Natural and anthropogenic rates of soil erosion
Regions of land that are brought into crop production from native vegetation typically undergo a period of soil erosion instability, and long term erosion rates are greater than for natural lands as long as the land continues being used for crop production. Average rates of soil erosion under natura...
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Published in | International Soil and Water Conservation Research Vol. 5; no. 2; pp. 77 - 84 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.06.2017
KeAi Communications Co., Ltd |
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Abstract | Regions of land that are brought into crop production from native vegetation typically undergo a period of soil erosion instability, and long term erosion rates are greater than for natural lands as long as the land continues being used for crop production. Average rates of soil erosion under natural, non-cropped conditions have been documented to be less than 2Mgha−1yr−1. On-site rates of erosion of lands under cultivation over large cropland areas, such as in the United States, have been documented to be on the order of 6Mgha−1yr−1 or more. In northeastern China, lands that were brought into production during the last century are thought to have average rates of erosion over this large area of as much as 15Mgha−1yr−1 or more. Broadly applied soil conservation practices, and in particular conservation tillage and no-till cropping, have been found to be effective in reducing rates of erosion, as was seen in the United States when the average rates of erosion on cropped lands decreased from on the order of 9Mgha−1yr−1 to 6 or 7Mgha−1yr−1 between 1982 and 2002, coincident with the widespread adoption of new conservation tillage and residue management practices. Taking cropped lands out of production and restoring them to perennial plant cover, as was done in areas of the United States under the Conservation Reserve Program, is thought to reduce average erosion rates to approximately 1Mgha−1yr−1 or less on those lands. |
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AbstractList | Regions of land that are brought into crop production from native vegetation typically undergo a period of soil erosion instability, and long term erosion rates are greater than for natural lands as long as the land continues being used for crop production. Average rates of soil erosion under natural, non-cropped conditions have been documented to be less than 2Mgha−1yr−1. On-site rates of erosion of lands under cultivation over large cropland areas, such as in the United States, have been documented to be on the order of 6Mgha−1yr−1 or more. In northeastern China, lands that were brought into production during the last century are thought to have average rates of erosion over this large area of as much as 15Mgha−1yr−1 or more. Broadly applied soil conservation practices, and in particular conservation tillage and no-till cropping, have been found to be effective in reducing rates of erosion, as was seen in the United States when the average rates of erosion on cropped lands decreased from on the order of 9Mgha−1yr−1 to 6 or 7Mgha−1yr−1 between 1982 and 2002, coincident with the widespread adoption of new conservation tillage and residue management practices. Taking cropped lands out of production and restoring them to perennial plant cover, as was done in areas of the United States under the Conservation Reserve Program, is thought to reduce average erosion rates to approximately 1Mgha−1yr−1 or less on those lands. Regions of land that are brought into crop production from native vegetation typically undergo a period of soil erosion instability, and long term erosion rates are greater than for natural lands as long as the land continues being used for crop production. Average rates of soil erosion under natural, non-cropped conditions have been documented to be less than 2 Mg ha−1 yr−1. On-site rates of erosion of lands under cultivation over large cropland areas, such as in the United States, have been documented to be on the order of 6 Mg ha−1 yr−1 or more. In northeastern China, lands that were brought into production during the last century are thought to have average rates of erosion over this large area of as much as 15 Mg ha−1 yr−1 or more. Broadly applied soil conservation practices, and in particular conservation tillage and no-till cropping, have been found to be effective in reducing rates of erosion, as was seen in the United States when the average rates of erosion on cropped lands decreased from on the order of 9 Mg ha−1 yr−1 to 6 or 7 Mg ha−1 yr−1 between 1982 and 2002, coincident with the widespread adoption of new conservation tillage and residue management practices. Taking cropped lands out of production and restoring them to perennial plant cover, as was done in areas of the United States under the Conservation Reserve Program, is thought to reduce average erosion rates to approximately 1 Mg ha−1 yr−1 or less on those lands. |
Author | Xie, Yun Nearing, Mark A. Liu, Baoyuan Ye, Yu |
Author_xml | – sequence: 1 givenname: Mark A. surname: Nearing fullname: Nearing, Mark A. email: mark.nearing@ars.usda.gov organization: USDA-ARS, Southwest Watershed Research Center, 2000 Allen Rd., Tucson, AZ 85719, USA – sequence: 2 givenname: Yun surname: Xie fullname: Xie, Yun organization: School of Geography, Beijing Normal University, Beijing 100875, China – sequence: 3 givenname: Baoyuan surname: Liu fullname: Liu, Baoyuan organization: School of Geography, Beijing Normal University, Beijing 100875, China – sequence: 4 givenname: Yu surname: Ye fullname: Ye, Yu organization: School of Geography, Beijing Normal University, Beijing 100875, China |
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Keywords | No-till Conservation reserve program Virgin Lands Campaign Soil conservation Hugh Hammond Bennett Row crop agriculture Residue management Beryllium10 Conservation tillage National Resource Inventory Northeast China Cerrado Permaculture Isotopes |
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