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CONSERVATION TILLAGE IN THE UNITED STATES: AN OVERVIEW



Daniel Walters and Paul Jasa

Institute of Agriculture and Natural Resources

University of Nebraska – Lincoln U.S.A.



INTRODUCTION



The growth of agricultural production in the United States over the past 100 years has

followed the westward expansion of population across the North American continent. In

the 1930’s, the Dust Bowl, which resulted from a severe long-term drought and

excessive tillage, prompted the formation of the U.S. Soil Conservation Service (now

the Natural Resources Conservation Service NRCS) and a concerted effort to improve

soil conservation practices to preserve soil resources for future generations. There are

currently 295 million acres (120 Mha) of cropland in the U.S. subject to some form of

tillage. Significant advances in machinery and cropping systems as well socioeconomic

changes in U.S. agriculture and government programs have influenced the rate of

conservation tillage (CT) adaptation in the US. This paper will briefly outline the state of

CT in the US with a discussion of the principal determinants governing adaptation of CT

across the nation.



DEFINITIONS (5)



Conservation Tillage (CT): Any tillage and planting system that covers 30 percent or

more of the soil surface with crop residue, after planting, to reduce soil erosion by water.

Where wind erosion is the primary concern, any system that maintains at least 1,000

lb/acre ( 1.1 Mg/ha) of flat, small grain residue equivalent on the surface throughout

the critical wind erosion period. The following define three broad classes of conservation

tillage.



No-till or Strip-till (NT): A tillage/planting system where the soil is left

undisturbed from harvest to planting except for nutrient injection. Planting is

accomplished in a narrow seedbed or slot created by coulters, row cleaners, row

chisels or roto tillers. Weed control is accomplished primarily with herbicides.

Less than 25% row width disturbance is considered no-till.



Ridge-till (RT): A tillage/planting system where the soil is left undisturbed from

harvest to planting except for nutrient injection. Planting is completed in a

seedbed prepared on ridges with sweeps, disk openers, coulters, or row

cleaners. Residue is left on the surface between ridges. Weed control is

accomplished with herbicides and when ridges are rebuilt during cultivation.



Mulch-till (MT): The soil surface is disturbed prior to planting. Tillage tools such

as chisels, field cultivators, disks, sweeps or blades are used. Weed control is

generally accomplished with herbicides and/or cultivation.

Reduced Till (RDT): Any tillage system that leaves 15–30 percent residue cover after

planting, or less than 500 lb/acre (0.55 Mg/ha) of small grain residue equivalent

throughout the critical wind erosion period.



Conventional Till (CVT): Any tillage system that leaves less than 15 percent residue

cover after planting or less than 500 lbs/acre (o

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Figure 2. Trends in CT adaptation in the United Staes, 1990-1998. Source (5)





Farm Size: The number of farms in the U.S. has declined from a high of 6.8

million in 1935 to 1.9 million today (11). At the same time, farm population has declined

from 33 million people to under 4.8 million or 1.9 percent of the national population (Fig.

3). Average farm size in the U.S. today is 508 acres (206 ha). The reduction in farm

labor and increase in farm size requires more timely tillage operation and less time with

machinery management. Where plowing required an average of 1.22 hrs/acre (3

hrs/ha), NT requires only 0.5 hrs/acre (1.2 hrs/ha) because of the reduction in primary

and secondary tillage operations.





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Figure 3. Trends in U.S. farm size, population and farm number. Source (11)

Environmental Awareness: Public awareness of environmental issues has

increased throughout the U.S. as information transfer has become more sophisticated.

Water quality is a principal public concern and there is increasing public financial

support for conservation programs to reduce non-point pollution of surface and ground

water. Nearly every major agricultural state has some tax support for cost sharing of

conservation structures on private land. Protection of watersheds with CT and forested

buffer strips along the nation’s watersheds is a part of national policy. Significant

progress has been made toward protecting the Mississippi River watersheds in the

Central U.S. (Fig. 4) however sedimentation of the nations waterways is still a major

offsite effect of soil erosion which costs the nation more than $7 billion dollars annually

(7 ).









Figure 4. Proportion of major US continental watersheds under conservation

tillage. Source CTIC (5).

Climate and Soil Factors:



Agriculture in the U.S. is practiced under a wide range of climatic regimes with

agricultural eco-regions that span a mix of rainfall patterns, solar energy load, day

lengths, altitudes, crop requirements, soil properties, irrigation water availability/quality

and pest problems. The national pattern of CT adaptation tends to roughly follow

latitudinal trends with growing season length, energy flux and crop heat requirements

dominating regional acceptance of high surface residue CT systems (Fig. 5). Several of

the more dominant state variables in the Central U.S. that inherently influence tillage

adaptation are:



Soil temperature: Seed germination and growth (especially maize) is reduced

under cool soil temperatures. Radical elongation and phenology is delayed under cool

soil conditions (1, 2 ) which reduces yield potential and increases the risk of yield loss at

latitudes where heat units are marginally adequate to achieve maize maturity (Fig.6).

