SUSTAINABLE DRYLAND AGROECOSYSTEM MANAGEMENT1
G.A. Peterson2,
D.G.
Westfall2, F.
B. Peairs3, L.R. Ahuja7, L.Sherrod4,
D. Poss5, W. Gangloff5
K. Larson6, D.L. Thompson6,
M.D. Koch5, and C. B. Walker5
INTRODUCTION
This
dryland agroecosystems project is a joint effort of the Colorado State
University Department of Soil and Crop Sciences, Colorado Agricultural
Experiment Station, and the USDA-ARS Great Plains System Unit in Fort Collins,
CO. This interdisciplinary project was initiated in 1985 and expanded
in 1998 to evaluate the bio-control of plant pests in dryland systems by
the Department of Bioagricultural Sciences and Pest Management. The
geographic region targeted by this project is the Central Great Plains
region of the US where 44,000,000 acres are devoted to dryland crop production.
As we
closed out the 20th century it became evident that the traditional stubble-mulch
tillage winter wheat-fallow cropping was neither economically nor environmentally
sustainable. Tillage and wheat-fallow cropping practices had resulted in
increased erosion by wind and water, and declines in soil organic matter
that altered soils properties that in turn decreased precipitation capture
and precipitation use efficiency. In short the system was not environmentally
sustainable. It was evident that a different approach to managing
our fragile dryland agroecosystem in this semi-arid environment was needed
for the 21st century.
| Efficient
use of the precipitation is critical if cultivated agriculture is to remain
viable in the region.
Dryland agriculture in this region is highly dependent on precipitation, both snow and rainfall. The water budget in Figure 1 shows how water received as rain or snow can be easily lost before it has an opportunity to be used by a crop. Water use by weeds and evaporation are the two most negative pathways of water loss that must be avoided if improvements in precipitation use efficiency are to be accomplished. Each unit of precipitation is critical to production in this highly water limited growing environment. For example, at Akron, CO each additional inch (25 mm) of precipitation above the initial yield threshold will result in 4.5 bu/A of wheat (12 kg/ha/mm); returns are highly related to water conservation. Consequently, capture and efficient use of our limited precipitation is vital to the success of dryland farming. |
Figure 2. Water budget for dryland systems. |
OBJECTIVES
The
general objective of the project is to identify dryland crop and soil management
systems that will maximize water use efficiency of the total annual precipitation
and economic return while ensuring environmental sustainability.
Specific objectives are to:
1. Determine if dryland cropping sequences
with fewer and/or shorter summer fallow periods are
economically and environmentally sustainable.
2. Quantify the relationships among climate
(precipitation and evaporative demand), soil type and cropping
sequences that involve fewer and/or shorter fallow periods.
3. Quantify the effects of long-term use
of no-till management systems on soil structural stability, micro-organisms
and faunal populations, and the organic C, N, and P content and cycling
of the soil as impacted by various
crop sequences.
4. Identify crop management systems that
will minimize soil erosion by promoting crop residue maintenance on the
soil surface.
5. Develop a data base across climatic zones
that will allow economic assessment of entire management systems.
6. Evaluate the effect of different cropping
systems on beneficial and pest insect populations with the ultimate goal
of
determining the bio-control potential of crop insect pests, particularly
Russian Wheat Aphid.
EXPERIMENTAL PROCEDURES
From
1986 - 1997 we studied interactions of climate, soils and cropping systems
at three sites, located near Sterling, Stratton, and Walsh, in Eastern
Colorado, that represent a gradient in potential evapotranspiration (PET)
(Fig. 2).
Figure 3. Experimental design with climate, soil
and cropping system variables.
Elevation, precipitation and evaporative demand for each site are shown in Table 1. All sites have long-term precipitation averages of approximately 16-18 inches (400-450 mm), but increase in PET from north to south. Open pan evaporation is used as an index of PET for the cropping season.
Table 1. Elevation, long-term average annual precipitation, and evaporation characteristics for each site.
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Precipitation 1 |
Pan Evaporation 1 |
(Precip. - Evap.) |
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| Briggsdale |
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| Sterling |
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| Akron |
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| Stratton |
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| Lamar |
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| Walsh |
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| The cropping system at these sites during the previous 50 years had been primarily stubble-mulch tillage of dryland wheat-fallow with some inclusion of grain sorghum at Walsh and corn at Sterling. At the these three original sites we placed cropping system treatments over the soil sequence (Figs. 2 & 3) to study the interaction of cropping systems and soils. In 1998 we initiated three new research sites at Briggsdale, Akron and Lamar, CO to evaluate Objective 6 above. At the three new sites we have only one soil type and the individual plots are larger, ranging in size from 1 to 6 A. Larger plots were needed to properly evaluate the interaction of cropping systems on insect population dynamics. Systems being studied at each site are listed in Tables 2a & 2b. All crops in each cropping system are present in the rotation each year. | Figure 4. Wheat-corn-fallow system at Sterling CO (note landscape aspect of experimental design.) |
Prior to 1998, wheat fallow (WF) was the "standard system" with which we compared the new cropping systems. In 1998, the WF system was discontinued because it had become obvious that WF was not economically viable under no-till management. We adopted WC(S)F as the "standard system" in 1998 and converted the WF plots to more continuous cropping systems and included soybeans. Prior to this time we had grown other summer cash crops such as millet and sunflowers. Millet is a well adopted crop for the region but we discontinued it because of the low price and are now investigating the potential of soybeans as a summer cash crop. All experiments are managed with no-till techniques which allows us to maintain as much crop residue on the soil surface as possible.
Table 2a. Cropping systems for each of the original
sites in 1999.
