
        effluent water in PVC pipe

47      Undersoil heating with greenhouse location--plot       105
        plan and details

48      Placement of temperature sensors in relationship       106
        to buried thermal water heat lines and soil  surface

49     Mean weekly 6, 12, and 24 in. depth soil  tempera-      108
       tures of non-heated control  plots:  January  1972
       to March 1973

                                xii

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No.                                                             Page


50     Comparison of mean weekly 6 in. depth soil tempera-       109
       tures recorded at two locations in heated soil with
       non-heated soil; the heated soil was warmed by cir-
       culating thermal water through 2-1/2 in. diameter
       piastiC'pipes buried 26 in. and spaced 5 ft apart
                             e    ,c:         ,
51     Comparison of mean weekly 12 in. depth soil tempera-      111
       tures recorded at two locations in heated soil with
       non-heated soil; the,heated soil was warmed by cir-
       culating thermal water through 2-1/2 in. diameter
       plastic pipes buried 26 in. and spaced 5 ft apart
                     ;:.;:  „ .<.   ••
52     Comparison of mean weekly 24 in. depth soil tempera-      112
       tures recorded at two locations in heated soil with
       non-heated soil; the heated soil was warmed by cir-
       culating thermal water through 2-1/2 in. diameter
       plastic pipes buried 26 in. and spaced 5 ft apart

53     Comparison of thermal water temperature at inlet to       115
       soil heat grid with soil temperature (24 in. depth)
       about 2 in. above thermal water heat pipe

54     Placement of soil moisture sensors in relationship        117
       to buried thermal water heat lines and soil surface

55     Sweet corn 'Jubilee' growing on soil heated by thermal     125
       water and on non-heated soil--July 20, 1972

56     Comparison of first year asparagus fern growth of         128
       '500-W on control soil  (left) and on heated soil
       (right); pictures taken October 4, 1972

57     Muskmelon vine development on non-heated soil             140
       (foreground 1/2 of melon block) and heated soil
       (background 1/2 of block)

58     Yield of Table Queen squash on four harvest dates         145
       during 1972

59     Minimum and maximum air temperatures recorded inside      148
       and outside soil heated greenhouse during December
       1972

60     Comparison of mean weekly minimum temperatures inside     150
       and outside the greenhouse at about 5 ft above the
       ground
                                xiii

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No.                                                             Page


61     Comparison of mean weekly 12 in. depth soil  tempera-      152
       tures recorded at two locations in soil  heated
       greenhouse with non-heated soil outside  greenhouse;
       greenhouse soil was heated with thermal  water cir-
       culated through plastic pipes buried 26  in.  and
       spaced 5 ft apart

62     Comparison of mean weekly 24 in. depth soil  tempera-      153
       tures recorded at two locations in soil  heated
       greenhouse with non-heated soil outside  greenhouse;
       greenhouse soil was heated with thermal  water cir-
       culated through plastic pipes buried 26  in.  and
       spaced 5 ft apart

63     Comparison of mean weekly 6 in. depth soil  tempera-       154
       tures recorded at two locations in soil  heated green-
       house with non-heated soil outside greenhouse;
       greenhouse soil was heated with thermal  water cir-
       culated through plastic pipes buried 26  in.  and
       spaced 5 ft apart

64     Greenhouse lettuce on April 24, 1972                      157

65     Tensiometer                                               184
                                xiv

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                          LIST OF TABLES
No.                                                             Page

 1     Precipitation and thermal water applied for frost         32
       control from February 15 to Hay 31, 1970

 2     Critical depths and allowable soil moisture deple-        58
       tion for various crops

 3     Natural precipitation and supplemental  irrigation         62
       received by filberts during June, July, and August
       1972

 4     Average accumulative radial trunk growth made by          75
       10-12 year old filbert trees irrigated with thermal
       and cold water as compared to trunk growth made
       by non-irrigated trees

 5     Yield of filbert nuts from cold and thermal water         76
       irrigated blocks compared to yields from non-
       irrigated controls

 6     Plant cooling with thermal water in walnut orchard        87

 7     Nutrient levels (dry wt basis) in tomato leaves of       119
       'Fireball' and 'Willamette1 from soil  heated and
       control plots

 8     Effects of soil heat and black plastic 4-mil film        120
       mulch on yield of 'Fireball' and 'Willamette'
       tomatoes

 9     Yield of sweet corn, cv. Jubilee, harvested Sep-         122
       tember 18 through 20, 1972, from thermal water
       heated and non-heated soil

10     Nutrient levels (dry wt basis) in leaves of sweet        123
       corn from soil heated and control plots

11     Effect of soil heat on early sweet corn ear develop-     126
       ment, cv. Jubilee; samples taken August 21, 1972

12     Weight of asparagus fern and stalks produced on          129
       soil heated and non-heated plots; samples cut
       September 27, 1972
                                 xv

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No.                                                             Page

13     Number and weight of first harvested asparagus            131
       spears (April 12, 1973) from 2 year old crowns
       planted in heated and non-heated soil

14     Effect of soil heat on weight of 2 year old aspara-       132
       gus crowns--April 1973

15     Weight and number of one-year old asparagus crowns        133
       produced on heated and non-heated soil

16     Growth, plant height and spread, of rhododendrons         135
       produced on heated and non-heated soil; measure-
       ments made on July 19, 1972

17     Growth, plant height and spread, of rhododendrons         136
       produced on heated and non-heated soil; measure-
       ments made on November 14, 1972

18     Coefficient of variation for plant height and             138
       spread of six rhododendron varieties grown in non-
       heated soil and soil heated by thermal  water—
       November 14, 1972

19     Effect of soil heat on grade and yield  of cantaloupe      141
       'Harper's Hybrid'

20     Effect of soil heat on grade and yield  of cantaloupe      142
       'Supermarket'

21     Yield of 'Table Queen' squash produced  on a control        144
       and soil  heated block

22     Yield and estimated value of 'Bibb'  and 'Grand            158
       Rapids' leaf lettuce grown in the project's green-
       house on check, black plastic film,  and aluminum
       foil mulches; harvested on April 24, 1972

23     Wholesale market price per lug box of California          163
       pinks and ripe tomatoes on Portland  market during
       period of July 13 through September  21, 1972
       (field grown tomatoes)

24     Weight, number of 6x7 lugs (126 fruit/lug), and           164
       estimated wholesale value of tomatoes produced
       in soil heated greenhouse

25     Gross cash returns, less direct marketing costs, at       166
       four price levels for different volumes of production
                                xvi

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No.                                                             Page


26     Yield and estimated value of Japanese salad cucum-        170
       bers (Burpless Fx Hybrid) grown in the project's
       soil heated greenhouse and harvested from May 12
       through September 11, 1972

27     Comparison of No. 1 greenhouse cucumber fruit yields      171
       produced in Ontario, Canada, on straw bales with
       cucumber yield produced in project's greenhouse

28     Microbiological results of aerobic plate count,           177
       coliforms, E. coli, and staphylococcus counts
       made on selected vegetables grown under different
       irrigation and/or soil heating conditions

29     Mold counts obtained on Sabouraud's medium from           178
       selected vegetables grown under different irriga-
       tion and/or soil heat conditions

30     Protein and moisture assays of vegetables grown           179
       under different irrigation and/or soil heat con-
       ditions

31     Precipitation and irrigation, both thermal and            185
       cold water, applied (inches) to plots during June,
       July, and August

32     Nutrient levels (dry wt basis) of selected vegetable      189
       crops from soil heated and control blocks (samples
       taken August 16 and 17, 1972)

33     Effect of soil heat on yield of 'Thaxter' lima beans      190

34     Effect of heated soil on yield of table beet, cv.         191
       Detroit Dark Red

35     Influence of heated soil and thermal irrigation on        192
       yield of snap beans, cv. Bush Blue Lake 274, on two
       harvest dates

36     Effect of soil heat on yield and grade of tomato          193
       cvs. H.I350, C. 1327, and New Yorker

37     Effect of soil heat on yield and grade of pickling        194
       cucumber, cv. Pioneer Hybrid

38     Effect of soil heat on grade and yield of onions,         195
       cv. Danvers Yellow Globe

39     Effect of soil heat on yield  'Golden Acre1 cabbage        196


                                xvii

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                        ACKNOWLEDGMENTS
Vitro Engineering gratefully acknowledges the contributions
of the Project farmers,* the Environmental Protection Agency,
the Eugene Water & Electric Board, Weyerhaeuser Company, and
Oregon State University.
* Listed in order of Project farm sites:

           Lester A. Patrick                   Farm 1
           James B. O'Brien                    Farm 2
           Rex Heide                           Farm 3
           W. William Puustinen                Farm 4
           William L. Cole                     Farm 5
           Dale Bartholomew                    Farms 5 & 6
           Robert W. Bennett                   Farm 7
           Virgil Nave (Present Owner)         Farm 7
                              xix

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                           CONSULTANTS
Alexander M. Dollar, Ph.D.
Department of Agriculture
State of Hawaii
George M. Pigott, Ph.D.
G. Burton Wood, Ph.D.
Larry S. Slotta, Ph.D.
Associate Professor
Department of Food Science
University of Washington

Associate Dean and Director
Agricultural Experiment Station
Oregon State University

Associate Professor of Civil
Engineering
Oregon State University
                               xxi

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                              CONCLUSIONS
GENERAL
Today we are experiencing a rapidly expanding population; agriculture
and  the development of energy resources are being forced to keep pace.
Wise utilization of water will be a key factor in this expansion.  It is
clear that multi-use of this resource will be a necessity.

Agriculture's  reuse of warm industrial water holds much promise in the
scheme of expansion since it will transform what appeared to be an envi-
ronmental threat into a beneficial influence.  This project has demon-
strated several of the agricultural benefits to be derived from the heat
content of thermal effluents and has found no detrimental effects.  Water,
after having been used for irrigating the Springfield project, has been
returned to the McKenzie minus the industrial heat; this in itself is
highly significant when one considers the enormously expensive cooling
procedures currently being employed by the electric power industry—pro-
cedures that totally waste the heat.

The  cooling-lake method of cooling  thermal  effluents is likely
to emerge as thermal-water agriculture comes to the fore.  The multi-use
possibilities  for the water in such a lake are exciting.  Surrounding
municipalities, agriculture, industry, power producers, and public re-
creation could all mutually benefit from such a body of water.

Specific methods have been demonstrated for using warmed condenser cool-
ing water for agricultural purposes.  For some applications, i.e., irri-
gation and plant cooling, such water does not offer significant benefits
which can be attributed to its elevated temperature alone; conversely,
no damage need be incurred.  For frost protection, warm water appears to
offer advantages over water at normal  temperatures.
                                 xxm

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Warm water use for underground soil heating, in open fields and under
greenhouses, shows significant potential for profitable use with selected
crops which demonstrated increased yields.
FROST PROTECTION
Significant accomplishments were achieved on this project in demonstrating
warm water use for frost protection.

The result of warm water frost protection was a reduction in frost damage
and crop loss, particularly for orchard crops under warm-water application.
For example, no fruit buds in thermal-water-protected orchards were damaged
by spring freezes.  A full crop of peaches was produced in the project
orchards.  Unprotected orchards in the surrounding countryside produced
no crop to a very light crop of peaches.

It can be concluded that thermal-water spray for frost protection has
several advantages over cold-water spray because less water is required
when the water is warm.  It was observed that there was no temperature
depression when sprinklers using thermal water were turned on for frost
protection.  Since no depression was noted, sprinklers could be activated
very close to critical bud temperatures.  Thus, much less water was applied
than if sprinklers had been activated every time the temperature fell to
33°F as suggested in the literature for cold water.  Temperature profiles
indicated that thermal water apparently compensates for the evaporative
cooling effects as the water leaves the sprinkler, so no initial tempera-
ture depression occurs.  Less limb breakage, lower water costs, and reduced
nutrient leaching from the soil are among the benefits to be derived from
this reduction in water volume.

An important factor in frost protection is the availability of precise
data on specific bud development stages and critical bud temperatures.
During the project's final frost-protection season, published data for
farmers became available through the Washington State University

                                 xx iv

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Agricultural Extension circulars that pinpoint these stages and related
temperatures.  This information also reduced the amount of water applied
to the crops and reduced the amount of spraying and dusting required for
insect and disease control.

Both above- and under-tree sprinkling was evaluated; it became evident
through project demonstrations that under-tree sprinkling with warm or
cold water is not satisfactory for frost protection.
UNDERSOIL HEATING
The results of the underground soil heating and greenhouse demonstrations
are considered among the most significant revelations of this project in
terms of potential applications for waste heat.

The effect of the warm water grid on soil temperature was most noticeable
directly above individual heating pipes; the effect also increased with
depth and varied throughout the seasons of the year.  At the 1-in. depth,
temperatures were not affected much during summer; for the rest of the
year, the increase was from 0.5 to 4°F.  At the 6 in. depth, maximum
temperature increases averaged 4.8°F based on measurements from January
1972 through March 1973.  For the same time span, increases at the 12 in.
and 24 in. depths were 7.8°F and 8.4°F, respectively.

Soil temperature increases on the heating grid portion covered with the
plastic greenhouse were higher than on the uncovered heat grid described
above.  The maximum temperature increase in the greenhouse at the 6 in.
depth averaged 9.5°F above control.  At the 12 in. level, the average
increase was 11.2°F.  At the 24 in. level, temperature increases averaged
20.7°F.

Air temperature was also sign-ificantly increased in the greenhouse due
to the soil  warming.  Greenhouse minimum temperatures averaged 8.2°F
higher than ambient minimums.  These temperatures indicated the effect
                                  xxv

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of the added heat since natural greenhouse solar heating would not in-
fluence night-time minimums to a great extent.
                     -                                    • ' v
Effects of soil heating on crop production were assessed for a number of
plants including tomatoes, sweet corn, asparagus, rhododendrons, canta-
                                                          - -,,'
loupes, and squash.  Not all crop production was affected significantly,
although differences were almost always noted in various growth stages.
                                                                         ;-

The demonstrations with various crops indicated that the closer the roots
are to the soil heat grid, the greater the effect on growth.  In illus-
tration, the roots of one-year-old asparagus crowns are relatively shallow;
crown production was not influenced by the soil heat grid to this age.
In contrast, two-year-old asparagus crowns, with more developed root sys-
tems, produced about 50 percent more fern growth on heated soil.  The
                                     ' •..  i     .    i    '           '  •
production of early spring asparagus spears was also stimulated by soil
heat; yields increased by 44 and 95 percent in terms of number and weight
of spears, respectively.

Accelerated root development of rhododendrons was noted on heated soil.
This nursery stock was ready for market approximately one year sooner
in some cases.  Quantitative data were not gathered on this accelerated
root development, but the quantitative results indicate that significant
benefits may be derived 1  Further' demonstrations are needed with orna-
mentals and tree crops.

Greenhouse crop production was also assessed for leaf lettuce, tomatoes,
and cucumbers.  Results are presented in terms of absolute production
potential from the soil-heated greenhouse rather than in comparative
terms involving control plots.

Production results and estimated cash values were also determined for
lettuce and cucumbers.  Of the greenhouse crops cultivated, Japanese
salad cucumbers exhibited the greatest potential for profitable growth.
The minimum wholesale value of this variety of cucumber, based on the
                                 xxvi

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project's greenhouse production and current wholesale prices, would ap-
proach $100,000 per acre.

Optimum soil temperatures for most crops are not known.  Lack of response
to soil heating may not necessarily indicate that soil heat is not bene-
ficial for a particular crop.  The thermal-water grid did not appear to
improve the yield of 'Fireball1 and 'Willamette1 tomatoes.  It is likely
that location of the test plantings and the growing season affected the
results.

The undersoil-heated greenhouse has demonstrated a good return on invest-
ment utilizing selective cropping and a 12-month period.
HEAT EXCHANGE WITH AIR, SOIL, AND PLANTS
At night during the growing season, the project's ambient air temperature
often dropped below the optimum level for plant growth.  Thermal  water
was applied during these cooler nights to determine if the air temperature
could be raised to a more beneficial level.  It was determined that no
measurable rise in air temperature occurred.

Selected measurements were made at various levels up to 40 ft to better
define local meteorological effects of water applications, and its effects
on microclimatology.

In May and July of 1969, it was demonstrated on the project that thermal
water cooled approximately 2°F per foot distance it traveled from the
sprinkler nozzle during periods of low relative humidity.  This was in
line with the findings of C. H. Pair that, during periods of high ambient
air temperatures, water in excess of 100°F at the sprinkler nozzle may
be below ambient air temperature by the time it reaches the plants.

Thermal  water can serve as a plant cooling agent in two respects:  1) it
is cooler than ambient air temperature in contact with the plants; and
                                 xxvn

-------
2) it increases the wetted surface area increasing evaporative cooling in
the plant environment.

Plant cooling was applied when plant temperatures exceeded 86°F, which is
near the temperature at which plant growth decreases and where plant in-
jury may occur through excessive transpiration.   During periods when plant
cooling was demonstrated, temperature decreases  from 4 to 6°F and rela-
tive humidity increases up to 20 percent were recorded in sprinkled areas.

The rate and amount of heat penetration in the soil were closely related
to the volume and temperature of the applied water.  Temperature altera-
tions caused by irrigation water take place slowly at depths of 12 in. or
more.  Soil temperatures at the surface, however, were rapidly modified.

Although no plant damage was noted on project soy beans and tomatoes
irrigated with 108°F, some varieties may be more sensitive to surface
thermal-water application.
IRRIGATION
The experiments with sprinkler and furrow irrigation showed that warm
water may be used for this purpose without adverse effects, if properly
managed.  Soil temperatures were raised by warm water applied in furrows;
the rate and amount of heat penetration was closely related to volume and
temperature of water applied.  Under normal applications,  the soil  heating
effect is rather short-lived.  No significant benefit to plants could be
associated with the presence of waste heat in irrigation water, except
that plant life did not enter a cold thermal  shock.
FUNGI, MOLDS, AND BACTERIA
No increase in fungi, mold, and bacterial  infestation  was  noted on the
project in any of the crops irrigated with thermal  water.
                                xxviii

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ECONOMICS

The project, after five years of operation, has completely demonstrated
the feasibility of thermal water's use for frost control, irrigation,
plant cooling, and undersoil heating.

Total cost for installation of the pumping system, buried main line,
laterals, and above-ground solid-set system, including high risers for
the 70 acres of orchard for frost control and 100 acres for row crop
plant cooling, was $220,000; this figure includes many costs that would
not be associated with a normal agricultural system not used for demon-
stration.  An estimate obtained from Western Irrigation Manufacturing,
Inc., Eugene, Oregon, indicates that a multi-use system would cost $675
per acre with an on-site source of water.  On 170 acres, the total ini-
tial cost would be $114,750.  Using a capital recovery factor of 0.1359*
and an estimated life of ten years, the annual  fixed cost of the facili-
ties (excluding taxes and insurance) would be $15,594.33.  This amounts
to an annual cost of $82.81 per acre for a solid-set, multi-use system.

A first approximation of the cost of frost protection and irrigation by
other methods must be compared to the costs of a multi-use system.  Since
a system purchased for irrigation (but not frost control) is usually
moved from setting to setting, plant cooling would not be feasible-  A
hand-move system would cost approximately $150+ per acre, or $25,500
for a 170-acre horticultural plot.

Of the commercially applied orchard heating systems for frost protection,
the central distribution system is rapidly gaining popularity because of
* Based upon 10-year amortization at 6 percent interest
+ Estimate obtained from Western Irrigation and Manufacturing, Inc,
                                xxix

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its effectiveness and nonpolluting characteristics.  A price of $525 per
                                                          '- -'.
acre covers the equipment and installation costs of a typical central
distribution system.*  Operation costs are frequently as high as $7 per
hour per acre.*  In addition to the fuel costs, these systems have an
increased labor cost (see Appendix A, Table A-l, page 204).

Solid-fuel systems such as "brick" and wax heaters have very low instal-
lation cost but high operation costs because of the nature of the fuel.
A figure of $50 to $75 per acre per night of protection is not uncommon.*

An approximation of the total annual fixed cost for the above-mentioned
three types of systems is given in Table A-l.  The multi-use thermal water
system has slightly greater annual fixed costs but can also be used for
plant cooling and irrigation.  Because of the initial  outlay for equipment,
the solid fuel plus irrigation system approach has a nominal annual fixed
cost per acre.

An approximation of annual operational costs per acre are shown on
Table A-2 (page 205).

Although the solid-set multi-use system may have a higher annual  fixed
cost, the annual operational costs are considerably less, equaling
approximately l/25th the costs of the other systems.

Combining the annual fixed and operational  costs (Tables A-l and  A-2) of
the various systems, the total annual cost is approximated (Table A-3,
page 206).  While figures are based on best estimates  and realistic
assumptions, they would vary somewhat from area to area since each area
has its own unique characteristics and problems.  Nevertheless, the cost
* Figures derived from literature by Spot Heaters, Inc.
+ Based upon 40 heaters per acre burning 1 gal  per hr of No. 2 diesel
  fuel at 17-l/2£ per gal.
* Based on advertisement and articles in February 1968 and February 1971
  AMERICAN FRUIT GROWER, Western Edition.
                                 xxx

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comparisons are accurate.  The multi-use thermal water system would be
approximately 33-1/3 percent as expensive as other various systems com-
bined to provide frost protection and irrigation.  In addition, the
multi-use system is the only one capable of providing plant cooling.

Although the cost estimates of the multi-use system have been based on
the actual installed costs of the pump and the closed-pressure under-
ground piping conduit, the possibility of financial or technical assis-
tance from industry in utilizing this method to overcome their potential
thermal water pollution problems has now been established during this
five-year program.

Based on research development work performed by L. L. Boersma at Oregon
State University, utilizing electrical heating cables to induce heat
into soil, a PVC 2-1/2 in. pipe grid was designed and installed to further
demonstrate that thermal water from an industrial plant could be used to
allow twelve months of horticultural cropping.

The total installed cost of the undersoil heating system was $14,550 and
covered an area of 83,000 sq ft.  Included in the installation cost was
special instrumentation inserts and valves.
                             i

A normal field installation of undersoil piping, using PVC pipe, 2-1/2 in.
diameter, buried 26 in. with 60-in. center spacing, would cost $7,000 per
acre. .Using a capital recovery factor of 0.1359 and an estimated life
span of ten years, the annual fixed cost of the system (excluding taxes
and insurance) is $111.30 for one acre.

In the Willamette Valley, the climate is relatively mild and year-around
cropping is possible when a greenhouse is placed over the soil heated area.

The cost of constructing a plastic greenhouse depends on the length of
service a grower desires from the structure.  Using pressure-treated
structural-grade lumber and plastic film (UV Poly), a rigid frame green-
house would cost $1.129 per sq ft.

                                 xxxi

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Based on the above costs shown In Table A-5 (page 208), the total cost
for a one-acre greenhouse would be $49,179.24.  Thus, the total cost for
undersoil heating and greenhouse would be $56,179.24.  Using a capital
recovery factor of 0.1359 and a life span of ten years, the annual fixed
cost of the one-acre installation (excluding taxes and insurance) is
$7,633.75.

Using actual crop harvest results from the greenhouse/undersoil heat
installation and selected varieties of produce,  the gross returns for a
one-acre installation (starting with lettuce transplants on March 8, 1972,
and ending with final harvest of Japanese salad  cucumbers and tomatoes on
September 12, 1972) are as shown in Table A-6, page 209; see Section VI
for more detai1,

Although for test purposes both Japanese salad cucumbers and tomatoes
were raised simultaneously, it must be recognized that, for calculation
of minimum and maximum returns per acre, both crops encompass the same
growing period.  Therefore, one of the crops, tomatoes, has been elimi-
nated from the calculation of gross returns.

It follows that the gross return per year, with  selective cropping,  could
be at a minimum of $161,837 and a maximum of $288,809  for a nine-month
operation (see Table A-7, page 210).
                               xxxi i

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                            RECOMMENDATIONS

It is recommended that Industry and agriculture apply the findings of
this project to help eliminate thermal pollution of our waterways while
benefiting agriculture.

The demonstration project has yielded much useful data relevant to the
economic analysis of thermal water application in agriculture.  Exten-
sive analysis is now possible through comparisons of thermal water farm-
ing capital costs, operating costs, and farm yields with those of non-
thermal farming.  Project data should now be applied within comprehensive
analysis formulas and computer models.

A fruitful area of investigation will be the cost comparisons of heat
dissipation partially or wholly through agricultural applications versus
                                                          • i
those associated with dissipating heat totally by conventional cooling
devices.  Thermal power plant siting will also affect these costs.

Examination of the costs, benefits, and environmental influences of ther-
mal and geothermal power sources as related to agriculture, fisheries,
and recreation should be an extension of this study.

Experience on this project suggests that there is significant potential
for undersoil heating in the production of a wide, range of high-value
ornamentals and flowers.  Root development responds favorably to soil
heat for many woody plants such as rhododendrons.  This effect should be
evaluated for various crops of this type to quantify growth enhancement
leading to quicker marketing.

Maximum beneficial temperatures of water need to be established for each
crop grown under thermal water; the ideal soil moisture levels for under-
soil heat transfer also need to be determined.

                                xxxiii

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Undersoil heating demonstration with young trees destined for reforesta-
tion programs is also an area of promise since transplant mortality might
be reduced by better root development.   A study should be conducted by
a college of forestry or appropriate commercial  organization to determine
the effects of warm water soil  heating  on the growth of young deciduous
and conifer trees.

Systems for using and controlling waste heat  should be refined to enable
design capability for meeting specific  requirements at minimum costs.
Monitoring systems should also be refined for cost minimization.
                                xxxi v

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         •

-
•
•
                         Frontispiece:  The Thermal Water Project on the McKenzie River

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                               SECTION I
                             INTRODUCTION
BACKGROUND
Many estimates have been made concerning United States electrical power
demands from the present to the year 2000.  A 5-percent annual growth
rate has been suggested, which would mean that energy availability must
double every 14 years.  Many utilities are predicting that energy
availability must double every 10 years.

We are even now seeing a proliferation of new generating facilities
across the land and rising concern over the affect they will have on
the environment.  In the nuclear power sector alone, there were 29
nuclear plants operating, 55 being built, and 76 on order at the end
of 1972.

The Environmental Protection Agency estimates that the U.S. will require
approximately 200 billion gallons of fresh water daily to cool the
condensers of the plants required to produce the two thousand billion
kilowatt hours needed by 1980.  Such water will be essentially free of
contaminants, but it will be discharged at 90 to 120°F.  Direct release
to fresh water or marine environment might cause biological pollution
because of the heat content.  Thus, these industrial waters must be
cooled before they are released, and such cooling will be a task of
major proportions because of the prodigious quantities involved (500,000
gallons a minute, or more, from one 1000 megawatt nuclear plant).

Current effluent water cooling for most plants in the 1000 MWe range
is through the use of cooling towers where effluent heat from the water
is dispersed to the atmosphere.

-------
This  cooling  procedure is extremely expensive (a tower initially costs
approximately $10 million and has a high annual  operating cost) and,
significantly, the heat is wasted.  At the time of this project's in-
ception, the  Eugene Water & Electric Board felt that possibly systems
could be developed whereby heated industrial effluents would serve agri-
culture as they were being cooled, thus turning a liability into an
asset.

New power from hydro-electric dams is no longer available in the North-
west.  Soon the Columbia River will be navigable slack water from the
Pacific Ocean almost to the Canadian border.

Many  spokesmen for agriculture, government, and educational institutions
now envision  plans whereby the joint development of thermal power with
irrigation could eventually bring water to many thousands of dryland
acres  in the  Northwest.  The effluent from one 1000 MWe nuclear reactor
could under optimum conditions be used to irrigate 100,000 acres with
four  acre-feet of water.

Between 1965  and 2010, agriculture in the Pacific Northwest is expected
to increase from 6-1/2 million to 17 million acres if water is. made
available.  The population will increase from 5 million to 14 million.
Irrigated acreage expansion in the 1970's is predicted at 175,000 acres
per year.*

Mutual development of power and irrigation could substantially increase
agricultural  output while lowering power costs.   One facet of such a
multi-use approach would be the sale of necessary power to agriculture
for pumping.  The irrigation of 100,000 acres would require some addi-
tional 35,000 hp of connected load to power pumps on the irrigated
farms.
* Bonneville Power Administration Power Distributors, 1966 Report.

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EARLY EVOLUTION OF THE PROJECT
     'V ,.!'•.
The five-year thermal water project was originally tied to the premise
that a nuclear power generating plant would be erected at the south end
of the Willamette Valley.  The plant, utilizing the latest pressurized
boiling water reactor concepts, was to have a capacity of between 1100
and 1250 megawatts, and its condenser cooling water requirements were to
range between 500,000 and 850,000 gallons of water per minute.  The cool-
ing water temperature increase after passing over the condenser was to
be from 17 to 33°F.

The Board of Directors of EWEB directed the manager and his staff to
form an internal planning and coordination group which was to assess the
various impacts of the plant--such as, regional growth and development,
economic influences, agriculture and industrial growth, urban development,
recreation, and environmental influence.                      ••••>•

   '-•:            ' .                    f    '-,-'•,
In its early review of impact, EWEB coordinated its efforts with Lane
County, the State of Oregon, the Pacific Northwest electrical industry,
the Edison Electrical Institute, Public Power Association, and the federal
agencies involved in producing and transmitting electric power (i.e.,
Bonneville Power Administration, Bureau of Reclamation, Corps of Engineers,
and the Soils Conservation Service of the U.S. Department of Agriculture*).

As part of its overall environmental review, EWEB was considering some
of the multi-use potentials of the future plant's thermal-water effluent;
thermal-water irrigation was one such use.
                                  I;                .
Dovetailing at that time (1967) with EWEB's efforts to assess environ-
mental influences of a power station was a proposal by seven farmers
near Weyerhaeuser's Springfield mill.  The farmers offered the use of
* The USDA is responsible for administrating the Small Water Sheds Act,
  which has jurisdiction over irrigation and water management of the
  Willamette River Basin.

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their land with its orchards and row crops as a demonstration area if
EWEB would establish and maintain an irrigation system which would trans-
port industrial thermal water from Weyerhaeuser to their properties.
Weyerhaeuser water, at that time, was being .discharged directly into the
McKenzie River.  This water approximated the temperature of cooling water
flowing from power stations.  After this reuse, the cooled water would
be returned to the McKenzie River in a manner and at a temperature satis-
factory to both environmental interests and sport fisheries associations.

Along with the gathering of data on thermal water use and its effects on
the environment, the project was to demonstrate the ability of industry,
farmer, engineer, and federal and state agencies to work in close coop-
eration to bring this new complex idea to a successful conclusion.

EWEB's management selected Vitro Engineering to perform a feasibility
study on the possibilities of utilizing water from a thermal plant that
would meet the necessary requirements of all participants.  Included in
the feasibility study was the outlining of Vitro's capability to establish
a program which would accommodate the climatological factors of the South
Willamette Valley and to establish advantageous agricultural schemes to
demonstrate the multiuse concept for eventual betterment of the 110,000
acres in the upper Willamette.  After several months of study, Vitro re-
ported that the project was not only feasible but practical.  Early in
1969, project construction commenced.  Four months later, thermal  water
was being applied within the demonstration acreage.

Limited irrigation with waste water had been tried in Oregon as far back
as the late thirties when several towns tried using waste from primary
sewage-treatment plants to water crops and pastures.  Public reaction
soon limited those efforts to pasture land, but the idea slowly built as
industry picked it up to solve waste-discharge problems.

In 1957, water from Weyerhaeuser's Springfield mill was sprayed on pasture
land.   This waste water was hot and it carried considerable organic materials
and, in general, was not desirable for direct discharge to the McKenzie

-------
River.  This irrigation served to cool the wastes and deposit the organic
material on the ground, where it was consumed by soil bacteria; the water,
in a cleansed condition, filtered back through the soil into the river.
Arthur King, a conservation specialist at Oregon State University, was
closely involved with this application of Weyerhaeuser water.
EARLY SITING PLANS
Based on "Oregon's Long-Range Requirements for Water" that was prepared
by the Oregon's Water Resources Board, it was estimated that the diver-
sion requirements in the year 2070 would be 4.3 acre-feet per acre for
all areas found to be suitable for development and that the irrigation
requirements would be 2.1 acre-feet per acre to support agriculture within
the Willamette and Sandy subbasins.  The gross water requirements would
be 4,073,000 acre feet.  The return flow would be 543,000 acre-feet per
year.

The consumptive use for irrigation was estimated to be 3,530,000 acre-
feet per year, which includes evaporation losses from storage reservoirs
and from the delivery systems.

In planning the location of a thermal nuclear power generating plant,
EWEB proposed to establish a 2500 surface acre cooling reservoir which,
during a normal growing season (mid-February through October), would
supply condenser cooling water to approximately 150,000 agricultural acres
(see Figure la).  Water would be delivered to the downstream base of Fern
Ridge reservoir and then divided between two major canals—one following
the contour of the east side of the valley and ending at Albany, and one
following the west side of the valley and terminating at Corvallis.

Two sites for power plant location were being considered—one at the con-
fluence of the Willamette and McKenzie Rivers and the other at Poodle
Creek, which flows into the Long Tom River, a tributary of the Willamette
(see Appendix E for the technical  rationale for early conceptual studies).

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                                I ARCS.
                                  WILLAMETTE BASIN

                                             LAND  AND

                               BASIN  DEVELQPMEMT-2G7Q
                                          Me. Jefferson
                                           JEFFERSON
                                         THERMAL POWER

                                         PULP AND PAPER

                                         FOOD PROCESSING

                                         HEAVY INDUSTRY
                                          Pollutants


                                          No Pollutants
                                         MAJOR URBAN AREA
                                          Included In Portland
                                         MINOR URBAN ^
                                         OTHtR MINORS  "•'  "
                                            -••• :   COMMUNPfY
Figure la. Willamette basin map

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OBJECTIVES
This project's tie with the generation of nuclear power in the Upper
Willamette afforded an exciting opportunity to materially assist in
building an effective regional water management program.  Along with the
gathering of data, the Project was organized to demonstrate the ability
of industry, farmers, engineers, Federal and State agencies, and edu-
cational institutions to work in close harmony in a new, complex agri-
cultural undertaking for the benefit of all.

