SOIL EROSION, CONSERVATION, AND ECO-ENVIRONMENT CHANGES IN THE LOESS PLATEAU OF CHINA
ABSTRACT As one of the best‐known areas in the world, the Loess Plateau, has long been suffering from serious soil erosion. The present paper reviewed the historical variation of climate, vegetation cover, and environment changes in order to understand the causes of severe soil erosion. Documentary...
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| Published in | Land degradation & development Vol. 24; no. 5; pp. 499 - 510 |
|---|---|
| Main Authors | , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Chichester
Blackwell Publishing Ltd
01.09.2013
Wiley Subscription Services, Inc |
| Subjects | |
| Online Access | Get full text |
| ISSN | 1085-3278 1099-145X |
| DOI | 10.1002/ldr.2246 |
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| Abstract | ABSTRACT
As one of the best‐known areas in the world, the Loess Plateau, has long been suffering from serious soil erosion. The present paper reviewed the historical variation of climate, vegetation cover, and environment changes in order to understand the causes of severe soil erosion. Documentary evidence indicated that climate changes and vegetation cover were the dominant natural factors influencing the soil erosion rates during the Holocene. Intensive human activities consisting of warfare, population growth, deforestation, and soil and water conservation measures were responsible for the changes of soil erosion during the anthropogenic period. Spatial and temporal changes of specific sediment yields presented significant decrease within the last several decades, which resulted from decreasing rainfall, large scale soil and water conservation measures, agricultural irrigation, and reservoir construction. Different phase of soil conservation measures demonstrated the development of policies and techniques on soil erosion control. Effective strategies of soil and water conservation, consisting of terracing, afforestation, natural rehabilitation, and check‐dams construction, were carried out on the Loess Plateau during the past six decades. The progress of soil conservation measures confirmed that the check‐dams systems might be suitable for Loess hilly Plateau, and natural vegetation rehabilitation is the best way for soil erosion control and should be implemented in other regions with emphasis of improving the quality of conservation measures based on natural rehabilitation. Copyright © 2013 John Wiley & Sons, Ltd. |
|---|---|
| AbstractList | As one of the best-known areas in the world, the Loess Plateau, has long been suffering from serious soil erosion. The present paper reviewed the historical variation of climate, vegetation cover, and environment changes in order to understand the causes of severe soil erosion. Documentary evidence indicated that climate changes and vegetation cover were the dominant natural factors influencing the soil erosion rates during the Holocene. Intensive human activities consisting of warfare, population growth, deforestation, and soil and water conservation measures were responsible for the changes of soil erosion during the anthropogenic period. Spatial and temporal changes of specific sediment yields presented significant decrease within the last several decades, which resulted from decreasing rainfall, large scale soil and water conservation measures, agricultural irrigation, and reservoir construction. Different phase of soil conservation measures demonstrated the development of policies and techniques on soil erosion control. Effective strategies of soil and water conservation, consisting of terracing, afforestation, natural rehabilitation, and check-dams construction, were carried out on the Loess Plateau during the past six decades. The progress of soil conservation measures confirmed that the check-dams systems might be suitable for Loess hilly Plateau, and natural vegetation rehabilitation is the best way for soil erosion control and should be implemented in other regions with emphasis of improving the quality of conservation measures based on natural rehabilitation. Copyright © 2013 John Wiley & Sons, Ltd. [PUBLICATION ABSTRACT] As one of the best‐known areas in the world, the Loess Plateau, has long been suffering from serious soil erosion. The present paper reviewed the historical variation of climate, vegetation cover, and environment changes in order to understand the causes of severe soil erosion. Documentary evidence indicated that climate changes and vegetation cover were the dominant natural factors influencing the soil erosion rates during the Holocene. Intensive human activities consisting of warfare, population growth, deforestation, and soil and water conservation measures were responsible for the changes of soil erosion during the anthropogenic period. Spatial and temporal changes of specific sediment yields presented significant decrease within the last several