Soil Erosion and Controls in the Slope-Gully System of the Loess Plateau of China: A Review
The Loess Plateau has long been suffering from serious soil erosion of which erosion from the slope-gully system is now dominant. The slope-gully system is characterized with distinctive erosion distribution zones consisting of inner and inter gully areas wherein erosion patterns spatially vary, act...
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Frontiers Media S.A.
2021-05-01
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Online Access: | https://www.frontiersin.org/articles/10.3389/fenvs.2021.657030/full |
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author | Bingbing Zhu Zhengchao Zhou Zhanbin Li |
author_facet | Bingbing Zhu Zhengchao Zhou Zhanbin Li |
author_sort | Bingbing Zhu |
collection | DOAJ |
description | The Loess Plateau has long been suffering from serious soil erosion of which erosion from the slope-gully system is now dominant. The slope-gully system is characterized with distinctive erosion distribution zones consisting of inner and inter gully areas wherein erosion patterns spatially vary, acting as both sediment source and the dominant sediment and water transport mechanism. In this paper, a substantial body of research is reviewed concentrating on the soil erosion processes and control practices in the slope-gully system. The inner gully area is identified as the main sediment source while runoff and sediment from the inter-gully upland is found to significantly affect down slope erosion processes. Correspondingly, the protective vegetation pattern and coverage should be strategically designed for different erosion zones with an emphasis on the critical vegetation cover and pattern to reduce sediment yield of the whole slope-gully system. Check-dam could change the base level of erosion and reduce the slope length of the gully side, which will further decrease the possibility and magnitude of gravity erosion. We concluded that understanding the erosion processes and implementing erosion practices for the slope-gully system are of importance and require more research efforts that emphasize: 1) the influence of upland runoff on erosion processes at downslope; 2) the relationship between hydraulic characteristics of overland flow and erosion process at a slope-gully system scale; 3) physical mechanisms of different vegetation patterns on the slope-gully erosion process. |
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id | doaj.art-9af1b8dbcffa4c6cbd12479014837b94 |
institution | Directory Open Access Journal |
issn | 2296-665X |
language | English |
last_indexed | 2024-12-16T13:08:11Z |
publishDate | 2021-05-01 |
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series | Frontiers in Environmental Science |
spelling | doaj.art-9af1b8dbcffa4c6cbd12479014837b942022-12-21T22:30:41ZengFrontiers Media S.A.Frontiers in Environmental Science2296-665X2021-05-01910.3389/fenvs.2021.657030657030Soil Erosion and Controls in the Slope-Gully System of the Loess Plateau of China: A ReviewBingbing Zhu0Zhengchao Zhou1Zhanbin Li2School of Geography and Tourism, Shaanxi Normal University, Xi’an, ChinaSchool of Geography and Tourism, Shaanxi Normal University, Xi’an, ChinaState Key Laboratory Base of Eco-hydraulic Engineering in Area, Xi’an University of Technology, Xi’an, ChinaThe Loess Plateau has long been suffering from serious soil erosion of which erosion from the slope-gully system is now dominant. The slope-gully system is characterized with distinctive erosion distribution zones consisting of inner and inter gully areas wherein erosion patterns spatially vary, acting as both sediment source and the dominant sediment and water transport mechanism. In this paper, a substantial body of research is reviewed concentrating on the soil erosion processes and control practices in the slope-gully system. The inner gully area is identified as the main sediment source while runoff and sediment from the inter-gully upland is found to significantly affect down slope erosion processes. Correspondingly, the protective vegetation pattern and coverage should be strategically designed for different erosion zones with an emphasis on the critical vegetation cover and pattern to reduce sediment yield of the whole slope-gully system. Check-dam could change the base level of erosion and reduce the slope length of the gully side, which will further decrease the possibility and magnitude of gravity erosion. We concluded that understanding the erosion processes and implementing erosion practices for the slope-gully system are of importance and require more research efforts that emphasize: 1) the influence of upland runoff on erosion processes at downslope; 2) the relationship between hydraulic characteristics of overland flow and erosion process at a slope-gully system scale; 3) physical mechanisms of different vegetation patterns on the slope-gully erosion process.https://www.frontiersin.org/articles/10.3389/fenvs.2021.657030/fullLoess plateau of Chinaslope-gully systemsoil erosionvegetation recovery and reconstructionvegetation pattern |
spellingShingle | Bingbing Zhu Zhengchao Zhou Zhanbin Li Soil Erosion and Controls in the Slope-Gully System of the Loess Plateau of China: A Review Frontiers in Environmental Science Loess plateau of China slope-gully system soil erosion vegetation recovery and reconstruction vegetation pattern |
title | Soil Erosion and Controls in the Slope-Gully System of the Loess Plateau of China: A Review |
title_full | Soil Erosion and Controls in the Slope-Gully System of the Loess Plateau of China: A Review |
title_fullStr | Soil Erosion and Controls in the Slope-Gully System of the Loess Plateau of China: A Review |
title_full_unstemmed | Soil Erosion and Controls in the Slope-Gully System of the Loess Plateau of China: A Review |
title_short | Soil Erosion and Controls in the Slope-Gully System of the Loess Plateau of China: A Review |
title_sort | soil erosion and controls in the slope gully system of the loess plateau of china a review |
topic | Loess plateau of China slope-gully system soil erosion vegetation recovery and reconstruction vegetation pattern |
url | https://www.frontiersin.org/articles/10.3389/fenvs.2021.657030/full |
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