The original focus of this project was the isolation of any harmful
aspects related to thermal water application in agriculture.  In addition,
it was proposed to demonstrate how heat energy in water could be dissi-
pated while moderating, to the benefit of agriculture, an area's naturally
occurring Conditions of temperature and humidity.  These benefit areas
were to be explored:

   • = Increased yield and quality of crops through control of soil
      temperature and moisture content.
   •  Prevention of frost damage through heat dissipation from warm
      water application during frost conditions.
   •  Prevention of sunburn on soft fruits through control of humidity
      and atmospheric temperature.
   •  Lengthening of growing season for row crops and the possibility
      of double cropping.
   •  Introduction of new crops.
   £
   •  Prevention of cold water shock.
   •  Fuller fruit and nutmeats through humidity control.
   •  The effect of thermal water irrigation on soil leaching and the
      run off of herbicides, fertilizers, and pesticides.

An undersoil-heating pipe network was installed on the project in early
May of 1971 to demonstrate this mode of thermal water heat dissipation
in agriculture.  This facet of the project was correlated with the

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undersoil electric cable experiments of Dr. L. L. Boersma at Oregon
State University.  A 22 ft x 55 ft double-walled plastic greenhouse was
erected over a portion of the soil heated area in 1971 to increase the
output of data from the soil-heat demonstration.

As the project moved into its final period, emphasis was placed on gather-
ing data that would be useful in quantifying the costs and benefits of
thermal water agriculture and in assessing its associated role with con-
ventional heat disposal techniques (i.e., cooling towers and ponds).
THE PROJECT'S ORGANIZATION

The project was to evolve into a cooperative venture.  Overseeing the
project were:  the co-sponsors (EWEB and the Environmental Protection
Agency) and the project manager (Vitro Engineering).  Weyerhaeuser Com-
pany provided the thermal water source (water from the cooling condensers
of the electrical generating plant for their Springfield mill).  The
demonstration took place on 170 acres under cultivation along the McKen-
zie River near .Springfield; the seven farmers who owned this land agreed
to use thermal water from the nearby (2 miles) Weyerhaeuser mill for
irrigation, frost protection, and plant cooling.
THE IRRIGATION SYSTEM

The heated water from the Weyerhaeuser mill is discharged into the pro-
ject's pumping pit (Figure 1).  Water temperature at the pumping pit
ranges from about 90 to 120°F.  Two 1750-gpm and one 500-gpm pumps were
used to deliver water to the project at about 80 to 90 psi.  Water was
pumped about 2 miles through a 16 in. diameter steel mainline (buried
30 in.) to the edge of the project's farms.  Laterals fed individual
farms.  The mainline continued across the project's farms and was gradu-
ally reduced in size to 8 in. diameter.

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Figure 1:   Weyerhaeuser Pumping  Pit

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At t'he end of the mainline, thermal water was sprayed into the air so
that warm water was continuously moving through the system and immediately
available at all project locations (Figure 2),  The water that was sprayed
into the air was cooled by evaporation to nearly ambient temperature and
collected in a pool around the spray exhaust.  The spray exhaust and pool
were about 50 ft away and 10 ft above the summer level of the McKenzie
River.
IRRIGATION SCHEDULING
Gypsum blocks  (Delmhorst type) and tensiometers were installed throughout
the project for monitoring soil moisture.  The root depth zone was deter-
mined for each crop, as were percent allowable moisture depletion levels for
each of the farm crops at various depths.  These values were used as guides
in determining when to irrigate.  Each farm crop was considered separately,
as much as possible, when irrigations were scheduled.
MONITORING EQUIPMENT

Wind  Recording  Systems
 (1)   1-Weather  Measure-Wl01-Remote Recording Skyvane I
      Specifications:

      Starting speed                  Approximately 1 mph
      Range of measurements                         0-65 mph
      Accuracy                        + 1 mph below 25 mph
                                     t 5% above 25 mph
      Sensor  location                 40 ft above ground

(2)   1-Weather  Measure W123-Recording Wind System
      Specifications:
                                  10

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                                                                   -.,
                 Figure 2:  Thermal Water System Exhaust


-------
     flange of measurements
     Sensor location
QklOO raph
12 ft above ground
Pressure Recording Systems
(3)  1-WM B211-Microbarograph
     Specifications:
     Sensor
     Scales
     Accuracy
     Operating range
14 cell, 2 1/2 in. dia. aneroid
27.9 to 31.0 in. of mercury
± 0.005 in. of mercury
Sea level to 12,000 ft
Humidity and Temperature Recording Systems
(4)  5-WM H311 Hygrothermograph
     Specifications:
     Temperature
       Range
       Accuracy
     Humidity
       Range
       Sensor
       Accuracy
       Sensitivity
110°F, adjustable
± 1%

0-100%
Human hair bundle
+ 1% between 20 and 80%
Less than "\%
(5)  1 WM H361-6 Remote Dew-Point and Temperature System
     Dew-point
       Sensing element
       Range
       Accuracy
       Cavity temperature sensor
Lithium Chloride bobbin
-40° to 120°F
t 2°F
Platinum resistance bulb
                                 12

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      Recorder
        Accuracy                             +0.5% of span
        Sensitivity                          0,1% of span
        Ambient temperature limits           0°  to 120°F

      Total  of 6 channels--!  for dew-point and 5 for ambient  temperature

 (6)  3 HM1  Sling Psychrometer
      Thermometer range                      -20 to +120°F

 (7)  T 641  Temperature Indicator/Alarm
      Specifications:
      Temperature range                      10°F to 60°F and 60°F  to  120°F;
                                             dual  range
      Alarm setpoint range                   25°F to 35°F
      Temperature resolution                 1°F
      Temperature probe                      Precision thermistors  in  stainless
                                             steel case

 (8)  1 WM T601 Remote Recording Thermograph
      Specifications:
      Calibration                            -10 to 110°F
      Accuracy                               ±0.2°C
      Sensors                                Mercury in  plastic-covered capillaries

 (9)  1 WM T601 Remote Recording Thermograph
      Specifications:
      Same as above except supplied with 1 probe

(10)  1 WM T611 Thermograph
      Specifications:
                                  13

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      Sensing element
      Accuracy
      Range

(11)  1  WM T622R-6 Temperature Recorder
      Specifications:
      Accuracy
      Sensitivity
      Sensors
      Temperature range

(12)  2 WM T622R-12 Temperature Recorder
      Specifications:
      Same as above except 12 points

(13)  TM-1 Exposed Mercurial  Thermometers
      Range

(14)  TM-2 Minimum-Maximum Thermometers
      Minimum range
      Maximum range

(15)  TM-2-LR Extra Minimum Thermometer
Aged bimetallic strip
±1%        ^,.
110°F, adjustable  „
+0.5% of full span
0.1% of full span
Platinum bulb 100 ohm
0 to 120°F
-38 to +130°F
-50 to +120°F
-38 to +130°F
Evaporation Systems
(16)  1  WM E-801 Recording Evaporimeter
      Specifications:
      Calibration
      Accuracy
      Sensor
0-10 min.
+1%
Wetted filter paper 8.29  cm2
                                   14

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Solar Radiation Recording Systems
(17)  1 WM-R401-Mechanical Pyranograph
      Specifications:
      Sensing Element
      Calibration
      Full scale
      Spectrum sensed
 (18)   PRT-10 Barnes Engineering Co.
       Infrared Thermometer

 (19)   PMS  Instrument Co.  Pressure Bomb

 (20)   Delta Temperature Unit

 Precipitation System

 (21)   1  P569 General Purpose  Rain Gauge
       (Forester  Type)
Black bimetallic strips
gm-cal/cm^/min
Approximately 2.5 gm-cal/cm2/min
90% transmission, 0.36 to 2.0
micron wave lengths
                                    15

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                             SECTION  II
                     THERMAL WATER CONDITIONS

THERMAL WATER TEMPERATURE
Temperature of  thermal water from the Weyerhaeuser plant is first
recorded  at the project's  pumping pit adjacent to the plant (Figure 1).
Water  temperature  is next  recorded at the inlet of the soil heat grid
on the Bartholomew farm  after  the water has traveled about 2.7 miles
through mainlines  buried 30  in. beneath the soil surface.

Water  temperature  is recorded  at the exit from the soil heat grid.
The soil  heat grid consists  of twenty-five 2-1/2 in. diameter plastic
pipes, each 470 ft long, connected to 8 in. diameter steel inlet and
outlet manifolds.   The grid  is buried about 26 in. and is described
in another section.
                         i
After  the thermal  water  exits  from the soil heat grid, it enters the
mainline  again  and ultimately  is exhausted into the air through a spray
bleed  valve (Figure 2).  The water temporarily collects in a pool around
the valve before filtering through several feet of gravel and soil into
the McKenzie River.  Water temperatures are recorded in the pool sur-
rounding  the spray exhaust (Figure 3).

Temperatures of heated soil  in the open field and in the project green-
house are partially dependent  upon thermal water temperature.  A summary
of thermal water temperatures  for 1972 and part of 1973 is shown in
Figure 3.  Relevant ambient  air temperatures are shown in Figure 4.

McKenzie River  water temperature tended to increase during mid-summer
and decrease during the cooler months.  This was also true of thermal
water temperature.  /
                                 17

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  130.
   30
         A
         •
         o
        >
Pumping-Pit
In'et
Outlet
Enhaust Pool
                                                                                                                                                              flow of thermal  water interrupted
                                                   1972
                                                                                                                       197E
                                                                                                                                                                           1973
Figure 3.  Meekly ne«n twioerjture of themal water as  It  leaves cooling condenser of Weyerhaeuser's electrical generating plant (Pumping Pit),.enters the soil  heat orld  (Inlet)  about 2.7 miles
           from pump,    exits from soil heat grid (Outlet), as It collects  In pool  surrounding spray exhaust (Exhaust Pool)  before It filters through gravel back to the river and anbltnt river
           temperature (River).

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     70-
      50-
      10
           • 1972-1973 mean daily teoperjture
           -. Long term average for Eugene 1931-1965
                                                                                               I—i—r-i   i   i—i—i—i  i—i—i—i—i—i—i—i—i—i—i—i—|—i—i—i
                                                                                                                                                                                           Mar
Figure 4.   Mean dally ambient air temperatures  averaged oj weeks from January 1972 to March 1973  and  long  torn weekly mean temperatures 1931-1965.

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The pumping pit temperature recorder had to be removed for repairs during
August 1972 and was not put back into operation until October.

During the first 4-1/2 months of 1972, there were greater temperature
differences between exhaust pool and river than desirable.  About mid-
Hay, a new spray exhaust system that broke up the water into finer par-
ticles and promoted more evaporative cooling was installed.  During June,
July, and August, river water was slightly cooler than exhaust pool, but
during the remainder of the year exhaust pool  temperatures were slightly
cooler than the river.  One reason that exhaust pool  temperatures showed
up warmer than river is that the pool was shallow and the temperature
sensor in the pool was found not to be fully shielded from the direct rays
of the sun during part of the day.  Thus, the average daily pool  tempera-
tures recorded were probably somewhat higher than the actual  exhaust pool
temperature.

Temperatures at the pumping pit ranged from a weekly  average  near 75°F
during December to about 125°F in July 1972.  River temperatures  during
the same period ranged from about 30°F in December to slightly above
                                                    •\
60°F in July;  The temperature drop of thermal  water  between  the  pump-
ing pit and the soil heat grid inlet (about 2.7 miles) averaged 10.6°F
for the period January 1972 through March 1973; temperature drop  ranged
from 2.8°F for the week beginning August 2, 1972, to  20.8°F for the
week of January 10, 1973 (Figure 3).  Thermal  water temperatures  re-
corded at sprinkler heads on the project were  about the same  as tempera-
tures recorded at the soil  heat grid inlet for any given period.

The temperature drop of thermal water between  the pumping pit and the end
of the line in the exhaust pool averaged 54.6°F for the period shown in
Figure 3.  The greatest difference in temperature between pumping pit
and exhaust pool  occurred during the week of January  24, 1973 (76.4°F
difference); the least was  for the week of December 20, 1972  (35.4°F
difference).
                               20

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                              SECTION III
                           FROST PROTECTION
INTRODUCTION
A solid set irrigation system that utilized thermal water with overtree
sprinklers was placed in project orchards to protect fruit buds against
frost damage.  This technique of frost protection, but utilizing cool
water, has been tested in nearly every major fruit district and has  been
proven practical.3

Sprinkler frost protection is possible because when water cools it gives
up a fixed amount of heat per degree of temperature loss.  One British
thermal unit  (Btu) of heat is given up per pound of water as it is
reduced one degree Fahrenheit (F).  However, when water is reduced to
32°F and freezes, it releases 144 Btu's per pound of water.  Heat re-
leased during ice formation is called "latent heat of fusion."  When a
continuous film of water is applied to plants through sprinklers, the
heat given off by actively freezing water keeps plant tissue at or above
31.5°F even though a layer of ice is formed on the plant.  Ice is actu-
ally a good conductor and heat produced at the freezing surface is con-
ducted readily to the buds.1*  The critical killing temperature of most
plant tissue is below 31.5°F.

There are problems associated with frost protection by overtree sprin-
kling.  The sprinkler system must be reliable and designed to irrigate
the entire orchard at one time.  If sprinkling is stopped at 32°F or
below, plant tissue may be killed.  Spur, twig, and limb breakage from
heavy ice loads may occur under prolonged periods of water application.
However, in apple and pear orchards in the Yakima Valley, limb breakage
has not been a problem after the first year.3  Proper pruning and addi-
tional  tree supports help hold breakage to a minimum.  Also, when large

                                 21

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quantities of water will  be required for protection in a particular area,
it may not be possible to move heavy mobile spray equipment in and out
of the orchard; fixed aerial  spray equipment should be included in such
a situation.

Although the sprinkler method is exacting,  operation costs  are lower
than with other methods of frost protection; it is convenient, clean,
and can be used for supplemental irrigation.

Project apple, cherry, peach, and pear orchards were located at the
confluence of the Mohawk and McKenzie River Valleys.  Cold  air from the
Cascade Mountains drains down these valleys in spring, and  temperatures
often fall below freezing during fruit bud  swelling and blossoming and
early fruit development.  Project farmers estimated that frost partially
damaged or destroyed fruit crops 2 or 3 years out of 5 before sprinkler
frost protection systems were installed.
FROST PROTECTION OBJECTIVES
Objectives of the program were to show that thermal water  could  be  used
for frost protection to determine advantages or disadvantages  in its
use, and to determine if thermal  water would modify orchard  air  tempera-
tures .
PROCEDURE
Aluminum laterals were set on staggered spacings  of 40  ft x  30  ft,  40  ft
x 40 ft, and 40 ft x 50 ft, depending on spacing  of trees.   Full-circle
sprinkler heads with a rotation rate of about 2 rpm were installed  above
tree height on 6, 10, or 15 ft risers.   Steel fence posts were  installed
beside each riser for support.  Depending upon sprinkler spacing, nozzle
sizes of 3/32 or 7/64 in. were used to insure a uniform application rate
of 0.12 in. per hr.  The orchard area under sprinkler frost  protection
required about 2900 gal. per acre per hr or about  50 gal. per acre per
                                 22

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minute.  Pressure regulators set at 60 psi were installed at the top of
each riser just below the sprinkler head.  Pressure regulators at the
nozzles were needed for uniform applications because mainline pressure
varied from about 80 to 100 psi.

A variety of equipment was used to record orchard temperatures.  Maximum
and minimum temperature thermometers mounted on Townsend supports and
hygrothermographs were placed inside standard U.S. Weather Bureau instru-
ment shelters in each orchard.  Temperatures were generally recorded
5 ft above soil surface.  All project thermometers were calibrated with
the U.S. Weather Bureau thermometers at Eugene's Mahlon Sweet Airport.

Exposed open-bulb minimum thermometers (Figure 5) were placed on Town-
send supports attached to white posts in sprinkler protected orchards
to record the equivalent temperature of exposed fruit buds during 1969,
1970, and 1971.  An exposed thermometer in an orchard can be used to
indicate the amount of protection when compared to a thermometer outside
the sprinkler area.5

In addition to the above equipment,  platinum resistance-bulb and therm-
istor temperature sensors connected to chart recorders were used to
monitor dry bulb temperatures.  The thermistors were used in a sensitive
recording system where temperatures were recorded plus or minus a refer-
ence temperature (temperature difference or Delta-T recording system).
Temperatures were recorded at 1, 5, 10, and 20 ft heights inside and
outside sprinkler protected orchards during the 1972 and 1973 seasons.

Detailed information on critical bud temperatures of apples, cherries,
peaches, and pears at different stages of blossom development was ob-
tained from Washington State University publications in 1972.6 789
The information was given to the fruit growers on the project and was
used to determine when frost protection was necessary.

A primary temperature alarm system was installed near the center of the
project and a backup alarm was placed at the eastern edge.  When the

                                 23

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•
'• •
                                                                                             uio     no  r  \vo

                                                                         *
                                 Figure 5:   Exposed  Open-Bulb  Minimum Thermometer

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temperature dropped to a selected level, an alarm was sounded by the
primary system in each orchard grower's house alerting them to possible
freeze damage.  The backup system operated in only one grower's house.
The systems were set to alarm about 2°F above critical bud temperature
throughout the spring frost protection period after buds broke dormancy.

The effect of thermal water (applied through under-tree sprinklers)  on
air temperature at 1, 5, 10, and 20 ft in a sour cherry orchard was
determined on March 23 and 24, 1973.  Temperatures were measured with
shielded thermistors connected to the Delta-T recording system.  Thermal
water was about 85°F at the sprinkler head, application rate was 0.22 in.
per hr, and sprinklers were mounted on 18 in. risers for this study
(Figures 6 through 9).

Row crops also were frost protected with thermal  water.  Eighteen-inch
risers and an application rate of 0.12 in. per hr was used in 1969 and
1970.  About 0.25 in. per hr was used in 1972.  The degree of air tempera-
ture modification under the sprinklers was measured with shielded mini-
mum thermometers in 1970.  In 1972 the effect of thermal and cold-well
water on temperatures 1, 5, 10, and 20 ft above the ground were measured
with shielded thermistors connected to the Delta-T recorders.  Irrigated
blocks of row crops were 48 ft wide (east-west) and 218 ft long (north-
south).  Non-irrigated control, thermal, and cold water irrigated blocks
were separated by 2 rows of sweet corn that were 7 to 9 ft tall.  Tempera-
tures were recorded near the middle of each irrigated block, and control
temperatures were recorded in an open area west of the irrigated blocks.
Thermal water was about 88°F and well water was about 56°F on nights
row crops were protected.  The row crops included tomatoes, peppers, snap
beans, lima beans, beets, onions, cabbage, and cucumbers.
RESULTS
1969
Construction of the water delivery system was completed on March 21,
1969.  At this time fruit buds were beginning to swell, and killing bud

                                 25

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IV)
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ro
          38 -
          36 -
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        d)
        en
        a)
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          32
          30
          28
                -$- Wind Speed       •;
                 •  Control
                 A Irrigated Orchard
                    1:30
                         2:30
3:30
6:30
7:30
8:30
                                                                                                                  - 5
                                                                                                               01 .c
                                                                                                               4-

                                                                                                               X) C3
                                                                                                               c *i-
                                                                                                                  _1
                                                 4:30        5:30
                                                     time - A.M.
Figure 7.  Influence of  thermal  water (85°F) applied through undertree sprinklers  (at  .22  in/hr)  on air temp-
           eratures 5  feet  above the ground on March 23, 1973.  (Dew point was 24°F to  26°F  outside orchard.)

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    38  '
    36  -
(L)
O)
    34  -
O

 I
u.
 VI

 £  32
    30   -
    28
             •  Control
             ^  Irrigated Orchard
                     irrigation on
1:30        2:30        3:30        4:30        5:30
                                      time •• A.M.
                                                                          6:30
7:30
8:30
 Figure 8.  Influence of thermal water (85°F) applied through undertree sprinklers (at .22 in/hr) on air temp-
            eratures 10 feet above the ground on March 23, 1973.  (Dew point was 24° to 26°F outside orchard).

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ro
          38 -
          36  -
          34  -
        -}i\
        tu 32

        o>
          30  -
          28
• Control

A Irrigated Orchard
                I
         irrigation on
                   1:30        2:30        3:30        4:30         5:30


                                                          time - A.M.
                                                               6:30
7:30
8:30
       Figure  9.   Influence  of thermal  water (85°F)  applied  through tmdertree sprinklers  (at .22 in/hr)  on air temp-

                   eratures 20  feet above the ground  on March 23,  1973.   (Dew point was  24°  to 26°F outside orchard.)

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temperature was judged to be about 25°F.  The sprinkler system was acti-
vated in all orchards on March 24, 1969, when the temperature dropped to
29°F; minimum temperature that night was 28°F.  Although thermal water
temperature was 110°F at the Weyerhaeuser pumping pit, water at the
sprinkler head was only 70°F because not enough thermal water had been
pumped through the system to warm soil  surrounding the main and submains.
Wind movement was out of the NNE at speeds up to 10 mph.  Ice formed on
buds and on those limbs of up to 2 in.  diameter.  Large limbs were dry or
only had a very thin ice coat.

The following night, March 25, the temperature dropped to 30°F and sprin-
klers were activated.  Water temperature was about 102°F at the pumping
pit and 90°F at the sprinkler nozzles in the orchards.  Minimum tempera-
ture was 30°F and wind movement was less than 2 mph.  No ice was formed
   «
on buds or limbs under these conditions.

Considerably fewer cold nights than normal were recorded during April  and
May of 1969, and by mid-May night temperatures were well above freezing.

Fifty acres of orchard including pears, peaches, apples, sour cherries,
and filberts were sprinkled with thermal water for frost protection in
1969.  Several unprotected control fruit trees were not damaged by frost
during the 1969 season.  Temperatures apparently did not fall below
critical levels.

Sprinkler-applied thermal water was used to protect 2 acres of straw-
berries from frost in 1969.  The early blossoms were saved and a rela-
tively early crop of berries resulted.

1970
An exceptionally warm two-week period during early February 1970 caused;
fruit buds to break dormancy about two weeks earlier than in 1969.  A
large quantity of water, was applied to the orchards because of the early
breaking of fruit bud dormancy and the subsequent cold nights.  Fourteen
                                 30

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to about 18 in. of water were used for frost protection in the various
orchards (Table 1).  The large amounts of applied water plus normal
rainfall made a rigorous spraying and dusting program necessary.

Late February, March, and April were colder than normal.  Minimum air
temperature dropped below 28°F four times, and thermometers exposed to
radiant-heat loss dropped below 28°F seven times.  Sprinklers were acti-
vated 26 times in 1970 for frost control.  Bud temperatures were held at
30.5°F to 31 °F as recorded by exposed open bulb minimum thermometers.
When sprinklers were activated during February and March, ice was formed
even with water in excess of 100°F at the sprinkler head.  During April
temperatures dropped and recovered rapidly so that there were only short
periods of freezing temperatures.  No ice load developed on trees during
frost protection in April.

A light fog was produced by thermal water applications on colder nights
in February and March.  When fog developed it was localized in the or-
chards and little fog drifted to adjacent residential  areas.  Sunlight
always dissipated the fog soon after daybreak.  Minimum orchard air
temperatures ranged from 0 to 3°F warmer in frost-protected areas than in
non-protected areas (Figure 10).  Temperature differences were measured
with minimum thermometers inside weather shelter.
         i
No frost damage was found in any of the project orchards.  There were,
however, varying degrees of frost damaged fruit buds reported in Spring-
field-Eugene area orchards.10 n  Danger of freeze damage to filberts
during spring did not appear to be great and no beneficial results were
observed.  Frost protection of filberts was discontinued after 1970.

In preparation for raising row crops under frost protection, low risers
(18 in.) were installed and temperature was measured at about the 1-ft
level.  It was possible to hold the ambient air temperature several de-
grees above that of the unprotected areas.  The thermal water from the
low risers consistently increased the ambient temperature of the air from
2 to 5°F as measured with sheltered minimum thermometers (Figure 11).

                                 31

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Table 1.   PRECIPITATION AND THERMAL  WATER  APPLIED  FOR  FROST  CONTROL  FROM
                        FEBRUARY  15  TO  MAY 31,  1970
Farm      Tree Crop

  1        Peaches
  4        Filberts
  5        Pie Cherries
          Apples
          Pears
  8        Apples
          Pears
Precipitation,
   inches
    6.2
    6.2
    6.2
    6.2
    6.2
    6.2
    6.2
Water Applied,      Total,
   inches           inches
     14             20.2
     14             20.2
     17.8           24.0
     17.8           24.0
     17.8           24.0
     18.1           24.3
     18.1           24.3
                              32

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                                               Minimum Air Temperature in Weather Shelter in Unprotected Section of Project

                                               Minimum Air Temperature in Weather Shelter in Protected Section of Project
CO
Co
                              19  2O  21  23  5   17  19 2O  22  23 25  27  3O 31   1   2   34  7   12  13  16  17  21
               Figure 10:   Air temperature modification  at the 5  ft level under  thermal  water applied

                             through  sprinklers  on  15 ft risers  (1970).

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                                            Minimum Air Temperature in Weather Shelter in Unprotected Section of Project
                                            Minimum Air Temperature in Weather Shelter in Protected Section of Project
CO
                             t-  30
                                                    19 21  24  25  27 3O  31   I   234   7  13  17 21  27
                        Figure  11:   Air  temperature modification at  the  1  ft  level  under thermal
                                       water using 18 inch risers  (1970).

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1971
Pear fruit buds had swollen but were still tight, and apple and peach
buds had just started to swell by late February.  The first serious
freeze of 1971 occurred on March 1 when the temperature dropped to a low
of 18°F; temperature was below 20°F for 1-1/2 hr.  Sprinklers were acti-
vated at 25°F (11:30 p.m., February 28) and remained on until 4:00 p.m.,
March 1, when air temperature reached 35°F.  Very little ice load damage
was found in peach and apple orchards in spite of an extremely heavy
ice load (Figure 12).  In the sour cherry orchard, 113 trees were damaged
to some extent.  Of those damaged, approximately 40 had to be replaced.
Almost all of the damaged cherry trees were infested with heart rot,
making them very susceptible to ice load damage.  However, some ice load
damage was noted on sound cherry trees.

On the following night (March 1-2), a low of 23°F was recorded.  Sprinklers
were turned on but no further ice load damage occurred.  Temperatures
dropped below freezing four more times during March, but did not drop
low enough to damage fruit buds.  The chance of freeze damage was les-
sened because buds developed slowly during spring of 1971.

Early severe frosts occurred in the fall of 1971 and a low of 28°F occurred
October 17, 1971.  The probability of 28°F occurring that early in the
fall was only 4 percent at Eugene.12  Walnuts were late in maturing and
only about 5 percent of the nuts had fallen from the trees by October 17.
The nuts that were on the ground were damaged by frost.  For this reason,
the thermal water sprinkler system was assembled under the walnut trees
so that it could be used to protect fallen nuts from further freezes.

On November 5 and 6, the temperature dropped to 26°F and 23°F, respec-
tively.  According to U.S. Weather Service records, there is only about
a 4 percent chance of temperatures this low occurring in early November.12
These freezes severely damaged walnuts in the entire Willamette Valley.

Only about half of the project walnut crop had dropped from the trees
before the November 5 and 6 frosts.  The fallen nuts were protected from
                                 35

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Figure 12:   Ice Load in  Peach  and  Apple  Orchard

-------
freeze damage with the thermal water sprinkler system.  However, nuts
remaining on the trees were severely damaged by the cold temperatures.
Trees in the project walnut orchard were nearly 50 ft tall, and it was
impractical to provide a sprinkler system capable of providing protection
to nuts hanging in the trees.

Immediately after the November 5 and 6 freezes, the frost damaged nuts
in the, trees began to fall and resulted in a mixture of sound and damaged
nuts on the ground.  Because of the freeze damage, Hudson House, which
buys approximately one-third of the state's walnut production, rejected
a high percentage of walnuts grown in the Willamette Valley.  Samples
of walnuts from the project were subjected to crack-tests by Brunner
Dryer, a nut drying firm.  As high as 45 percent of the walnuts were found
to be damaged and were rejected by the nut packer.  However, the project
grower was successful in marketing all of the commercially rejected nuts
by selling them at his farm for a reduced price that reflected the average
percent of damaged nuts.
1972
Temperatures below 32°F were recorded 10 times between March 7 and April  30,
1972.  Sprinklers were activated on March 28, April 19, 22, and 30.  Cri-
tical blossom bud temperatures for all project fruits were judged to be
near 28°F by March 24 and throughout April, according to information in
the literature.6 7 8 9

The temperature dropped to 32°F at 11:50 p.m. on March 28, 1972, but
remained around 31°F until early morning.  Cold air moved out of the
Mohawk Valley and the sprinklers were activated at 2:30 a.m., March 29,
when the temperature fell to 29°F.  The low for the night was 28°F.
Sprinklers were turned off when the temperature reached about 35°F; this
occurred between 8:00 and 8:30 a.m., March 29.  Very little ice accumu-
lated on the trees and no tree damage was observed.
                                 37

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During early April, 20-ft towers with shielded temperature sensors lo-
cated at 5, 10, and 20 ft above the ground were placed in the sour cherry
orchard and in adjacent open areas to monitor temperatures during periods
of sprinkler frost protection.  The towers located in the open areas
served as non-irrigated checks.  Temperatures were recorded on 6-channel
recorders.  Temperatures recorded with the above equipment during frost
protection periods on April  19 are shown in Figures 13 through 15.

There was a rise in orchard  temperature of about 1°F within the first
15 minutes of sprinkler operation.  Temperatures at 5 ft and 10 ft were
.5 to 1°F warmer, and 20 ft  temperatures were 1 to 2.25°F warmer in pro-
tected orchards than in non-protected areas.   The data shown for April  19,
1972, is representative of what occurred on other nights of frost pro-
tection.  After the sun rose between 6:00 and 7:00 a.m., temperature
build-up in the orchard was  slower than in the non-irrigated check area.

In late summer 1972, cold and thermal water were used to protect a variety
of vegetable crops from frost.  The effect of cold and thermal water on
vertical temperature gradients was recorded with the Delta-temperature
recorders.  The irrigated blocks were 48 ft wide (east-west) and 218 ft
long (north-south).  Non-irrigated, thermal,  and cold water irrigated
blocks were separated by two rows of sweet corn that were about 8 ft tall.
Temperatures were recorded by shielded thermistors near the middle of
each block at 1, 5, 10, and  20 ft above ground.  Non-irrigated check
block temperatures were recorded in an open area west of the irrigated
blocks.

Thermal water temperature was 88 to 90°F and  cold well water was 56°F
at the sprinkler head.  Sprinklers were on 18 in. risers and water appli-
cation rate was about .25 in. per hr.

Sprinklers were turned on for frost protection on September 27 and Octo-
ber 24, 1972.  On the night  of September 27,  the coldest air (31.5°F)
was near the ground and the  warmest air (36°F) recorded was at the 20 ft
                                38

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                44-

                43-


                42 -


                41 -


                40 -

                39 .


                38 .


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    32 -


    31 -


    30 -


    29


    28


    27
-$—$• Non-irrigated control area, 5 ft height

 A—A Irrigated orchard, 5 ft height

 A	* Wind speed, 40 ft height
                  A
                                               Thermal water temperature 104°F
                                               Application rate - 0.12 in/hr
                /  \
               /
                                   A
                                                                 A

                       \
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                                              sprinklers  activated in orchard
                                                                                                -3
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35


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33 -


32 -


31 -


30 -


29 -


28 .
     27
               o—o  Non-irrigated control area, 10 ft height


                     Irrigated orchard, 10 ft height
                                                                   Thermal water temperature - 104°F
                                                                   Application rate - 0.12 in/hr
                                                                                                     sprinklers
                                                                                                         off
                                    sprinklers activated in orchard
                   1:00
                          2:00
3:00        4:00        5:00
         time:  April  19, 1972
6:00
7:00
8:00 A.M.
 Figure 14.  Air temperature at 10 ft height in a sour cherry orchard frost protected with overtree, sprinkler applied
             thermal water and  in an open area adjacent to orchard.                                                    '

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03
i-

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level before the sprinklers were turned on.  Air temperature throughout
the 20 ft profile fluctuated fairly rapidly with changing air speeds.
One-foot level temperatures hovered near 32°F before sprinklers were
turned on at 5:15 a.m. (Figure 16).  Generally, temperatures at all
recorded heights in the cold and thermal water irrigated blocks were
slightly cooler than in the control block before the irrigation was
started.  Cold and thermal water did not appear to modify temperature
profiles much on the night of September 27 (Figures 16 through 19).
However, non-irrigated crops were slightly damaged by frost.  No frost
damage was noted on sprinkled crops.

Sprinklers (18 in. risers) were turned on for frost protection of vege-
table crops on September 27 and October 24, 1972.   On the morning of
September 27, the coldest air was near the ground  (31.5°F) and the warm-
est air temperature recorded was at the 20 ft level (36°F) before the
sprinklers were turned on.  Air temperatures throughout the 20 ft profile
fluctuated fairly rapidly with changing air speeds.  One-foot level
temperatures hovered near 32°F before sprinklers were turned on at 5:15 a.m.
(Figure 16).  Generally, temperatures at all recorded heights in the
cold and thermal water irrigated blocks were slightly cooler than in the
                              •;
control block before the irrigation was started.  Cold and thermal water
did not appear to modify temperature profiles much on the morning of
September 27 (Figures 16 through 19) or on October 24, 1972.  Although
air temperature was not modified much on these nights, non-protected
plants were slightly damaged by frost while protected ones were not.
The air temperature rise noted in thermal water protected areas with
18 in. risers in 1970 (Figure 11) were not detected in the fall of 1972.

Temperature profiles recorded on October 24, 1972, were similar to those
                                                                  ;
recorded on September 27.  Little apparent temperature profile modifica-
tion was induced by sprinkling, but protected crops were not damaged by
frost while non-protected crops were.
                                 42

-------
               40°-
               35
                 e ;
CO
            v>
            
-------
      45-
                     5 ft Check
                     5 ft Cold water irrigation
                     5 ft Warm water irrigation
      40-
 
-------
                45-
                           £ 10 ft Check

                           • 10 ft Cold water irrigation

                           o 10 ft Warm water irrigation
                40-
en
               01

               *
               o
               
-------
                         A  20 ft Check

                         •  20 ft Cold water irrigation

                         o  20 ft Warm water irrigation
                45-
                40.
cr»
             V)
             
             o
                35
                30
                                                       T
                                                                   T
                              5:00
                  6:00
  7:00        8:00

September 27, 1972
9:00
	1	

 10:00 A.M.
            Figure 19.
Air temperature at 20 ft height in blocks of vegetable crops that were frost protected with sprinkler
applied thermal and cold water and in non-irrigated area:  wind speed recorded about 1200 ft east of
vegetable plots.

