Crop Production Systems In Arid & Semi-Arid
Cool Temperate Zones

Introduction
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Long cold winters.
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Cool or cold soils.
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Short growing season.
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High daytime summer temperatures.
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Potential evapotranspiration rates exceed precipitation much of growing
season
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Low humidity, cool nights
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Soil relatively unweathered.
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PH - 7+.
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Soils contain significant soluble salts.
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Low in organic matter.
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Without irrigation, severe water stress occurs on almost a yearly basis.
Drought common.
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Damaging late spring and early fall freezes.
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Crops damaged by soil particles carried by wind.
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Subject to significant wind erosion.
Management Under Dryland Conditions
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Much more done 1910-1935.
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Tillage and seeding machines largely based on farmer innovations.
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Major increase in production after 1945.
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Large tractors
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Chemical herbicides
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Fertilizers
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Dryland technology new.
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Goseen and Bieroff received Lenin prize in USSR in 1972 for production
system in central Siberian Plains
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Work nearly identical to that used in North American Plains
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Crops and crop growth.
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Climate limits crop species
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Short growing season
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Continuous water shortage
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Dominant crops:
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Small grains
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Oil seed crops (safflower, rape, flax, sunflower, mustard)
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Need about 10 cm of available water to produce seed crops
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Need 25 cm to produce satisfactory yields
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Stress at critical period (bloom) will always cut yields even if 25 cm
water available in season
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In U.S. - efficiency of stored water and precipitation equal north of 450,
precipitation more efficient south of 45o (South Dakota)
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One of direct effects of proper fertilization is increased root growth
and density - better water absorption
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Water conservation
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PET exceeds precipitation
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Avg. Daily PET at peak far exceeds precipitation at this time
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Critical stages of plant growth coincides with period of peak daily PET
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20-30% of annual precipitation in zone is snow
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Snow accompanied with high winds
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Snow swept from fields
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Unprotected fields lose over 90% of winter precipitation
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Stubble effective means of conserving snow
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Soil storage efficiency of winter precipitation can approach 99% at 40
degrees N, only 37% at 50 degrees N
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Stubble height controls the depth of snow retained
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A deep layer of snow is insulator and cuts down on soil freezing - better
water penetration
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Intermittently spaced barriers effective means of conserving water in snow
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Short, stiff stemmed plants like wheatgrass, sunflower, mustard
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Wheatgrass 1.2 m in single or double rows perpendicular to wind spaced
10-15 m - 60% efficiency
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Temporary barriers, 2 to 3 rows of mustard 10-12 m apart used in USSR
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Mechanically formed snow ridges used in USSR
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Soviets snow depth reaches 30-40 cm between ridges
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Yield increases in both USSR and Canada from ridges
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Tree and shrub shelter belts not efficient
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Uneven snow accumulation
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Take up excessive amount of land
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Level bench terraces significantly increase the soil water in North America
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Especially when used with barriers
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Allow retention of melted snow after and greater infiltration
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Conservation of summer precipitation in fallowed land largely dependent
on condition of soil surface, intensity of storms and weed control
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Stubble protects the soil surface from mechanical forces
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Falling and running water
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Water moved deeper into profile/retained against evaporation
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Normal fallow periods
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14 mo. if winter grain
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21 mo. if spring crop planted
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Total water retained by soil
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75% stored first fall and winter
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16% following spring and summer
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9% second fall and winter
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Summer fallow has been significant factor in stabilizing yields in this
zone
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Accumulation of nitrates in soil another benefit of summer fallow
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Also gives better weed control
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Spreads out labor on large farms
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Alternate year fallow system in North America, 2 to 3 crop, 1 fallow in
USSR
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Summer fallow can have detrimental effect
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Saline seeps caused by downward movement of water
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Common in North and South Dakota, Montana, and Canadian Provinces
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Lower profiles over shale contain high soluble salts (sodium and mg sulfates)
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Prior to farming area, broad spectrum of plants with variable rooting depths
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Water entering profile all used
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Without plants, water buildup in soil often moves below root zone
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Water moves over shale, comes to surface and evaporates leaving thick deposit
of salt
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A modification of standard crop-fallow system will have to be developed
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It will involve more intensive cropping and more diverse rotations
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Will need greater efficiency in winter precipitation storage, weed control
system (grass weeds) and equipment design
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Erosion
a. Both wind and water common in zone
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Soil and management factors that influence erosion are:
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Slope
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Surface texture
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Surface roughness
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Soil protection
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Most serious wind erosion occurs with strong winds in fall and early spring
on tilled lands
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Two most successful methods of wind erosion control are:
