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Dryland farming caused a large dust storm in parts of Eastern Washington on October 4, 2009. Courtsey: NASA/GSFC, MODIS Rapid Response^[1]

Dryland farming is an agricultural technique for non-irrigated cultivation of land which receives little natural rainfall.

Locations

Dryland farming is used in the Great Plains, the Palouse plateau of Eastern Washington, and other arid regions of North America, the Middle East and in other grain growing regions such as the steppes of Eurasia and Argentina. Dryland farming was introduced to the southern Russian Empire by Russian Mennonites under the influence of Johann Cornies, making the region the breadbasket of Russia^[2]. It is widely practiced in all states of Australia (except the Northern Territory).

Crops

Winter wheat is the typical crop although skilled dryland farmers sometimes grow corn, beans or even watermelons. Successful dryland farming is possible with as little as 9 inches (230 mm) of precipitation a year, higher rainfall increases the variety of crops. Native American tribes in the arid SouthWest subsisted for hundreds of years on dryland farming in areas with less than 10 inches (250 mm) of rain.^{[citation needed]}

Process

Dryland farming has evolved as a set of techniques and management practices used by farmers to continually adapt to the presence or lack of moisture in a given crop cycle. In marginal regions, a farmer should be financially able to survive occasional crop failures, perhaps of several years running^{[citation needed]}. Survival as a dryland farmer requires careful husbandry of the moisture available for the crop and aggressive management of expenses in order to minimize losses in poor years.

System

Dryland farming is uniquely dependent on natural rainfall, which can leave the ground vulnerable to dust storms, particularly if poor farming techniques are used or if the storms strike at a particularly vulnerable time. The fact that a fallow period must be included in the crop rotation means that fields cannot always be protected by a cover crop, which might otherwise offer strong protection against erosion.

Key Elements

Capturing and Conservation of Moisture - In regions such as Eastern Washington state, the average precipitation available to a dryland farm may be as little as 8.5 inches (220 mm). Consequently moisture must be captured until the crop can utilize it. Techniques include summer fallow rotation (in which one crop is grown on two seasons' precipitation, leaving standing stubble and crop residue to trap snow, and preventing runoff by terracing fields.

"Terracing" is also practiced by farmers on a smaller scale by laying out the direction of furrows to slow water runoff downhill, a practice known as contour plowing. Moisture can be conserved by eliminating weeds and leaving crop residue to shade the soil.

Effective Use of Available Moisture - Once moisture is available for the crop to use, it must be used as effectively as possible. Seed planting depth and timing are carefully considered in order to place the seed at a depth at which sufficient moisture exists, or where it will exist when seasonal precipitation falls. Farmers tend to use crop varieties which are drought and heat-stress tolerant, (even lower-yielding varieties). Thus the likelihood of a successful crop is hedged if seasonal precipitation fails.

Soil Conservation - The nature of dryland farming makes it particularly susceptible to erosion, especially wind erosion. Some techniques for conserving soil moisture (such as frequent tillage to kill weeds) are at odds with techniques for conserving topsoil. Since healthy topsoil is critical to sustainable dryland agriculture, its preservation is generally considered^{[citation needed]} the most important long-term goal of a dryland farming operation. Erosion control techniques such as windbreaks, reduced tillage or no-till, spreading straw (or other mulch on particularly susceptible ground), and strip farming are used to minimize topsoil loss.

Control of Input Costs - Dryland farming is practiced in regions inherently marginal for non-irrigated agriculture. Because of this, there is an increased risk of crop failure and poor yields which may occur in a dry year (regardless of money or effort spent on the crop). Dryland farmers must evaluate the potential yield of a crop constantly throughout the growing season and be prepared to decrease inputs to the crop such as fertilizer and weed control if it appears that it is likely to have a poor yield due to insufficient moisture. Conversely, in years in which moisture is in abundance, farmers may increase their input efforts and budgets in order to maximize yields and to help offset poor harvests.

Notes

^ "Dust Storm in Eastern Washington : Image of the Day". earthobservatory.nasa.gov. Retrieved 2009-10-10.
^ Smith, C. Henry (1981). Smith's Story of the Mennonites. Newton, Kansas: Faith and Life Press. pp. 263–265. ISBN 0-87303-069-9. {{cite book}}: Unknown parameter |other= ignored (|others= suggested) (help)

@@ Line 31: / Line 31: @@
 "Terracing" is also practiced by farmers on a smaller scale by laying out the direction of furrows to slow water runoff downhill, a practice known as [[contour plowing]].  Moisture can be conserved by eliminating weeds and leaving crop residue to shade the soil.
-'''Effective Use of Available Moisture''' - Once moisture is available for the crop to use, it must be used as effectively as possible. Seed planting depth and timing are carefully considered in order to place the seed at a depth at which sufficient moisture exists, or where it will exist when [[seasonal precipitation]] falls. Farmers tend to use crop varieties which are drought and heat-stress tolerant, (even lower-yielding varieties). Thus the likelihood of a successful crop is [[hedged bet|hedged]] if seasonal precipitation is fails.
+'''Effective Use of Available Moisture''' - Once moisture is available for the crop to use, it must be used as effectively as possible. Seed planting depth and timing are carefully considered in order to place the seed at a depth at which sufficient moisture exists, or where it will exist when [[seasonal precipitation]] falls. Farmers tend to use crop varieties which are drought and heat-stress tolerant, (even lower-yielding varieties). Thus the likelihood of a successful crop is [[hedged bet|hedged]] if seasonal precipitation fails.
 '''Soil Conservation''' - The nature of dryland farming makes it particularly susceptible to erosion, especially wind erosion. Some techniques for conserving soil moisture (such as frequent tillage to kill weeds) are at odds with techniques for [[conserving topsoil]]. Since healthy [[topsoil]] is critical to sustainable dryland agriculture, its preservation is generally considered{{fact|date=January 2010}} the most important long-term goal of a dryland farming operation. Erosion control techniques such as [[windbreak]]s, [[reduced tillage]] or [[no-till]], spreading straw (or other [[mulch]] on particularly susceptible ground), and [[strip farming]] are used to minimize topsoil loss.