-------
1973
Thermal water applied at 0.22 in. per hr through sprinklers on 18 in.
risers increased air temperatures in a sour cherry orchard 3 to 5°F at
the 1 ft level (Figure 6).  At the 5 ft level, temperature in the sprin-
kled area was raised .5 to 2°F above the non-protected area (Figure 7);
at the 10 ft and 20 ft height, a rise of 0 to 1.25°F was noted (Fig-
ures 8 and 9).  Wind speed was recorded about 800 ft north of the sprin-
kled area and ranged from 0 to 5 mph during the time sprinklers were
on (Figure 7).  Dew points ranged from 24 to 26°F outside the sprinkled
orchard area.
DISCUSSION
The temperature at which fruit buds are injured depends on their stage
of development.  Buds are most resistant to cold temperature damage
during the winter when fully dormant.  As the buds swell and expand
into blossoms, they become less resistant to freeze damage and their
critical temperature moves upward.  For example, in March fruit buds
may withstand 18°F but in late April they may not be able to withstand
28°F without injury.  The resistance of buds to freezing can change
from day to day in the spring and within any season; if frost should
occur, buds are hardier following cold days than on mild or warm days.13
The resistance of buds to freeze injury also can vary in the same tree
because buds at different locations in the tree develop at different
rates and have different exposure to the sun.  Flowers or fruits exposed
directly to the sky are usually colder than those that are sheltered.
Fruit variety, tree vigor, humidity, wind speed, and duration of cold
temperature all influence the degree of freeze damage and are important
factors in determining whether or not a crop, particularly at full bloom
and earlier, will survive.

Although critical bud temperature may be below 33°F, it has been sug-
gested that irrigation for frost protection start when temperature of
                                 47

-------
shielded thermometers drops to 34 to 33°F.3 ltf  This has been suggested
because:

   •  It has been difficult to identify bud development stage and cor-
      responding critical temperature.
   •  Evaporative cooling has been reported to reduce air temperature
      when water is initially turned on.14 15
   •  Water in stand pipes may freeze and clog nozzles if the tempera-
      ture drops below 32°F.

Washington State University's Extension Circulars 369, 370, 371, and
373 for apples, pears, cherries, and peaches have colored photographs
of each bud development stage and their corresponding critical  tempera-
ture.6 7 8 9  These publications became available in 1972 and made identi-
fication of specific bud development stages and critical bud temperature
easier and served as a guide for sprinkler activation.  Temperature
profiles indicated that thermal water temperature apparently compensated
for evaporative cooling effects, and no initial  temperature depression
was detected when sprinklers were first turned on (Figures 13 through 15).
Because no temperature depression was noted, sprinklers were not turned
on until the temperature dropped near critical bud temperature in 1972.
Freezing of water in stand pipes and sprinkler heads was not a problem
because the main and submain lines were buried.   Water was not turned
into the above ground lines and risers  until it was needed for frost
protection.  By allowing the temperature to drop near the critical bud
temperature before sprinklers were activated, much less water was applied
than if sprinklers had been activated every time the temperature fell to
about 33°F as suggested in the literature for cold water.  For example,
if sprinklers had been turned on at 32°F on April 19, 1972, they would
have been on for several hours longer than they were (Figures 13, 14,
and 15).  Many more nights of frost protection in April 1972 would have
been required if sprinklers had been turned on at about 33°F.  The sav-
ings in water applications can 1>e^even  greater in the early spring when
critical bud temperature may be as low as 15 to 18°F.  Fewer and lower
water applications lessen the danger of ice load damage, reduce nutrient

                                 48

-------
leaching from the soil, and reduce the times spray materials have to
be reapplied.

It can be seen in Figures 13 through 15 that temperatures were allowed
to drop to a point between 28.5 and 29.5°F before thermal water sprinklers
were turned on.  Although sprinklers were not activated until  temperature
was near the critical bud temperature (about 28°F during April 1972),
there was no freeze damage and a depression of orchard temperature was
not detected.

Sprinklers were activated 26 times in 1970, but dry bulb temperature
dropped below 28°F only 4 times.  Fruit buds will withstand about 28 to
30°F for a short period of time at their most sensitive stage  of develop-
ment.6 789  Therefore, it is probable that trees were protected more
often than necessary, especially early in the spring, because  of lack
of detailed bud temperature data.  Perhaps the quantity and number of
irrigations could have been reduced in 1970, and this could have aided
general farm operations.

On March 1, 1971, ice loads damaged cherry trees.  The temperature was
below 20°F for 1-1/2 hr and a low of 18°F occurred.  Cherries  and apples
had not broken dormancy by March 1 and may have withstood 18°F without
great damage.6  Pears and peaches had just broken dormancy by  March 1
and may have withstood 18 to 20°F without extensive damage. As pointed
out earlier, many factors would have determined the extent of  freeze
damage and a great risk would have been run if nothing had been done.
If the critical bud information had been available, the sprinklers could
have been activated somewhat later and the ice load damage might have
been reduced.

In reviewing 1970 and 1971, it is only hypothetical what might have
been.  Problems encountered during 1970 and 1971 may have not  been les-
sened even with the more recent information on critical bud temperatures
and the indication that thermal water sprinklers do not have to be turned
                                 49

-------
on until near critical bud temperature.  However, further research is
needed to confirm the observations reported here on handling thermal
water for frost protection before it is used on large acreages.

In 1970 minimum temperatures were measured with minimum alcohol thermome-
ters and the protected orchards were up to 3°F warmer than non-protected
areas at the 5 ft level.  Temperature profiles up to 20 ft were recorded
with remote recording equipment in 1972 and 1973.

Temperatures at 5, 10, and 20 ft heights in the non-protected areas were
nearly the same or slightly higher than temperatures in the orchard be-,
fore thermal water sprinklers were activated on April 19 (Figures 13
through 15), 22, and 30, 1972.  The orchard temperature sensors placed
20 ft above the ground were located above the tree canopy but underneath
the highest part of the water arc from the sprinkler.  As the water fell,
it was cooled and the difference between temperatures inside and outside
the irrigated orchard at 10 ft (Figure 14) and 5 ft (Figure 13) levels
was less than at the 20 ft level (Figure 15).

When water is applied to several acres through a solid set irrigation
system, the micro-climate within the irrigated block will be changed.
Temperature and humidity will likely be raised in the zone below the
level of the sprinklers.  As much as 4°F increase in air temperature has
been measured in a pear orchard with overtree sprinkling using cool
water.16  Thus, the temperature rise recorded in project orchards appears
to be very reasonable.

On April 19, 1972, wind speed during the frost protection period ranged
from 0 to 3.5 mph and averaged about 2 mph until 5:30 a.m. (Figure 13).
Evaporative cooling is governed partly by wind speed.  A vapor pressure
deficit of 1 millibar (about 75% RH at 32°F) can cause a temperature
depression of more than 1°F with a wind less than 0.5 mph; when the wind
exceeds 2.5 mph, temperature depression is about 2.5°F.15  The rate of
wind movement during the April 19 frost protection probably lessened the
                                 50

-------
rise of temperature in the overtree irrigated block.  Wind speed on other
nights of frost protection in 1972 averaged higher than on April 19 and
rises in orchard temperatures were slightly less.

No fruit buds in thermal-water-protected orchards were damaged by 1972
spring freezes.  A full crop of peaches was produced in the project
orchards.  Unprotected orchards in the Eugene-Springfield area produced
no crop to a very light crop of peaches.

Although fruit buds were in no danger from 29°F on March 23 and 24, 1973,
undertree sprinklers were turned on in a sour cherry orchard to determine
the effect of thermal water applied through the sprinklers on air tempera-
tures.  Only temperature profiles for the morning of March 23 are shown
(Figures 7, 8, and 9) but are representative of what occurred on March 24.
The largest rise in temperature occurred in the sprinkled orchard at
the 1 ft level (Figure 7).  The greater the height of recorded tempera-
ture above the ground, the less temperature rise detected.  Wind speed
appeared to influence temperatures at recorded heights up to 10 ft.
For example, as wind speed dropped at 6:30 a.m. (Figure 7), temperature
at 5 and 10 ft levels increased by about 1.5°F.  Wind speed may have
reduced the influence of thermal water through evaporative cooling.
Measurements made in an almond orchard in California showed that cold
water applied through undertree sprinklers showed an advantage of 1 to
2°F.17  The fact that there was almost no temperature modification at
the 20 ft level and very little at the 10 ft level indicates that under-
tree sprinklers are not satisfactory for frost protection even when thermal
water is used.
                                 51

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                              SECTION IV
              THERMAL WATER IRRIGATION AND PLANT COOLING

THERMAL WATER IRRIGATION/,

Introduction
Although the 30 yr mean annual precipitation for the Eugene area is
over 40 in., less than 2 in. of rain fall during the months of June,
July, and August, which is the major portion of the growing season.18
Thus for good crop production, irrigation is required in the Eugene/
Springfield area.

Two major soil series are located within the project.  Most of the
soil is Newberg sandy loam with interspersed areas of Camas gravelly
sandy loam.19  The entire area is subject to flooding by the McKenzie
River, which in the past has left sandy deposits throughout the soil
profile.  The water holding capacity of the soil is 1.25 in. per ft
of soil with a permeability of about 2 in. per hr.20  This is a light
textured soil in which about 80% of its holding capacity is available
water.  Therefore, of the 1.25 in. of water held per, foot, about 1 in.
is available for crop use.  The total available soil moisture was
never allowed to be depleted below the critical level before the addi-
tion of irrigation water.  The amount of water depletion allowed de-
pended upon a number of conditions including the type of crop and
stage of growth.  The root depth of various crops directly influences
the amount of soil moisture available to them.  A shallow-rooted crop
that relies upon only the top 1 ft of soil for its water will require
less amounts but more frequent irrigations than a deep-rooted crop.

Theoretically, a water droplet passing through the air after leaving a
sprinkler nozzle should approach wet-bulk temperature of the air.21
                                53

-------
The wet-bulb temperature is defined as the temperature that the air
assumes when water at current temperature is introduced gradually and
evaporated adiabatically at constant pressure until  the air is satu-
rated.  Temperature of sprinkler spray water is changed by evaporation,
conduction, and to some extent by radiation of heat  to or from the air.
When initial water temperature is higher than air temperature, the
droplet temperature will decrease as it passes through the air by
evaporative cooling and by loss of heat through molecular collisions.
After cooling to air temperature, droplets continue  to cool  by evapora-
tion to the wet-bulb temperature, if the droplets remain in the air
long enough.  The actual rate of cooling depends on  the difference
between the wet-bulb and dry-bulb temperatures of the  air, the Volume
and shape of the droplet, and the velocity of the droplet relative
to the air through which it is passing.  If the initial  temperature of
water leaving a sprinkler is below wet-bulb temperature, the droplet
will be warmed as it passes through the air by molecular collision;
if it is in the air long enough, the droplets could  reach wet-bulb
temperature.

Studies by Pair22 indicated that hot water could be  used for sprinkler
irrigation of crops without much concern for the effects of high water
temperatures.  His tests demonstrated that water temperature increased
as much as 15°F when it was initially below wet-bulb temperature, and
cooled as much as 135°F when it was intially above wet-bulb temperature.
According to Pair, water temperature varied little with distance from
the sprinkler.  The smaller drops traveled a shorter distance, but
because of size their temperatures approached wet-bulb equilibrium
more rapidly.  The larger drops traveled a greater distance and thus
had more opportunity to approach wet-bulb temperature.

It was determined that thermal water cooled about 2°F  per ft distance
it traveled from the sprinkler nozzle during periods of low relative
humidity in tests conducted on the project in May and  July 1969 (Fig-
ures 20 and 21).  This confirms the findings of Pair that, during.
                                 54

-------
in
01
 105







 100








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                                          \
                               AIR TEM?EMATURE
\
   0  I  2 3  4  5 S  7  8 9 10 II 12 13 14 lo

              DISTANCE FROM NOZZLE If I)
                                                                                   110'-
                                                                                     i  i
                                                                                   IO&
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                                         !  I  !  ;NJ j  I  I  I  '  !  '  '  '  '  '
                                                                                   75 [
                                                                                   70 (-
                                                                                   65
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                                                                                                                  ,

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                                                                                                                          m
                                                                                     0   2   4   o
                                                                                                    a   to   12   14   is   is   20

                                                                                                 DISTANCE KSOIv, NOZZLE iff.)
              Figure  20:   Water Temperature  Drop Through

                            Sprinkler Application (5-12-69)
                                                    Figure 21:   Water  Temperature  Drop  Through

                                                                  Sprinkler Application (7-15-69)

-------
periods of high ambient air temperatures, water in excess of 100°F at
the sprinkler nozzle may be below ambient air temperature by the time it
reaches the plants.

Thermal irrigation water was not available from May 6 to July 19, 1971,
because the Weyerhaeuser plant, which supplies the thermal  water, was
not in operation.  During this period, relatively cool water from the
McKenzie River was used for irrigation (Figure 22).  By the time thermal
water was available, pole beans were within one week and sweet corn
within three weeks of harvest.  Because thermal water was not available
for much of the 1971 growing season, it was not possible to determine
the effects of it on crop production.  However, studies were conducted
to determine the effect of thermal  water on soil temperature when applied
by rill and flood irrigation late in the growing season.


Procedure
Each farm crop was considered separately, as much as possible, when
scheduling irrigations.  The critical root-depth zone was determined
for each crop, and it varied from the deep root zone of the walnut tree
to the shallow zone of snap beans.   Gypsum blocks and tensiometers
were installed throughout the project for monitoring soil moisture and
the information was used for irrigation scheduling.  The critical depth
and percent allowable moisture depletion level for most of the crops
are listed in Table 2.

On July 28, 1971, the effects of thermal and cool water furrow irriga-
tion on soil temperatures were observed in a soybean plot.   Furrows
were about 2 in. deep and 10 in. to the sides of the plant row.  Tempera-
ture sensors were placed at 6 and 12 in. depths beneath the bottom of
the furrow and soil surface halfway between the furrows (Figure 23).
Temperature sensors were placed at the same depths in a non-irrigated
check plot.  The furrow irrigation plots were underlaid with soil heat-
ing pipes that were at a 2 ft depth (see Soil Heating Study for des-
cription of soil heating system).

                                 56

-------
en
                                 60
                               U-
                               o
                               0)
                               $_
                               rs



                               150

                               n.

                               to
                               Cl



                               •r-

                               C-'.
                                 30
                                        Apr
May
June
July    Aug
Sep
                         Figure  22:   Mean monthly temperature  of McKenzie River in  1971

-------
                 Table 2.  CRITICAL DEPTHS AND ALLOWABLE SOIL MOISTURE DEPLETION FOR VARIOUS CROPS
en
oo

Crop
Peaches
Apples
Cherries
Pears
Filberts
Walnuts
Tomatoes


Crop
Potatoes
Beans
Corn

Instrument
Critical Depth,
ft
1.5
1.5
1.5
1.5
1.5
1.5
1.0


Instrument
Critical Depth,
ft
0.5
1.0
1.0
Gypsum Blocks

Minimum
Allowable Meter Reading,
mmohs
170
170
170
170
170
170
170
Tensiometers

Maximum
Allowable Instrument Reading,
atmospheres
0.3
0.4
0.5
Maximum Allowable Available
Soil Moisture Depletion
At Critical Depth,
%
50
50
50
50
50
50
50

Maximum Allowable Available
Soil Moisture Depletion
At Critical Depth,
%
40
50
50

-------
       temperature sensors
                      6"

                      V
                      6"

                      v
                      w
Figure 23:   Temperature sensor placement.
                    59

-------
Thermal water at 88°F and well water at 60°F were applied to adjacent
plots at a rate of about 10 gpm starting at 10:45 a.m.  Soil moisture
in the sandy loam soil was about 60 percent of field capacity when
water applications started.

On August 3, 1971, mature tomato plants were flood irrigated with 108°F
water for one hour at the rate of about 2 gpm (equivalent of about
2.7 acre feet water applied).  Soil temperatures were monitored at
6, 9, and 12 in. depths below the plants.  The soil  temperature at the
6 in. depth increased 31°F but only increased 10°F at the 12 in. depth .
(Figure 24).  Equilibrium temperatures had not been  attained after
one hour of flooding, but the trial was terminated because excessive
water had been applied.

The effects of thermal and cold water sprinkler irrigation on plant
growth were compared in more detailed studies in 1972.

During June 1972, a study was initiated to compare trunk growth made
by filbert nut trees on plots irrigated with cold well water, thermal
water, and on non-irrigated plots.   The average tree age was 10 to
12 yrs.  Tree spacing was 20 x 20 ft.  The cold water and non-irrigated
block contained 30 trees each; the  thermal water block contained
48 trees.

Temperature of well water used for  irrigation was about 50 to 55°F.
Thermal water temperature at the header averaged about 100 to 110°F,
about the same as temperatures recorded at the inlet of the soil heat
grid.  The thermal and cold water blocks were irrigated at the same
time and the same amount of water was applied to each block.  The
following is a summary of filbert irrigation applications:  July 13,
.70 in. water; July 19 and 20, 2.4  in. water; and August 8, 3.5 in.
water (Table 3).

Trunk growth was measured with the  Verner-type dendrometer.  This
instrument has been used to measure growth of fruit  trees and various

                                 60

-------
o
 0)
CL
Ol
O
CO
     no-
     100 -
      90 -
80 -
      70 :
      •—• 6 in. depth
      O—o 9 in. depth
            12 in. depth
            6 in. check
                     10
                                                                           60
                                20          30          40           50
                          Time From Beginning of Flooding (minutes)
Figure 24.   Effect of  flood  irrigating with 108°F water applied  at  rate of about 2 gpm on soil temperature.

-------
Table 3.  NATURAL PRECIPITATION AND SUPPLEMENTAL IRRIGATION RECEIVED BY
                FILBERTS DURING JUNE, JULY,  AND AUGUST  1972
Date
June 7
8
9
10
11
15

Inches water
0.08
0.49
0.68
0.59
0.05
0 .02

Date
July 8
13
: 19 & 20
August 8
14
16
20
Inches water
0.06
0.70Z
2.40 z
3.50Z;
0.02
1.41
0.27
 'Supplemental irrigation.
                                62

-------
 forest tree species.23 2J*  Unlike dial-gauge dendrometers, this lever-
 type instrument is not affected by daily trunk shrinkage and always
 shows maximum radius attained by the trunk since the previous reading.

 Dendrometers were installed on 5 different trees in cold and thermal
 water irrigated blocks and in the check block.  Trees on which den-
 drometers were installed were picked for uniformity of size and vigor.
 The dendrqmeters were read 3 times each week starting in mid-July 1972.
'? >; '.' :. •: :  I  ' ."• '" '   ? . '-'; -- ..v' '         '

 Filberts were collected "from 5x5 ft plots on the east side of 4 trees
 in the check, cold, and thermal water irrigated blocks on October 19,
 1972.  THe'plots were beneath trees with dendrometers.  The nuts were
 counted;, weighed at harvest; weighed after drying on January 3, 1973;
 and then cracked so the kernels could be examined.

 Another study conducted in 1972 compared the effects of cold and thermal
 water sprinkler irrigation on growth and production of vegetable crops
 (see Soil Heat X Cool and Thermal Water Irrigation, Section VIII).  The
 vegetable crops were:  bush snap beans, 'Bluelake 274'; tomatoes,  'New
 Yorker,1 'C. 1327,'  and 'H. 1350'; pepper, 'Calwonder1; cabbage, 'Golden
 Acre1; onion, 'Yellow Globe Danvers'; lima bean, 'Thaxter1; beets,
 'Detroit Dark Red'; cucumber, 'Pioneer1; and sweet corn, 'Jubilee.'
 Results
 Some mechanical  failures of equipment occurred in the early  periods of
 the 1969 season.  These included faulty valves, problems  with  branch
 saddles on the plastic subheaders, and line leaks; these  adverse  con-
 ditions were corrected without curtailing the demonstration.   Inadver-
 tent leaks in the system caused limited flooding of a small  area  with
 water at 125 to  130°F.  Some cherry trees and bean plants were killed
 by the ponded water; sweet corn was only temporarily set  back.  In
 general, no adverse affects were observed from using thermal water
 sprinkler irrigation after the first season.
                                  63

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More emphasis was placed on proper scheduling of irrigations in 1970.
Gypsum blocks and tensiometers were installed throughout the project to
monitor soil moisture in the different crop areas.   Table 2 lists the
criteria used to schedule irrigations and Figures 25 and 26 show typical
moisture curves for sweet corn and filberts.                   '

Several tests were conducted to find the effect of thermal  water irriga-
tion on ambient air temperature in 1970.  At night the air temperature
often dropped below the optimum level for plant growth'.   By applying
sprinkler applications of thermal water during these cooler night
periods, it was thought that perhaps the heat given off from the thermal
water would modify the air temperature and thus reduce the temperature
drop.  However, it was found that the thermal water heat release had no
measurable effect on the air temperature during the periods observed
(measurements made with minimum thermometers).

Soil temperatures beneath furrows irrigated with thermal and cool water
were affected by the water applications (Figures 27 and 28).  Within
2 hrs after initial application of 88°F water, the temperature at 6 in.
beneath the furrow was 11°F above the check and after 5 hrs it was
16°F above the check (Figure 27).  Temperatures at the 6 in. depth in
the plant row increased 3°F after a 5 hr period.  Cool 60°F water
reduced soil temperatures by 6°F six inches beneath the furrow after
2 hrs and did not cause any further reduction in temperatures.  No
temperature reduction was caused in the plant row at 6 in.  depth by
the 60°F water at the end of 2 hrs, but soil temperature was 3° lower
than check at end of a 5 hr application.

Soil temperatures at the 12 in. depth were not affected by water applica-
tions as much as at the Gin. depth.  The 88°F water increased soil
temperature 12 in. beneath the furrows by 6°F and the cool  60°F water
decreased temperatures by 8°F after 5 hr application (Figure 28).  Soil
temperature at 12 in. depths in the plant row, halfway between furrows,
was not altered by either 88°F or 60°F water (Figure 28>.       :.
                                 64

-------
       0.6


       0.5


       0.4
     c
     o
     S 0.3
     s-
     03
       0.2


       0.1


       0.0
                    15
                   June
                          30.
 15
July
31
  15
August
31
Figure  25:   Soil Moisture Curve  at One Foot Depth  in Sweet Corn  Field.
.5.190


>180


  170
     o
     3
     •o
     o
     o
     10
     £160
     o
     O)
       150
       140
                    15
                   June
                          30
 15
July
                                                     31
            15
         August
                                                                       31
Figure  26:   Soil Moisture Curve  at  18 Inch Depth in Filbert  Orchard.
                                      65

-------
                     90
                     85-
o>
                 Q.
                 O)
                 Q
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-------
CT>
                    90 -J
                    85 H
                    80-
                 cu
                 Q
                    75.J
                 Ol
                 s~
                 3
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                 It!
                 S-
                 cu
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                 01
                    70-
                    65-
                    60
                                 Check
                         -£	P"  furrow
        row


        88°F water
        furrow

o-.—a   plant row


        60°F water
o—o   furrow
                                 plant row
                                 0123            45


                                            Time  From  Beginning of Irrigation (hrs)


              Figure 28.  The effects of 60° and  88°F  water  applied in furrows on soil temperatures 12 inches beneath
                          furrow and plant row.

-------
The sensors 12 in. beneath the furrow were actually 2 to 3 in. closer
to the thermal water pipe than were sensors 12 in. beneath the plant.
The movement of heat from the buried pipes may have contributed to the
2° difference between furrow and plant row checks at the 12 in. depth.
Apparently the plant row and furrow checks at 6 in. were not influenced
in the same manner (Figure 27).

Since the trial was on soil heated by circulation of thermal water
through buried pipes, the vertical soil temperature profile was some-
what different than normally encountered in unheated soil.  The 24 in.
soil profile heated by thermal water was generally several degrees
warmer than non-heated soil (Figure 29).  In unheated soil, temperatures
were about the same or slightly cooler at 24 in.  as at the 12 and 6 in.
depths.  In heated soil, the 24 in. depth was generally warmer than at the
12 in. depth and as warm or warmer than the 6 in. depth.

Because of heat emitted from the buried pipe, the 60°F irrigation water
had to absorb increasing amounts of heat as depth of water penetration
increased.  The heat from the buried pipe may have also influenced soil
profile temperatures where thermal irrigation water was used.  The effect
of 60°F and 88°F water on soil profile temperatures could not be sepa-
rated from the effect of heat flow from the soil  heating pipe because it
was not possible to duplicate the trial on unheated soil in 1971.

The 60°F irrigation water apparently reached an equilibrium of 69°F
twelve inches beneath the furrow after about 4-1/2 hr, and an equilibrium
temperature of 64°F six inches beneath the furrow about 2 hr after
irrigation started.  With 88°F water equilibrium temperatures at 6 and
12 in. beneath the furrow were not reached at the end of 5-1/4 hr.

No visual plant damage was noted in any of the plant furrows irrigated
with the thermal  water (88°F).
                                 68

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                                                                        Soil Surface
                                          check, no heat
                                          soil temperature directly above thermal water pipe
                                   O—o  soil temperature halfway between water pipes
                              6 -
CTl
(O
l/l
O)
-C
o
                          I

                         
-------
Even in the study where a high application rate of 108°F water was
applied to tomatoes, there was no apparent visual damage to plant and
none developed later in the season from the thermal water.

The rate and amount of heat penetration in the soil is closely related
to volume and temperature of water applied.  Temperature alterations
caused by irrigation water take place slowly at depths of about 12 in.;
however, soil surface temperatures were rapidly modified.  Although no
plant damage was noted here, some crops may be more sensitive than
soybeans or tomatoes to surface thermal water applications.

Soil moisture levels for the 1972 non-irrigated check, thermal, and cold
water irrigated filbert blocks are shown in Figures 30, 31, and 32.
Soil moisture at the 6 in. depth in thermal and cold water irrigated
plots was about the same through July and August.  Soil moisture level
at 18 and 24 in. depths was somewhat lower in the cold water block
during August than in the thermal water block (Figure 32 vs 31).  By
the end of July and throughout August, moisture levels in the surface
24 in. were low (Figure 30) in the non-irrigated check.  The high value
for August 17 in Figure 30 was caused by 1.41 in. of rain that fell on
August 16, 1972.

The average accumulative radial trunk growth made by trees under the
various treatments is shown in Figure 33.  The slightly lower moisture
levels recorded at 18 and 24 in. depths in the cold water compared to
the thermal water block (Figure 32 vs 31) apparently did not reduce
radial trunk growth (Figure 33).  There was no significant difference
in radial trunk growth made by trees irrigated with thermal and cold
water (Table 4).  Trunks of trees from the non-irrigated check plot
grew 66 to 70 percent less than irrigated trees.

Table 5 contains filbert yield data from the various treatments.  Size
and vigor of all sample trees were judged to be nearly equal when
selected in June, and average diameter of tree foliage spread was about
                                 70

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   180-
   150-
   120-

-------
ro
              180-
              150-
              120-
            Id
            01
            i-
            OJ
            « 90-
            o
            c:
            E
           r™
            QJ
           Q

            C
            •O
    60'
              30-
                 6  in.
          o—o  18 in
          a	a  24 in
                                               10    12    14    16    18    20    22    24    26    28    30
            2468

                                                  August  1972

Figure 31.  Delmhorst meter readings  in  thermal water  irrigated  block  of  filberts  at three depths.

-------
•-J
CO
                 180-
                 150-
              g>  120
                   90
              in

              O
              01
              O
              10
              O)
                   60
                   30
                         o—o  18 in
                               24 in
                                        6
8    l6     12    14    16    18    20    22    24    26    28    30
                                                                  August. 1972
                Figure 32.  Delmhorst meter readings in cold water irrigated block of filberts at three depths.

-------
 U
 K
 o
 o
 t:
 01

 o
 s_
 o
 c:
 -a
 (O
 ce:

 ai
 +J
 nj
 u
 o
550-




500"


450.




400-





350-




300-




250 _
 •£  200-
    150_
    100 _
     50
                     Cold
                     Thermal

               o—o  Check
      17  lb  2\    2*4  26  2*8    si55     5    lb 11   14   h   18    2!   23    25     28'-. 30   1      4   6~

                 July                          August. 1972         "                                     September

        Seasonal curves of radial trunk growth of filbert trees (10-12  years old) grown  on  non-irrigated check

        plots and on thermal and cold water irrigated plots.
Figure 33.

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Table 4.  AVERAGE ACCUMULATIVE RADIAL TRUNK GROWTH MADE BY 10-12 YEAR
      .,                       - .                                   t       -r

OLD FILBERT TREES IRRIGATED WITH THERMAL  AND COLD WAT&ER AS COMPARED TO


               TRUNK GROWTH MADE BY NON-IRRIGATED TREES     ":       *

                                                          . !



     Irrigation               Average accumulative radial trunk

      Treatment              «	growth - 1/5,000 inch2



Cold water                                    579.6  a       •••


Thermal  water                                 505.8  a


Non-irrigated check                           169J6  b
z Means followed by different letters are significantly different at 1%
  level - Duncan's Multiple Range Test.
                                75

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Table 5.  YIELD OF FILBERT NUTS FROM COLD AND THERMAL WATER IRRIGATED BLOCKS  COMPARED TO  YIELDS  FROM



                                         NON-IRRIGATED CONTROLS
Irrigation
treatment
Thermal water
Check
Cold water
Avg. foliage
spread of trees,
diameter - ft
16.2
15.6
16.4
Nut yield/plot2
at harvest-! 0/1 9/72
No. Wt-g
132.2
120.7
96.0
556.2
556.2
461.2
Avg. dry wt (g) plot
January 3, 1973
Gross
452.8
430.0
378.3
Shell
279.9
277. 8
238.8
Kernel
168.0
146.5
134.0
Avg. number/plot
Shrivels Blanks
3.2
8.2
4.0
17.5
18.7
14.0
 Plot size 5 X 5 ft.

-------
equal in all treatment blocks in October (Table 4).  Average nut yield
was not significantly influenced by irrigation treatments.  However,
there was a below average crop of nuts in 1972 because fruit buds were
damaged by an early freeze the previous fall.  Perhaps irrigation would
have made a greater difference in production if a heavy nut crop had
existed.  Individual nut kernel size was not influenced by irrigation
and the percentage of blank nuts was about the same for all treatments.
Tree trunk growth was increased by the irrigations (Table 4), and after
several seasons with irrigation, yields might be influenced by greater
tree vigor.

A severe cold period with -12°F,occurred in December 1972 and probably
eliminated or greatly reduced the chances for a good filbert crop in
1973.  Thus, it will be difficult to judge if the irrigations and extra
growth made in 1972 will benefit the crop in 1973.  It can be safely
said that thermal water, which is considered to be a pollutant to rivers,
was not harmful to filbert trees or crop in 1972.
PLANT COOLING

Crops are frequently injured by excessive transpiration during periods of
high temperature and low humidity.  Associated high solar radiation re-
ceived directly by the plant as well as that reflected and reradiated
from the soil surface contributes to the high water loss.  Even when
soil moisture is adequate, diurnal wilting of plant (caused by excessive
transpiration during hot dry weather) may cause permanent damage if the
condition persists.25  Plant growth rate decreases with increase in
temperature above approximately 88°F for a very wide range of crops
(Figure 34).  Sprinkler applied water can be used to create a more
favorable microclimate for plants by lowering temperature through eva-
poration, increasing humidity, and minimizing plant water loss through
transpiration.  The more favorable microclimate is induced by applying
light and sometimes intermittent applications of watir during periods
of high temperatures and low humidity.

                                 77

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                             GROWTH CURVE
           BASE
           TEMPERATURE
                 OPTIMUM DAILY
                 MEAN TEMPERATURE
                                        LINEAR RELATIONSHIP
40      50      60       70      80

                  TEMPERATURE  °F
                                                  90
                                                         100
Figure 34:   Plant  Growth Rate as,  Related to Atr Temperature
                                   78

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During periods of high atmospheric stress, flowers and small pods of
snap beans drop from the vine.  Applications of .04 to .06 in. of water
per hour from 10:00 a.m. to 3:00 p.m. during bloom and pod development,
when atmospheric stress was high, resulted in a 22 to 52 percent increase
in snap bean yields.26  Sprinkling reduced atmospheric stress by reducing
temperature and raising humidity and resulted in a greater yield.

Potatoes are benefited by cool temperatures which minimize their sugar
loss from high respiration, a well aerated soil to promote tuber develop-
ment, and conditions that favor low transpiration.  In experiments on
muck soil in which light sprinkling was practiced during the growing
season when air temperatures were above 85°F and the relative humidity
below 50 to 60 percent, the yield of No. 1 tubers of the 'Sebago'
cultivar was increased by 44 percent.26

Misting or light irrigations may not be advisable for all crops.  The
onion, a warm weather crop, was not benefited by a cooler microclimate
induced by misting.  Misting reduced bulb yield by 50 percent.

In review of the possible deleterious effects of high temperatures and
subsequent low relative humidities, the initial plan of operation for
the project included plant cooling and relative-humidity control.  By
applying light applications of water during high temperature periods,
relative humidity is increased and temperature decreased.  The plant is
then able to maintain turgor, keep its stomates open for gas exchange,
and withdraw the needed water from the soil without undue stress.

Thermal water was used to cool pole snap beans, tomatoes, cabbage,
corn, apples, and peaches at various times during the operation of
this demonstration project.

Procedure
Thermal water was used for plant cooling of pole snap beans, sweet corn.
and a walnut orchard in 1969 and 1970.  Over-crop sprinklers were used

                                 79

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for vegetable crops and under-tree sprinklers  were used  in  the  walnut
orchard for plant cooling.   Hygrothermographs  and minimum and maximum
thermometers were placed in pole snap bean and sweet corn fields  and  in
the walnut orchard in 1970  to measure cooling  effect of  the water.
Temperature and humidity measurements were recorded inside  a standard
U.S. Weather Bureau shelter at a height of about 5 ft.

