Estimation Model of Soil Freeze-Thaw Erosion in Silingco Watershed Wetland of Northern Tibet

The freeze-thaw (FT) erosion is a type of soil erosion like water erosion and wind erosion. Limited by many factors, the grading evaluation of soil FT erosion quantities is not well studied. Based on the comprehensive analysis of the evaluation indices of soil FT erosion, we for the first time utili...

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Main Authors: Bo Kong, Huan Yu
Format: Article
Language:English
Published: Wiley 2013-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1155/2013/636521
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author Bo Kong
Huan Yu
author_facet Bo Kong
Huan Yu
author_sort Bo Kong
collection DOAJ
description The freeze-thaw (FT) erosion is a type of soil erosion like water erosion and wind erosion. Limited by many factors, the grading evaluation of soil FT erosion quantities is not well studied. Based on the comprehensive analysis of the evaluation indices of soil FT erosion, we for the first time utilized the sensitivity of microwave remote sensing technology to soil moisture for identification of FT state. We established an estimation model suitable to evaluate the soil FT erosion quantity in Silingco watershed wetland of Northern Tibet using weighted summation method of six impact factors including the annual FT cycle days, average diurnal FT phase-changed water content, average annual precipitation, slope, aspect, and vegetation coverage. Finally, with the support of GIS, we classified soil FT erosion quantity in Silingco watershed wetland. The results showed that soil FT erosion are distributed in broad areas of Silingco watershed wetland. Different soil FT erosions with different intensities have evidently different spatial and geographical distributions.
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issn 1537-744X
language English
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publisher Wiley
record_format Article
series The Scientific World Journal
spelling doaj-art-bff86083d6c14837bfb10d9bcbe028102025-02-03T01:03:11ZengWileyThe Scientific World Journal1537-744X2013-01-01201310.1155/2013/636521636521Estimation Model of Soil Freeze-Thaw Erosion in Silingco Watershed Wetland of Northern TibetBo Kong0Huan Yu1Chinese Academy of Sciences of Mountain Hazards and Environment, Chengdu 610041, ChinaCollege of Earth Sciences, Chengdu University of Technology, Chengdu 610059, ChinaThe freeze-thaw (FT) erosion is a type of soil erosion like water erosion and wind erosion. Limited by many factors, the grading evaluation of soil FT erosion quantities is not well studied. Based on the comprehensive analysis of the evaluation indices of soil FT erosion, we for the first time utilized the sensitivity of microwave remote sensing technology to soil moisture for identification of FT state. We established an estimation model suitable to evaluate the soil FT erosion quantity in Silingco watershed wetland of Northern Tibet using weighted summation method of six impact factors including the annual FT cycle days, average diurnal FT phase-changed water content, average annual precipitation, slope, aspect, and vegetation coverage. Finally, with the support of GIS, we classified soil FT erosion quantity in Silingco watershed wetland. The results showed that soil FT erosion are distributed in broad areas of Silingco watershed wetland. Different soil FT erosions with different intensities have evidently different spatial and geographical distributions.http://dx.doi.org/10.1155/2013/636521
spellingShingle Bo Kong
Huan Yu
Estimation Model of Soil Freeze-Thaw Erosion in Silingco Watershed Wetland of Northern Tibet
The Scientific World Journal
title Estimation Model of Soil Freeze-Thaw Erosion in Silingco Watershed Wetland of Northern Tibet
title_full Estimation Model of Soil Freeze-Thaw Erosion in Silingco Watershed Wetland of Northern Tibet
title_fullStr Estimation Model of Soil Freeze-Thaw Erosion in Silingco Watershed Wetland of Northern Tibet
title_full_unstemmed Estimation Model of Soil Freeze-Thaw Erosion in Silingco Watershed Wetland of Northern Tibet
title_short Estimation Model of Soil Freeze-Thaw Erosion in Silingco Watershed Wetland of Northern Tibet
title_sort estimation model of soil freeze thaw erosion in silingco watershed wetland of northern tibet
url http://dx.doi.org/10.1155/2013/636521
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