The inherent characteristics of conservation tillage likely to influence soil temperature

are surface residue reflectance (albedo), thermal conductivity and soil drainage class.

The relative popularity of ridge till and strip till systems in northern latitudes is

attributable to increased aspect (in RT) (13 ) and reduced albedo.





Conservation Tillage by Region, 1998 Lake States

Northeast





Pacific Northern

Mountain

Plains







Corn Belt





Appalachian









Southern

Plains Delta



Southeast



Tillage practice by Type







Ridge-Till No-Till Mulch-Till





Circle size represents conservation tillage area in million acres

Source: Conservation Technology Information Center

(range in ascending size): 1.6 million acres B 35.9 million acres





Pacific







Figure 5. Proportion of agricultural land area under conservation tillage practice in the

continental USA. Source CTIC (5).

Figure 6. Daily total undepleted solar radiation received on a horizontal surface as a

function of latitude and time of year (8). (US latitudes between 30 & 50)







Soil Drainage: Since the principal component of soil heat capacity is water

content, CT systems that improve energy absorption in poorly drained soils through

reduced albedo or increased aspect will improve conditions for seed germination and

timing of spring planting operations. Conversely, soils that have low water storage

capacity have improved water retention and are aided by high surface residue CT

systems. Poorly drained soils susceptible to compaction are especially vulnerable to

the high axel loads associated with heavier CT equipment. Even under NT, 30 to 50%

of the soil surface may be subjected to wheel traffic (14 ).





Water Conservation in Fallow Tillage Systems: Dryland fallow systems are

practiced in the High Plains of the western USA where two wheat crops are grown in

three cropping season. During the lengthy fallow period (14 mo.) soil is managed for

weed control, water harvest, snow capture and wind erosion protection. Tillage systems

that result in erect stubble and high surface residue with a greater reliance on

herbicides for weed control have dramatically increased fallow efficiencies (Table 1).

However, economic return to land, labor, capital, and management in fallow systems

are reduced under no-till as the cost of conversion to no-till from stubble mulch is

greater than the yield advantage from increase fallow efficiency. Costs for NT are $8 -

$11.00 more per acre than stubble mulch (6,10). Intensification of cropping toward

shorter fallow periods, however, can improve profitability under NT (Table 2) (12 ).

Table 1. Evolution of Fallow Tillage systems, Akron, Colorado. (9)

Fallow Efficiency

Years Management system % ppt. Stored as

soil water



1916 – 1930 Maximum Tillage (Dust Mulch) 16-22

Conventional Tillage : shallow disk and

1931 – 1945 24-27

rod-weeder

Improved Conventional Tillage

1946 – 1960 27-30

Stubble Mulch in 1957

Stubble Mulch, began minimum tillage

1961 – 1975 33-38

with herbicides

1975-present No-Till with contact herbicides 40-55









Table 2. Relative Return to Capital Investment on a 1200 acre farm as

affected by cropping system and fallow tillage system in NE Colorado (12 )

Tillage Preceding Cropping System

Wheat Planting WF WCF WCFM



Conventional 100% 140% 127%



Reduced Till 92% 136% 120%



No-Till 72% 125% 113%



WF=Wheat Fallow; WCF = Wheat-corn-fallow; WCMF=Wheat-corn-millet-fallow







Water and Wind Erosion Hazard: Obviously conditions that reduce runoff and

improve water infiltration will reduce water erosion potential. Conservation tillage

practices tend to increase the tortuosity of surface runoff path and increase infiltration

time. Conservation tillage systems dominate regions of the country where farming is

practiced on sloping lands, soil texture is conducive to crusting and erosive rains are

frequent during soil preparation for planting. Wind erosion is the dominant hazard in the

wheat-fallow regions of the Central Plains and CT systems that preserve erect residue

will reduce wind velocity at the soil surface. At times, tillage operations are performed

to increase soil roughness and aggregate size to reduce saltation under extreme

conditions.

Crop Management Factors:



Weed Control: Conservation tillage systems most often result in increased

reliance on chemical weed control. Weed control can be a significant problem in CT

systems where pH stratification affects herbicide activity or where residue cover may

intercept herbicides rendering them inactive. At times, emergency tillage is required to

offset herbicide failures resulting in less than 30% residue cover. In specific situations,

the most effective herbicide compounds will require soil mixing limiting the choice of CT

systems. Conversely, CT systems can also afford reduction in herbicide use when

banded in strip- or ridge-tillage operations. Cooler soils in residue-laden zones may

suppress the emergence and competitive ability of weeds relative to the crop. Weed

control in continuous cropping systems are usually the most problematic for CT systems

because weeds with similar biological characteristics and growth periods to the crop

tend to predominate over time. In these situations, rotation of crop species may be the

most effective weed control measure under CT. The introduction of herbicide resistant

crops has revolutionized CT weed control strategies in the maize belt but the safety and

ecological impact of these crops is being questioned.