The influence of cold and thermal  irrigation water on temperatures
1, 5, 10, and 20 ft above the ground  was recorded with the  Delta-
temperature system on September 15,  1972.   The irrigated blocks were
48 ft wide (east-west) and  218 ft long (north-south). Control, thermal,
and cold water irrigated blocks were  separated by two rows  of sweet corn
that were 7 to 9 ft tall.  Temperatures were recorded by shielded
thermistors near the middle of each  block. Non-irrigated check block
temperatures were recorded  in an open area west of the irrigated  blocks.

Thermal water temperature was 88 to  90°F and cold well water was  56°F
at the sprinkler head on September 15, 1972 (Figures 35  through 38).
Sprinkler heads were 18 in. above ground and water application  rate
was about .25 in. per hr.

Some high variable clouds were present during  the irrigation and  did
influence air temperatures.

Results
Thermal water serves as a cooling agent in two respects: 1) it is
cooler than ambient air temperature  on contact with the  plants, and
2) it increases the wetted  surface area and by so doing  increases
evaporation in the plant environment.  The heat necessary for evaporation
(539 cal/gm or 971 Btu/lb water vaporized) is  drawn from the surrounding
air, plants, and soil.

In July 1969, 86°F was exceeded only 4 times and on these dates the
sprinklers over the pole bean fields  designated for plant cooling

                                 80

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00
          o
          VI

          01
          o
          .a
           o
           0)
            1 ft Check, No Irrigation
    • 1 ft Cold Water Irrigation
    o 1 ft Warm Water Irrigation
      •<>-W1nd Speed,  12 ft  height
      & R. H. Check  Area,  No  Irrigation
      • R. H. Cold Hater Irrigation
      o R. H. Warm Water Irrigation
                                             Thsrmal  Water Temperature - 88-90°F
                                             Cold (well) Water Temperature - 56°F
                                             Application Rate - .25 in/hr
                        2:00
                    3:00
4:00
5:00
6:00
7:00  P.M. - DST
                                                September  15,  1972
            Figure  35.   (Upper)  Temperatures  one foot above  the  ground  in  cold and thermal water  irrigated, and non-irrigated
                        blocks.
                        (Lower)  Wind  speed  recorded  adjacent to  irrigated  blocks and relative humidity  in  irrigated and  control
                        blocks on  September 15,  1972.

-------
00
ro
                 90 -
                 80 -
                 70
                 60
             en
             Oi
            O
                 50 -
                                                        Irrigation On
                               2:30  3:00  3:30  4:00  4:30  5:00  5:30  6:00  6:30  7:00  7:30  8:00  8:30   9:00  P.M.  -  DST
                                   &5 ft Check
                                   •5 ft Cold Water Irrigation
                                   o5 ft Warm Water Irrigation
                                                                September 15,  1972
              Figure 36.  Comparison of temperatures 5 ft above ground in cold water,  thermal  water,  and  non-irrigated blocks on
                          September 15, 1972.

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00
CO
                  TOO-
                   90-
                   80-
                   70-
               en
               0)
                   60-
                   50
A  10 ft Check
•  10 ft Cold Water Irrigation
o  10 ft Warm Water Irrigation
                                                  Irrigation On
                           :^0  3:60  3:30   4:bo  4:^0  5:6o  5:5fl  6:60  6:^0  7:00  7:^0   8:bo  8:30  9:bo P.M. - DST

                                                          September 15, 1972
          Figure 37.   Comparison  of temperatures  10 ft above ground in cold water,  thermal  water, and non-irrigated blocks
                      on September 15,  1972.

-------
CD
-£»
             O)
             Ol
                 100
                  90-
                  80-
                  70-
                  60-
                  50
A  20 ft Check
•  20 ft Cold Water Irrigation
o  20 ft Warm Water Irrigation
                                                Irrigation On
                         2:30  3:00  3:30  4:00   4:30  5:00  5:30  6:00  6:30  7:00  7:30  8:00  8:30  9:30  P.M.  - DST
                                                          September 15, 1972
               Figure  38.  Comparison of temperatures 20 ft above ground in cold water, thermal  water, and non-irrigated
                          blocks on September 15, 1972.

-------
demonstration were activated as were those in the designated orchards.
A temperature decrease of 4 to 6°F and a relative-humidity increase of
up to 20 percent were recorded in sprinkled areas.

August 1969 was a cool month and temperatures greater than 86°F occurred
only six times.  On the last four of these occasions, the pole beans
were not sprinkled because harvest had been completed.  The pears,
cherries, and early apples had also been harvested by this time.  The
walnuts and filberts had reached full size and the shells were in the
hardening process.  Therefore, no plant cooling was attemped in these
orchards.

The effect of thermal water on temperature in a pole bean field in 1970
is shown in Figure 39.  Air temperature was reduced from 90 to 82°F
while the temperature in an adjacent field continued to climb to 92°F.
Immediately after activation of the sprinklers located above the bean
rows, the humidity rose from 40 to 65 percent.  In the control  areas,
the humidity fell to 32 percent.

Under-tree sprinklers located in the walnut orchard produced air tempera-
ture and humidity changes similar to those recorded in the bean field
(Table 6).  No increase in fungus, mold, bacterial infestation, or any
other detrimental effects were noted in any of the crops that were
cooled by the application of thermal water.

The effect of thermal and cold water on air temperature was compared
with each other and with temperatures in a non-irrigated area on Septem-
ber 15, 1972.  One-foot-level air temperature in the check block at
5:30 p.m. (Figure 35) was 82.5°F and at 6:00 p.m. had dropped to 68°F.
By 6:30 p.m., the temperature was back up to 75°F.  This temperature
fluctuation was caused by a passing cloud.  When the check temperatures
dropped, there was a corresponding rise in relative humidity.

Wind speed also contributed to some temperature fluctuations.  Wind
speed was recorded 12 ft above the soil surface and ranged from about

                                 85

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                                   ioc ;-
CO
OT
                                   0"00
                                   - - - Te.-pera'.u-e of Cooled Field
1000      TOO       1200
    "2 of Uncooked Field
0      '1400
  Time of Day
 July 1?, 1370
                                                                                           1 500
                                                                                                    1600
                                                                                                              7700
                    1803
                    Field
	Humidity of Cooled Field
                                   Figure  39:   Plant  Cooling with Thermal  Water  in  Pole  Bean  Field.

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Table 6.  PLANT COOLING WITH THERMAL WATER IN WALNUT ORCHARD
  Date
August 10
August 12
August 14
August 15
         Maximum Air Temperature
                  (F)	
              Minimum Relative Humidity
           Normal
           ambient
             95
             86
             82
             89
 Cooled
orchard
   85
   80
   76
   80
Normal
 R.H.
  21
  21
  30
  20
 Cooled
orchard
   48
   47
   53
   47
                               87

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.5 to 2.5 mph.  Wind was from the west and southwest during the irriga-
tion period.  At 4:00 p.m. wind speed increased to an average of about
2.5 mph.

Temperatures in the irrigated block dropped relatively more than in the
control area at 4:00 p.m.  The increased wind speed probably caused more
rapid evaporative cooling of the irrigation water and depressed tempera-
tures in irrigated blocks (Figure 35).
                                  -i

Temperatures at the 1 ft level were near 90°F in all blocks before the
irrigation was started.  Shortly after irrigation started (4:00 p.m.),
temperatures in the cold and thermal water blocks dropped 15 to 20°F
at the 1 ft level.  Control temperatures dropped about 1°F.  By 4:00 p.m.
relative humidity reached 20 to 25 percent higher than in the non-irri-
gated control block at the 5 ft level.

One foot level temperatures in the thermal water block tended to be
slightly cooler and humidity slightly higher than in the cold water
block.

Temperature fluctuations and differences between irrigated and non-irri-
gated blocks were not as great at the 5 ft level as at 1 ft (Figures 35
and 36).  Temperatures in the thermal water block were about 11 to 12°F
cooler, and cold water block temperatures were 6 to 8°F cooler than in
the control block through most of the irrigation.

The influence of increased wind at 4:00 p.m. and the clouds about 6:00 p.m.
on 5 ft level temperatures can be seen in Figure 36, but the temperature
depressions are not as large as occurred at the 1 ft level.
The cloud influence on 10 ft level  temperatures at 6:00 p.m.  was not
detectable (Figure 37).  Temperature differences among blocks were not
large or consistant at the 10 ft level.  Temperatures at the  20 ft level
tended to be warmer above the irrigated plots than above the  control
block (Figure 38).

                                  88

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                             SECTION V
                         UNDERSOIL HEATING

Recent experimentation with undersoil heatinq has indicated that signi-
ficant increase in plant growth can be realized with relatively small
increases in soil temnerature.  Boersma27 found that soil  heatinq had
significant effects on the yield and maturity of several crons but
concluded that long-term studies must be made to determine the relation-
ship between soil temperature and other variables involved in nlant
production.  Much of Boersma's work was carried out with heating cables
spaced 6 ft apart and 3 ft deep.

An underground thermal water pipe grid system was a logical combination
with warm water irrigation since the hot water would be available at
each distribution point where above ground irrigation lines are attached.
For this project, a pilot clot of aDoroximately two acres  was chosen
to demonstrate the field use of thermal water.  Figure 40  shows the
area in which an underground thermal water pipe grid system was in-
stalled.  It was hoped that the effect of heated soil on extending the
growing season, accelerating germination of seedbeds, and  increasing
yields could be demonstrated under field conditions.  In addition, this
is an economically attractive method for utilizing another portion of
the warm water effluent that will become increasingly available as more
power plants are put on stream.

DESIGN INFORMATION AND ASSUMPTIONS*

1.  Temperature--The following temoeratures were selected for heat
    transfer calculations:
* This section is derived from sources listed in Soil Heatinq Literature
  Survey on pages 102 and 103.
                                  89

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IQ
O
                                                                                                        *>•«
                                  AGRICULTURAL UTILIZATION  OF THERMAL WATERS
                               Figure 40.  Location plan

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    a.   Mean low air temnerature at Springfield, OR, during February
        (the earliest one might expect to plant seed is  35°F).

    b.   Optimum seed germination temperature ranges from 53 to  59°F
        with an average of 56°F.

    c.   Maximum soil temoerature at 18 in. below soil  surface to  be  84°F.

    d.   Soil surface temperatures will not vary more than 2°F at  anv
        point above the pipe grid system to obtain  the best practical
        uniform growth.

2.  Soil—The soil in the 2-acre olot selected for  the demonstation  is
    sandy loam.

3.  Thermal conductivity of soil (kg) is 1 Btu ft/ft2  hr °F.

4.  Hot water effluent temperature is 100°F ± 10°F.

5.  Pipe grid system depth~24 in. below soil surface.

6.  Water supply—Installation of tie-in to be located in the main
    water supply header near the 2-acre plot where  the pressure head
    is approximately 100 psig.

Selection of Pipe Material

Aluminum, galvanized, and PVC pine were investigated as  possible  materials
for the piping grid system.  PVC pine has some excellent nroperties
since it is corrosive resistant and lends itself to easy installation;
however, its heat transfer characteristics and strength  are quite in-
ferior to that of any metal pipe.

At higher temperatures, PVC loses fiber strength and,  therefore,  the
equivalent amqtint of working pressure (Figure 41).   Pipe fabricated  of
PVC is not recommended for use at temperatures above 140°F.

                                 91

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  100-1
   90 -
   80 .
   70 -
   60 -
OJ
S-
a.
en
c
o
   50 _
   40 _
X
(O
   30 H
                       TYPE  I  PVC PIPE
   20 _
   10
Too"
Tso
      70
15"
120
                                       LIQUID TEMPERATURE (°F)


              Figure 41:  Temperature of pipe as' related to working pressure.
                                      92

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The thermal conductivity of PVC is approximately 0.08 Btu ft/hr ft2 °F
compared to 118 for aluminum and 30 for iron.  Calculations indicate that
there should be a 26°F temperature drop across the wall of buried
Schedule 40 PVC pipe that carries water at 100°F.  In comparison, there
is less than a 0.1°F drop across the wall of the aluminum or galvanized
steel pipe.

Aluminum suppliers recommend a soil analysis before considering the use
of aluminum pipe.  Some types of soil (cinders, mine wastes, and others)
are specifically not suitable for the burial of bare aluminum pipe.
Cathodic protection may be required in soils that have a specific elec-
trical resistance lower than 1500 ohm cm.  Alclad aluminum pipe does,
however, provide its own cathodic protection for soil burial conditions.
Alclad pipe is 6061 aluminum pipe with a 5 percent thick cladding of
high purity aluminum containing 1 percent zinc.  Aluminum piping can be
either joined by Swage-Bond Process or welded.

Zinc-clad steel pipe is the only type extensively used for underground
applications.  However, even galvanized pipe will deteriorate rapidly  in
some soils and galvanic protection may be necessary for long service life.

Unit material and installation costs for 2-1/2 in. diameter pipe are
approximately $2.20, $1.80, and $0.68 per ft respectively for aluminum,
galvanized steel, and PVC used in an agricultural or farming type in-
stallation.  Aluminum and galvanized pipe are most attractive from the
standpoint of heat transfer.  However, the extreme differences in require-
ments for corrosion control in different soil areas is a problem for
standardizing a system.  Therefore, in order to standardize on a workable
system for all soil conditions and to minimize the captial investment,
PVC was chosen for the demonstration plots.

Heat Transfer
The design basis giving no more than 2°F variation in soil surface
temperature required a grid system of pipes 24 in. below the surface and

                                 93

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5 ft apart (Figures 42 and 43).  The heat transfer from each pipe was
calculated from the following heat transfer equation for the steady trans-
fer of heat from buried isothermal heat sources to the air:
where:
                                 D4-II
          <  =  Heat Flow. (hr)(ft of p1-pe)
          tw =  Water Temp., (°F)

          tA =  Air Temp., (°F)
          Rn =  Heat Transfer Resistance, (nr)(ftH°F)
           0                                  Btu
The overall heat transfer resistance (R )  can be subdivided into the
following individual resistances:
          R    =  Pipe wall resistance
          RS   =  Soil resistance
          R    =  Soil -air interface resistance
The pipe wall resistance, R  , is calculated from the equation:
                           pw
where:
          X   =  Wall thickness, (ft)
          AL  =  Log Mean Area of Pipe Wall, (ft2)
          K   =  Thermal conductivity of pipe wall,   (Btu)(ft)	
                                                     (ft*)(hr)(°F)
                                 94

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01
                                 spacing  between  pipes




               Figure 42.  Undersoil  pipe  grid.

-------
                    90_
1C
                 s_
                 OJ
                 o
                 I/)
                    60-
                    50-
                    40
10          15           20

         Soil  Depth (inches)
                  Figure 43.   Soil  temperature vs.  soil  depth.
                                                                                    I
                                                                                    25
  Air Tenperature - 35°F

  Soil K = 1 Btu"ft

             Hr-ftz°F
30

-------
The resistance of the soil, Rg, is calculated from the following equation
for a horizontal cylinder of length L  (ft) and diameter D (ft) with axis
at distance Z (ft) below the surface:
          R   .   _i_    ,„   ,_«_,
           5       2irl_K            D
          k  =  Thermal conductivity of soil  -   Btu ft
                                                  ft2 hr °F

The soil-air heat transfer resistance is inversely related to the sum of
the natural convection film coefficient (h ) and the radiation coeffi-
cient (h ) multiplied by the Area  (Acfl) of the soil-air interface.
        i                           oA
                      R
                      K-n
                                    hr> ASA
where:

                                °F hr-ft
                      RSA
                                  Btu
                                    Btu
                       r     ^,
                       c     r     hr ft2 °F

                      A    =  ft2
                      ASA      rt

The area  (A-J  1s eclual to tne surface area of the heated plot, that is
the length  (L)  and width of  the soil air interface.

The natural convection film  coefficient (h  )  is calculated from the fol-
                                          L*
lowing relationship:

                      hr  =  0.27 (t/L)°-25
                       L»

where:
          t  =  differential temperature between  soil  and air  - °F

                                 97

-------
The radiation coefficient (h ) is calculated from the following rela-
tionship:

                           (T  )**     (T )4
                 0.173 el
                            100        100
          \	r—f	
                          'SA     'A
          BI  =  Emmissivity of the soil  surface at Tj

          TS« =  Absolute temperature of soil  surface in °R
          T.  =  Absolute temperature of air °R

Sizing of pipe within the grid must be determined within these para-
meters:  seed germination occurring at 53 to 59°F, pipe carrying 100°F
water, and pipe burial 24 in. below soil  surface.

Assuming a soil-air interface temperature (tSA), the heat flux was cal-
culated.  The calculated heat flux was then substituted in the following
two equations to prove the assumption:
          q  ,        *SA                         q   =   *SA - 35
                   RS                                     RSA
The temperature of the soil vs depth and their relationship to effluent
water temperature is shown on Figure 43.

Utilizing a 2-1/2 in. diameter pipe (Figure 44)  grid system with parallel
pipes spaced at 5 ft centers (Figure 45) containing 100°F effluent water,
the soil-air interface temperature would be 45°F (Figure 46).   The soil-
air interface temperature, however, between and  above the pipes would be
44°F.
                                 98

-------

                                                                               :-
Figure 44.   Grid layout for soil heating study

-------

Figure 45.   Installation of underground pipe grid system for soil
            warming study

-------
                                                                45°F Soil-Air Interface
                                                	j/	  Temperature
                                               >7///////yf//////
Figure 46.  Soil-Air Interface Temperature Variation.   100°F effluent water  in PVC pipe.

-------
                    Soil  Heating Literature Survey

1.   L.  L.  Boersma.   "Nuclear Waste  Heat  Could  Turn Fields  into  Hotbeds,"
    Crops  & Soils  Magazine,  Vol.  22,  No.  7,  pp.  15 and  16.   April-May  1970.

2.   A.  S.  King.   "Irrigation-Nuclear  Power-Partners  in  the Future?"  Oregon
    Farmer, Vol.  93, No.  2;  pp.  7 and 8.   January 15, 1970.

3.   "New Sources  of Heating  for  Agriculture,"   Canner/Packer, pp.  41 and
    42.  July 1969.

4.   J.  R.  Barrett,  Jr.,  et al.   "Commercial  Electric Turf  Heating,"
    (abstract), Agricultural  Engineering,  Vol.  50,  p.  363.  January 1969.

5.   J.  Bornstein,  et al.   "Insulated  Soil-Heating System to Prevent  Forest
    Heaving of Field Instrumentation," Journal  of Agricultural  Engineer-
    ing Research,   Vol.  14,  pp.  100-103.   May  1969.

6.   D.  F.  Greenland.  "Soil  Heat Flow Investigations at Cass, S.  Island
    High Country,11  New Zealand Journal of Agricultural  Research,  Vol.  12,
    pp. 352-66.   May 1969.

7.   J.  M.  Walker.   "One Degree  Increments in Soil Temperature Effects  on
    Maize Seedling Behavior,"  Proceedings of the Soil Science Society
    Vol. 33, pp.  729-36.   September 1969.

8.   D.  K.  Cassel.   "Soil-Water Movement  in Response to  Imposed  Temperature
    Gradients,"  Proceedings  of  the  Soil  Science Society, Vol. 33, pp.  493-
    500.  July 1969.

9.   N.  H.  MacLeod and A.  M.  Decker.  "Temperature Control  of Soil in Field
    Plots:  Equipment Design," Agronomy  Journal,  Vol.  60, pp.  444-5.
    July 1968.
                                102

-------
10.   H. Robinette.  "Electrically Heated Hotbed,"  Horticulture, Vol.  47,
     pp. 26-7.   March 1969.

11.   J. R. Barrett and W. H. Daniel.  "Turf Heating with Electrical  Cables,"
     Agricultural Engineering, Vol. 47, pp. 526-9.   October 1966.

12.   M. G. Cropsey.  "Analysis of Soil as a Heat Source for a Heat Pump
     Systern,"  Transactions of the American Society of Agricultural  Engineers,
     Vol. 9, No. 6, pp. 846-8.  1966.

13.   J. R. Gingrich.  "Low Cost Method for Maintaining Constant Soil
     Temperatures in the Greenhouse," Agronomy Journal.  Vol. 57,
     pp. 316-317.  May 1965.,

14.   A. R. Mack and W. A. Evans,  "Soil Temperature Control Systems  for
     Field Plots," Canadian Journal of Soil Science, Vol. 45, pp.  105-7.
     February 1965.

15.   A. W. Dimock.  "A Soil Temperature System Employing Air as the  Heat-
     Transfer Medium" Plant Disease Reporter.  Vol. 51, No. 10, pp.  873-76.
                                103

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GENERAL PROCEDURE

The thermal water soil heating system was completed and installed in
early May 1971.  Figure 47 is a schematic of the project site and shows
the locations of the two blocks of heated soil.   The smaller heated
block was 510 ft x 60 ft.  A small adjacent area served as  a check block.
The large heated block was 120 ft x 470 ft with  a 60 ft x 470 ft plot
on the north and south of the heated block reserved for control, plots.
The system consisted of a grid work of 2-1/2 in. diameter black poly-
vinylchloride (PVC) pipe buried about 26 in. deep and 60 in. centers
(Figure 47).  The PVC pipes of the larger block  were connected to a
6 in. diameter steel inlet and outlet manifold;  PVC pipes of the smaller
heated block were connected to 4 in. diameter steel inlet and outlet
manifolds.  About 350 and 100 gpm of thermal water were pumped through
the large and small blocks, respectively.  All heater soil  temperatures
referred to in this report were from the large heated block.

Although the soil heat grids were completed for  the 1971 growing season,
there was no thermal water because of a labor strike at the Weyerhaeuser
plant that started in the spring and lasted through mid-summer.  Thus,
the first data on soil temperatures and crop responses were collected in
1972.

Platinum bulb temperature sensors connected to chart-type recorders
were placed in tomato rows on black plastic mulched and non-mulched
plots split between heated and non-heated soil during the 1972 growing
season.  Temperature sensors on heated soil were placed at  1, 6, 12, and
24 in. depths in a vertical line above and halfway between  buried heat
pipes (Figure 48).  Temperature probes were also placed in  non-heated
control plots at 1, 6, 12, and 24 in. depths.
                                104

-------
                                            I    ,  pw,.,,.
                                            U-  *S .- -I


                                            ^- k-VHlSEHSfrJIJ.U^CIM^
Figure 47.   Undersoil heating with greenhouse  location — plot plan and details

-------
      soil surface
 Thermal Water
        Pipe
O
                                         1 inch •$-


                                         6 inch -$-



                                        12 inch -$-


                                                        Temperature Probes
24 inch •$-                           -$-
        O<	2-1/2-	H                             O
 Figure 48.  Placement of temperature sensors in relationship to buried thermal water heat lines and soil surface.

-------
RECORDED SOIL TEMPERATURES

Soil  temperatures are influenced by changing solar load and related air
temperatures.  Temperatures of non-heated soil  at 6, 12, and 24 in. are
shown in Figure 49.  As would be expected, 6 in. depth temperatures
averaged somewhat warmer than 12 and 24 in. depth temperatures during
mid-summer and averaged cooler than 12 and 24 in. depths during the
remainder of the year.  Although it is not shown in Figure 49, the
diurnal temperature fluctuation at the 6 in. depth was greater than at
the deeper recorded levels.
                                               •i.
During June, July, August, and the first part of September 1972, soil
temperatures at the 1 in. depth were not influenced by the thermal  water
grid.  During the spring, fall, and winter months, mean weekly 1 in.
depth soil temperatures of the heated area ranged from .5 to about 4°F
warmer than non-heated soil.
              =                  '          .:•                 s
Temperatures at the 6, 12, and 24 in. depths,,were modified by the thermal
water circulated through the buried soil heat grid, but temperatures
were not uniform for any given depth in a horizontal line across the soil
heat grid.  Soil farthest from the .pipes at any;given depth:was cooler
than soil closer to the heat lines.  The coolest soil at any given depth
in the heated blocks was mid-way between the heat lines that were buried
on 5 ft centers (Figure 48).  As was the case with non-heated soil,
temperatures of heated soil were warmer during mid-summer than during  the
rest of the year.

The warmest 6nn. depth soil temperature, recorded in a vertical line
above the buried heat line, averaged 4.8°F warmer than unheated 6 in.
depth soil temperature for January 1972 through March 1973 (Figure 50).
The coolest 6 in. depth soil temperatures recorded mid-way between
buried heat lines in the heated area averaged 2.8°F warmer than the un-
                         j,'
heated 6 in. depth soil temperature for the same period of time (Fig-
ure 50).  During the warmest part of the growing season from June 22
                                107

-------
          75-
          70
          45-
                           6 Inch depth
                           12 inch depth
                           24 inr.h di;pth
                          . — -.^.u
          35
              —I—
               3
              Jan
 7
Feb
—I—
  1
 Mar
—i	:—r—
  5          3
 Apr  1972  May
 7
Jun
 5
Jul
 2
AuS
 6
Sep
Figure 49.  Hem weekly 6, 12. and 24 Inch depth soil temperatures of non-heated control plots:  January 1972 - March 1973.
  4
 Oct
1972
 1
Nov
 6
Dec
 3
Jan
    7
   FeS
1973
 1
Mar

-------
   75-
   70-
i5"1
   60-
£  55-
   50-
                    Above burled heat pipes
                    Halfway between burled heat pipes
                    Control - no ^oll heat
                    Ho records	
 7          S          2
Jun        Jul         Aug
                                                                                                             flow of thermal
                                                                                                             ter Interrupted
                       1
                      Feb
 1
Mar
 5          3
Apr        Hay
      1972
 6
Sep
                                                                                                               1972
 I          i—
 4          1
Oct        Nov
 6
Dec
—I—
  3
 Jan
                                                                                                                                                                 1973
                                                                                                                               son

-------
through August 9, there was little temperature difference between
heated and non-heated soil at the 6 in.  depth.

Temperatures of heated soil at the 12 in.  depth were closer to those of
heat lines, and heated soil temperatures were modified relatively more
than 6 in. depth temperatures.  The greatest temperature difference be-
tween 12 in. depth non-heated and heated soil averaged 7.8°F for the
recorded periods between January 1972 and  March 1973 (Figure 51); the
least difference averaged 3.4°F.  From June 28 through August 2, 1972,
there was little difference in non-heated  soil and the coolest soil  in
the heated block at the 12 in. depth (Figure 51).   The warmest soil  in
the heated block averaged 6.7°F warmer than non-heated soil  during the
same June 28 through .August 2 period.     '.-.

The greatest difference between heated and non-heated soil  occurred at
the 24 in. depth, closest to the heat lines that were buried at about
26 in.  The average temperature difference at 24 in. depth  between the
coolest soil in the heated block at a 24 in. depth and the  24 in. depth
in the non-heated soil was 8.4°F (Figure 52).
                    v.,                                   't.:   I
                                                   *,     •' '
THE INFLUENCE OF SOIL HEAT ON SELECTED PLANTS     ,  '*

Although it is known that yields of rice and greenhouse,crops are
affected by low rootvzone temperature, little is known about the effect
                                                ?
of soil temperature: on production of most  crops.  Low temperature irri-
gation water that in'turn cools the soil is considered to be an important
limiting factor in Japanese rice production, and when cold  water from
Shasta Dam was first used to irrigate rice in northern California, the
rice would not mature in time for harvest.28  When cold water irrigation
caused soil  temperature to drop below 59°F, greenhouse cucumber plants
ceased to grow and were-damaged.29  Soil temperature lower  than optimum
for crops of tropical origin may well occur in the field during the
growing season.             '"
                                110

-------
    804
     75-
             O Above burled heat pipes
             ^. HalftKy between burled heat nines
             • Conti-ol - no sol! Nut
          —-— No  records
     65
 -   60-
     55-
 5  50
Figure 51.
                                                                                                                                                                               1573
        on of mean weekly 12  Inch depth soil temperatures recorded «t two locations In heated soil with non-heated  tall:  the heated sotl was wanned by circulattnp thcnral water th-o^-i
Z-l/2 Inch diameter plastic pipes burled  26  Inches and spaced 5 ft apart.

-------
  100-


   95-


   90


   85


*  SC
u
c

•a-  75-
t
2  65
   50-
   4S-
   40-
             Directly above buried heat pipes
             Halfway between burled heat pipes
             Control - no soil  heat
             No records
                                                                                                                          —T—
                                                                                                                            4
                                                                                                                           Oct
 3
Jan
 >
Feb
 1
Mar
                                                                                                                                       Nov
—i—
  6
 Dec
 3
Jan
 7
Feb
                         1
                                                      S          T             7           r         2              6
                                                     Apr         May            Jun         Jul         Aug            Sep
                                                           1972               .                                                                      1972
Ffojre 52.  Comparison of mean weekly 24 Inch depth soil temperatures recorded at  two locations In  heated  soil with non-heated soil:  the heated soil was wanned by circulating thermal water through

            2-1/2 Inch diameter plastic pipes burled 26 Inches and spaced 5 ft apart.
 ro

-------
Small changes in soil temperature can cause large differences in growth
of many woody plants, and the roots of these plants may function only in
a narrow range of soil temperatures.30  For example, Lonicera cv. Zabel
and Wei gel a cv. Ferrie produce good root growth over a wide range of
temperature (54-90°F), while Physocarpus opulifolius v. nanus and Ribes
alpinum had narrower optimum soil temperature ranges, 62.5-79°F and
66-80.5°F, respectively.31  Although plant shoots depend upon roots for
water and nutrients, the same soil temperature may affect the develop-
ment of shoots and roots differently.  Generally, soil temperatures
that produce the most shoot growth are higher than soil temperatures
needed to produce the greatest root growth.31  Roots produced at rela-
tively low soil temperatures were whiter, more succulent, thicker, and
had fewer lateral roots than roots produced at relatively higher tem-
peratures.

Water use by plants is also influenced by soil  temperature.   Generally,
the use of water increases as the soil temperature increases.31

The detailed effects of soil temperature on plant growth and development
probably can be determined only in controlled experiments where  specific
plant shoot and root conditions are maintained.  Any field studies with
soil heat are complicated by:  1) variable field conditions, 2)  changing
environmental factors that influence soil temperature throughout a grow-
ing season, and 3) soil temperature variations through the root  zone.

Another complicating factor is that crops in these studies had dif-
ferent genetic backgrounds and indigenous habitats and probably  did not
require the same root temperature for optimum growth.  Also, when a
commercial source of thermal water is used, the temperature will probably
fluctuate (Figure 3) and will not be under complete control  of the
agriculturist.

Therefore, the results of these studies with the selected crops  reflect
all  of the above variables.  When detailed information becomes available
                                113

-------
on optimum root zone temperature for different crops, some facet of
these studies might be changed to alter results for individual crops.

The greatest variation in soil temperature within the heated block it-
self also occurred at the 24 in. depth where the warmest soil averaged
17.4°F warmer than the coolest soil (Figure 52).  At depths closer to
                                                                i
the soil surface and further from the heat lines, temperature variations
were less in a horizontal line than at the 24 in. depth.  Temperature
differences between warmest and coolest heated soil  at 12 and 6 in.
depth averaged 4.3 and 1.6°F, respectively (Figures  51 and 50).  Gener-
ally, the greatest soil temperature variation at any given depth in  the
heated block occurred during the cooler months and the least variation
occurred during the summer months.

The mean weekly temperatures depicted in Figures 50, 51, and 52 for
heated soil are the products of solar input, related ambient air tempera-
ture, other, less well defined environmental factors, and the temperature
of thermal water passed through the soil heat grid.

As can be seen in the various Figures, no constant soil  or air tempera-
tures were maintained.  The thermal water was used as it was supplied
and probably represents a realistic view of what might be expected with
a larger installation that relied on industrial waste thermal water.
Any crop responses to soil heat that are discussed later in this section
were modified or not modified by the sum total of heat differences
shown in Figures 50, 51, and 52.

Although no actual measurement of temperature drop across the wall of
buried PVC pipe were made, temperature sensors were  placed about 1-1/2
to 2 in. directly above the heat lines.  An average  of 13.2°F tempera-
ture drop occurred between the thermal water as it entered the buried
pipes and the temperature recorded about 1-1/2 to 2  in.  from the outside
of the pipe (Figure 53).  This temperature drop was  greater from July 12
through September 6 than during late September through November (Fig. 53).
                                114

-------
en
        
-------
The greater temperature drop during mid-summer probably was due to a
reduction in soil moisture around the pipes, resulting in reduced heat
transfer.

Tomatoes

Procedure—Ferti 1 izer (1000 Ib 10-20-20/acre) was broadcast and incor-
porated with a rototiller into the area for tomatoes on May 4,  1972.

Thermal water heated and non-heated soil were compared as main  plots
and replicated twice.  Sub-plots consisted of 4 mil  black plastic film
mulched and non-mulched rows.  Tomato cvs. Fire ball and Willamette
were transplanted into the field during May 9 through 11, 1972, on
2 x 4 ft spacings.  Each plant received 1 pt of 9-45-15 fertilizer
mixed at the rate of 1 oz material per gal water.

Delmhorst soil moisture blocks were installed in black plastic  mulched
and non-mulched plots on heated and non-heated soil  during June 1972.
Moisture blocks on heated soil were placed in tomato rows at 6, 12, 24,
and 30 in. depths in a vertical line with and halfway between buried
heat pipes (Figure 54).  Moisture blocks were placed at the same depths
in non-heated control plots.  Thermal water applied  through sprinklers
was used for all irrigations.

The first mature leaf down from the plant tip was taken for nutrient
analyses from 12 plants per plot on June 22, 1972.   Tomato plants were
in early bloom.  Chemical composition was determined by Oregon  State
University Soil Analyses Laboratory.

The herbicide "Enide" was applied at the rate of 6  Ibs active per acre
on June 28.  "Diazinon" insecticide was applied to  tomato foliage at
.25 Ibs active per acre for aphid control.  "Sevin"  insecticide was
applied on July 25 and August 2 at rate of 1 Ib active per acre.  The
fungicide "Maneb" at 3 Ibs per acre was applied on  August 2 and 26, 1972,
to check Early Blight development.

                                116

-------
         soil surface
6 inch -f +
12 inch -f -f
w -
Thermal Water
Pipe ,
^ 24 inch -<
0 C
Moisture Blocks
or
Tensiometer Placement ,
c -4-
<^ ?-!/?' ^^1 ^)
^ \if _., ^.j \^
30 inch + +
1 _^_ A c' ^^
I^-'V ' >
^T 5' thJ
^ 5 1^|
Figure 54.  Placement of soil moisture sensors in relationship to buried thermal water  heat lines  and  soil  surface.

