Analysis of spatial and temporal changes of soil erosion in Anning river basin
Anning River basin as an important soil erosion monitoring and reserve in Sichuan Province. It is of great significance to grasp the temporal and spatial changes of soil erosion in this area in time to realize the comprehensive treatment of regional soil erosion. Based on the revision of the general...
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2019-01-01
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doaj-2c48602530a5446c974f04b61dca770b2021-04-02T15:34:08ZengEDP SciencesE3S Web of Conferences2267-12422019-01-011180401110.1051/e3sconf/201911804011e3sconf_icaeer18_04011Analysis of spatial and temporal changes of soil erosion in Anning river basinYao Kun0Chen Jian-Bin1Yang Yong-Sheng2Zhang Yong3Liao Cheng-Hao4School of resources and Environment, Xichang UniversitySchool of resources and Environment, Xichang UniversityState Grid Liangshan Power Supply CompanyLiangshan Four Brothers Agricultural Development Limited companySchool of resources and Environment, Xichang UniversityAnning River basin as an important soil erosion monitoring and reserve in Sichuan Province. It is of great significance to grasp the temporal and spatial changes of soil erosion in this area in time to realize the comprehensive treatment of regional soil erosion. Based on the revision of the general soil erosion equation (RUSLE), the present situation of soil erosion erosion in 1995-2015 years in this area was monitored, and the classification was completed according to the national grading criteria, and the following results were mainly achieved:(1) Soil erosion in Anning river basin as a whole presents a low gradient change in the eastern High West.(2) The proportion of raster in soil erosion area of each grade also showed different structural differences, which showed that the degree of micro > Mild > Moderate > Strong > Extremely > severe, and the proportion of raster in mild and below intensity erosion area reached more than 80%, and the whole basin was at mildly below erosion level.(3) One-dimensional linear regression analysis shows, within 20 years, about 90% of the raster cell slope in this area is negative, the overall change trend of soil erosion in this area shows a significant improvementhttps://www.e3s-conferences.org/articles/e3sconf/pdf/2019/44/e3sconf_icaeer18_04011.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Yao Kun Chen Jian-Bin Yang Yong-Sheng Zhang Yong Liao Cheng-Hao |
spellingShingle |
Yao Kun Chen Jian-Bin Yang Yong-Sheng Zhang Yong Liao Cheng-Hao Analysis of spatial and temporal changes of soil erosion in Anning river basin E3S Web of Conferences |
author_facet |
Yao Kun Chen Jian-Bin Yang Yong-Sheng Zhang Yong Liao Cheng-Hao |
author_sort |
Yao Kun |
title |
Analysis of spatial and temporal changes of soil erosion in Anning river basin |
title_short |
Analysis of spatial and temporal changes of soil erosion in Anning river basin |
title_full |
Analysis of spatial and temporal changes of soil erosion in Anning river basin |
title_fullStr |
Analysis of spatial and temporal changes of soil erosion in Anning river basin |
title_full_unstemmed |
Analysis of spatial and temporal changes of soil erosion in Anning river basin |
title_sort |
analysis of spatial and temporal changes of soil erosion in anning river basin |
publisher |
EDP Sciences |
series |
E3S Web of Conferences |
issn |
2267-1242 |
publishDate |
2019-01-01 |
description |
Anning River basin as an important soil erosion monitoring and reserve in Sichuan Province. It is of great significance to grasp the temporal and spatial changes of soil erosion in this area in time to realize the comprehensive treatment of regional soil erosion. Based on the revision of the general soil erosion equation (RUSLE), the present situation of soil erosion erosion in 1995-2015 years in this area was monitored, and the classification was completed according to the national grading criteria, and the following results were mainly achieved:(1) Soil erosion in Anning river basin as a whole presents a low gradient change in the eastern High West.(2) The proportion of raster in soil erosion area of each grade also showed different structural differences, which showed that the degree of micro > Mild > Moderate > Strong > Extremely > severe, and the proportion of raster in mild and below intensity erosion area reached more than 80%, and the whole basin was at mildly below erosion level.(3) One-dimensional linear regression analysis shows, within 20 years, about 90% of the raster cell slope in this area is negative, the overall change trend of soil erosion in this area shows a significant improvement |
url |
https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/44/e3sconf_icaeer18_04011.pdf |
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