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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Main Authors: Yao Kun, Chen Jian-Bin, Yang Yong-Sheng, Zhang Yong, Liao Cheng-Hao
Format: Article
Language:English
Published: EDP Sciences 2019-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/44/e3sconf_icaeer18_04011.pdf
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spelling 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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AT yangyongsheng analysisofspatialandtemporalchangesofsoilerosioninanningriverbasin
AT zhangyong analysisofspatialandtemporalchangesofsoilerosioninanningriverbasin
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