-------
The middle 20 ft of each plot were harvested four times between August 26
and October 20, 1972.  Fruit from each plot were weighed,  counted, and
classed as U.S. No. 1 and No. 2 canning32 and culls.

Results and Discussion—The nutrient level  data for tomatoes were not
statistically analyzed, but plants from soil heated plots  tended to have
more N, P, K, Ca, Mg, and Zn than plants from non-heated plots (Table 7).
Mn was the exception; plants from soil heated plots tended to have less
Mn than control plants.  In general, these  trends are in agreement with
other findings.33"37  The lower Mn in plants from soil  heated plots is in
contrast to studies with strawberries38 where Mn was  decreased by lower
soil temperature.
                                                                  - r*-'' .•-; - '' -
Soil heat did not influence tomato yields in this study (Table 8).
Black plastic mulch increased yield of No.  1 'Fireball'  fruit, but did
not significantly affect yield of 'Willamette.1   There  was no inter-
action between the plastic mulch and soil heat or control  plots.

Although soil heating has increased tomato  yields by  50 percent,39
yield of 'Fireball' and 'Willamette' tomatoes was not increased by soil
heating during 1972 in this trial.  Differences  in location of test
sites, growing seasons, time of planting, and type and  placement of soil
heating equipment probably contributed to lack of yield response at the
project site in 1972.

Sweet Corn

Procedure—The area for sweet corn was fertilized with  96  Ib N and
130 Ib P per acre in 1 ft wide bands spaced on 4 ft centers on June 1972.
The fertilizers were incorporated into the  soil  with  a  rototiller.
Sweet corn cv. Jubilee was seeded with a Planet Jr. planter into the
fertilized bands on June 13, 1972.  In-row  spacing of plants averaged
about 10 in.  apart.  Rows were 4 ft apart.
                                118

-------
Table 7.  NUTRIENT LEVELS (DRY WT BASIS) IN TOMATO LEAVES OF 'FIREBALL'
           AND 'WILLAMETTE'  FROM SOIL HEATED AND CONTROL PLOTS

                       Nutrient Level - Dry Vit Basis
               Total N,   P,     K,     Ca,    Mg,    Zn,      Mn,
 Treatment        %       %_     %_     _%_     %     ppm      ppm
Fireball:
  Soil heat      4.59   0.57    3.78  0.43   0.96     37.5   59.0
  Control        4.56   0.51    3.62  0.41   0.94     33.0   75.7

Willamette:
  Soil heat      4.70   0.65    4.13  0.39   0.82     42.0   55.5
  Control        4.61   0.58    4,01  0.33   0.80     34.5   65.5
                                119

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ro
o
         Table 8.  EFFECTS OF SOIL HEAT AND BLACK PLASTIC 4-MIL FILM MULCH ON YIELD OF 'FIREBALL'  AND


                                              'WILLAMETTE'  TOMATOES2
U.S. Canning Grades
Fireball
Soil heat
Control
Mulch
No-mulch
Willamette
Soil heat
Control
Mulch
No-mulch
No
Tons/Acre
39.7
42.3
46. 4a
35. 7b

57.5
55.2
52.9
59.8
. 1
Avg. fruit
wt, Ibs,
.22
,24
.23
.24

.33
.31
.32
.32
No. 2
Avg
Tons/Acre wt
13.7
13.7
13.9
13.6

12.5
10.4
11.2
11.7

. fruit
, Ibs
.21
.23
.21
.23

.32
.30
.32
.30
Cull and rotten
Avg.
Tons/Acre wt,
16.0
14.0
14.4
15.6

18.8
17.9
19.6
17.2
fruit
fruit
Ibs
20
21
20
21

27
24
26
24
         zMeans within a column in each series followed by different letters differ significantly

          at 5% level.

-------
'Jubilee' was planted in soil heated and non-heated blocks (2 rows per
plot, 30 ft long) and replicated four times.  Thermal water applied
through sprinklers was used for all irrigations.

Leaf samples were taken from corn plants that had just started to pro-
duce tassels in each plot on August 16, 1972.  Samples consisted of
leaf sections about 10 in. long taken from the mid-section of middle
aged leaves.  The samples from Replications 1 and 2 were combined and
3 and 4 were combined before they were analyzed for P, K, Ca, Mg, Zn,
Mn, and total N by Oregon State University's soil testing laboratory.

The number of immature ears less than 3 in. in length and ears between
3 and 6 in. long were counted on August 21, 1972, to determine if soil
heat hastened early development.

Corn plots were harvested September 18 through 20, 1972.  The fresh
weight and number of ungraded, graded, and immature ears were recorded.
Plant height and weight also were recorded.

A 20 ft section of row was harvested from the center of each  plot
September 18 through 20, 1972.  Fresh plant and ear weights were recorded
and ears were husked and graded (Table 9.)

Results and Discussion—Nutrient uptake trends for selected elements are
shown in Table 10.  Only two samples were analyzed per treatment for each
element, so the data was not statistically analyzed.  However, the re-
sults are similar to other findings.  Less N was taken up by  corn on
cooler control soil than on heated soil (Table 10).  N levels in shoots
have been reported to decrease as root temperature decreases  in chry-
santhemums33 and strawberries.40  The lower P levels associated with the
lower soil temperature control, plots parallel findings of Knoll35 on
corn.  K and Ca uptake was not altered much by soil heat.  Mg in corn
has been observed to increase with warmer soil temperatures37 and was
increased by soil heating.  Zn uptake was not influenced by soil heat, but
Mn uptake was increased by soil heat as occurred with chrysanthemums.33

                                121

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    Table 9.  YIELD OF SWEET CORN, CV.  JUBILEE,  HARVESTED SEPTEMBER  18 THROUGH 20, 1972, FROM THERMAL



                                      WATER HEATED AND NON-HEATED SOIL2
ro
Soil heat
Control
Ungraded ears
with husks
Doz./A Tons/A
l,859a 7.4a
l,368,b 5.8b
Graded ears
minus husks
Doz./A Tons /A
l,473a 5.0a
l,196b. 3.9b
Immature ears
Doz./A Tons /A
387 a 0.3 a
169b 0.2 a
Plant wt.
minus ears
Tons /A
3.4,a
3.5a
Average
plant
Heiqht-ft
8.8a
8.4a
    Within one vertical column, values followed by different letters differ at the  5%  level.

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Table 10.  NUTRIENT LEVELS (DRY WT BASIS) IN LEAVES OF SWEET CORN



               FROM SOIL HEATED AND CONTROL PLOTS
Nutrient Level -Dry Wt Basis
Total-N,
Treatment %
Soil heat 3.52
Control 3.33
P, K, Ca, Mg, Zn, Mn,
% % % % ppm ppm
0.42 2.68 0.08 0.33 41.5 77.5
0.32 2.57 0.07 0.25 42.0 61.5
                               123

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Sweet corn on heated soil was visually larger than on non-heated soil
on July 20, 1972 (Figure 55), and early ear development was stimulated
by soil heat (Table 11).  The soil heated plots averaged 72 percent more
ears between 3 and 6 in. than control  plots on August 21, 1972.   There
was no difference in the number of ears less than 3 in. between  soil
heated and control plots.

At harvest, the weight of ungraded, graded, and immature ears  was in-
creased by 28, 35, and 50 percent, respectively, compared to production
from control plots (Table 9).  On a number basis, ungraded, graded, and
immature ears were increased by 36, 23, and 129 percent by heated soil
when compared to control plot production.

Overall, soil heated plots produced more but slightly smaller  ears
(.66 Ib per ear from soil heat vs .70  Ib per ear from control) than
the controls.  There also was little difference in average ear weight
of graded ears from soil heated and control plots (.56 Ib per  ear from
soil heat vs .54 Ib per ear from control).

More immature ears were formed on heated soil  than on control  plots but
the ears did not develop, and there was little difference in weight of
immature ears at harvest (Table 9).

Most of the difference in size of corn plants  between soil  heated and
control blocks that was noted in July  (Figure  55) was not apparent at
harvest.  There was little difference  in average height and weight of
plants from heated and control plots on September 20, 1972 (Table 9).
Asparagus Crown Planting

Procedure—Fertilizer was broadcast at the rate of 300  Ib  16-20-0,  88 Ib
P, and 40 Ib K per acre on the area for asparagus  crowns.   "Diazinon"
insecticide was applied at the rate of 9.8 Ib  active material  per acre
for Symphlan and wire-worm control.  Fertilizers and insecticide were
rototilled into the soil.
                                124

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                   Soil  Heat
Control
Figure 55:   Sweet corn 'Jubilee'  growing on soil  heated by thermal  water and  on
            non-heated soil—July 20, 1972.

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Table 11.  EFFECT OF SOIL HEAT ON EARLY SWEET CORN EAR DEVELOPMENT,  CV.

                JUBILEE; SAMPLES TAKEN AUGUST 21,  1972



                                                                    •  ',
                            Average Number of Ears/Plant
Treatment
Soil Heat
Control
Total ears
per plant
1.09a
0.70b
Less than
3" length
0.26a
0.2Ta
Between 3" and
6" length
Q.83a
0.48b
Within one vertical  column,  values  followed  by  different  letters  differ
at the 5% level.
                                126

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Asparagus crowns, cv. 500-W, were transplanted into single-row plots
4 ft apart and 40 ft long (4 replications) in blocks of heater and non-
heated soil on May 5, 1972.  Crowns were placed 6 in. apart in furrows
8 in. deep and initially covered with about 4 in. of soil.  By June 1,
a good stand of asparagus was established and the crowns were covered
with an additional 4 in. of soil.

Asparagus ferns were cut off at ground level on three random 10 ft row
sections from heated and non-heated soil blocks and weighed on Septem-
ber 27, 1972.  The fern and stalks were brown and dry at time of cutting.

Although,asparagus spears are not usually cut the second season after
crown transplanting, a single harvest was made on April  12, 1973.  The
new asparagus spears from the middle 10 ft of each plot were cut off at
ground level, counted, and weighed.

Two year old asparagus crowns from 10 ft row sections in each plot were
dug, counted, and weighed on April 30, 1973.


Results and Discussion—The first asparagus spears emerged May 10, 1972.
Initial spear emergence and subsequent growth appeared to be more rapid
on heated soil than on control blocks.  By October 1972, crowns in
heated soil appeared to have produced about 50 percent more fern growth
than crowns in control soil (Figure 56).  Asparagus fern on control plots
was about 2 ft in height while fern on heated soil was at least 3 ft
tall on October 4, 1972.

The weight of asparagus fern and stalks cut in September from soil
heated plots averaged 95 percent more than from the control blocks
(Table 12).

Early spring production of asparagus spears was stimulated by soil heat.
On the harvest of April 12, 1973, the soil heated plots yielded 44 and
                                127

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f 3
00




•1






,




I

SprfU
,
i.

         Figure 56:  Comparison of first year asparagus fern growth of '500-W on control soil (left) and

                    on heated soil (right); pictures taken October 4, 1972.

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Table 12.  WEIGHT OF ASPARAGUS FERN AND STALKS PRODUCED ON SOIL HEATED

         AND NON-HEATED PLOTS; SAMPLES CUT SEPTEMBER 27, 1972Z
                   Average no. crowns            Avg. wt (g) of fern and
Treatment       per 10 ft of row sampled         stalks per 10 ft of row
Soil heat
Control
13.6
13.6
1,581
810
zMeans within columns followed by different letter differ significantly
 at 5% level - Duncan's Multiple Range Test.
                               129

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98 percent more asparagus spears than control plots based on number and
weight, respectively (Table 13).

Two-year-old asparagus crowns were dug from heated and control  plots in
April 1973.  The greater asparagus fern growth produced during  the 1972
growing season on heated soil plots apparently resulted in larger crowns,
Heated soil produced crowns that averaged about 40 percent larger than
crowns from control areas (Table 14).  The larger crowns should even-
tually produce greater yields of asparagus, but only prolonged  experi-
ments will determine the effect of heated soil on long-term asparagus
yields.


Asparagus Nursery

Procedure^--Fertilizer was broadcast at the rate of 300 Ib 16-20-0 and
88 Ib P per acre to the area for the asparagus nursery.  'Diazinon1  was
applied at the rate of 9.8 Ib active material per acre.  Fertilizer
and insecticide were incorporated into the soil with a rototiller.

Asparagus seeds of cv. Mary Washington were planted about 2 in. apart
with a Planet-Jr. seeder in rows 4 ft apart in soil heated and  non-
heated blocks on June 13, 1972.  Each plot consisted of a single row
and was replicated four times.

The crowns were dug, counted, and weighed from the middle 10 ft of row
in each plot on April 5, 1973.
Results and Discussion—The production of 1  yr old asparagus crowns was
not influenced by soil heat (Table 15).

The roots of the 1 yr old crowns were relatively shallow.   The soil heat
grid has least effect in the soil surface layers.  Therefore, there may
not have been much difference in soil temperature between  heated and
                                130

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Table 13.  NUMBER AND WEIGHT OF FIRST HARVESTED ASPARAGUS SPEARS (APRIL

12, 1973) FROM 2 YEAR OLD CROWNS PLANTED IN HEATED AND NON-HEATED SOIL2
                        Avg. no. spears                Avg. wt (g)
Treatment                per 10 ft plot               per 10 ft plot


Soil heat                    41.2a                        3,420a

Control                      28.5b                       17,206b
zMeans within columns followed by different letter differ significantly
 at 5% level - Duncan's Multiple Range Test.
                                131

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Table 14.  EFFECT OF SOIL HEAT ON WEIGHT OF 2  YEAR OLD ASPARAGUS  CROWNS2

                              APRIL 1973
                                            Avg.  wt/crown
               Treatment                        -Ibs
               Soil  heat                       0.69a

               Control                          0.49b
 zMeans followed by different letters  differ  significantly  at  5%  level.
                               132

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Table 15.  WEIGHT AND NUMBER OF ONE YEAR OLD ASPARAGUS CROWNS PRODUCED
                   ON HEATED AND NON-HEATED SOIL
         Treatment
         Soil heat
         Control
1 year old asparagus crown/plot
       Average   Average
        wt. g     number
         692
         778
52
52
                               133

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non-heated soil in the root zone of the asparagus crowns.  Crown produc-
tion might have been modified if different soil  temperatures had been
maintained.
Rhododendrons

Procedure--The following six cultivars of rhododendrons were planted in
soil heated and non-heated control areas during the first two weeks of
July 1971:  'Vulcan,1 'Jean Marie,1  'Fastausum Plena,'  'Lord Roberts,1
'Anna Krusckka,1 and 'Old Port.1

Prior to transplanting, about 2 in.  of sawdust and hemlock bark were in-
corporated 6 to 8 in.: into the soil.  The sawdust and bark were used to
improve the water holding capacity of the soil and to form the lighter
root ball required for plants dug for shipment.

Measurements of plant growth were made about one year after transplanting
on July 19, 1972.  Height was measured from soil surface to bud tips on
four axes per plant.  The maximum and minimum plant spreads were measured
on the same plants that were used for height determinations.  The cultivar
blocks of rhododendrons on heated and control soil were not replicated, so
height and spread measurements were made on 10 random plants per variety
from heated and control soil blocks.  The average values are in Tables  16
and 17.

Height and spread measurements were taken again on November 14 at the end
of the 1972 growing season.

Results and Discussion—Plants of most cultivars from soil heated blocks
were generally larger than from control  blocks on July 19, 1972.  How-
ever, some varieties did not respond as  much to soil heat as others.
'Old Port1  and 'Lord Roberts' responded  least to heated soil (Table 16).
Height of 'Old Port' was not influenced  by soil heat, but maximum and
                                134

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CO
     Table 16.   GROWTH,  PLANT HEIGHT AND SPREAD,  OF RHODODENDRONS  PRODUCED ON HEATED AND NON-HEATED SOIL-

                                       MEASUREMENTS MADE  ON  JULY 19,  1972
Average plant
height-inches2
Vulcan
Jean Marie
Fastousum Plena
Lord Roberts
Anna Krusckka
Old Port
Check
10.1
7.1
10.9
10.7
9.3
11.5
Soil
11
10
13
11
10
11
heat
.8
.1
.4
.2
.1
.5
% height
increase of
soil heated
plants
over checks
17
42
23
5
9
0
Average plant
Check
Max
11.
7.
10.
11.
10.
11.
•
4
7
5
8
6
4
Min.
8.7
5.6
6.5
8.4
8.2
9.5
spread- inches
Soil heat
Max.
13.6
10.6
12.6
12.0
12.5
12.8
Min.
11.3
7.9
9.7
8.9
9.8
10.0
% increase of soil
heated plants
over checks
In max.
Spread
19
38
20
2
18
12
In min.
Spread
30
41
49
6
19
5
     zHeight measurements from 4 axes/plant (average of 10 plants)  from which maximum and minimum measure-
      ments were taken.

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co
      Table  17.   GROWTH,  PLANT HEIGHT AND SPREAD,  OF  RHODODENDRONS  PRODUCED ON HEATED AND NON-HEATED SOIL:

                                         MEASUREMENTS MADE  ON  NOVEMBER  14, 1972
Average plant
heiqht-inches7
Vulcan
Jean Marie
Fastousum Plena
Lord Roberts
Anna Krusckka
Old Port
Check
14.8
9.3
12.8
12.5
11.8
13.4
Soil
14.
11.
14.
12.
12.
14.
heat
5
8
9
8
0
4
% height
increase of
soi 1 heated
plants
over checks
0
27
38
2
2
7
Average plant
Check
Max
16.
9.
13.
14.
12.
15.
a
2
3
9
1
8
0
Min.
11.3
7.1
8.8
10.4
9.6
11.0
spread-inches
Soil heat
Max.
17.3
11.4
14.7
13.5
14.8
17.0
Min.
13.7
8.5
11.9
10.3
10.3
12.9
% increase of soil
heated plants
over checks
In max.
spread
7
23
6
0
16
13
In min.
spread
21
20
35
0
7
17
      zHeight measurements from 4 axes/plant (average of 10 plants)  from which  maximum and  minimum measure-
       ments were taken.

-------
minimum spread averaged 12 and 5 percent, respectively, greater than
'Old Port1 control plants.  'Lord Roberts' plant from heated soil  aver-
aged only larger in spread and height than control plants.

On the other hand, maximum and minimum spread of 'Jean Marie'  plants
on soil heat were increased 38 and 41 percent, respectively, and height
was increased by 42 percent compared to plant size on control  soil  blocks
(Table 16).  The growth response of  'Vulcan,1 'Fastausum Plena,1  and
'Anna Krusckka' to soil heat was between that of 'Jean Marie1  and 'Old
Port.'

There was less difference in size between plants grown on heated and
control soil by the end of the 1972 growing season than in July.   On
November  14, 1972, soil heated plants of 'Jean Marie' averaged 27 percent
taller, 23 percent greater maximum, and 20 percent greater minimum
spread than control plants (Table 17).  By November, the small difference
that had  existed in size of 'Lord Roberts' plants in July was  not
apparent.

Although  there was less difference in plant size between soil  heated and
control plants in November, most cultivars on soil heat still  appeared
more symmetrical and uniform in size.  This is supported by the lower
coefficients of variation for maximum-minimum spread of plants grown on
heated soil compared to the controls (Table 18).

Generally, soil heated plants also had less variation in height than
plants from control soil.  'Jean Marie,' 'Fastausum Plena,1 'Lord Roberts,1
and 'Old  Port' plants from control soil blocks had greater coefficients of
variation for height than plants in soil heated blocks (Table 18).

Cantaloupes

Procedure—Plots were fertilized with 800 Ib 16-20-0 per acre in a 1 ft
wide band on top of the beds.  "Diazinon" insecticide also was applied in

                                137

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Table 18.  COEFFICIENT OF VARIATION FOR PLANT HEIGHT AND SPREAD  OF  SIX
   RHODODENDRON VARIETIES GROWN IN NON-HEATED SOIL  AND SOIL  HEATED
                   BY THERMAL WATER -  NOVEMBER 14,  1972
Vulcan
Jean Marie
Fastausum Plena
Lord Roberts
Anna Krusckka
Old Port
                                Coefficient of Variation  -  %
                              Height
Check   Soil  heat
 16.9     17.9
 31.3     19.6
 25.6     13.9
 20.2     18.2
 17.8     19.4
 29.8     17.0
Max.-min. spread
Check   Soil heat
 22.8
 29.5
 28.8
 20.6
 20.0
 24.6
14.9
18.9
15.9
20.9
20.2
19.3
                                   138

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a wide band on top of the rows at the rate of 4 Ib active per acre on
May 26, 1972.  The insecticide and fertilizer were incorporated into the
soil with a rototiller.

Black plastic film (4-mil) was put down in rows over the incorporated
fertilizer and insecticide on May 30* 1972.  Rows were spaced 5 ft
apart.  About 2 ft of plastic were exposed on top of each bed with 6 in.
buried on each side of the bed.  Five inch diameter holes were punched
into the plastic ^every 4 ft;  The plastic mulch was placed over heated
and non-heated soil.  Two cantaloupe cultivars, 'Supermarket1 and.
'Harper's Hybrid,1 were seeded on June 2, 1972, in heated and non-heated
                                   * *.
soil and replicated twice.  Seeds were planted 1 in. deep in each hole
punched in the plastic mulch (4 ft x 5 ft plant spacing).  Muskmelons
were harvested from 40 ft plots starting on September 5 and ending on
October 19, 1972.  'Fruit were separated into grades of U.S. No.  1,
Commercial, Unmarketable, and Immature.1*1                        ,

Results and Discussion—Soil heat speeded early vine development of
muskmelons (Figure 57).  The area in the foreground of Figure 57 is
non-heated soil and the area between rows is not covered with melon
vines.  The melons in, the background of Figure 57 are on heated soil,
and the areas between rows were completely covered with vines by mid-July.

Although early vegetative growth of cantaloupes was stimulated by soil
heat, the yield of fruit was not.  There was no significant difference
in yield of soil heated and control areas of 'Harper's Hybrid' and
'Supermarket' in this study (Tables 19 and 20).  Soil heat appeared to
delay fruit maturity as indicated by the number of immature fruit at the
end of the harvest season (Tables 19 and 20), but this has to be confirmed
in other studies.  Temperatures of heated soil at 6 and 12 in. depths
were generally warmer through June and into July than non-heated soil
(Figures 50 and 51), and this probably accounts for the early stimula-
tion of vegetative growth of cantaloupe plants.  Perhaps a different
                                139

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Figure 57:   Muskmelon  vine  development  on  non-heated  soil  (foreground  1/2  of melon  block)
            and  heated soil  (background 1/2  of  block).

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Table 19.  EFFECT OF SOIL HEAT ON GRADE AND YIELD OF CANTALOUPE
                         'HARPER'S HYBRID1

              	   	Lbs/Acre	
Soil heat
Control
U.S.
no.l
4215
8059
   U.S.
commercial
    523
   1329
Unmarketable
  (rots &
  splits)
    2780
    1147
Immature
  918
  373
                                141

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Table 20.  EFFECT OF SOIL HEAT ON GRADE AND YIELD OF CANTALOUPE
                         'SUPERMARKET'
              .    ,                 Lbs/Acre
                                       Unmarketable
               U.S.         U.S.           (rots &
               no.1      commercial        splits)        Immature
  Soil heat    3989         1220            1729           2301
  Control      7498         2110             485            518
                           142

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growing season, planting date, or soil temperature range would have
altered the effect of soil heat on yields.
Squash
Procedure-'-'Table Queen1 squash was seeded through black plastic mulch
on heated and non-heated soil on June 24, 1972.  Hill  spacing was
4 ft x 6 ft.  The planting was not replicated.  Fertilizer and insecti-
cide quantity, type, and date of applications are the same as outlined
for cantaloupes.  'Table Queen1 squash was first harvested on October 4,
1972.  Only good, mature fruit without cracks and free of disease were
counted on each harvest.
Results and Discussion—The soil heated block of squash produced 24 per-
cent more fruit by number and 13 percent more fruit by weight than the
non-heated control block (Table 21).  In this case, early maturity of
squash appeared to be enhanced by the soil heat.  At first harvest, the
yield from the soil heated block was 10.2 tons; control yielded only
3.5 tons (Figure 58).  The 10.2 tons of fruit represented 36.2 percent
of the heated block's production, while the control had only produced
14.1 percent by October 4, 1972.  Production from controTand heated
block was about the same on October 9 and 16.  .On the last harvest,
November 6, the control block produced 4.6 more tons per acre than the
soil heated block.
                                143

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Table 21.  YIELD OF 'TABLE QUEEN'  SQUASH PRODUCED ON A CONTROL  AND



                          SOIL HEATED BLOCK
Harvest
date
10/4/72
10/9/72
10/16/72
11/6/72
Number of fruit/A.2
Soil heat
10,010
4,368
2,548
14,560
31 ,486
Control
3,276
2,912
1,820
17,472
25,480
Tons fruit/A.z
Soil heat
10.2
3.9
2.0
12.0
28.1
Control
3.5
3.3
1.5
16.6
24.9
 Plant spacing was 4 X 6 ft.
                                 144

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             16 -
             14 -
             12 -
              10  -
              o   J
              6   -
              4   -
              2   -
                          Soil Heated Block
                          Control Block
                          i i
                          10-4        10-9        10-16        11-6
                                        Harvest Dates

Figure 58.   Yield  of Table Queen squash on four harvest dates  during 1972.
                                  145

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                              SECTION VI
                        SOIL HEATED GREENHOUSE

Initially, the idea was to keep greenhouse construction simple, rela-
tively inexpensive, and to use the structure to lengthen the time in
spring and fall that the undersoil heated block could be used for crop-
ping.  However, because of the relatively mild climate in the Eugene
area, it was found that year-around cropping was possible with selected
crops in the simple greenhouse structure described below.  The crops
grown and their production in the greenhouse will  be covered in subse-
quent sections.

A 55 by 22 ft "Port-a-Green" plastic film greenhouse was constructed
over a portion of the large under-soil heated block in January 1972.
The soil underneath and surrounding the greenhouse was heated by thermal
water circulated through 2-1/2 in. diameter plastic pipe, buried about
26 in., and spaced 60 in. apart (for complete description, see Section  V)
Ventilation fans were installed in the greenhouse, but no supplemental
heaters were added.  The only heat in the greenhouse was that radiated
from the buried soil heat grid and the solar energy trapped in the
greenhouse during the day.
GREENHOUSE AIR TEMPERATURES

Maximum greenhouse temperatures were dependent to a large degree upon
daily solar energy, but greenhouse highs were modified by the thermostat
controlled ventilation fans.  Even when the air temperature was cold,
greenhouse highs during the day were relatively warm if there was no cloud
cover.  For example, December 8, 1972, was a clear day with a maximum
air temperature of only 15°F but maximum greenhouse temperature reached
55°F (Figure 59).  December 20, 1972, was cloudy (not as cold) and
                                147

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00
            s
                80-
                70-
                60
                50
           o
           —   40
            R)
            S.
           ff.
                30-
               20-
                10-
                0-
               10
                    Greenhouse Maximum Air Temperature
                  ° Outside Maximum Air Temperature
                  * Greenhouse Minimum Air Temperature
                  * Outside Minimum Air Temperature
                                          8
10   12
20
22
 I
24
26
 I
28
                                                                                                          30
                                                   —T	1	r~
                                                    14    15     18
                                                     December 1972
Figure 59.  Minimum and maximum air temperatures  recorded  inside and outside soil heated greenhouse during December 1972.

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maximum temperatures inside and outside the greenhouse were the same.
Another reason that greenhouse maximum temperatures were no higher than
outside the house was that thermal water flow was interrupted on this and
several other dates during December 1972.  The temperature of thermal
water during December was also cooler than usual.

Only the minimum temperatures inside and outside of the greenhouse, 5 ft
above the ground, are included in Figure 60.  Greenhouse minimums aver-
aged 8.2°F higher than ambient minimums for the March 1972 through March
1973 period.  There was often less difference between minimum tempera-
ture inside and outside the greenhouse during the summer than during the
winter.  This was because greenhouse doors were often left open during
the summer for added ventilation.  The least difference between green-
house and outside minimums occurred during the week of August 9, 1972
(,2°F difference), and the largest difference occurred during the week
of December 6, 1972 (19°F difference).  Greenhouse minimums may have
been somewhat warmer during December 1972 if thermal water temperatures
had been warmer.
GREENHOUSE SOIL TEMPERATURES

As already stated, greenhouse soils were heated by the buried thermal
water grid described  in Section V.  The soil heat grid by itself modified
soil temperatures, and the addition of a greenhouse further modified
temperatures of soil  beneath the structure.

Platinum bulb temperature sensors connected to chart-type recorders
were placed at 6, 12, and 24 in. depths in a vertical line above and
halfway between buried heat pipes (Figure 48) within the greenhouse.

Greenhouse soil temperatures at 6, 12, and 24 in. depths were modified by
the thermal water circulated through the buried soil heat grid.  As was
the case with the soil heated block outside the greenhouse, temperatures
were not uniform for  any given depth in a horizontal line across the soil
                                 149

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                   •  Minimum Air Temperature Inside Greenhouse
                   o  Minimum Atr Temperature Outside Greenhouse
Oi
O
              60 -
              50 -
£
3
t-
ftl
C*.
I
              a>  -i
              10  -
                                                                                                                                      1   I—I—I—I—I—I—I—I—I—I—I—1—I—I—1—I—I—I
                  Figure 60.  Comparison of mean weekly minimum temperatures Inside and outside the greenhouse at about 5 ft above the ground.

-------
profile.  Soil farthest away from the buried heat pipes was cooler than
soil closer to the heat lines.  However, the temperature difference
between soil temperature midway between and nearest to the pipes was
generally less in the heated greenhouse soil than in the heated soil out-
side the greenhouse.  For example, the average temperature difference in
soil at points midway between (coolest heated soil) and nearest (warmest
heated soil) heat lines at 12 and 24 in. depths averaged 1.9°F (Fig-
ure 61) and 6.2°F (Figure 62) in the greenhouse and 4.3°F (Figure 51)
and 17.4°F (Figure 52) in heated soil outside the greenhouse, respec-
tively.  The reduction of radiated heat loss from the soil by the green-
house structure apparently helped maintain more uniform temperatures in
a horizontal line across the soil profile.

The warmest areas of heated greenhouse soil at the 6 in. depth (recorded
in a vertical line above heat pipes) averaged 9.5°F warmer than unheated
control soil for the recorded periods from May 1972 through January 1973
(Figure 63).  During the May through July period, greenhouse soil tempera-
tures were recorded beneath rows of trellised tomatoes.  Soil temperatures
outside the greenhouse were recorded beneath low growing field tomatoes.
Greenhouse tomatoes were between 5 and 6 ft tall and formed a continuous
plant cover inside the greenhouse.  With vegetation of such thickness,
the ground surface loses its function as a boundary surface with the
atmosphere and site of major heat exchange.  The radiation received by
the greenhouse soil was not as great as if the ground were bare and pro-
bably not as great as received by soil outside the greenhouse with the
low growing, less dense field tomatoes.  The difference in foliage cover
probably accounts for the lower 6 i,n. depth soil temperatures recorded
in the greenhouse during the May through July period.

Temperatures of heated greenhouse soil at the 12 in. depth were modified
relatively more than 6 in. depth temperatures.  The warmest areas of
greenhouse soil at the 12 in. depth averaged 11.2°F higher than controls
for the recorded periods between May 1972 and January 1973 (Figure 61);
the coolest areas of greenhouse soil averaged 9.3°F warmer than control
                                 151

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01
ro
       Q_
       
-------
  100-


   95-


   90-


   85-


£  80-


   75-


   70-


   65-
£  60-J
01
O-
01
. Halfway between buried  heat pipes - greenhouse
         • Control  -  no soil heat
                                     —P—
                                       2
                                      Aug
                                                                             T
                                               	1	1	
                                                        641               63
                                                       Sep         Oct         Nov            Dec         Jan
                                                      1972                                                1973
Figure 62.  Comparison of mean weekly 24 inch depth soil temperatures recorded at two locations in soil  heated greenhouse
            with non-heated soil outside greenhouse:  greenhouse soil was heated with thermal  water circulated through
            plastic pipes buried 26 inches and spaced 5 ft apart.
—P_
  7
 Jun
—r~
  5
 Jul

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tn
-P.
          75-
           70-
          65-
        Cu
        O)
           60-
 55-
        .c
        o
        c
        o

        
        Q.
        d)
           45-
           40-
                              flow of  thermal
                             water interrupted
                                                                                         flow  of  thermal
                                                                                       water  interrupted
        o  Above buried heat pipes- greenhouse
       <>-  Halfway between buried heat pipes - greenhouse
        •  Control - no soil heat
           35'
Figure 63.
                                                                                         /
            —I—
              7
            Jun
—r~
  5
 Jut
                                               2
                                              Aug
—i—
   6
  Sep
 1972
Oct
                                                                                      r
 1
Hov
 6
Dec
 3
Jan
 1973
                     Comparison of mean weekly 6 inch depth soil temperatures recorded at two locations  in  soil  heated greenhouse
                     with non-heated soil outside greenhouse:  greenhouse soil  was heated with thermal water circulated through
                     plastic pipes buried 26 inches and spaced 5 ft.  apart.

-------
soil during the same period.  The 12 in. depth greenhouse soils averaged
3.1 to 5.7°F warmer than the 12 in. depth in the heated soil block outside
the greenhouse.

The greatest temperature difference between greenhouse and control soil
occurred at the 24 in. depth.  The warmest areas of greenhouse soils
averaged 20.7°F warmer than control soil, and the coolest greenhouse areas
of greenhouse soil averaged 14.2°F warmer than control soil at the 24 in.
depth (Figure 62).
GREENHOUSE CROP PRODUCTION

A variety of crops were grown in the greenhouse, some of which are not
normally considered to ba greenhouse crops.  This was done to determine
if crops that are tolerant to cool temperatures could be produced through
the Winter in the greenhouse when low light intensity and coolest tempera-
tures prevail.

