Quantitative study on influences of terraced field construction and check-dam siltation on soil erosion

To study the influences of terraced field construction and check-dam siltation on soil erosion of a watershed, we built a simplified watershed model for the Loess Plateau hilly-gully region including terraced fields, slope farmlands, steep-slope grasslands, and dam farmlands and defined three states...

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Published in	Journal of geographical sciences Vol. 22; no. 5; pp. 946 - 960
Main Authors	Gao, Haidong, Li, Zhanbin, Li, Peng, Jia, Lianlian, Zhang, Xiang
Format	Journal Article
Language	English
Published	Heidelberg SP Science Press 01.10.2012 Springer Nature B.V Institute of Soil and Water Conservation, CAS and Ministry of Water Resources, Yangling 712100, Shaanxi,China%Institute of Soil and Water Conservation, CAS and Ministry of Water Resources, Yangling 712100, Shaanxi,China Key Lab of Northwest Water Resources and Environment Ecology of Ministry of Education, Xi'an University of Technology, Xi'an 710048, China%Key Lab of Northwest Water Resources and Environment Ecology of Ministry of Education, Xi'an University of Technology, Xi'an 710048, China%Upper and Middle Yellow River Bureau, Yellow River Conservancy Commission of the Ministry of Water Resources, Xi'an 710021, China
Subjects	Agricultural land Asia Bgi / Prodig Check dams China Earth and Environmental Science Geographical Information Systems/Cartography Geography Grasslands Gullies Nature Conservation Physical Geography Quantitative research Remote Sensing/Photogrammetry Soil erosion Water conservation Watersheds 分水岭土壤侵蚀模数梯田建设泥沙淤积流域模型淤地坝通用土壤流失方程黄土高原丘陵沟壑区 China Shaanxi China, People's Rep., Loess Plateau succession soil-and-water conservation Revised Universal Soil Loss Equation the Loess Plateau Human impact Loess Plateau Soil erosion Slope gradient Erodibility Gully erosion Dam Soil properties Watershed Soil water Model Hydraulic works Terrace cultivation Quantitative analysis
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ISSN	1009-637X 1861-9568
DOI	10.1007/s11442-012-0975-5

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Abstract	To study the influences of terraced field construction and check-dam siltation on soil erosion of a watershed, we built a simplified watershed model for the Loess Plateau hilly-gully region including terraced fields, slope farmlands, steep-slope grasslands, and dam farmlands and defined three states of watershed （i.e., pioneer, intermediate, and climax stages, respec- tively）. Then, the watershed soil erosion moduli at various stages were studied by using a revised universal soil loss equation. Our results show that the pioneer and climax stages are the extreme states of watershed soil-and-water conservation and control; in the pioneer stage the soil erosion modulus was 299.56 t.ha-l.a 1 above the edge of gully, 136.64 t.ha-La-1 below the edge of gully, and 229.74 t.ha-~.a-~ on average; in the climax stage, the soil erosion modulus was 39.10 t.ha .a-1 above the edge of gully, 1.10 t.ha-La-1 below the edge of gully, and 22.81 t-ha-La-1 on average; in the intermediate stage, the soil erosion modulus above the edge of gully exhibited an exponential decline along with the increase in terraced field area percentage, while the soil erosion modulus below the edge of gully exhibited a linear decline along with the increase in siltation height.