Site
Rotations
Sterling
1) Wheat-Corn-Fallow (WCF)
2) Wheat-Corn-Soybean (WCSy)
3) Wheat-Wheat-Corn-Soybean (WWCSy)
4) Opportunity Cropping*
5) Perennial Grass
Stratton
1) Wheat-Corn-Fallow (WCF)
2) Wheat-Corn-Soybean (WCSy)
3) Wheat-Wheat-Corn-Soybean (WWCSy)
4) Opportunity Cropping*
5) Perennial Grass
Walsh
1) Wheat-Sorghum-Fallow (WSF)
2) Wheat-Corn-Soybean (WCSy)
3) Wheat-Wheat-Sorghum-Soybean (WWSSy)
4) Continuous Row Crop (Alternate corn & sorghum)
5) Opportunity Cropping*
6) Perennial Grass
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*Opportunity cropping is designed to be continuous cropping
without fallow, but not monoculture.
Opportunity Cropping History
Table 2b. Cropping systems for the new sites in
1999.
Site
Rotation
Briggsdale
1) Wheat-Fallow (WF)
2) Wheat-Hay Millet-Fallow (WHF)
3) Wheat-Wheat-Corn-Soybean-Sunflower-Pea (WWCSySnPea)
4) Opportunity
Akron
1) Wheat-Fallow (WF)
2) Wheat-Corn-Fallow (WCF)
3) Wheat-Corn-Proso-Fallow (WCPF)
4) Wheat-Corn-Proso (WCP)
Lamar
1) Wheat-Fallow (WF)
2) Wheat-Sorghum-Fallow (WSF)
SUMMARY OF PROJECT RESULTS
Grain
yields, stover yields, crop residue amounts, soil water measurements, and
crop nutrient content have been published annually in Colorado State University
Agricultural Technical Bulletins. Technical Bulletins can be accessed
at www.colostate.edu/Depts/AES/
Pubs. Select TB 98-1 or TB 99-1 from the publications
displayed.

Figure 5. Grain yields averaged over soil position and 14 years of production for each location.
Complete data for each crop are available in previously
published bulletins.
We included
yields in Figure 4 from all years, even those where yield losses occurred
due to hail, early and late freezes, insect pests, winter kill of wheat,
and herbicidal carryover. Fluctuations in corn and sorghum yields
are of most interest because they represent the highest input crops. Corn
yields have averaged 65 bu/A (Ranging from 14 to 107 bu/A) at Sterling
and 76 bu/A (Ranging from 37 to 112 bu/A) at Stratton. These averages
include the disastrous yields recorded in 1994, which were caused by drought,
and the low yields caused by early frost in 1995. Grain sorghum was
produced at Stratton for 4 years and yielded an average of 44 bu/A
(ranging from 20 to 63 bu/A), but corn has averaged 76 bu/A for the past
9 years, making it a better choice for this environment. At Walsh
grain sorghum yields have averaged 48 bu/A (ranging from 27 to 75 bu/A),
including the results from the very dry 1995 season and severe hail in
1996. Dryland corn yields at Walsh, using Bt varieties, have averaged
57 bu/A from1997-1999.
The
3- and 4-year systems like wheat-corn(sorghum)-fallow and wheat-corn-millet-fallow
or wheat-sorghum-sorghum-fallow have increased average annualized grain
production by 74% compared to the 2-year wheat-fallow system (Figure 5).
Yields are annualized to account for the nonproductive fallow year in rotation
comparisons. Economic analysis has shown there was a 25-40% increase
in net annual income for the three-year rotation in northeastern Colorado.
However, in higher ET region of southeastern Colorado the three year wheat-sorghum-fallow
rotation, using stubble mulch tillage in the fallow prior to wheat planting,
netted about the same amount of return as reduced till wheat-fallow.
New herbicide programs with fewer residual materials have shown promise
and are less expensive.

Our data
have shown that cropping intensification is certainly possible in the west
central Great Plains. More intensive rotations like wheat-corn(sorghum)-fallow
and wheat-corn(sorghum)-millet-fallow have more than doubled grain water
use efficiency in all three study environments when compared over years.
Water conserved in the no-till systems has been converted into increased
grain production. Our opportunity cropping systems have maximized production
at all sites relative to all other rotations, but have not been the most
profitable. The 3-year rotations have been most profitable.
Producers
in northeastern Colorado have been adopting the more intensive cropping
systems at an increasing rate since 1990. Corn is one of the principal
crops used in more intensive systems, and we use its acreage as an "index"
of adoption rate by producers (Table 3). Area planted to dryland
corn in northeastern CO increased from about 20,000 acres per year in years
previous to 1990 to 220,000 acres in 1999. Total dryland corn acreage
in Colorado increased from 23,700 historically to 290,000 in 1999.
Corn acreage is expanding into areas once thought to be too dry for corn
production as exemplified in Lincoln county where corn acreage increased
from 1500 in 1996 to 18,000 in 1999. Adoption of the new systems also is
reflected in sunflower and proso millet acreage increases. For example,
sunflower acreage increased from 63,000 in 1991 to 270,000 in 1999.
Table 3. Dryland Corn Acreage in Eight Northeastern Colorado
Counties and total for state from 1971 to 1998.
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The key to the future of Central Great Plains agriculture is the expansion
no-till systems with more crop diversity, meaning more markets for farmers.
Our most recent system changes even include the use of Round Up Ready soybean
(Fig. 7). We are testing continuous cropping systems where we plant
winter wheat directly into the soybean stubble a few days after harvest.
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Figure 8. Soybean planted no-till into corn stalk stubble in a wheat-corn-soybean continuous crop system. |