Interest was expressed in the value of these crops.  In order to put an
economic value on the crops, Portland market wholesale prices42 were
assigned to the crops during the time they were harvested.  Therefore,
some of the crops may have been worth more or less if harvested at other
times of the year than was done in these studies.  The dollar value for
the crops is higher than received at the farm.  No real attempt was made
to study market supplies and gear specific crop production to periods of
least supply and highest price.  However, this would be an important
consideration if studies continued or a large scale project were under-
taken.  The main emphasis in the following studies was to obtain approxi-
mate yield estimates for various crops grown in the simple greenhouse
constructed over a portion of the heated soil block.

Leaf Lettuce
Transplants of 'Bibb' and 'Grand Rapids' leaf lettuce were obtained from
a local greenhouse nursery and transplanted into the project's greenhouse
                                155

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on March 8 and 9, 1972.  Plant spacing was 6 by 6 and 8 by 8 in. for
'Bibb' and 'Grand Rapids,1 respectively.  The two leaf lettuce cultivars
were transplanted into 9 by 10 ft blocks of 4 mil black plastic and
aluminum foil mulches and in non-mulched control blocks.

The lettuce crop was harvested (Figure 64) on April 24, 1972; yield and
estimated crop values are given in Table 22.  Dollar values in Table 22
are based on Portland wholesale market prices reported by USDA Agri-
cultural Marketing Service for April 24, 1972.^

If all  'Bibb' and 'Grand Rapids' plants had been spaced on exactly 6 by
6 and 8 by 8 in. spacing, respectively, there would have been the equiva-
lent of about 174,240 'Bibb' and 'Grand Rapids' plants per acre.  The
primary reason that plant populations reported in Table 22 are lower than
the possible maximum is that transplants were placed slightly further
apart than the intended 6 by 6 and 8 by 8 in. spacings.

A few plants had to be discarded shortly before or at harvest because of
disease (appeared to be SjcJ^ejrotlnja, soft rot).  Although there was very
little disease, more soft rot occurred in the check areas (about 3 percent
of plants) than in the black plastic and aluminum foil mulched plots (less
than 1 percent diseased plants).  Although the greenhouse soil was not
sterilized before planting, disease contributed little to reducing
harvested plant number.

The black plastic and aluminum foil mulch materials were included to
determine if they would influence soil temperatures.  Initially, when
lettuce plants were small, surface soil temperatures were slightly warmer
underneath the mulches than in check plots.  As soon as the plant canopy
developed over the entire soil surface, temperatures underneath the mulches
were no different than in the check plots.  The mulch materials did reduce
plant foliage contact with the bare soil and thus reduced the incidence
of disease.
                                156

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-
                             Figure 64:  Greenhouse lettuce on April  24, 1972.

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Table 22.  YIELD AND ESTIMATED VALUE OF BIBB AND GRAND RAPIDS LEAF LETTUCE GROWN  IN  THE  PROJECT'S

GREENHOUSE ON CHECK, BLACK PLASTIC FILM, AND ALUMINUM FOIL MULCHES; HARVESTED ON  APRIL 24,  1972.
No. of plants
harvested/acre
Pounds of
^ lettuce/acre
00
No. of 2 doz
crates/acre
Value/Acre: at
$1.60/2 doz era tea
$2.25/2 doz crate*
CHECK
Grand Rapids
81 ,556
65,701
3,398
$5,437
$7,645
BLACK PLASTIC
Bibb
127,188
60,089
5,299
$8,478
$11,923
Grand Rapids
81,556
63,672
3,398
$5,437
$7,645
Bibb
151,460
56,019
6,311
$10,098
$14,200
ALUMINUM
Grand Rapids
87,381
66,099
3,641
$5,826
$8,192
FOIL
Bibb
161,169
64,264
6,715
$10,744
$15,109
aValue based on wholesale price range received in Portland, on April  24,  1972,  for California
 butter and leaf lettuce.

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Forty to 50,000 Ibs 'Grand Rapids' and 20,000 to 25,000 Ibs 'Bibb'  lettuce
per acre are considered to be good yields for greenhouse leaf lettuce.^
The yield of 'Grand Rapids' in the project greenhouse ranged from about
63,672 to 66,099 Ibs per acre and the yield of 'Bibb' lettuce ranged
from 56,019 to 64,264 Ibs per acre (Table 22).  The yields of both  leaf-
type lettuce compare very favorably with yields of leaf lettuce produced
in conventionally heated greenhouses.  Because of the short time needed
to produce a greenhouse lettuce crop, multiple crops of lettuce could be
produced each year depending upon the marketing situation.

The wholesale value of the crop on April 24, 1972, ranged from about
$5,400 to $8,200 per acre for 'Grand Rapids' and $8,400 to $15,000  per
acre for 'Bibb1 (Table 22).  The value of the crop could range higher
than reported here depending upon market supply and demand.  For example,
the wholesale orice for Oregon grown butter and leaf lettuce at the Port-
land market was $3 per 2-dz crate on May 8, 1972, or about 33 percent
more than the top value used in Table 22.

A second planting of greenhouse lettuce was made in the fall of 1972.
'Bibb' and  'Grand Rapids' lettuce were seeded in flats of vermiculite
and placed in the project's greenhouse on October 5, 1972, to germinate.
Small  'Bibb' and 'Grand Rapids' lettuce plants were transplanted on
6 by 6 and 8 by 8 in. spacings, respectively, on November 1, 1972.
Each cultivar was placed in a 5 x 14 ft ground bed.

Ambient air temperatures for December 4 through 12, 1972, averaged  10 to
26°F below normal .^ and the subzero lows in most of Oregon set many new
December and all-time records.  A record low of -12°F was recorded  at
the Eugene airport on December 8, 1972.  At the project site, lows  of
-5°F were recorded on December 8 and 10, 1972.

The delivery of thermal  water to the project was interrupted several
times during December.  The Weyerhaeuser plant had to stop pumping
thermal water on December 8 and 11 in order to make repairs.  A joint

                                159

-------
in the 16 in. steel mainline developed a leak on December 12, but was
repaired by the evening of December 13.  No thermal  water was pumped to
the project from December 22, 1972, to January 2, 1973.   The Weyerhaeuser
plant was down December 22 through 26 for the Christmas  holidays.  Thermal
water was delivered to the pumping pit from December 27, 1972, through
January 1, 1973, but the volume was not great enough to  be pumped to the
project.  This is why in Figure 3 thermal water temperature at the pump-
ing pit was going up while soil heat grid inlet and outlet temperatures
were going down.

The low ambient air temperature outside the greenhouse on December 7 was
near 0°F, and the low greenhouse temperature was 20°F at 5 ft above ground.
The following night, December 8, a low of -5°F was recorded outside the
greenhouse and a low of 17°F inside the house at the 5 ft height.  'Bibb'
and 'Grand Rapids' leaf lettuce were not frozen by low temperatures during
the coldest weather.  Greenhouse air temperatures remained at 36°F at the
1 ft level and slightly warmer within the plant foliage  on the coldest
nights.  Apparently enough heat was radiated from the soil to keep tempera-
tures above freezing to a height of more than 1 ft in the greenhouse.
Temperatures outside the greenhouse were probably coldest near the ground
but greenhouse temperatures were warmest near the soil because of heat
radiated from the buried thermal water grid.  Greenhouse soil and air
temperatures may have been somewhat warmer during this cold December
period if the thermal water supply had been warmer and had not been
interrupted.

The growth of the lettuce plants was slow because of relatively low
temperatures and the low light quality experienced during the winter
months.  Disease was more of a problem in the second crop than in the
first, and 'Grand Rapids' was more susceptible than 'Bibb.1  By the end
of December, nearly 25 percent of the  'Grand Rapids' plants were removed
because of soft-rot-type decay, but only about 9 percent of the  'Bibb1
plants had to be removed for this reason.
                                160

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Tomatoes

Most greenhouse tomatoes  are  grown on a trellis system where the main
plant axis is  trained to  a string suspended from overhead wires.  All
lateral plant  branches  are removed by hand from the main plant axis.  The
labor requirement  for this method is high but increased yields, less
disease, greater air circulation through the foliage, and ease of harvest
make the system economical.

At  the  time  the first tomato  crop was planted in the project's greenhouse,
no  overhead  trellis was available.  Therefore, the tomatoes were either
trained to 5 ft stakes  or allowed to grow on the ground.  The stake
system  kept  fruits off  the ground, helped air movement (in addition to the
removal of excess  foliage), reduced disease, and made it possible to use
.more plants  per acre than when  plants were grown on the ground.

The first planting of tomatoes  in the greenhouse was made in February 1972.
Cultivars  'H.  1439,'  'Fireball,1 and  'H. 1350' were seeded at a high rate
in  short rows  in the greenhouse soil on February 17, 1972.  Soil tempera-
ture at the  6  in.  depth was about 64°F at time of seeding.

 'H. 1439' plants were transplanted from the closely spaced seedling rows
to  double rows 1 ft apart with  plants 1 ft apart in the row.  Double rows
were on 4 ft centers.   The  'H.  1439' yield record block contained
28  plants.

 'H, 1350' and  'Fireball1  were transplanted from the short closely spaced
seedling rows  into rows with  about 1-1/2 in. between plants on March 16,
1972.   They  were transplanted again on May 2, 1972, to a 4 by 2 ft spacing.
The blocks of  'Fireball1  and  'H. 1350' contained 24 plants each.

On  May  9, 1972, transplants of  tomato cultivar  'Willamette' were obtained
from the McKenzie  Nursery and transplanted to the greenhouse in a block of
24  plants on 2 by  4 ft  spacings.   'Willamette1 plants were smaller and less
                                 161

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mature than the other cultivars.  These transplants were also placed out-
side the greenhouse in heated and non-heated soil on the same day.

Plant spacing of 'H. 1350,' 'Fireball,1 and 'Willamette1 was equivalent
to 5,445 plants per acre (8 ft*/plant); the spacing of  'H. 1439' was
equivalent to 14,520 plants per acre (3 ft2/plant).  'H. 1439' vines
were trained on stakes with two main branches per plant.  'Fireball,'
'H. 1350,' and  'Willamette5' were grown on the ground like normally grown
field tomatoes.

Pollination of  greenhouse tomatoes was induced by the air blast from a
small engine-driven backpack sprayer-duster.

Prior to the time that tomato cultivars were transplanted, 625 Ibs of
16-20-20 fertilizer were incorporated into the greenhouse soil with a
rototiller on April 28, 1972.  Periodic applications of 9-45-15 and/or
potassium nitrate fertilizer were applied to the plants as a liquid and
watered into the soil surrounding the tomato plants during the growing
season.

The first greenhouse tomato crop was planted relatively late, and fruit
matured when field-grown tomatoes from California were plentiful and
when some local tomatoes were available.  Although greenhouse tomatoes
usually receive a premium price above field tomatoes, the Portland
market wholesale price for field tomatoes was assigned to the greenhouse
crop.  Table 23 lists the wholesale price for field-grown tomatoes of
various sizes from July 13 through September 21, 1972.   Greenhouse fruit
were not graded for size, but it was estimated that all marketable fruit
were at least grade size 6x7 (2-1/16 in. minimum to 2-10/16 maximum
diameter) or larger.  The net weight of a 3-layered 6x7 tomato lug is
30 Ibs with about 126 fruit per lug46 and an average fruit weight of
about .23 Ib.

Tomato cultivars grown in the greenhouse produced 32 to 76 tons of
marketable fruit per acre (Table 24) during the harvest period of

                                 162

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Table 23.  WHOLESALE MARKET PRICE PER LUG BOX OF CALIFORNIA PINKS AND
RIPE TOMATOES ON PORTLAND MARKET DURING PERIOD OF JULY 13 THROUGH SEP-
            TEMBER 21, 1972.a  (FIELD GROWN TOMATOES)
1972
Date
Jul 13
17
20
24
27
31
Aug 3
7
10
14
17
21
24
28
31
Sep 5
7
11
. ;14
18
21
Mean
7/13-
9/21
2-Layer
5X6
$5.00 -
4.50
4.50
5.25
5.00
5.25
5.75
5.00
5.00
5.00
5.50
5.75
5.75
5.75
5.50
4.50
3.90
4.70
5.00
5.25
5.25


5.10
Lug
's
$5.75
5.00
5.00
5.50
5.50
5.75
6.25
6.25
5.50
5.50
6.50
6.00
6.00
6.00
5.90
4.70
4.75
5.00
5.50
5.70
6.00


5.62
3-Layer
6X6
$7.50 -
5.25
5.25
5.25
7,00
7.00
7.25
-
-
6.50
6.75
7.25
7.25
7.25
7.70
5.50
5.50
6.00
6.00
7.00
7.00


6.54
Lug
's
$8.20
6.00
6.00
6.00
7.25
7.25
8.20
-
-
7.50
7.50
8.20
8.20
8.20
8.20
6.70
6.70
6.70
7.70
7.70
8.20


7.39
3-Layer
6X7
$6.50 -
5.00
5.00
5.75
6.00
6.26
6.75
5.50
6.25
6.25
5.50
6.00
5.50
6.50
6.00
4.75
4.75
5.50
5.50
6.00
6.25


5.79
Lug
's
$7.25
5.50
5.50
6.00
6.75
6.75
7.25
6.50
6.50
7.70
7.70
6.75
6.50
7.70
7.20
5.25
5.25
5.75
5.75
7.20
7.25


6.57
3-Layer
7X7
$6.00 -
4.50
4.50
4.75
4.75
5.50
5.50
5.00
5.00
4.25
4.25
5.50
5.00
5.50
5.00
4.50
4.50
5.00
5.25
5.25
5.75


5.01
Lug
's
$6.75
5.00
5.00
5.50
5.50
6.00
6.00
5.50
5.50
5.00
5.75
5.75
5.50
6.70
6.20
5.20
5.20
5.25
6.20
6.20
6.75


5.74
 a Prices  from  Fresh  Fruit  and Vegetable Market News - Portland Daily
   Report  - Vol.  LXI.   No's  4 through 16.  USDA, Ag. Market Service.
                                  163

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CT»
      Table 24.   WEIGHT,  NUMBER OF 6 X 7 LUGS  (126  FRUIT/LUG), AND ESTIMATED WHOLESALE VALUE OF TOMATOES PRO-
                                          DUCED  IN  SOIL HEATED GREENHOUSE.




Tomato
Variety
H.I 439a

H.1350&

Fireball b

Willamette13



1972
Harvest
Period
Jul 14-
Sep 12
Jul 22-
Sep 12
Jul 14-
Sep 12
Jul 29-
Sep 12

-
Tons
Marketabl e
Fruit/ Acre

76.1

34.0

32.0

33.9


Aug
Fruit
Wt-Lbs

.25

.23

.23

.26

Number of
Marketable
3-layered
6X7 Lugs/Acre

4,783

2,299

2,174

2,036


Wholesale
$5.79/Lug
Mean Low

$27,693

$13,311

$12,587

$11,788


Value/ Acre
$6.57/Lug
Mean High

$37,424

$15,104

$14,283

$13,376


No. 816
Boxes/Acre
x 100

190

85

79

85
Market-
able
Fruit/
plant
Ibs

10.5

12.5

11.7

12.5
      a Plants staked (14,500 plants/acre).
        Plants grown on ground like most field-grown  tomatoes  (5,445 plants/acre).

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mid-July through mid-September.  Tomato plants were removed from the
greenhouse on September 12, 1972, so that the soil could be prepared for
another planting of vegetables.  There was the equivalent of 20, 10, and
4.8 tons green fruit per acre left of  'H. 1439,'  'Willamette,1 and
'H. 1350,' respectively, when plants were removed.  Many of these fruit
would have been marketable if they had been allowed to mature.  Cultivar
'H. 1439' produced more than twice the yield of other cultivars listed
in Table 24.  The yield difference was primarily because of training
systems used with the different cultivars.  Many fruits of cultivars grown
on the ground developed ground rot and had to be discarded; therefore,
their yields were reduced.

The value of the greenhouse crop was calculated in two ways.  The first
was based on the Portland wholesale price received for field-grown toma-
toes during the period that the greenhouse crop was harvested.  The second
was based on approximate prices received for greenhouse tomatoes on the
Chicago market.

Individual  'Fireball' and  'H. 1350' fruit averaged about .23 Ib and
'H. 1439' and 'Willamette1 were somewhat larger (Table 24).  Therefore,
fruit of the latter two cultivars averaged somewhat larger than 6 x 7's
and would have been worth more than that indicated in Table 24.  The
wholesale values per acre based on average low and high Portland market
tomato prices during the harvest period (Table 23) for production of
3-layered 6 x 7 lugs are included in Table 24.  The value per acre ranged
from $11,788 for 'Willamette' to $37,424 for  'H. 1439.'

Greenhouse tomatoes sold on the Chicago market are usually sold in 8 Ib
cardboard baskets.  Table 25 lists a production range of 8 Ib baskets and
prices received for greenhouse tomatoes in the Chicago area in 1965.47
Costs may have to be adjusted to bring them in line with present costs;
however, the prices are probably still within the range being paid for
greenhouse tomatoes.  The.number of 8 Ib boxes produced by each variety
(Table 24) was assigned to the appropriate production level in Table 25,
and the values per acre estimates are as follows:

                                 165

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Tabled 25.  GROSS CASH RETURNS, LESS DIRECT MARKETING COSTS,  AT FOUR

          PRICE LEVELS FOR DIFFERENT VOLUMES OF PRODUCTION
Production
of 8-lb
baskets


2,000
4,000
6,000
8,000
10,000
12,000
14,000
16,000
18,000
20,000
22,000
24,000
26,000
Cost of
basket and
haulinga


$ 600
1,200
1,800
2,400
3,000
3,600
4,200
4,800
5,400
6,000
6,600
7,200
7,800
Averaae orices
$1.50
(1.35)b
Total

$ 2,100
4,200
6,300
8,400
10,500
12,600
14,700
16,800
18,900
21 ,000
23,100
25,200
27,300
$1,75
(1.57)
gross cash
marketing
$ 2,540
5,080
7,620
10,160
12,700
15,240
17,780
20,320
22,860
25,400
27,940
30,480
33,020
of 8-lb basket'
$2.00
(1.80)
returns less
costsc
$ 3,000
6,000
9,000
12,000
15,000
18,000
21 ,000
24,000
27,000
30,000
33,000
36,000
39,000
$2,25
(2.02)
direct

$ 3,440
6,880
10,320
13,760
17,200
20,640
24,080
,27,520
30,960
34,400
37,840
41 ,280
44,720
a Calculated at 30 cents per 8-lb basket (14 cents  for basket,  lid and
  paper and 16 cents for hauling).

b Figures in parentheses are grower's returns per basket minus  10 per
  cent commission.

c Direct marketing costs are cost of basket, hauling,  and commission. '
  Table from Courter, J.  W.  et al.   1965.   The feasibility of growing
  greenhouse tomatoes in  Southern Illinois, University of Illinois.
  Coop. Ext. Ser.  Circular 914.
                               166

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               Cultivar                        Val ues per acre
              Willamette                     $ 8,906 to $14,589
              H. 1439                         19,993 to  32,750
              H. 1350                          8,929 to  14,626
              Fireball ,                        8,376 to  13,725
By using Table 25 for value-per-acre estimates, the cost of baskets,
hauling, and a 10 percent commission were subtracted from the price per
basket before the above values were calculated.  Therefore, the value per
acre is slightly lower than when calculated on just wholesale prices.

Tomato plants of cultivars  'Michigan-Ohio, Hybrid' and 'Veegan' were
seeded in flats about August 15, 1972, for the second greenhouse tomato
crop.  One hundred pounds N, 125 Ib P205, and 100 Ib K20 were applied to
the greenhouse soil as 16-20-0 and KC1 and incorporated with a rototiller
on September 13 and 14, 1972.  After the greenhouse ground bed was pre-
pared, it was covered with a plastic tarp and methyl bromide was injected
under the tarp at the rate of 1 Ib per 100 ft2 on September 19, 1972.
The tarp was removed on September 22.  Trellis supports for tomatoes were
put in place on September 26.  An additional ventilation fan and perfo-
rated plastic convection tube was installed inside the greenhouse on
November 3, 1972, to aid air circulation.

A drip irrigation system was installed in the greenhouse on November 15.
A "Twin-wall" hose from Chapin .Watermatics, Inc., with orifices 8 in. apart
was used.  "Twin-wall" hose was placed beside each tomato row.

'Michigan-Ohio' and 'Veegan' were transplanted into the greenhouse on
October 2, 1972.  Tomatoes were placed in double rows 1 ft apart, and
plants were 1 ft apart in the row.  The double rows were on 5 ft centers.
Two sets of double rows (14 plants per row) of each variety were included
in half the greenhouse.  Plant spacing was equivalent to about 15,000
plants per acre or about 2.9 ft2 per plant.  Tomatoes were 10 to 14 in.
                                167

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tall when transplanted.  One pint of 9-45-15 fertilizer mixed at the
rate of 28 grams per gallon was applied to each plant after transplant-
ing.  Tomatoes were fertilized with KN03 and 9-45-15 in a liquid band
application at 76, 148, and 217 Ibs per acre of N, P205, and K20, re-
spectively, on October 30, 1972.

Foliage damage that appeared to be "Early Blight" was noted on Novem-
ber 2, and "Maneb" was applied at the rate of 3 Ibs per acre for control
Blossoms were open on both tomato cultivars by November 7, 1972.

Vegetative growth of tomato plants was good despite short days and low
solar energy during October and November.  The cool temperatures pro-
duced plants with thick, sturdy stems.  Most day temperatures were
adequate for growth and fruiting, but night temperatures during Novem-
ber" and December were not sufficient for fruit production.  The flower
clusters were vibrated daily with an electrical vibrator to induce
pollen to shed, but very few fruit developed because of the low night
temperatures.

The record low temperatures in December 1972, described in the green-
house lettuce section, damaged the tomato plants; they were removed
from the greenhouse in December.
Japanese Salad and European Cucumber

Cucumbers are usually visualized as 8 to 9 in.  long, about 2 in. in
diameter, and with a fairly tough skin and seeds.  Nearly all  outdoor-
grown cucumbers are of this type as are most of the greenhouse-grown
cucumbers in this country.  However, there has  been increasing interest
in production of seedless cucumbers in greenhouses.  These cucumbers
have grown in Europe for many years and are often referred to as Euro-
pean or Dutch.  They are 12 to 18 in. long, seedless, mild, non-bitter,
of high quality, and have a thin edible skin.  Some Japanese cultivars
are very similar in quality but have a rough skin.  Some varieties are

                                 168

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referred to as "burpless" cucumbers.  Although the total production of
the European types is not great, their production in Canada and the
United States has increased substantially during the last 5 years.

Because the European-type cucumbers are so tender and thin-skinned,
careful handling is essential.  The fruits tend to wilt and break down
more quickly than the shorter American types unless proper handling
and storage conditions are provided.  Some growers film-wrap each cucum-
ber to reduce wilting and increase storage life.

These type cucumbers are not common in all areas of the United States
and may not be immediately accepted on the local market until people
become familiar with the commodity.  For example, it was reported that
European cucumbers produced in the Salt Lake area could not be marketed
there, but had to be air freighted to the Los Angeles area where they
were readily accepted.

The first cucumber type grown was a Japanese Salad type, 'Burpless FI
Hybrid,1 from the Robson Seed Company of Hall, New York.  This variety
was seeded in the greenhouse on February 17, 1972, and seedlings were
transplanted to 12 x 40 in. spacings (3.3 ft2/plant) on March 9, 1972.

Cucumber harvest started May 12, and fruit were picked when they reached
10 to 12 in. in length and about 2 in. in diameter.  Cucumber yields
reported in Table 26 are based on 13,200 plants per acre.  About 30 per-
cent of the crop was not classed as Nos. 1 or 2 fruit because of non-
symmetrical shape or oversize.  A regular picking schedule was not
maintained; this could have eliminated most fruit discarded because of
oversize.  Greenhouse production of 'Burpless FI Hybrid1 cucumbers for
a 5 month harvest period is given in Table 26.  Yields included Nos. 1
and 2 cucumbers.

The cucumber plant spacing used in the project's greenhouse was closer
than the 4 ft2 per plant (10,890 plants/acre) suggested in "Greenhouse
                                 169

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Table 26.  YIELD AND ESTIMATED VALUE OF JAPANESE SALAD CUCUMBERS (BURPLESS FI  HYBRID)  GROWN IN THE



      PROJECT'S SOIL HEATED GREENHOUSE AND HARVESTED FROM MAY 12 THROUGH SEPTEMBER 11, 1972.
Yield/ Acre
Plant
Population
13,200a
o 10,000
8,000
Sq. Ft.
/Plant
3.3
4.3
5.4
Fruit
Number
643,950
489 ,402
392,809
Fruit
Wt-Tons
391
' 297
238
Avg No.
Fruit/
PI ant
48.7
48.7
48.7
Avg
Fruit
Wt-lbs
1.21
1.21
1.21

at avg
$156,400
$118,800
$ 95,200
Estimated
at avg
35<£/lb
$273,700
$207,900
$166,600
Value/Acre
Based on
$3.00/doz
$160,986
$122,349
$ 98,202

Based on
$4.00/doz
$214,648
$163,132
$130,936
apopulation used in greenhouse.

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Table 27.  COMPARISON OF NO. 1 GREENHOUSE CUCUMBER FRUIT YIELDS PRODUCED IN ONTARIO, CANADA ON
               STRAW BALES WITH CUCUMBER YIELD PRODUCED IN PROJECT'S GREENHOUSE.
Variety
Toskaa
Toska3
Toska3
Toska3
Burpless
Hybridb
Year
1970
1970
1970
1972
1972
Harvest Period
Mar
Mar
Mar
Feb
May
9-Jul 6
9-Jul 6
23-Jul 13
11-Jul 13
12-Jul 25
Sq Ft/
Plant
9.
7.
8.
9.
3.
2
5
5
6
3
Plants/
Acre
4,752
5,808
5,124
4,537
13,200
No. Fruit/
Plant
32.5
36.6
30.6
35.1
30.5
Avg Fruit/
Wt-Lbs
1
1
1
1
1
.36
.35
.30
.36
.20
Wt Fruit/
Plant-Lbs
44.1
49.4
39.7
47.7
36.9
Tons/
Acre
117.6
128.4
101.8
108.2
170.5
3Grown on straw bales in Ontario, Canada.
bQrown in soil heated ground bed in project's greenhouse.

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Vegetable Production in Ontario"48 and the 9.6 ft2 per plant (4,537
plants/acre) used in European cucumber trials in Harrow, Ontario, in
1972.49  Yields of European-type cucumbers ranged from 15 to 25 Ib per
plant50 to 49.4 Ib per plant.49  The high yield in Ontario's trials was
produced by cultivar 'Toska' with straw bale culture and 7.5 ft2 per
plant (Table 27).  The average yield per plant of 'Burpless Fx Hybrid1
was 48.7 Ib (Table 26).

Cucumbers in the project's greenhouse were harvested longer than in
the Canadian trials and there were more plants per acre in the project
house.  Therefore, the cucumber yields produced per acre were consider-
ably higher in the project greenhouse than in the Canadian trials.
Table 27 was included to show that yields of European cucumbers pro-
duced in the project's greenhouse were in line with yields obtained in
other areas when harvest period and plant populations are taken into
consideration.

The season in which cucumbers are planted will probably influence plant
populations that can be used.  More plants per acre can be used in a
spring-summer crop than for a winter crop because of greater light
intensity in the spring months.  Local environment will also influence
plant populations that can be used.  The plant population used in this
first planting of cucumbers may have to be reduced in a large scale
planting.  Reducing plant number per acre would probably reduce yields
and values indicated in Table 26 for the 13,200 plants per acre.  Esti-
mated values for plant populations of 10,000 and 8,000 plants per acre
are also given in Table 26.  It was assumed that the number of fruit
and fruit weight per plant would not be lower than was produced with
13,200 plants per acre.

Jensen51 reported wholesale prices ranging from 20£ to 40£ for European
cucumbers.  European cucumbers grown in Washington State are sold in
boxes of 12, and the grower reportedly receives from about $4.00 to
$4.25 per box.  These prices were taken into consideration in Table 26
                                172

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in estimating the value of the Japanese Salad cucumber crop.  The value
of the crop could range from about $95 to $273 thousand per acre.  These
cucumbers are still a specialty item and impact of large acreages could
affect prices received for the crop.

A second crop of European (cv. Toska) and Japanese (cv. Burpless F],
Hybrid) cucumbers was planted in the greenhouse on October 3, 1972, on
48 x 18 in. spacings.  Plants emerged October 10.  By November 2,
cucumber seedlings were 2 to 3 in. tall.  Cool greenhouse temperatures
were not ideal for good cucumber growth, and the plants were removed
after the cold December period described in the lettuce section.
                                173

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                            SECTION VII
             MOLD COUNT, BACTERIA, AND MYCOTOXIN STUDY

Studies were conducted in cooperation with Dr. George Pigott to determine
if crops grown under different irrigation and/or soil heatinq conditions
would influence levels of mold, bacteria, or mycotoxins.

The objective of the study was to compare safety of raw crops grown
under four different conditions on the thermal irrigation test farm.

The samples were picked 4:00 to 4:30 D.ID., August 15, 1972, at the Pro-
ject's test plots and delivered to Schick Laboratories at 9:30 p.m.
The samples were olaced in a refrigerator at 9:50 p.m. and analyses was
started the next morning at 8:00 a.m.

The following is a description of how the samples were grown:

     Beets
          Soil heat              Cold water
          Soil heat              Warm water
          No soil heat           Cold water
          No soil heat           Warm water
     Beans
          Soil heat              Cold water
          Soil heat              Warm water
          No soil heat           Cold water
          No soil heat           Warm water
                                175

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      _'Willamette/  Tomatoes
           Soil heat                  No mulch
           No soil  heat               No mulch
           Soil heat                  Black plastic mulch
           No soil  heat               Black plastic mulch

      'Fireball'  Tomatoes
           Soil heat                  No mulch
           No soil heat               No mulch
           Soil heat                  Black plastic mulch
           No soil heat               Black plastic mulch

 Each sample (200-300g) was homogenized in a high speed blender from
 which aliquots were taken for analysis.  Aliquots of each homogenate
 were used for determination of aerobic plate count, most probably number
 of coliforms and Escherichia Coli.*  A second aliquot was used for cul-
 ture of yeast and molds in Sabouraud's medium.  A 100 gram aliquot was
 extracted with a chloroform-methanol mixture for aflotoxin and ochra-
 toxin assays.+

 Samples of homogenate were frozen for moisture and protein nitrogen
 determination.^  Initial results are outlined in Tables 28, 29, and 30.
*Microbiological Methods used are described in:  Official Methods of
 Analysis of the Association of Official Analytical Chemists (AOAC),
 Eleventh Edition, 1970.  pp. 839-852.
+Aflotoxin and Ochratoxins were determined by thin layer chromatography
 of Chloroform-Methanol extracts:  Fishbein, L. and Falk, H. L.  1970.
 Chromatography of Mold Metabolites, I. Aflotoxins, Ochratoxins and
 related compounds.  Chromatog. Rev, 12:  42-87.
'Moisture and protein nitrogen.  AOAC, llth ed., 1970, pages 272 and
 16-17.

                                  176

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Table 28.  MICROBIOLOGICAL RESULTS OF AEROBIC PLATE COUNT, COLIFORMS, E.  COLI, AND STAPHYLOCOCCUS

COUNTS MADE ON SELECTED VEGETABLES GROWN UNDER DIFFERENT IRRIGATION AND/OR SOIL HEATING CONDITIONS

Vegetable
Beets



Beans



Variety-
Willamette Tomatoes





Variety-
Fireball Tomatoes



Treatment
soil heat-cold water
soil heat-warm water
no soil heat-cold water
no soil heat-warm water
soil heat-cold water
soil heat-warm water
no soil heat-cold water
no soil heat-warm water

soil heat-no mulch
no soil heat-no mulch
soil heat-black plastic
mulch
no soil heat-black plastic
mulch

soil heat-no mulch
no soil heat-no mulch
soil heat-black plastic
Total Aerobic
Count/ gm
1200
800
500
700
700
500
600
900

600
900
400

600


600
500
700
Total
Col i forms
1
0
2
0
2
1
0
2

2
0
0

0


2
0
3
E.
Coll
0
0
0
0
0
0
0
0

0
0
0

0


0
0
0

Staph.
0
0
0
0
0
0
0
0

0
0
0

0


0
0
0
                        mulch
                      no soil heat-black plastic
                        mulch
600

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Table 29.  MOLD COUNTS OBTAINED ON SABOURAUD'S MEDIUM FROM SELECTED VEGE-

 TABLES GROWN UNDER DIFFERENT IRRIGATION AND/OR SOIL HEAT CONDITIONS.
     Vegetable
           Treatments
Colom'es/gm
Beets
Beans
Variety-
 Willamette Tomatoes
Vari ety-
 Firetail Tomatoes
soil heat-cold water                   5
soil heat-warm water                  10
no soil heat-cold water                4
no soil heat-warm water                6

soil heat-cold water                  15
soil heat-warm water                   4
no soil heat-cold water                8
no soil heat-warm water               10
soil heat-no mulch                    10
no soil heat-no mulch                 15
soil heat-black plastic mulch         10
no soil heat-black plastic mulch       4
soil heat-no mulch                    16
no soil heat-no mulch                 20
soil heat-black plastic mulch         20
no soil heat-black plastic mulch      14
                                178

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            Table 30.   PROTEIN AND MOISTURE ASSAYS  OF VEGETABLES  GROWN  UNDER  DIFFERENT  IRRIGATION  AND/OR SOIL



                                                    HEAT CONDITIONS
                        Vegetables
Treatment
vo
                                                                               Moisture
                                       Protein
Beets



Beans



Variety-
Uillamette Tomatoes



Variety-
Fireball Tomatoes



soil heat-cold water
soil heat-warm water
no soil heat-cold water
no soil heat-warm water
soil heat-cold water
soil heat-warm water
no soil heat-cold water
no soil heat-warm water-

soil heat- no mulch
no soil heat-no mulch
soil heat-black plastic mulch
no soil heat-black plastic mulch

soil heat-no mulch
no soil heat-no mulch
soil heat-black plastic mulch
no soil heat-black plastic mulch
85.5
84.2
86.3
84.8
90.1
38.9
89.5
89.2

94.2
95.1
95.0
93.7

95.4
95.2
94.6
95.6
1.56
1.48
1.57
1.58
2.20
2.15
2.14
2.10

0.91
0.92
0.90
0.93

0.95
0.94
0.89
0.96

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Gram stains were made of the principal  colonies in order to identify
them.  Principal organisms were aerobacter, aerogenes, and bacillus
subtilis.  Examination of the molds showed that Aspergillus niger and
Rhizopus nigricans were the principal  molds,

One hundred gram aliquots were used for aflotoxin and ochratoxin assays.
All 16 samples were negative for either aflotoxin, which are toxic
mold metabolites.