Crop Rotation: Crop rotations allow selection of different herbicides, planting

dates and tillage systems resulting in greater opportunities to control weeds, disease

and insect pests. Certain CT systems are not amenable to crop rotations. For example,

RT systems that require ridge construction during a row crop season are unsuited to

rotation with solid seeded or sod crops. This fact tends to limit the acreage devoted to

RT. Often CT systems alternate with crop rotations in response to residue management

needs or fertilization strategies. Crop rotations of all sorts are becoming the dominant

cropping strategy as they provide market diversity as well as management flexibility.



Soil Fertility: Stratification of soil chemical properties and nutrient distribution is a

commonly observed phenomenon of CT systems. Non-mobile nutrients such as P and

K can accumulate in the upper portions of the soil profile from surface placement of

fertilizer materials and/or deposition from decomposed residues (3). The extent of soil

acidification produced by nitrification of ammonium N will depend on soil buffering

capacity and inherent N mineralization potential. Redistribution and mixing of nutrients

varies with the degree of soil mixing so the choice of CT system and duration of CT

practice will depend on native soil fertility and the resistance of soil to chemical change.



SUMMARY



There are 294 million acres of cropland subject to tillage each year in the United States.

Conservation tillage systems (> 30% residue cover) are practiced on 37% of these

acres with 26% maintained with > 15% residue cover. Government incentives tied to

the Food Security Act of 1985 have been the primary reason for growth in CT in the

past decade. A growing threat from agriculture to surface water quality continues to

drive public initiatives and support for soil conservation programs. The diversity of

cropping systems, climate and soil resources across the agricultural regions of the U.S.

has resulted in a broad array of CT strategies that include innovative machinery design,

biological pest control, alternative crops and crop rotations, herbicide formulations and

genetically modified crops.





REFERENCES:

1. Alessi, J. and J.F. Power. 1971. Corn emergence in relation to soil temperature.

Agron. J. 63:717-719.

2. Barlow, E.W., L. Boersma, and J.L. Young. 1977. Photosynthesis, transpiration and

leaf elongation in corn seedings at suboptimal soil temperatures. Agron. J. 69:95-

100.

3. Blevins, R.L., M.S. Smith, G.W. Thomas, and W.W. Frye. 1983. Influence os

conservation tillage on soil properties. J. Soil Water Conserv. 38(3):301-307.

4. Clark, R.T. 1989. The Conservation of Highly Erodible Lands: A Layman’s Guide to

Conservation Compliance and Sodbuster. University of Nebraska, Coop. Ext.

NebGuide G89-909-A. http://www.ianr.unl.edu/PUBS/farmmgt/g909.html.

5. Conservation Technology Information Center (CTIC).

http://www.ctic.purdue.edu/CTIC/CTIC.html

6. Dhuyvetter, K.C., C.R. Thompson, C.A. Norwood, and A.D. Halvorson. 1996.

Economics of dryland cropping systems in the Great Plains: A review. J. Prod. Agric.

9:216-222.

7. Economic Research Service – USDA. 1986. Reducing Soil Erosion: Offsite Benefits.

Agric. Econ. Report # 561.

8. Gates, D.M. 1962. Energy Exchange in the Biosphere. Harper and Row, NY.

9. Greb. B.W. 1983. Water Conservation: Central Great Plains. In H.E. Dregne and

W.O. Willis (eds) Dryland Agriculture. Agronomy monograph 23. ASA, CSSA, SSSA,

Madison, WI.

10. Halvorson, A.D., R.L. Anderson, N.E. Torman, and J.R. Welsh. 1994. Economic

comparison of three winter wheat-fallow tillage systems, J. Prod. Agric. 7:381-385.

11. National Agricultural Statistics Service, USDA.

http://www.usda.gov/nass/nassinfo/nassinfo.htm

12. Peterson, G.A. and D.G. Westfall, N.E. Toman, and R.L. Anderson. 1993.

Sustainable dryland agroecosystems: Economic analysis. Colo. State Univ. Agric.

Exp. Stn. Bull. TB93-3.

13. Radke, J.K. 1982. Managing early season soil temperature in the northern Corn Belt

using configured soil surfaces and mulches. Soil Sci. Soc. Am. J. 46:1067-1071.

14. Voorhees, W.B. and M.J. Lindstrom. 1983. Soil compaction constraints on

conservation tillage in the northern corn belt. J. Soil Water Conserv. 38(3):307-311.



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