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Stubble mulch
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Strip cropping with alternate fallow-cropped strips
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Erosion more difficult to control in sandy loam or loamy sand soils
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Don=t hld clods
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Lower water holding capacity
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Soil that moves on the erodible strip is trapped in stubble
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Strips may vary from 50 to 150 m in width
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Loamy sands may require strips as narrow as 8 to 9 m
h. Intermittent barriers can also efficiently control wind erosion
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Permanent barriers, grass, shrubs
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Temporary barriers, mustard, sorghum
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Tree barriers not used because:
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Occupy too much land
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Utilize soil water
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Cause excessively large snow banks
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Provide harbor for weeds
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Permanent grass barriers appear to have real promise
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About 7% of field provides permanent wind erosion protection and good snow
trapping
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During drought periods might need to resort to emergency tillage
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Formation of clods on surface
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Sheet erosion problems with water from storms or melting snow
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Farming across slope helps prevent this
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Fertilization
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Soils of this zone generally unleached and have pH range of 7-10
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7-8.7 most productive soils
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Have many unique fertilizer problems
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Palouse area in E. Washington, molybdenum essential for legume production
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P often deficient in this zone
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Phosphorus utilized by grain more efficiently banded - it takes 2-3 times
as much broadcast
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Grain needs .05 kg N/ha to produce 1 kg/ha of seed
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Soil tests are used to determine N in root zone
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In MT, from 30-40 kg/ha of NO3-N becomes available during growing
season where most straw returned to land
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Some estimate of expected yield based on available water is essential
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Emphasize importance of stored soil water in determining N fertilization
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Significant quantities of N can be added to soils by including legumes
in rotation
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Deep root systems beneficial in saline seep control
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But, deep roots dry soil deeply - fallow 1 season after removing legume
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Significant economical response from K 50% of time with wheat, 40% of time
with barley, and 25% of time with spring wheat on soils that test high
in K
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Weeds
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Major factor determining both the production costs and productivity of
dryland agriculture of the zone
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Important weeds
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Pigweed
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Russian thistle
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Canada thistle
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Field bindweed
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Perennial sowthistle
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Wild buckwheat
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Wild oats
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Pigeon grass
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Downy brome
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Volunteer small grains
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Summer fallow one of most effective means of weed control
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Many weeds (especially broadleaves) controlled by chemicals
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Others, especially perennials are only set back or top killed
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Timing of chemical application is important
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Buckwheat can be easily killed with 2,4-D but spraying at that stage can
damage small grain
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Weeds can be best controlled when crops diversified
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Inclusion of a broadleaf crop in systems will further improve weed control
because grass chemicals can be used in broadleaves
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Saline-sodic soils
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Under nonirrigated conditions, reclamation of saline and sodic soils difficult
and slow
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Deep plowing can be effective in reclaming sodic soils if sodium is concentrated
at or near surface
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Addition of gypsum will help
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Machinery
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Power to speed up operation on larger scale, seedbeds can be prepared quickly
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Large acreage can be planted on time to take advantage of rainfall
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Seedbed preparation material has had dramatic evolution
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Moldboard plow/replaced by rolling disc plow
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Stronger steel beams, tool bar cultivator or chisel plow came into use
- mixes stubble with only surface soil
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Deep furrow press drill
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Deep furrow press drill
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Moves surface dry soil away so seed falls in moist soil
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4-8 cm deep furrow creates more favorable microclimatic, reduces frost
damage or winter killing
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Moved winter wheat belt about 300 km north
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Except for some oil-seed crops, most herbicides applied post-emergence
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Greater percentage of cereal grains harvested standing at maturity with
combine
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In areas with short growing season, grain is swathed and left to dry until
mature - can be done 10-12 days earlier, reduces chances of storm damage
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Cropping systems
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A fixed sequence of cropping, either crop-fallow or 3-year rotation including
1 year fallow general pattern throughout zone
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Cereal grains do well in harsh environment of the zone
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Near monoculture of spring wheat-fallow-spring wheat has caused disease,
insect and weed problems
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Excessive fallow has led to seep problems
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Wider adoption of flexible cropping systems is in order with root zone
water storage as the decision-controlling factor.
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Probability of success of proposed flexible system would be improved by
doing a better job of snow conservation and by including broadleaf crops
in the system for improved weed and disease control
Management Under Irrigated Conditions
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Yields of all crops mentioned can be increased with irrigation.
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Less drought tolerant crops such as sugar beets, potatoes, silage corn,
beans, etc. could be grown.
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Greater crop diversity would facilitate disease, insect and weed control.
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Capital cost of crop diversity can be tremendous.
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A typical irrigated farm might grow potatoes, sugar beets, small grain,
silage corn, and alfalfa
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Each has its own specialized equipment
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In recent years, high equipment costs has forced many farmers to revert
to almost monoculture farming
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