Regardless of the conditions under which the crop was grown, there was
no difference in the microbiological results, total mold counts, or the
general type of organism found under the four different conditions for
these particular vegetables.  There was no toxic mold metabolites as
determined by the absence of aflotoxins and ochratoxins in all  16 samples.

The nutritive quality of the vegetables grown under four different
conditions are the same as reflected by the similarity of the protein
nitrogen values and total moisture in the four samples for each vegetable.

It appears that the vegetables are safe and wholesome as indicated by
the low bacteria and mold counts in addition to the absences of E. coli
and staphylococcal organisms.  Further, the absence of mycotoxins
(aflotoxins and ochratoxins) confirm safety from mold contamination or
abnormal mold flora.

The protein nitrogen values and moisture content for each vegetable,
some grown under four different conditions, show no variations and are
in good agreement with published results.

Increased soil heat or the use of thermal water had absolutely no effect
                              v
on the mold or bacterial populations normally used as an indicator.
                                 180

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                             SECTION VIII

                         SOIL HEAT/IRRIGATION
PLOT DESCRIPTION
An area 216 ft long by 218 ft wide was used for this experiment.  An
area 120 ft by 216 ft was over the soil heating pipes.  On each side
was an area with no soil heat,  The total area was divided into 4 repli-
cations.  Each replication was divided into 4 plots; each plot measured
about 2400 sq ft and had the same crops but with a different combination
of treatments.  Treatments included soil heat vs no soil heat and cold
water irrigation vs thermal water irrigation.  Each replication had
2 plots off soil heat and 2 plots on soil heat.  Separating the plots
north and south (at right angles to the soil heat area) were 2 rows of
sweet corn cv. Jubilee.  This served as a barrier between the cold water
irrigation and thermal water irrigation treatments.

Irrigation pipe was laid along each side of the plot beside and parallel
to the corn rows.  Rain Bird 25A sprinklers with 3/32 in. nozzles were
spaced on 40 ft centers giving an overall, spacing of 40 ft x 40 ft.
Sprinklers were set for 180° rotation so only the plot area between corn
rows would be irrigated with a particular irrigation treatment, cold or
thermal water.
PROCEDURE

The following information applies to the entire area and any additional
details that apply to one particular crop will be covered in the discus-
sion of individual crops.

On May 20, 1972, fertilizer was applied in band form down the center of
each bed.  Row centers were 4 ft apart.  Fertilizers included 600 Ibs

                                 181

-------
16-20-0 per acre, 400 Ibs treble super phosphate per acre, and 83 Ibs
muriate of potash per acre.  Granular "Diazinon" insecticide was applied
in the same manner at the rate of 4 Ibs active material  per acre.  This
rate was used for control of wireworms as suggested in the 1971  Oregon
Insect Control Handbook.  Following application of the fertilizer and
insecticide, it was incorporated into the soil by rototilling.

In each plot, there were 9 different crops planted.  Each crop,  except
tomatoes, was planted in three 20 ft long rows spaced 4 ft apart.  *
There was only one row of each variety of tomato planted instead of
the 3 rows of each of the other crops.  Two rows of variety 'C.  1327'
were planted in Reps II and IV instead of 1 row 'C, 1327'  and 1  row
'H. 1350' due to short supply of variety 'H.  1350.'

Crops were:

           bush beans                    Blue Lake 274
           tomato                        New Yorker, C.  1327, &  H.  1350
           pepper                        Calwonder
           cabbage                       Golden Acre
           onion                         Yellow Globe Danvers
           lima (baby)                   Thaxter
           beets                         Detroit Dark Red
           celery                        Utah #15
           cucumber                      Pioneer

Bush beans, limas, onions, celery, cucumbers, peppers, and tomatoes were
planted with a Planet-Jr. on May 25.

On May 26, the red beets were planted; the cabbage was planted June 5.
A Panet-Jr. seeder was used for both crops.

The celery seed did not germinate properly so there was no celery crop
to harvest.  Shortly after the other crops began to emerge, flea beetles
                                182

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and cucumber beetles began doing some damage to certain of the seedlings.
On June 21, all crops were sprayed with the insecticide Sevin 50 W at a
rate of 1 Ib active material per acre, mixed at rate of 100 gals water
per acre.

Tensiometers were placed at several locations in rows of peppers both
on and off soil heat.  Each location included three tensiometers, at
depths of 6, 12, and 18 in.  Readings were taken regularly (Figure 65)
and were used to aid in the scheduling of irrigations.

When irrigations were made, cold well water (50-55°F) and thermal water
(98-118°F) were applied at the same tiime and quantities (Table 31).

Tomatoes and cucumber seedlings were thinned on June 28.  The tomatoes
were at approximately the 4th to 5th true leaf stage and were thinned to
a spacing of one to two plants per 12 in. of row.

The crops were again sprayed with Sevin 50 W at the rate of 1 Ib active
material per acre on July 4.  Spraying was primarily for the control of
flea beetles and cucumber beetles.  A few hornworms were noted on some
of the tomato plants but populations and damage were not great enough to
merit a special spray program for their control.

Weeding of the area was done by pulling or hoeing.  No herbicides were
used due to the many varieties of crops grown in a small area.

On July 17, cabbage plants were thinned to 15 in. apart; they were 5 to
7 in. tall and had five to six true leaves at thinning.  The peppers
were thinned the same day at the same spacing as the cabbage (15 in.
apart); they were 4 to 5 in. tall and at the four to five true leaf
stage.

Several root maggots were observed on some of the young cabbage plants;
however, the problem wasn't severe enough to warrant a special spray
program.
                                183

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Figure 65:   Tensiometer

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Table 31.  PRECIPITATION AND IRRIGATION, BOTH THERMAL AND COLD WATER,
APPLIED (INCHES) TO PLOTS DURING JUNE, JULY, AND AUGUST.
June 2
7
8
9
10
n
15
22
29
.55
.08a
.49a
.68a
.59a
.05a
.02a
1.00
1.20
July 8
8
14
29
August 9
14
16
20
29
.55
-06a
1.10
1.50
2.00
.02a
1.41a
.27a
1.50
Values followed by a were rainfall, others were irrigation applications,
                              185

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Two more sprayings of the crops with Sevin 50 W were carried out (July 7
and August 3) during the rest of the growing season.  The insecticide
was applied at the rate of 1  Ib active material  per acre, but instead of
mixing it with 100 gal  water, it was concentrated to 1  Ib active material
per 20 gal water per acre.

On August 16 and 17, foliar samples were taken from several  of the  crops
and analyzed for N, P,  K, Ca, Mg, Zm, and Mn.   Samples  consisted of:

        Table beets—Petiole  of mature leaf, not from leaves that
        were very old or showed signs of drying
        Onions—Mature  leaf but not those that were dried
            i
            i
        Peppers—4th mature leaf down from tip of plant
        Lima beans—4th trifoliate leaf
        Cabbage—Mid-rib of wrapper leaf

Cucumbers
A 10 ft section of one  row in each plot was harvested seven  times during
the period July 26 to September 7.  After each harvest, the  cucumbers
from each plot were counted,  weighed, and graded into six classes—
Nos. 1, 2, 3, over 3, crooks, and nubs and culls.
Snap Beans
Two harvests were made of a 5 ft section  from one  row  in  each  plot.
The plants from the 5 ft section were pulled and all the  beans were
taken at each harvest.  This simulated a  typical machine  harvesting
operation.  The beans were taken immediately to Oregon State University
and run through a commercial-type bean grader.  Beans  were  graded  out
into five classes and each was weighed separately.   Classes (accord-
ing to seive size) were as follows:   1-2, 3, 4, 5,  and 6-7.  The harvest
dates were July 31 and August 2, 1972.
                                 186

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Cabbage was harvested on two dates as the heads became mature—August 24
and September 11, 1972.  The heads from a 15 ft section of one row in
each plot were harvested, counted, and weighed.  A grading system was not
used.

Peppers
Peppers were harvested on September 18 and November 8, 1972; a 10 ft
section was taken from one row in each plot.  Harvested fruit were weighed,
counted, and graded in classes of U.S. Fancy, No. 1, No. 2, and culls.

Tomatoes
On August 26 the tomatoes were sprayed with the fungicide Maneb.   It
was applied at the rate of 3 Ib Maneb, mixed in 20 gal water per acre.
It was applied for the control of Early Blight.  There were three harvests
of the variety 'New Yorker1—September 20, October 6, and October 27,
1972.  Varieties 'H. 1350' and 'C. 1327' were harvested only two times,
October 6 and October 27, 1972.  A 10 ft section of each variety in
each plot was harvested.  Fruit from each plot were weighed, counted, and
classed as U.S. No. 1 and No. 2 canning and culls.
        " '      -'        •'    ,i
Lima Beans
A 10 ft section from each plot was harvested on September 22, 1972.
The beans from each plot were shelled and weighed.  Grading was not done.
                   '{'•
Onions
On October 4, 1972, a 10 ft section of one row of onions in each plot
was harvested, weighed, counted, and graded into three classes:  U.S.
No. 1, No. 2, and culls.
                                  187

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                  TABULAR DATA:  SOIL HEAT/IRRIGATION
Table

 32.     Nutrient Levels (Dry wt Basis)  of Selected Vegetable Crops
         from Soil Heated and Control  Blocks

 33.     Effect of Soil Heat on Yield  of 'Thaxter1  Lima Beans

 34.     Effect of Heated Soil on Yield  of Table Beet,  cv.  Detroit
         Dark Red

 35.     Influence of Heated Soil and  Thermal  Irrigation on Yield  of
         Snap Beans, cv. Bush Blue Lake  274, on  Two Harvest Dates

 36      Effect of Soil Heat on Yield  and Grade  of  Tomato cvs.  H.  1350,
         C. 1327, and New Yorker

 37.     Effect of Soil Heat on Yield  and Grade  of  Pickling Cucumber,
         cv.  Pioneer Hybrid

 38.     Effect of Soil Heat on Grade  and Yield  of  Onions,  cv.  Danvers
         Yellow Globe

 39.     Effect of Soil Heat on Yield  'Golden  Acre1  Cabbage
                                188

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00
                                    Table  32.  NUTRIENT LEVELS  (DRY MT BASIS) OF SELECTED VEGETABLE CROPS FROM SOIL HEATED AND CONTROL BLOCKS.
                                                                      (SAMPLES TAKEN AUGUST 16 and 17. 1972).
                                                                            OREGON STATE UNIVERSITY
£EETS* ONIONS"
Soil heat Control
Total
N (%)
P W
K W
Ca (%)
Mg {»)
2n (ppat)
Mn (ppm)

2.77
0.49
5.66
0.07
U?
30
95

2.78
0.51
6.46
0.07
1.20
36
90
Soil heat Control

4.68
0.41
3.32
0.17
0.55
25
72

4.62
0.43
3.76
0.16
0.49
28
lOp
SNAPBEANSV
Soil heat

5.09
0.47
3.42
0.23
0.67
45
93
Control

5.06
0.44
3.42
0.19
0,62
39
90
PEPPERS*
Soil heal

5.79
0.46
4.99
0.19
1.00
112
263
t Control

5.69
0.42
4.89
0.19
0.97
105
242
LIMA
Soil heat

5.02
0.34
2.49
0.36
0,70
42
100
BEANS):
Control

4,21
0.33
2.42
0.30
0.63
75
144
CABBAGE*
Soil heat Control

4.11
0.68
4.12
0.23
0.49
42
70

4.23
0.69
4.66
0.22
0.49
39
69
SWEET CORN2
Soil heat Centre 1

3.52
.42
2.68
.08
.26
41
77

3.33
0.33
2.57
0.07
0.33
42
61
                                      Samples consisted of:
                                      t  petiole of mature, but not old leaf
                                      u  mature leaf-taken before drying starts
                                      v  4th trifoliate leaf
                                      w  4th mature leaf down from tip
x  4th trifoliate leaf
y  midrib of wrapper leaf
z  midrib from center section of mature leaf

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Table 33.  EFFECT OF SOIL HEAT ON YIELD OF 'THAXTER1  LIMA BEANS.
                             Lbs/10 ft plot

Treatment
Soil heat
Control

Fresh plant
wt
10. 3a
7.4b

Fresh pod Ungraded shelled bean
and bean wt
10. 3a
8.9a

wt
4. la
3.2b
'-, ' V r- -,
 Means within a column followed by different letter differ signifi-
 cantly at 5% level; means followed by same letter are not signifi-
 cantly different.
                                  190

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Table 34.  EFFECT OF HEATED SOIL ON YIELD OF TABLE BEET,  CV.  DETROIT

                              DARK RED2
Treatment
                                        Lbs/acre
 Larger than
1-1/2 in.  dia
Smaller than
1-1/2 in.  dia
Soil heat
Control
623a
431 b
8389a
9150a
zMeans followed by different letters significantly different at 1%
 level.
                                 191

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Table 35.   INFLUENCE OF HEATED SOIL AND THERMAL IRRIGATION ON YIELD

    OF SNAP BEANS, CV.  BUSH BLUE LAKE 2/4,  ON TWO HARVEST DATES
     Treatments
                           July 31, 1972,  Harvest
                              % seive size
  Avg No.          Yield      distribution
plants/ft row    tons/acre    1-4   5   6-7
     Soil heat

     Control
     7.3

     7.2
   4,0        80   10   10

   4.4        75   25    0
                           August 2,  1972,  Harvest
     Treatments
  Avg No.
pi ants/ft row
   Yield .
tons/acre^
% seive size
distribution
1-4   5   6-7
     Soil  heat

     Control
     7.2

     6.6
   8.7e.       45   40  15

   4.8b       60   30  10
"Means followed by different letters significantly different at 1% level
                                192

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Table 36.  EFFECT OF SOIL HEAT ON YIELD AND GRADE  OF TOMATO  CVS.  H  1350,

                         C. 1327, AND NEW YORKER2
H. 1350

Treatment
Soi 1 heat
Control
C. 1327


Soil heat
Control
New Yorker


Soil heat
Control

Fresh wt
No. 1 Mo. 2
5.5a 13.7
11. 7b 15.5

Fresh wt
No. 1 No. 2
7.6 13.7
7.2 15.1

Fresh wt
No. 1 No. 2
^17.3 24.5
16.3 20.8

in tons/ acre
Green Culls
21.7 20.3
20.6 36.8

in tons/acre
Green Culls
18.1 26.5
18.3 19.5

in tons/ acre
Green Culls
5.4 18.7
4.2 15.6


Total
61.7
34.6


Total
65.0
60.1


Total
66.0
57.4
zMeans within a column in each series followed by different letters dif-
 fer significantly at 5% level; other means nonsignificantly different.
                                 193

-------
Table 37.  EFFECT OF SOIL HEAT ON YIELD AND GRADEX  OF PICKLING
                 .CUCUMBER, CV.  PIONEER HYBRID.2
                          Tons Cucumbers/avfl

                  No.  1    No.  2   No.  3    d Nubs    Culls

     Soil heat    3.2a    12.la    9.la    10.9a     3.5a

     Control      3.6b    15.2b   11.9b    10.3a     2.7a
^
 Grades based on diameter:   No.  1  (under 1  in.  dia),  No.  2  (1 to
 1-1/2 in. dia), No.  3 (1-1/2 to 2 in.  dia).


zMeans within a column followed  by different  letters  differ sig-
 nificantly at the 5% level.
                                194

-------
Table 38.  EFFECT OF SOIL HEAT ON GRADE  AND YIELD OF ONIONS,  CV.

                      DANVERS YELLOW GLOBE



                                 Ibs/acre
                      U.S.         U.S.
                      No. I        No. 2        Culls

     Soil heat        12660        1231          48

     Control          12712        1343         464
                              195

-------
Table 39.  EFFECT OF SOIL HEAT ON YIELD 'GOLDEN ACRE1 CABBAGE
                                  cwt/acre
                     Soil heat       253

                     Control         284
                         196

-------
                               SECTION IX
                               REFERENCES

 1.   Technology Review (MIT),  November 1971.

 2.   AEC Public Information Announcement No. 623, January 25, 1973.

 3.   J.  K.  Ballard.   Frost and Frost Control in Washington Orchards.
     Extension Bulletin 634.  Washington State University, 1972.

 4.   J.  K.  Ballard.   Tree Fruit Newsletter.  Yakima County Extension
     Service, Yakima, WA, January 1969.

 5.   C.  B.  Cordy.  Frost Protection in Pear Orchards with Over-Tree
     Sprinklers. Co-op Extension Service Special Report 196.  Oregon
     State University.

 6.   J.  K.  Ballard,  E. L. Proebsting, and  R. B. Tukey, Cherries—
     Critical Temperatures for BTIossom Buds. Extension Circular 371.
     Washington State University, 1971.

 7.   J.  K.  Ballard,  E. L. Proebsting, and  R. B..Tukey.  Pears—Critical
     Temperatures for Blossom Buds. Extension Circular 370.  Washington
     State University, 1971.

 8.   J.  K.  Ballard,  E. L. Proebsting, and  R. B. Tukey,  .Apples—Criti-
     cal Temperatures for Blossom Buds. Extension Circular 369.  Wash-
     ington State University, 1971.

 9.   J.  K.  Ballard,  E. L. Proebsting, and  R. B. Tukey.  Peaches—Critical
     Temperatures for Blossom Buds. Extension Circular 373.  Washington
     State University, 1971.

10.   Oregon Crop-Weather Summary Report.   U.S.D.A.  Statistical  Reporting
     Service, Portland, OR, April 6, 1970.

                                 197

-------
11.  Oregon Crop-Weather Summary Report.   U.S.D.A.  Statistical  Reporting
     Service, Portland, OR,  April  13,  1970.
                                                             ' I '
12.  Climatological  Handb^^^                                        Vol.  1,
     Part A.  Pacific Northwest River  Basins  Commission,  Vancouver, WA,
     1968.

13.  E. L. Proebsting and H. H. Mills.   "A Comparison  of  Hardiness Re-
     sponses in Fruit Buds of 'Bing1 Cherry and  'Elberta'  Peach",  Journal
     of the Amejr^^                                   Vol.  97, No. 6,
     1972, pp. 802-806.

14.  H. B. Schultz and J. V. Lider.  Frost Protection  wHh Overhead
     Sprinklers. Extension Leaflet 201.   University of California, 1968.

15.  J. W. Wolfe.  Sprinkling[for^ Frosj:  Prot^ection, Experiment  Station
     Special Report 280.  Oregon State University,  1969.

16.  C. B. Cordy.  Frost Protectioni_J_n Pear^Orchards wjth  Over-tree
     Sprinklers, Experiment Station  Special Report  196.   Oregon State
     University, 1965.

17.  F. A. Brooks.  Agrioilture Engineer's Handbook.  McGraw-Hill, New
     York, 1961, pp. 532-534.

18.  D. 6. Watts, C. R. Dehlinger, J.  W.  Wolfe,  and M.  N.  Shearer.
     Consumptive Use jaf New Irrigation A6^.^!^^^!!^^^?1,* Agri-
     culture Experiment Station Circular of Information 628.  Oregon
     State University, 1968.

19.  Soil Survey of tjie Eugene Area. Oregon,  U.S.D.A.  No.  33 Series,  1925.

20.  LaneCountyjJSpij1j Survey Area, Form  0. R.  127.   Lane  County Soil
     Conservation Service, Eugene, OR.
                               198

-------
21.  K. R. Frost and H. C. Schwalen.  "Sprinkler Evaporation Losses,"
     Agricultural Engineer. Vol. 6, No. 8, 1955, pp.  526-528.

22.  C. H. Pair, J. L. Wright, and M. E. Jensen.  Sprinkler Irrigation
     Spray Temperatures. Transactions of the ASAE, Vol.  12, No.  3,  1969,
     pp. 314-315.

23.  Leif Verner.  A New Kind of Dendrometer. College of Agriculture
     Experiment  Station Bulletin 389.  University of Idaho, 1962.

24.  Leif Verner, et al.  Trunk Growth as a Guide in  Orchard Irrigation.
     College of Agriculture Research Bulletin 52.  University  of Idaho,
     1962.

25.  Ceel Van Den Brink and Robert L. Carol us.  Removal  of, Atrnospher i c
     Stresses from' PjAn_^^                               Michigan
     Agricultural Experiment Station Quarterly Bulletin, Vol.  47, No. 3,
     1965, pp. 358-363.

26.  Claude H. Pair, et al.  "Environmental Control," Sprinklejr  inriCa-
     tion.  Sprinkler  Irrigation Association, Washington, DC,  1969,
     pp. 345-349.

27.  L. Boersma.  "Nuclear Waste Heat Could Turn Fields  Into Hotbeds,"
     Crops and Science. Vol. 22, No. 7, 1970, pp. 15-16.

28.  F. C. Raney and Y. Mihara.  "Water and Soil Temperature," Irriga-
     tion of Agricultural Lands.  R. M. Hayan, H. R.  Haise, and  T.  W.
     Edminster, ed., American Society of Agronomy, Madison, WI,  1967,
     pp. 1024-1036.

29.  R. A. Shroeder.  The Effect of Root Temperature Upon the Absorp-
     tion of Water by the Cucumber. PhD Thesis,  University of Missouri,
     1938.
                               199

-------
30.  S. J. Richards, R.  M.  Hagan, and T.  M.  McCalla.   Soil Temperature
     and Plant Growth—Soil Physical  Conditions  and  Plant Growth.
     B. T. Shaw, ed., Academy Press,  Inc., NY,  1952,  pp. 303-480.

31.  W. Barr and H.  Pellett.   "Effect of Soil Heat on Growth  and  Develop-
     ment of Some Woody  Plants," Journal  of the  American Society  of
     Horticultural Science, Vol. 97,  No.  5,  1972,  pp. 632-635.

32.  0. W. Carncross. American Tomato Yearbook> Vol. XXI.  C.  Stedman
     MacFarland, Jr., Westfield, NJ,  1969.

33.  R. N. Rosenthal, C. G. Woodbridge, and  C. L.  Pfeiffer.   "Root
     Temperature and Nutrient Levels  of Chrysanthemum Shoots,  " Horti-
     cultural Science. Vol. 8, No.  1, 1973,  pp.  26-27.

34.  G. T. Nightingale.   "Effects of  Temperature on  Metabolism  in Tomato,"
     Botanical Gazette.  Vol.  95, 1933, pp. 35-38.

35.  H. A. Knoll, N. C.  Brady, and D. J.  Lathwell.   "Effect of  Soil
     Temperature and Phosphorus Fertilization on Growth and Phosphorus
     Content of Corn," Agronomy Journal,  Vol. 56,  1964, pp. 145-167.

36.  R. L. Carol us.   "Calcium and Potassium  Relationships in Tomatoes
     and Spinach," Proceedings of the American Society of Horticultural
     Science, Vol. 54, 1949,  pp. 281-285.

37.  K. F. Nielsen,  et al.   "The Influence of Soil Temperature  on Growth
     and Mineral Composition  of Corn, Bromegrass,  and Potatoes,"  Pro-
     ceedings of the Soil  Science Society of America, Vol. 25,  1961,
     pp. 369-372.

38.  A. N. Roberts and A.  L.  Kenworthy.  "Growth and  Composition  of
     Strawberry Plant in Relation to  Root Temperature and Intensity of
     Nutrition," Proceedings  of theAmerican Society  of Horticultural  ?
     Science, Vol. 68, 1956,  pp. 157-168.

                                 200

-------
39.  L. Boersma.  "Warm Water Boosts Crop Yields," Oregon's Agricultural
     Progress. Oregon State University, Fall 1970.

40.  E. L. Probesting.  "The Effect of Soil Temperature in Mineral
     Nutrition of Strawberry," Proceedings of theAmericanSociety  of
     Horticu1tural Sci ence. Vol. 69, 1957, pp. 279-281.

41.  E. W. Roberts.  Cantaloupes, Fruit and VeqetablIe Facts and Pointers .
     United Fresh Fruit and Vegetable Association, Washington, DC,  1959.

42.  Portland Fresh Fruit and Vegetable Wholesale Market Prices. U.S.D.A
     Consumer and Marketing Service, Fruit and Vegetable Division,  Market
     News Branch, Portland, OR, 1972.

43.  "Fresh Fruit and Vegetable Market News," Port!and Daily Report.
     U.S.D.A. Agriculture Marketing Service, Vol. LVV, No. 33.

44.  S. H. Wittwer, S. Honma, and W. Robb.  Practices for Increasing
     Yields_Af1-xGr^j^_sje_j-_ettyc_e> Agricultural Experiment Station
     Research Report 22.  Michigan State University,  East Lansing.

45.  Weekly Weather and Crop Bulletin.  Lucius W. Dye, ed., U.S. Dept.
     of Commerce—U.S. Dept. of Agriculture, Vol, 59, 1972.

46.  C. E. Magoon.  Tomato—Fruit and Vegetable Facts and Pointers.
     United Fresh Fruit and Vegetable Association, December 1969.

47.  J. W. Courter, et al.  The Feasibility of Growing Greenhouse Tomatoes
     in Southern 111inois, Co-op Extension Service Circular 914.  University
     of Illinois, College of Agriculture, 1965.

48.  John Wiebe.  Greenhouse Vegetable Production in Ontario. Ontario
     Ministry of Agriculture and Food Publication 526.

                                201

-------
49.  Preliminary Greenhouse Cucumber Variety Trial  Studies  (Unpublished).
     Horticulture Research Institute of Ontario,  1970-1972.

50.  Hunter Johnson.   Greenhouse Vegetable  Production, One-Sheet Answer
     Series, OSA #249.  University of California, Riverside.

51.  Merle H. Jensen.   "Take a Look at Seedless Cukes," American Vegetable
     Grower.  Meister  Publishing Co., Willoughby, OH, 1971, p. 20.
                                 202

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                             SECTION X

                            APPENDICES
                                                             Page

A.     Economics Data                                         204

B.     Letters of Endorsement                                 211

C.     Water Analyses                                         214

D.     Soils Map                                              233

E.     Technical Rationale                                    234
            Area Water and Power Requirements                 234
                                203

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o
                                              TABLE A-l

                          ANNUAL COST/ACRE FOR CROP PROTECTION AND IRRIGATION

                                                                                             Total Annual
                      Frost Protection          Irrigation            Plant Cooling            Fixed Cost
	System	(Per Acre Per Year)    (Per  Acre Per Year)     (Per Acre Per Year)     (Per Acre Per Year)


Multi-use                  	                	                 	                $82.81



Solid Fuel Plus Irrigation	                $20.385^)             Not Possible              20.385



Central Distribution       $71.3470)            20.3850)             Not Possible              91.732
(1)  Based upon a capital recovery factor of 0.1359  (10-year amortization at 6% interest)

-------
rv>
o
01
                                           TABLE A-2


               ANNUAL OPERATIONAL COST FOR CROP PROTECTION AND IRRIGATION SYSTEM




                                                   Solid Fuel & Hand-        Central Distribution
System Cost                                        Moved Irrigation          & Hand-Moved Irriga.

Factor/Acre	Multi-use	Cost per Acre                Cost per Acre




Frost Protection                   $ 1.16              $250.00                      $280.00


Power/Fuel                           1.80                 2.57                         2.57





Irrigation & Plant Cooling



Pawer                                4.64                 3.48                         3.48


Labor                                3.60                 9.00                         9.00
          TOTAL ANNUAL COST/ACRE             $11.20             $265.00                      $295.00

-------
                                           TABLE A-3

           TOTAL ANNUAL COST PER ACRE FOR THREE CROP PROTECTION AND IRRIGATION SYSTEMS
System
Annual Fixed
   Cost
Annual Operational
   Cost per Acre
Total Annual
    Cost
Multi-Use
Solid Fuel & Hand-Move
Irrigation
Central Distribution
& Hand-Move Irrigation
   $82.81
    20.385
    91.732
     $ 11.20
      265.05
      295.05
  $ 92.74
   285.435
   386.782

-------
                                 TABLE A-4


Calculations for annual operational costs/acre for crop protection and irrigation.
A.   Multi-use System
     1.   Frost  Protection:   Annual Pumping (Ibs H?0) x total head (ft)  $	
          a)  Power cost1 = 1,980,000 ft-lbs x 1.34~hp x efficiency    X KWH
                                         H        KW
                                         hp
                             75.751.200x170         m = $80 89/orchard
                           « 1,980,000 x 1.34 x .60  * '01   $80-8(9o/°rchard

                                                            80^80 = $1l6/acre

              Annual  pumping = 54 gpm/acre x 70 acres x 60 min/hr x 40 hrs x 8.35 Ibs/-
                                 gal = 75,751,200 ibs water
              Overall efficiency = 60%
              Total head= 170ft
          b)   Labor cost = assuming time is equal  to  that required for one complete irri-
              gation with a hand-move system as  in Part 82 = 0.9 man hrs/acre x $2.00/man
              hr = $1.80/acre
     2.   Irrigation and Plant Cooling:
          a)  Power cost — same formula as above
              Assuming  five 24 hr  irrigation and ten 4 hr plant cooling periods during the
              summer season at 54 gpm = $4.64/acre
          b)   Labor cost — assuming time is equal to  that required for two complete irri-
                fationswith a hand-move system as in Part B2 = 0.9 x $2.00 x 2  irrigations —
                3.60
B.   Soiid Fuei  & Hand-Move irrigation System
     1.   Frost  Protection:
          a)  Fuel - $50.00 worth of material/night x 5 nights = $250.002
          b)  Labor — assuming 6 men are needed for 3 hrs/night/70 acre orchard
              6 men x 3 hrs/night x 5 nights x $2.00/man hr x 1/70 acres = $2.57/acre
     2.   Irrigation:
          a)  Power — same as for irrigation in Part A, rate of application of water only
              differs = $3.48/acre
          b)  Labor1  -  0.9 man hrs/acre/irrigation
              Assuming  labor at $2.00/hr and 5 irrigations/season
              0.9  man hrs/acre/irrigation x  5 irrigations/$2.00/man hr = $9.00/acre
C.   Central Distribution & Hand-Move  Irrigation System
     1.   Frost  Protection:
          a)  Fuel3  - 40 heaters/acre x 1 gal/heater/hr x 40 hrs  x 17.5«f/gal  = $280.00/acre
          b)  Labor — assuming 6 men are required for 3  hrs each night for a 70 acre orchard4
              6 men x 3 hrs x 5 nights x $2.00/man hr x 1 /70 acres = $2.57/acre
     2.   Irrigation
          a)  Power - same as Part B = $3.48/acre
          b)  Labor - same as Part B = $9.00/acre

1 Jensen (1966) listed in Reference Section
2 From information in advertisements and articles in February, 1963 and February, 1971 American Fruit Grower, Western Edition
3 Anon., 1968 - listed in Reference Section
4 Anon., 1968 - listed in Reference Section
                                        207

-------
                                                    TABLE A-5
ro
o
oo
                        ITEM                                              DOLLARS/SQ FT
Materials for framework
Labor to erect framework and attach film
Plastic film (UV "Poly")
Structure Sub-total
Thermal water heating & ventilation system
Electric Wiring
Environmental Control Sub-total
$0.222
0.082
0.029

0.492
0.038




$0.333


0.530
                                                           Bal. Fwd.
              Irrigation System                                               0.078        0.078
              Contingency Factor (20%)                                        0.188        0.188
                                                           TOTAL COST/SQ FT               $1.129

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ro
o
10
                                                   TABLE A-6


                                CROP VALUE USING WHOLESALE PRICE IN PORTLAND, OR
Harvest Date
April 24, 1972

July 14-
Sept. 12, 1972



Type of Produce
Lettuce—Grand Rapids
Lettuce—Bibb
Tomatoes— H.I 439
— H.1350
Fireball
Willamette
Min/Price/Acre
$ 5,437
8,478
27,693
13,311
12,587
11,788
Max/Price/Acre
$ 8,192
15,109
37,424
15,104
14,283
13,376
        May 12-

          Sept. 11,  1972        Japanese  Salad Cucumbers             156,400                273,700

-------
                         TABLE A-7
           SELECTED  CROPS—MINIMUM RETURN $  (1972)
         Crop                              Price per Acre

Lettuce—Grand Rapids                          $  5,437
Tomatoes—H.I439  (See comments on xxxii)
Japanese Salad Cucumbers                        156,400
               Gross Return                    $161,837

           SELECTED CROPS—MAXIMUM RETURN $  (1972)

         Crop                              Price per Acre

Lettuce—"Bibb"                               $15,109
Tomatoes—H.I439  (See comments on xxxii)
Japanese Salad Cucumbers                        273,700
               Gross Return                    $288,809

-------
               i:<[ i
              ^ *. ' . a
                            73
OFFICE OF THE GOVERNOR

     STATE CAPITOL

      SALEM 973IO
TOM McCALL
 GOVERNOR
                                           June 7, 1973
 Mr.  Byron Price
 General Manager
 Eugene-Water & Electric Board
 P.  0.  Box 10148
 Eugene, Oregon  97401

 Dear Byron:

           I  take this opportunity to congratulate you and
 the Eugene Water & Electric Board for a significant research
 effort in your warm water studies.

           The Springfield warm water demonstration project
 pioneered by the Eugene Water & Electric Board has proved
 the value of warm industrial waste water for agricultural
 uses.             '                     ff-

           This project utilizing warm water for frost protection,
 soil heating and irrigation will have far-reaching effects on
 future agri-nuclear projects.

           The information gained by this endeavor will
 encourage close cooperation between the power industry and
 agriculture  in developing nuclear thermal power plants
 in  conjunction with agricultural irrigation projects.