decades, which resulted from decreasing rainfall, large scale soil and water conservation measures, agricultural irrigation, and reservoir construction. Different phase of soil conservation measures demonstrated the development of policies and techniques on soil erosion control. Effective strategies of soil and water conservation, consisting of terracing, afforestation, natural rehabilitation, and check‐dams construction, were carried out on the Loess Plateau during the past six decades. The progress of soil conservation measures confirmed that the check‐dams systems might be suitable for Loess hilly Plateau, and natural vegetation rehabilitation is the best way for soil erosion control and should be implemented in other regions with emphasis of improving the quality of conservation measures based on natural rehabilitation. Copyright © 2013 John Wiley & Sons, Ltd. ABSTRACT As one of the best‐known areas in the world, the Loess Plateau, has long been suffering from serious soil erosion. The present paper reviewed the historical variation of climate, vegetation cover, and environment changes in order to understand the causes of severe soil erosion. Documentary evidence indicated that climate changes and vegetation cover were the dominant natural factors influencing the soil erosion rates during the Holocene. Intensive human activities consisting of warfare, population growth, deforestation, and soil and water conservation measures were responsible for the changes of soil erosion during the anthropogenic period. Spatial and temporal changes of specific sediment yields presented significant decrease within the last several decades, which resulted from decreasing rainfall, large scale soil and water conservation measures, agricultural irrigation, and reservoir construction. Different phase of soil conservation measures demonstrated the development of policies and techniques on soil erosion control. Effective strategies of soil and water conservation, consisting of terracing, afforestation, natural rehabilitation, and check‐dams construction, were carried out on the Loess Plateau during the past six decades. The progress of soil conservation measures confirmed that the check‐dams systems might be suitable for Loess hilly Plateau, and natural vegetation rehabilitation is the best way for soil erosion control and should be implemented in other regions with emphasis of improving the quality of conservation measures based on natural rehabilitation. Copyright © 2013 John Wiley & Sons, Ltd. |
| Author | Mu, X. Wang, F. Wen, Z. Gao, P. Zhao, G. |
| Author_xml | – sequence: 1 givenname: G. surname: Zhao fullname: Zhao, G. organization: Institute of Soil and Water Conservation, Northwest A&F University, 26 Xinong Road, 712100, Yangling, Shaanxi Province, China – sequence: 2 givenname: X. surname: Mu fullname: Mu, X. email: Correspondence to: X. Mu, Institute of Soil and Water Conservation, Northwest A&F University, 26 Xinong Road, Yangling, 712100, Shaanxi Province, China., xmmu@ms.iswc.ac.cn organization: Institute of Soil and Water Conservation, Northwest A&F University, 26 Xinong Road, 712100, Yangling, Shaanxi Province, China – sequence: 3 givenname: Z. surname: Wen fullname: Wen, Z. organization: Institute of Soil and Water Conservation, Northwest A&F University, 26 Xinong Road, 712100, Yangling, Shaanxi Province, China – sequence: 4 givenname: F. surname: Wang fullname: Wang, F. organization: Institute of Soil and Water Conservation, Northwest A&F University, 26 Xinong Road, 712100, Yangling, Shaanxi Province, China – sequence: 5 givenname: P. surname: Gao fullname: Gao, P. organization: Institute of Soil and Water Conservation, Northwest A&F University, 26 Xinong Road, 712100, Yangling, Shaanxi Province, China |
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| CODEN | LDDEF6 |
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As one of the best‐known areas in the world, the Loess Plateau, has long been suffering from serious soil erosion. The present paper reviewed the... As one of the best‐known areas in the world, the Loess Plateau, has long been suffering from serious soil erosion. The present paper reviewed the historical... As one of the best-known areas in the world, the Loess Plateau, has long been suffering from serious soil erosion. The present paper reviewed the historical... |
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| SubjectTerms | Anthropogenic factors Check dams Climate change Deforestation Development policy eco-environment changes Erosion control Erosion rates Holocene Irrigation water Loess Plateau Natural vegetation Population growth Reservoir construction runoff and sediment Sediment yield soil and water conservation Soil conservation Soil erosion Vegetation cover Water conservation |
| Title | SOIL EROSION, CONSERVATION, AND ECO-ENVIRONMENT CHANGES IN THE LOESS PLATEAU OF CHINA |
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