AbstractList	To study the influences of terraced field construction and check-dam siltation on soil erosion of a watershed, we built a simplified watershed model for the Loess Plateau hilly-gully region including terraced fields, slope farmlands, steep-slope grasslands, and dam farmlands and defined three states of watershed （i.e., pioneer, intermediate, and climax stages, respec- tively）. Then, the watershed soil erosion moduli at various stages were studied by using a revised universal soil loss equation. Our results show that the pioneer and climax stages are the extreme states of watershed soil-and-water conservation and control; in the pioneer stage the soil erosion modulus was 299.56 t.ha-l.a 1 above the edge of gully, 136.64 t.ha-La-1 below the edge of gully, and 229.74 t.ha-~.a-~ on average; in the climax stage, the soil erosion modulus was 39.10 t.ha .a-1 above the edge of gully, 1.10 t.ha-La-1 below the edge of gully, and 22.81 t-ha-La-1 on average; in the intermediate stage, the soil erosion modulus above the edge of gully exhibited an exponential decline along with the increase in terraced field area percentage, while the soil erosion modulus below the edge of gully exhibited a linear decline along with the increase in siltation height. To study the influences of terraced field construction and check-dam siltation on soil erosion of a watershed, we built a simplified watershed model for the Loess Plateau hilly-gully region including terraced fields, slope farmlands, steep-slope grasslands, and dam farmlands, and defined three states of watershed (i.e., pioneer, intermediate, and climax stages, respectively). Then, the watershed soil erosion moduli at various stages were studied by using a revised universal soil loss equation. Our results show that the pioneer and climax stages are the extreme states of watershed soil-and-water conservation and control; in the pioneer stage, the soil erosion modulus was 299.56 t·ha −1 ·a −1 above the edge of gully, 136.64 t·ha −1 ·a −1 below the edge of gully, and 229.74 t·ha −1 ·a −1 on average; in the climax stage, the soil erosion modulus was 39.10 t·ha −1 ·a −1 above the edge of gully, 1.10 t·ha −1 ·a −1 below the edge of gully, and 22.81 t·ha −1 ·a −1 on average; in the intermediate stage, the soil erosion modulus above the edge of gully exhibited an exponential decline along with the increase in terraced field area percentage, while the soil erosion modulus below the edge of gully exhibited a linear decline along with the increase in siltation height. To study the influences of terraced field construction and check-dam siltation on soil erosion of a watershed, we built a simplified watershed model for the Loess Plateau hilly-gully region including terraced fields, slope farmlands, steep-slope grasslands, and dam farmlands, and defined three states of watershed (i.e., pioneer, intermediate, and climax stages, respectively). Then, the watershed soil erosion moduli at various stages were studied by using a revised universal soil loss equation. Our results show that the pioneer and climax stages are the extreme states of watershed soil-and-water conservation and control; in the pioneer stage, the soil erosion modulus was 299.56 t·ha−1·a−1 above the edge of gully, 136.64 t·ha−1·a−1 below the edge of gully, and 229.74 t·ha−1·a−1 on average; in the climax stage, the soil erosion modulus was 39.10 t·ha−1·a−1 above the edge of gully, 1.10 t·ha−1·a−1 below the edge of gully, and 22.81 t·ha−1·a−1 on average; in the intermediate stage, the soil erosion modulus above the edge of gully exhibited an exponential decline along with the increase in terraced field area percentage, while the soil erosion modulus below the edge of gully exhibited a linear decline along with the increase in siltation height. To study the influences of terraced field construction and check-dam siltation on soil erosion of a watershed, we built a simplified watershed model for the Loess Plateau hilly-gully region including terraced fields, slope farmlands, steep-slope grasslands, and dam farmlands, and defined three states of watershed (i.e., pioneer, intermediate, and climax stages, respectively). Then, the watershed soil erosion moduli at various stages were studied by using a revised universal soil loss equation. Our results show that the pioneer and climax stages are the extreme states of watershed soil-and-water conservation and control; in the pioneer stage, the soil erosion modulus was 299.56 t?ha-1?a-1 above the edge of gully, 136.64 t?ha-1?a-1 below the edge of gully, and 229.74 t?ha-1?a-1 on average; in the climax stage, the soil erosion modulus was 39.10 t?ha-1?a-1 above the edge of gully, 1.10 t?ha-1?a-1 below the edge of gully, and 22.81 t?ha-1?a-1 on average; in the intermediate stage, the soil erosion modulus above the edge of gully exhibited an exponential decline along with the increase in terraced field area percentage, while the soil erosion modulus below the edge of gully exhibited a linear decline along with the increase in siltation height.
