Assessing the declining trend in soil erodibility across China: A comparison of conventional and digital K-factor maps
Soil erodibility is a measure of soil susceptibility to water erosion and serves as an essential element, also known as the K-factor, in empirical soil erosion prediction models, such as USLE, RUSLE, and CSLE. The currently available map of the K-factor for China was generated based on the conventio...
Saved in:
Main Authors: | , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
KeAi Communications Co., Ltd.
2025-03-01
|
Series: | International Soil and Water Conservation Research |
Subjects: | |
Online Access: | http://www.sciencedirect.com/science/article/pii/S2095633924000297 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
_version_ | 1841556958260232192 |
---|---|
author | Zhiyuan Tian Yan Zhao Longxi Cao Yuan Zhao Yin Liang |
author_facet | Zhiyuan Tian Yan Zhao Longxi Cao Yuan Zhao Yin Liang |
author_sort | Zhiyuan Tian |
collection | DOAJ |
description | Soil erodibility is a measure of soil susceptibility to water erosion and serves as an essential element, also known as the K-factor, in empirical soil erosion prediction models, such as USLE, RUSLE, and CSLE. The currently available map of the K-factor for China was generated based on the conventional soil polygon linkage method and soil species survey conducted in the 1980s. For update, an investigation of 4262 samples from the soil series survey in the 2010s and a random forest regression model were used to generate a new K-factor map for China. A digital K-factor map at the 250 m spatial resolution was generated by calculating the K values from soil survey points as training data and using environmental information as predictive variables. The comparison results between the digital and conventional K-factor maps show that there has been a decreasing trend in the K-factor over recent decades. The K value decrease was mainly attributed to the update of soil survey data (the mean K value changed from 0.03193 t ha·h/(MJ·mm·ha) in the soil species database to 0.02988 t ha·h/(MJ·mm·ha) in the soil series) and was less influenced by the replacement of the mapping methods (the mean K value changed from 0.03197 t ha·h/(MJ·mm·ha) in the soil polygon linkage method to 0.03193 t ha·h/(MJ·mm·ha) in the random forest). This study quantified the sources of change between previous and updated national K-factor maps and demonstrated that there is a decreasing trend in K values, which is consistent with the increasing soil organic matter and improved ecological environment in China. |
format | Article |
id | doaj-art-9b93125bd04c4bf084416e532e3fe11b |
institution | Kabale University |
issn | 2095-6339 |
language | English |
publishDate | 2025-03-01 |
publisher | KeAi Communications Co., Ltd. |
record_format | Article |
series | International Soil and Water Conservation Research |
spelling | doaj-art-9b93125bd04c4bf084416e532e3fe11b2025-01-07T04:17:15ZengKeAi Communications Co., Ltd.International Soil and Water Conservation Research2095-63392025-03-011311526Assessing the declining trend in soil erodibility across China: A comparison of conventional and digital K-factor mapsZhiyuan Tian0Yan Zhao1Longxi Cao2Yuan Zhao3Yin Liang4State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, Jiangsu, 211135, ChinaState Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, Jiangsu, 211135, ChinaCollege of Ecology and Environment, Chengdu University of Technology, Chengdu, Sichuan, 610059, ChinaMonitoring Centre of Soil and Water Conservation, Ministry of Water Resources, Beijing, 100053, ChinaState Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, Jiangsu, 211135, China; Corresponding author. NO.298 Chuangyou Road, Nanjing, 211135, China.Soil erodibility is a measure of soil susceptibility to water erosion and serves as an essential element, also known as the K-factor, in empirical soil erosion prediction models, such as USLE, RUSLE, and CSLE. The currently available map of the K-factor for China was generated based on the conventional soil polygon linkage method and soil species survey conducted in the 1980s. For update, an investigation of 4262 samples from the soil series survey in the 2010s and a random forest regression model were used to generate a new K-factor map for China. A digital K-factor map at the 250 m spatial resolution was generated by calculating the K values from soil survey points as training data and using environmental information as predictive variables. The comparison results between the digital and conventional K-factor maps show that there has been a decreasing trend in the K-factor over recent decades. The K value decrease was mainly attributed to the update of soil survey data (the mean K value changed from 0.03193 t ha·h/(MJ·mm·ha) in the soil species database to 0.02988 t ha·h/(MJ·mm·ha) in the soil series) and was less influenced by the replacement of the mapping methods (the mean K value changed from 0.03197 t ha·h/(MJ·mm·ha) in the soil polygon linkage method to 0.03193 t ha·h/(MJ·mm·ha) in the random forest). This study quantified the sources of change between previous and updated national K-factor maps and demonstrated that there is a decreasing trend in K values, which is consistent with the increasing soil organic matter and improved ecological environment in China.http://www.sciencedirect.com/science/article/pii/S2095633924000297Soil erosionRandom forestEnvironmental variablesSoil survey databaseSpatiotemporal variation |
spellingShingle | Zhiyuan Tian Yan Zhao Longxi Cao Yuan Zhao Yin Liang Assessing the declining trend in soil erodibility across China: A comparison of conventional and digital K-factor maps International Soil and Water Conservation Research Soil erosion Random forest Environmental variables Soil survey database Spatiotemporal variation |
title | Assessing the declining trend in soil erodibility across China: A comparison of conventional and digital K-factor maps |
title_full | Assessing the declining trend in soil erodibility across China: A comparison of conventional and digital K-factor maps |
title_fullStr | Assessing the declining trend in soil erodibility across China: A comparison of conventional and digital K-factor maps |
title_full_unstemmed | Assessing the declining trend in soil erodibility across China: A comparison of conventional and digital K-factor maps |
title_short | Assessing the declining trend in soil erodibility across China: A comparison of conventional and digital K-factor maps |
title_sort | assessing the declining trend in soil erodibility across china a comparison of conventional and digital k factor maps |
topic | Soil erosion Random forest Environmental variables Soil survey database Spatiotemporal variation |
url | http://www.sciencedirect.com/science/article/pii/S2095633924000297 |
work_keys_str_mv | AT zhiyuantian assessingthedecliningtrendinsoilerodibilityacrosschinaacomparisonofconventionalanddigitalkfactormaps AT yanzhao assessingthedecliningtrendinsoilerodibilityacrosschinaacomparisonofconventionalanddigitalkfactormaps AT longxicao assessingthedecliningtrendinsoilerodibilityacrosschinaacomparisonofconventionalanddigitalkfactormaps AT yuanzhao assessingthedecliningtrendinsoilerodibilityacrosschinaacomparisonofconventionalanddigitalkfactormaps AT yinliang assessingthedecliningtrendinsoilerodibilityacrosschinaacomparisonofconventionalanddigitalkfactormaps |