           Your pioneering efforts in the field of warm
 water utilization will have far-reaching benefits to the
 economy of Oregon.
                                    Sincerely,
                                    Governor
 TM:cs
                             211

-------
                      KM.P jV'
                   Fiinr. •  .•,
      CECIL D. ANDrtUS:
         GOVERNOR
                      -8
IDAHO NUCLEAR ENERGY
DONALD J. MACKAY, CHAIRMAN -. IDAHO FALLS

ALBERT E. WILSON. VICE CHAIRMAN -• POCATELLO

EUGENE P. BERRY - BLACKFOOT

ROBERT M. BRUGGER - IDAHO FALLS
                               STATE OF  IDAHO
                                          OFFICE OF
                                  NUCLEAR ENERGY DEVELOPMENT


                                     May 21.  1973
 GENE P. RUTLEDGE
  EXECUTIVE DIRECTOR

     STATEHOUSE
  BOISE, IDAHO 83707


    P. O. BOX 2234
IDAHO FALLS, IDAHO 834OI
TELEPHONE 208.923.2886
       Mr.  Byron  Price,  General  Manager
       Eugene  Nater and  Electric Board
       P. 0. Box  1112
       Eugene, Oregon 97401

       Dear Byron:

       It certainly was  a pleasure to see you in Boise a few days ago at the
       Energy  Symposium  sponsored by our University of Idaho.

       During  this  session it became more and more apparent that our energy
       needs are  going to climb  swiftly in the near future and that the amount
       of reject  (or waste) heat will also get greater and greater.

       I would like to commend you for your effort on the agricultural
       utilization  of hot water  from the industrial plant near Springfield,
       Oregon. Our office is trying to do something similar in Idaho, albeit
       on a much  more modest scale.  Therefore, I plan to read the final
       report  of  your thermal water demonstration project in detail.

       I hope  that  more  people will follow your lead in an effort to utilize
       the  potential  energy that is tied up in our industrial and nuclear
       thermal  effluents.

                                            Yours truly,
                                            Gene P.'Rutledge
                                            Executive Director
       GPRem
                                            212

-------
                          P.O.  BOX 15038  •  LAKEWOOD,  COLORADO  80215  •  (303) 238-8383
DR. ALFRED T. WHATLEY
   Executive Director
                 May 9,  1973
                 Mr.  Byron Price, General  Manager
                 Eugene Water and Electric Board
                 P. 0.  BOX 1112
                 Eugene, Oregon  97401

                 Dear Mr. Price:

                 Our  Western Interstate Nuclear Board 1s very Interested In the
                 meaningful utilization of warm water from Industrial  (especially
                 nuclear) plants.  This Interest 1n our WINB has been  so strong
                 that we formed a Thermal  Effluents Application Committee which
                 Is addressing Itself to the utilization of these low  grade BTU's.

                 As 1t now stands, our projects that are underway will utilize
                 the  Information that you have gained during your Thermal Water
                 Demonstration Project  near Springfield, Oregon.

                 Your 1nter1um progress reports have been very valuable to us,
                 and  we are anxious to  study your final report.

                 Our  Western Interstate Nuclear Board appreciates the  many con-
                 siderations that you have shown to our board representatives.
                 We also express our pleasure at the foresight that you and your
                 associates have shown.
                 Yourj truly,
                 Donal
                 Chairman
                 Western Interstate Nuclear Board

                 DCG/cm
                                                 213

-------
                                GENERAL LABORATORY REPORT
          Sample Source:   Weyerhaeuser Corporation     No:    A-105-1
                           Springfield, Oregon
                                                        Date:  September 5, 1968

          Material:        Cooling Water                By:    Vitro Corporation
                                   Physical Properties


          General Appearance:   Clear

          Odor:                 None



                                         Analysis


          pH                                            6.8

          P Alkalinity                                  0.0  ppm

          M Alkalinity                                 37.0  ppm

          Total Solids                                 86.0  ppm

          Suspended Solids                           Trace

          Dissolved Solids                             86.0  ppm

          Calcium as Ca                                 6.4  ppm

          Magnesium as Mg                               3.8  ppm

          Sodium as Na                                  4.6  ppm

          Iron as Fe                                    0.05 ppm

          Phosphate as .PO^                              0.0  ppm

          Chloride as Cl                                3.6  ppm




                                             Signature    Lee Henry
                                             Date	9-13-68
WATER TREATMENT CORP. OF AMERICA - 2852 N. W. 31st Ave., Portland, Ore. - Phone  (503) 226-1451

                                              214

-------
                                                REPORT
                   ViTRO CORPORATION OF AMERICA
   Sample  Source:  22%k OaUont Way
                   Eugene. Oregon    97^02
                   ATTN:  Mr. Col in Nilsson
   Haterial:       Weyerhaeuser Coo!ing Water
                                   No:   A-212-2
                                   Date: 8-25-69
                                   By:   Vitro Corporation
                              Physical  Properties
    General  Appearance:  Clear
    Odor:
None
                                      Analysis
                   PH
                   P Alka!inity as CaCO,
                   M Alkalinity as CaCO,
                   !otal Sol ids
                   Suspended Sol ids
                   D is solved Sol ids
                   Calcium as Ca
                   Magnesium as Mg
                   Sodium as Na
                   Iron as Fe
                   Phosphate as PO,
                   Chloride as Cl
                             7-1
                             0.0
                            29.0
                            71.0
                             8.0
                            63.0.
                             4.0
                             2.2
                             3.8
                             0.1
                             0.0
                             1.6
                   NOTE:  The above results are reported in
                          mg/1 (ppm) with the exception of pH
 E-2
              (215)
                                              Signature
                                              Oate
WATER TREATMENT COW, OF AMERICA - 2852 N.W. 31st Ave.. Portland. Ore. - Phone {503i 226-1^3!

-------
         WATER TREATMENT PRODUCTS AND SERVICES SINCE 1915
             The
                       Corporation
         EXECUTIVE OFFICES • 2O6OO CHAGRIN BLVD. • CLEVELAND, OHIO
     June  15,  1970
                                              Reply to:
                                              Watcoa Division
                                              2852 N. W. 31st Avenue
                                              Portland, Oregon 87210
     Mr. Dick Tipton
     Vitro Hanford Engineering Services
     2284  Oakmont Way
     Eugene,  Oregon  97401
     LABORATORY REFERENCE NO.
                     A-314-A, A-314-B
     Dear Mr.  Tipton:

     The following information summarizes the  results  we obtained
     from the  McKenzie River water and the pumping  pit samples
     we received in our laboratories on June 11,  1970.

                     MCKENZIE RIVER WATER ANALYSIS

                     pH                         7.2
                     P Alkalinity as CaCO3      0.0
                     M Alkalinity as CaCO3    30.0
                     Total Solids             19.0
                     Suspended Solids           3.0
                     Dissolved Solids         16.0
                     Calcium as Ca              3.5
                     Magnesium as Mg            2.0
                     Sodium as Na               3.7
                     Iron as Fe                 1.0

                     Phosphate as P0>           1.27
                     Chloride as Cl             0.9
                                    216
         Plants
Chagrin Falls. Ohio
Charlotte. North Carolina
Arlington, Texas
Phoenix, Arizona
    Canada
Continental Chemicals. Ltd.
 Winnipeg. Manitoba
     Australia
The Nightingale Supply Co.. Ltd.
    Sydney. N.S.W.

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Mr. Dick Tipton                                  Page 2
Vitro Hanford Engineering Services               June 15, 1970
                     PIMPING  PIT ANALYSIS

               pH                        6.9
               P Alkalinity  as CaC03     0.0
               M Alkalinity  as CaC03    36.0
               Total Solids             30.0
               Suspended  Solids          3.0
               Dissolved  Solids         27.0
               Calcium as Ca            5.3
               Magnesium  as  Mg           3.5
               Sodium as  Na              4.7
               Iron as Fe               1.5
               Phosphate  as  PO,          0.67
               Chloride as Cl            1.7
NOTE:  All  above results  are reported  in milligrams per liter,
       except pH.
If we  can be of  further assistance -to  you concerning the
analyses  or evaluation of the data, .please ask.
 Sincerely,
 Lee Henry
 Director  of Laboratories
 LH/ejl
                              217

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                                                                      22 1970
          WATER TREATMENT PRODUCTS AND SERVICES SINCE 1915
             The HMPUI" Corporation
          EXECUTIVE OFFICES • aoSOO CHAGRIN BLVD. • CLEVELAND, OHIO. 4.4122
                                                              Reply to:
                                                              Northwest Division
                                                              2852 N. W. 31st Avenue
                                                              Portland, Oregon 97210

     October 21, 1970
     Vitro Hanford Engineering Services
     2284 oakmond Way
     Eugene,  Oregon  97401
     Attention:  Mr. Dick Tipton
     Laboratory Reference No.:  A-401-1,  A-401-2
     Dear Mr. Tipton:
     The  following information summarizes the results we  obtained
     from the McKenzie River water and the pumping pit  samples
     collected by you and received in our laboratories  on October
     16,  1970.
                      McKENZIE RIVER WATER ANALYSIS
                      pH                          6.7
                      P Alkalinity as CaC03     0.0
                      M Alkalinity as CaCO,    30.0
                      Total Solids              56.0
                      Suspended Solids           2.0
                      Dissolved Solids          54.0
                      Calcium as Ca           -   4.0
                      Magnesium as Mg            3.0
                      Sodium as Na               5.0
                      Iron as Fe                 1.2
                      Phosphate as PO,           2.4
                      Chloride as Cl             1.1
                                      218

 Executive Offices    Plants: Chagrin Falls. Ohio Arlington, Texas         Canada              Australia
20600 Chagrin Blvd.    Charlotte. North Carolina  Phoenix, Arizona    Continental Chemicals, Ltd.   The Nightingale Supply Co.. Ltd.
 Cleveland, Ohio     Minneapolis. Minnesota  Portland, Oregon      Winnipeg, Manitoba         Sydney, N.S.W.

-------
                              -2-
Vitro Hanford Engineering Services           October 21, 1970
Attention:  Mr. Dick Tipton
                    PUMPING PIT ANALYSIS
                pH                        6.7
                P Alkalinity as CaCO,     0.0
                M Alkalinity as CaCO.,    40.0
                Total Solids             56.0
                Suspended Solids          4.0
                Dissolved Solids         52.0
                Calcium as Ca             5.0
                Magnesium as Mg           4.0
                Sodium as Na              5.5
                Iron as Fe                1.0
                Phosphate as PO^          2.1
                Chloride as Cl            1.8
NOTE:  All of the above results are reported in milligrams
       per liter, except pH.
If we can be of further assistance to you concerning the
analyses or evaluation of the above data, please ask.
Sincerely,
THE MOGUL CORPORATION
Lee Henry,
Director of Laboratories
                              219

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         WATER TREATMENT PRODUCTS AND SERVICES SINCE 1915
            The Htfip**  Corporation
                              NORTHWiST DIVISION
            2862 N. W. 31»t AVENUE • PORTLAND, OREGON 97210 • TELEPHONE (503) 226-1461
     March  19,  1971
     Vitro Hanford Engineering Services
     2284 Oakmond Way
     Eugene, Oregon 97401
     Attention:   Mr.  Dick Tipton
     Laboratory  Reference No. s  A-484-1, A-484-2,  & A-484-3
     Dear Mr. Tipton:
     The following information summarizes  the  results we obtained
     from the McKenzie River water, pumping  pit,  and base sample
     north.  These samples were collected  by you  and received in
     our laboratories on March 17, 1971.
                      MCKENZIE RIVER WATER  ANALYSIS
                      pH                         6.9
                      P Alkalinity as CaCO3     0.0
                      M Alkalinity as CaCO3    26.0
                      Total Solids              54.0
                      Suspended Solids           5*0
                      Dissolved Solids          49.0
                      Calcium as Ca              4.7
                      Magnesium as Mg            1.6
                      Sodium as Na              35.5
                      Iron as Fe                 0.10
                      Phosphate as PO4           0.23
                      Chloride as Cl             0.8
                                    220

 Executive Offices    Plants: Chagrin Falls, Ohio Arlington, Texas        Canada              Australia
20600 Chagrin Blvd.   Charlotte, North Carolina Phoenix, Arizona   Continental Chemicals, Ltd.   The Nightingale Supply Co., Ltd.
 Cleveland, Ohio    Minneapolis. Minnesota  Portland, Oregon     Winnipeg, Manitoba         Sydney, N.S.W.

-------
Vitro Hanford Engr. Services -2-            March 19, 1971

                    PUMPING PIT ANALYSIS
                PH                        6.9
                P Alkalinity as CaC03     0.0
                M Alkalinity as CaC03    20.0
                Total Solids             59.0
                Suspended Solids          8.0
                Dissolved Solids         51.0
                Calcium as Ca             5.5
                Magnesium as Mg           1.6
                Sodium as Na      '       35.5
                Iron as Pe                0.15
                Phosphate as PO^          0.20
                Chloride as Cl            1.6

                 BASE SAMPLE NORTH ANALYSIS
                pH                        6.5
                P Alkalinity as CaCO,     0.0
                M Alkalinity as CaC03    20.0
                Total Solids            352.0
                            i
                Suspended Solids        155.0
                Calcium as' Ca            12,4
                Magnesium as Mg           3.5
                Sodium as Na             47.0
                Iron as Fe                9.0
                Phosphate as P04          2.45
                Chloride as Cl            2.0
                Dissolved Solids        197.0
Note:  All of the above results are reported in milligrams
       per liter, except pH.
If we can be of further assistance to you concerning the
analyses or evaluation of the above data, please ask.
Sincerely,
THE MOGUL CORPORATION
Lee Henry,
Director of Laboratories      £21

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         WATER TREATMENT PRODUCTS AND SERVICES SINCE 1915
            The fft©©ftH>* Corporation
                              NORTHWEST DIVISION
           2852 N. W. 31st AVENUE  •  PORTLAND, OREGON 97210  •  TELEPHONE (503) 226-1451
     June 23, 1971                                      ;
     Vitro Corporation
     204 Oakmont Building
     2300 Oakmont Way                            !
     Eugene, Oregon 97401
     Attention:  Mr. Richard B.  Tipton
     Laboratory Reference  No's:   A-613-1,2,3, & 4
     Dear Mr. Tipton:
     The following information summarizes the results we obtained
     from the North Drain  Line,  South Drain .Line, The.McKenzie
     River, and Pumping  Pit.   These samples were collected by you
     and were received in  our laboratories on June  16,  1971.
                            NORTH DRAIN LINE
                    pH                            7.1
                    P Alkalinity as CaC03        0.0
                    M Alkalinity as CaCO3       24.0
                    Total  Solids               176.0
                    Suspended Solids            21.0
                    Dissolved Solids           155.0
                    Calcium as Ca               20.0
                    Magnesium as Mg             10.0
                    Sodium as Na                19.0
                    Iron as Fe                   2.0
                    Phosphorus as P              0.313
                    Chloride as  Cl               1.4
                    Ammonia (as  N)                2.48
                                    222

 Executive Offices    Plants: Chagrin Falls, Ohio Arlington, Texas         Canada              Australia
20600 Chagrin Blvd.   Charlotte. North Carolina  Phoenix, Arizona  Continental Chemicals, Ltd.   The Nightingale Supply Co., Ltd.
 Cleveland. Ohio    Minneapolis. Minnesota  Portland, Oregon     Winnipeg. Manitoba         Sydney, N.S.W.

-------
                              -2-
Vitro Corporation                               June 23, 1971

                     SOUTH DRAIN LINE
               pH                           7.4
               P Alkalinity as CaCCU        0.0
               M Alkalinity as CaC03       24.0
               Total Solids               164.0
               Suspended Solids            16.0
               Dissolved Solids           148.0
               Calcium as Ca               15.0
               Magnesium as Mg             10.0
               Sodium as Na                14.5
               Iron as Fe                   2.0
               Phosphorus as  P              0.251
               Chloride as Cl              1.5
               Ammonia (as N)               3.10

                     THE MCKENZIE RIVER
               pH                           7.5
               P Alkalinity as CaCO,        0.0
               M Alkalinity as CaCO3       24.0
               Total Solids               150.0
               Suspended Solids             8.0
               Dissolved Solids           142.0
               Calcium as Ca                5.0
               Magnesium as Mg              5.0
               Sodium as Na                14.0
               Iron as Pe                  <0.1
               Phosphorus as  P              0.020
               Chloride as Cl              0.7
               Ammonia (as N)               0.08

                        PUMPING PIT
               pH                           7.1
               P Alkalinity as CaC03        0.0

                               223

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                             -3-
Vitro Corporation                               June 23, 1971

               M Alkalinity as CaCOj       ,24. OT
               Total Solids                46.0
               Suspended Solids             6.0
               Dissolved Solids            40.0
               Calcium as Ca                5.0
               Magnesium as Mg              5.0
               Sodium as Na                13.0
         i
               Iron as Fe                  <0.1
               Phosphorus as P      .        0.020
               Chloride as Cl               0.75
                                               *    "i • •
               Ammonia (as N)               0.16
All of the above results are reported in milligrams per liter
(mg/1), except pH.
If we can be of further assistance to you concerning the
analyses, please ask.
Sincerely,              ,
THE MOGUL CORPORATION
  /,  >^{i''"i
Lee' flenry,   y
Director of '"Laboratories
LH/kmc
                              224

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         WATER TREATMENT PRODUCTS AND SERVICES SINCE 1915

                                                                  JUl ,
             The  |ft©®Ot. Corporation
                               NORTHWEST DIVISION
           2852 N. W. 31st AVENUE  .  PORTLAND, OREGON 97210  . TELEPHONE (503) 226-1451
         July 28, 1971
         Vitro Corporation
         204 Oakmont Building
         2300 Oakmont Way
         Eugene, Oregon   97401
         Attention:  Mr. Richard B.  Tipton
         Laboratory Reference  Number:   A-675
         Dear Mr. Tipton:
         The following information summarizes the results we  obtained
         from the McKenzie River,  the  North Drain Line, the South
         Drain Line, and Pumping Pit.   These samples were collected by
         you and were received in our  laboratories on July 8,  1971.
                          THE  MCKENZIE RIVER

               Ammonia (as N)                   <0.2
               pH                                6.9
               P Alkalinity  as CaCX>3            0.0
               M Alkalinity  as CaC
-------
Vitro Corporation       - 2 -
                  NORTH DRAIN LINE

      Ammonia (as N)                  <0.2
      pH                               6.2
      P Alkalinity as CaCOs            0.0
      M Alkalinity as CaCOs           24.0
      Total Solids                   242.0
      Dissolved Solids               218.0
      Suspended Solids                24.0
      Calcium as Ca                   16.5
      Magnesium as Mg                  5.5
      Sodium as Na                     5.5
      Phosphorus as P                  0.248
      Chloride as Cl                   0.8
      Iron as Fe                       1.2
                  SOUTH DRAIN LINE

      Ammonia (as N)                  <0.2
      pH                               6.1
      P Alkalinity as CaCQ3            0.0
      M Alkalinity as CaCOs           22.0
      Total Solids                   244.0
      Dissolved Solids               240.0
      Suspended Solids                 4.0
      Calcium as Ca                   16.5
      Magnesium as Mg                  5.0
      Sodium as Na                     6.0
      Phosphorus as P                  0.294
      Chloride as Cl                   1.1
      Iron as Fe                   '0.7
                           226

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Vitro Corporation       - 3 -
                     PUMPING PIT

      Ammonia  (as N)                  <0.2
      PH                               6.9
      P Alkalinity as CaCC>3            0.0
      M Alkalinity as CaCO$           28.0
      Total Solids                   188.0
      Dissolved Solids               185.0
      Suspended Solids                 3.0
      Calcium  as Ca                    4.5
      Magnes ium as Mg                  4.5
      Sodium as Na                     3.5
      Phosphorus as  P                  0.016
      Chloride as Cl                  1.6
      Iron as  Fe                      <0.05

All  of the above results  are reported in milligrams per liter
 (mg/1), except pH.

If we can be of further assistance  to you concerning the
analyses, please ask.

Sincerely,
THE  MpGUL CORPORATION
Lee Henry,
Director  of  Laboratories

LH/nv
                           227

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          WATER TREATMENT PRODUCTS AND SERVICES SINCE 1915
             The
            2852 N. W. 31st AVENUE  .
       August 9,  1971
                         Corporation
                  NORTHWEST DIVISION
                 PORTLAND, OREGON 97210  •  TELEPHONE (503) 226-1451
       Vitro Corporation
       204 Oakmont Building
       2300 Oakmont Way
       Eugene, Oregon   97401
       Attention:   Mr.  Richard B. Tipton
       Laboratory  Reference Number:  A-707
       Dear Mr.  Tipton:
       The following information summarizes the results we  obtained
       from the  McKenzie River, the  Irrigation Water, the North Drain
       Line  (Cold) ,  and the South Drain Line (Warm) .  These samples
       were collected by you and were  received in our laboratories on
       July 29,  1971.
                           THE MCKENZIE RIVER
                 PH
                 P Alkalinity as CaC03
                 M Alkalinity as CaCOs
                 Total Solids
                 Total Dissolved Solids
                 Total Suspended Solids
                 Chloride as Cl
                 Calcium as Ca
                 Magnesium as Mg
                 Sodium as Na
                 Phosphorus as P
                 Iron as Fe
                 Ammonia (as N)
                                      7.3
                                      0.0
                                     30.0
                                     54.0
                                     51.8
                                      2.2
                                      1.5
                                      2.0
                                      2.0
                                      3.0
                                      0.03
                                      0.15
                                     <0.2
                                    228
 Executive Offices
20600 Chagrin Blvd.
 Cleveland, Ohio
Plants: Chagrin Falls, Ohio
Charlotte, North Carolina
Minneapolis. Minnesota
Arlington, Texas
Phoenix, Arizona
Portland, Oregon
     Canada
Continental Chemicals, Ltd.
  Winnipeg, Manitoba
      Australia
The Nightingale Supply Co., Ltd.
    Sydney, N.S.W.

-------
Vitro Corporation         - 2 -
                  THE IRRIGATION WATER

         PH                             7.1
         P Alkalinity as CaC03          0.0
         M Alkalinity as CaC03         32.0
         Total Solids                 120.0
         Total Dissolved Solids       119.0
         Total Suspended Solids         1.0
         Chloride as Cl                 1.12
         Calcium as Ca                  2.5
         Magnesium as Mg                2.0
         Sodium as Na                   3.5
         Phosphorus as P                0.35
         Iron as Fe                     0.15
         Ammonia  (as N)                <0.2

              THE NORTH DRAIN LINE  (COliD)

         pH                             6.2
         P Alkalinity as CaCC>3          °-°
         M Alkalinity as CaCOs         36.0
         Total Solids                 176.0
         Total Dissolved Solids       170.2
         Total Suspended Solids         5.8
         Chloride as Cl                 1.8
         Calcium as Ca                  7.5
         Magnesium as Mg                5.0
         Sodium as Na                   6.25
         Phosphorus as P                0.30
         Iron as Fe                     1.10
         Ammonia  (as N)                <0.2
                             229

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Vitro Corporation         - 3 -
              THE SOUTH DRAIN LINE  (WARM)

         pH                             5.9
         P Alkalinity as CaC03          0.0
         M Alkalinity as CaC03         28.0
         Total Solids                 174.0
         Total Dissolved Solids       171.4
         Total Suspended Solids         2.6
         Chloride as Cl                 1.35
         Calcium as Ca                  9.5
         Magnesium as Mg                6.0
         Sodium as Na                   6.25
         Phosphorus as P                0.42
         Iron asFe                      0.50
         Ammonia  (as N)                <0.2

All of the above results are reported in milligrams per liter
 (mg/i), except pH.
If we can be of further assistance to you concerning the
analyses, please ask.
Sincerely,
THE MOGUL CORPORATION
              boratories
                             230

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         WATER TREATMENT PRODUCTS AND SERVICES SINCE 1915
             The
                        Corporation
                               NORTHWEST DIVISION
           2852 N. W. 31st AVENUE  .  PORTLAND, OREGON 97210  .  TELEPHONE (503) 226-1451
    August 25. 1971

    Vitro Corporation
    204  oakmont Building
    2300 Oakmont Way
    Eugene,  Oregon  97401
    Attention:  Mr. Richard B. Tipton
    Laboratory Reference Number:  A-726
    Dear Mr. Tipton:
    The  following information summarizes  the results we obtained
    from the Irrigation Line and the Filter Dam.  These samples
    were collected by you and were received in our laboratories on
    August 12, 1971.
                          THE IRRIGATION LINE
                 pH                                 6.9
     f            P Alkalinity as CaCOs             0.0
                 M Alkalinity as CaC03            36.0
                 Total Solids                     42.0
                 Total Dissolved Solids          41.4
                 Total Suspended Solids           0.6
                 Phosphorus as P                   0.06
                 Chloride as Cl                    3.9
                 Calcium as Ca                     2.8
                 Magnesium as Mg                   2.5
                 Sodium as Na                      4.0
                 Ammonia as N                     <0.2
                 Iron  as Fe                        0.10
                                     231
 Executive Offices
20600 Chagrin Blvd.
 Cleveland. Ohio
Plants: Chagrin Falls, Ohio Arlington. Texas
Charlotte, North Carolina Phoenix, Arizona
Minneapolis. Minnesota  Portland, Oregon
     Canada
Continental Chemicals, Ltd.
  Winnipeg, Manitoba
      Australia
The Nightingale Supply Co., Ltd.
    Sydney. N.S.W.

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Vitro Corporation           - 2 -           August 25, 1971
                       THE FILTER DAM

            pH                               7.1
            P Alkalinity as CaC03            0.0
            M Alkalinity as CaC03           32.0
            Total Solids                    56.0
            Total Dissolved Solids          41.0
            Total Suspended Solids          15.0
            Phosphorus as P                  0.07
            Chloride as Cl                   1.1
            Calcium as Ca                    3.0
            Magnesium as Mg                  2.5
            Sodium as Na                     4.1
            Ammonia as N                    <0.2
            Iron as Fe                       0.55
All of the above results are reported in milligrams per liter
 (mg/1), except pH.
 If we can be of further assistance to you concerning the
 analyses, please ask.
Sincerely,
THE MOGUL CORPORATION
     H. McDonald
Manager - Water Quality Services
JMD/nv
                               232

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                           -:-, a--H=
             sssss-'^Hs-T-j-"" -.- .".^--7;- I--T^:V^:. -v-~-.--.- =-^=
I   1   KtWBERS S. I.
        CAMAS 6. S.  L.
        CLOOUATO SILT L
        SIFTON G. L
        CHEHAUS SILTY C. L.
                                                   SOUS MAP
                                               233

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                   AREA WATER AND POWER REQUIREMENTS

The thermal power requirements of the region form the basis for the
thermal water demonstration project at Springfield, Oregon.  Power plants
are designed to meet loads and conditions facing the power supply agen-
cies at the time the plant is designed.  The one settled on was to be
rated at 1 million kW with a load factor of 80 percent.  This plant
would require a flow of 1420 cfs.

A million kW plant would raise the river water's temperature .3°F if the
flow is 100,000 cfs.  A detailed study would be required to estimate the
effect of a large number of such plants if located on the Columbia and
Willamette.  For example, if one or two plants were built in Oregon using
Columbia and Willamette flows, the indicated temperature rise would be
3°F when the flow in the Columbia below Portland is 100,000 cfs.

Raising the temperature of the Willamette and Columbia by the amount
indicated is not permitted under current water-quality standards, and
a relaxation of these standards probably will not occur.  The present
tendency is to make them more stringent.  Three alternative solutions
are:  1) assume plants will have cooling towers with consequent losses
of water to evaporation; 2) assume plants will have a closed cooling
system similar to an automobile radiator with only a minor loss of a
makeup water; or 3) assume that heated water will be used for irrigation.

With induced-draft cooling towers, the cost of power will be increased
by 5 to 15 percent over the cost where once-through cooling is used.
No heat would be added to the stream.  With a closed cooling system,
the amount of makeup water required has been estimated to be about 1/10
or less of cooling tower requirements.
                                  234

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Use of heated water for  irrigation would require application of effluent
for 160 hrs per week throughout the growing season.  Bypassing this con-
tinuous flow back  into the river would not be permitted if, for some
reason, the irrigation need fluctuated to a level considerably below the
scheduled output.  The flow in a once-through basis has been estimated
to be 1300 cfs in  the initial study of Washington's requirements, and the
Portland General Electric Company has estimated a once-through flow of
2000 cfs would be  required for its Trojan plant (1050 kW).

In the Willamette  basin, the diversion rate for irrigation is 4.3 acre-
ft per acre.  Using a flow rate of 1600 cfs, one plant of 1 million kW
capacity would furnish the diversion requirements for more than
110,000 acres, assuming  a constant rate of diversion over the irrigation
system.  Some difficulties may be experienced in achieving a proper
balance between irrigation development and low "growth" in power plants.
Use of this solution also would unduly restrict the design of future
generating plants.

Estimates of the cooling water evaporation loss by several agencies and
authors cover a large range.  They have been converted where necessary
here to Ibs of water per kW generation for ease of comparison.  Burns
and Roe, designers of the Fort Martin West Virginia plant (1,080,000 kW)
state that 16 million gallons of water will be evaporated daily, equi-
valent to 5.6 Ibs  of water per kilowatt hour.
     I  •   v  '  -
A joint power-planning council in April 1967 stated that the consumptive
use would be 22 million gallons per day or per 1000 megawatts of installed
capacity, and they also  indicate that a plant factor is approximately
equivalent to load factor at 90 percent.  The consumptive use per kilo-
watt hour would be 8.5 Ibs.  Battelle Northwest indicates that the con-
sumptive use of a  1 million kW plant with 80 percent plant factor would
be 12,588 acre-ft, equivalent to 4.9 Ibs per kilowatt hour.  The engineer-
ing text Water Demands for Steam Electric Generation by Kootner and Loth,
John Hopkins Press, 1965, states that minimal consumptive use requirements

                                235

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will decrease with the present .7 toward .5 gallons per kilowatt hour,
equivalent to 5.8 to 4.2 Ibs per kilowatt hour.  From this stage 1n eva-
poration rates, a value of 5.6 Ibs per kilowatt hour of generation 1s
selected.  This corresponds to an annual evaporation of 14,500 acre-ft
for each standard size plant.

An advisory committee study indicates that a total of 109 plants each
with a generating capacity of 1 million kW will be necessary to meet
Oregon's load, and these have been assigned to various river basins.
Generally in accord with projected 2070 population for the basin, the
committee suggested that the environment be considered when locating
thermal power plants; but no method of doing this by use of presently
available climatic factors is feasible.  Also, the science of predicting
the effect that a cooling tower would have on the surrounding atmosphere,
particularly the prediction of whether or not a detrimental fog condi-
tion would be created, has not been advanced to a readily usable state.
Several sites should be investigated for each proposed plant and data
on climatological factors pertaining to each site are vital.

An adjustment was made in the basins along the eastern and southeastern
part of the state.  These areas will be short of water when irrigable
areas are developed and transportation of large heavy units for the con-
struction of nuclear power plants will be difficult.  All the required
generation for these basins was assigned to plants below the John Day
Basin.  In July 1968, Eugene Water & Electric Board engaged Vitro Engineer-
ing to perform a feasibility study on the possibilities of utilizing water
from a thermal plant that would meet necessary requirements.  This report
was completed and submitted to EWEB in September 1968.

Included in the feasibility study was the outlining of Vitro's capability
to establish a program which would accommodate the climatological fac-
tors of the south Willamette Valley and to establish advantageous agri-
cultural schemes to demonstrate the multi-use concept for eventual better-
ment of the 110,000 acres in the upper Willamette.
                                236

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EWEB's consultants established  a mathematical  projection  of utilization
of cooling water and  how  it  could  be  used  for  frost control, irrigation,
and plant cooling.  In  addition, they established  a rationale of environ-
mental effect.  The purpose  of  the atmospheric program is somewhat  dif-
ferent than, but directly associated  with, the demonstration farm and
agronomic program.  The atmospheric measurement would  concentrate on
micro-climatological  effect  rather than  research or the development of
techniques to  answer  two  questions:

   •  How does the irrigation with warm  water  differ from irrigation
      with cold water with respect to influence on energy balance?

   •  If there is a significant difference between warm and cold water
      irrigation, what  is its significance in  terms of large and small
      scale  climate modification?
  . GOVERNMENT PRINTING OFFICE: 1974 546-318/375 1-3
                                   237

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  SELECTED WATER
  RESOURCES ABSTRACTS

  INPUT TRANSACTION FORM
f. Repbtttfo.
 3. Accession ?fc..
  4.  Title
 A  Demonstration of Thermal Water Utilization  in Agriculture
                                                                         rjaitt* 0rgaaf$aifDa ' •'
                                                                                    • -   '"
  7. . AuthoT(s)

    Berry, James W. and Herman H. Miller, Jr.
                   10.  Project No,
  9.  Organization
    Eugene Water and Electric Board
    with project management by
    Vitro Engineering
                   11.  Contract/Grant No.
                    S802032
13,
                                  *«?
                                   '
  15. Supplementary Notes
    Environmental  Protection Agency report No. EPA-660/2-74-011,  April 1974.
  16. Abstract
        A five-year demonstration project was conducted  to  determine benefits and identify
   harmful effects of using waste heat in condenser  cooling water (90°F-110°F) for
   agricultural purposes.

        Initial phases of the demonstration emphasized the  use and evaluation of warm
   water for spring frost protection, irrigation, and plant cooling during summer.
   Various row crops and fruit and nut trees were included  in the evaluation.

        Undersoil heating was demonstrated on a  1.2  acre soil plot.  Two and one half
   inch plastic pipes were buried 26 inches deep and 5 feet on center, connecting to
   6 "inch steel headers. >Warm water was circulated  through the grid, heating soil ori
   which row crops were grown.

        A plastic greenhouse (22' x 55') was constructed on a portion of the undersoil
   heat grid.  Greenhouse crop production was thoroughly evaluated.

        Conclusions indicate that the greatest potential  benefit of waste heat use in
   agriculture is in the area of greenhouse soil heating.   Monetary benefits from industri
   al  waste heat appear achievable through proper management.
  17a. Descriptors
   *Beneficial use-Industrial water, *Thermal water,  *Water utilization, Heated water,
   Water pollution control, Thermal pollution, Agriculture, *Frost protection, Irrigation
   water, *Soil-water-piant relationships, Soil  temperature.


  17b. Identifiers
   Waste heat use in agriculture, Thermal pollution control, *Soil heating.
  . 17c. CO WRR Field & Group  Q5F
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Send To:
WATER RESOURCES SCIENTIFIC INFORMATION CENTER
U.S. DEPARTMENT OF.THE INTERIOR
WASHINGTON. D. C. ZOZ4O
Abstractor Alden 6. Christiansen | institution Environmental Protection Aaencv
WRSIC 102 (REV. JUNE 1971)

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