Author	GAO Haidong LI Zhanbin LI Peng JIA Lianlian ZHANG Xiang
AuthorAffiliation	institute of Soil and Water Conservation, CAS and Ministry of Water Resources, Yangling 712100, Shaanxi, China; Key Lab of Northwest Water Resources and Environment Ecology of Ministry of Education, Xi＇an University of Technology, Xi＇an 710048, China Upper and Middle Yellow River Bureau, Yellow River Conservancy Commission of the Ministry of Water Resources, Xi＇an 710021, China
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Cites_doi	10.1016/0022-1694(89)90073-5 10.13031/2013.33893 10.1080/02626669909492199 10.1016/0022-1694(94)90110-4 10.13031/2013.28273 10.13031/2013.30576 10.13031/2013.27535 10.1080/00690805.2001.9714133
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Keywords	succession soil-and-water conservation Revised Universal Soil Loss Equation the Loess Plateau Human impact Loess Plateau Soil erosion Slope gradient Erodibility Gully erosion Dam Soil properties Watershed Soil water Model Hydraulic works Terrace cultivation Quantitative analysis
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Notes	soil-and-water conservation; Revised Universal Soil Loss Equation; succession; the Loess Plateau To study the influences of terraced field construction and check-dam siltation on soil erosion of a watershed, we built a simplified watershed model for the Loess Plateau hilly-gully region including terraced fields, slope farmlands, steep-slope grasslands, and dam farmlands and defined three states of watershed （i.e., pioneer, intermediate, and climax stages, respec- tively）. Then, the watershed soil erosion moduli at various stages were studied by using a revised universal soil loss equation. Our results show that the pioneer and climax stages are the extreme states of watershed soil-and-water conservation and control; in the pioneer stage the soil erosion modulus was 299.56 t.ha-l.a 1 above the edge of gully, 136.64 t.ha-La-1 below the edge of gully, and 229.74 t.ha-~.a-~ on average; in the climax stage, the soil erosion modulus was 39.10 t.ha .a-1 above the edge of gully, 1.10 t.ha-La-1 below the edge of gully, and 22.81 t-ha-La-1 on average; in the intermediate stage, the soil erosion modulus above the edge of gully exhibited an exponential decline along with the increase in terraced field area percentage, while the soil erosion modulus below the edge of gully exhibited a linear decline along with the increase in siltation height. 11-4546/P ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23
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Publisher	SP Science Press Springer Nature B.V Institute of Soil and Water Conservation, CAS and Ministry of Water Resources, Yangling 712100, Shaanxi,China%Institute of Soil and Water Conservation, CAS and Ministry of Water Resources, Yangling 712100, Shaanxi,China Key Lab of Northwest Water Resources and Environment Ecology of Ministry of Education, Xi'an University of Technology, Xi'an 710048, China%Key Lab of Northwest Water Resources and Environment Ecology of Ministry of Education, Xi'an University of Technology, Xi'an 710048, China%Upper and Middle Yellow River Bureau, Yellow River Conservancy Commission of the Ministry of Water Resources, Xi'an 710021, China
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Snippet	To study the influences of terraced field construction and check-dam siltation on soil erosion of a watershed, we built a simplified watershed model for the...
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SubjectTerms	Agricultural land Asia Bgi / Prodig Check dams China Earth and Environmental Science Geographical Information Systems/Cartography Geography Grasslands Gullies Nature Conservation Physical Geography Quantitative research Remote Sensing/Photogrammetry Soil erosion Water conservation Watersheds 分水岭土壤侵蚀模数梯田建设泥沙淤积流域模型淤地坝通用土壤流失方程黄土高原丘陵沟壑区
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Title	Quantitative study on influences of terraced field construction and check-dam siltation on soil erosion
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