Excerpt
L and drainage has been central to the development of North America since colonial times, with the first organized drainage efforts occurring as early as the 1600s (Evans et al. 1996). Drainage has been encouraged to improve public highways, reduce public health risks, promote increased crop yield and reduced yield variability, reduce surface runoff and erosion, and increase land value. Agricultural drainage includes artificial subsurface drainage and surface drainage. Most agricultural producers improve the drainage on their land for better trafficability, to enhance field conditions, to facilitate timely planting and harvesting operations, and to help decrease crop damage from saturated soil and standing water during the growing season. Agricultural drainage improvement also decreases year-to-year variability in crop yield, ensuring consistent production.
Increasingly, agricultural drainage is being targeted as a conduit for pollution, particularly nutrient pollution (Needelman et al. 2007). Considerable resistance exists in some regions to the expansion of drainage systems despite their importance to food production, with up to 50% of the cropland in some states under artificial drainage. However, because drainage ditches and subsurface drainage systems convert diffuse flows from the landscape into concentrated flows, they also provide opportunities for precision conservation, the targeting of specific practices to…
Footnotes
Jeffrey S. Strock is an associate professor with the University of Minnesota based in Lamberton, Minnesota. Peter J.A. Kleinman is a soil scientist with the USDA Agricultural Research Service in University Park, Pennsylvania. Kevin W. King is an agricultural engineer with the USDA Agricultural Research Service in Columbus, Ohio. Jorge A. Delgado is a soil scientist with the USDA Agricultural Research Service in Fort Collins, Colorado.
- © 2010 by the Soil and Water Conservation Society