Erosion Evolution in the Source Regions of the Yangtze and Yellow Rivers From a Climate-Ecology-Hydrology Zoning Perspective

IF 4 2区 农林科学 Q2 SOIL SCIENCE
Wenying Zeng, Qiqi Zhang, Zicheng Yu, Wenyi Sun
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Abstract

Combining soil erosion with comprehensive zoning can reflect the spatial differentiation of soil erosion and reveal the driving forces behind changes in soil erosion. Here, the Köppen climate classification and K-means unsupervised clustering analysis were used to categorise the source regions of the Yangtze and Yellow Rivers (SRYYR) into eight integrated climate-ecology-hydrology zones, considering vegetation, climate, runoff, and sediment transport. The CSLE model was used to analyse soil erosion rate evolution patterns and the impacts of extreme rainfall events in each zone. The study found that the eastern source of the Yangtze River and the northern source of the Yellow River experienced severe erosion. Vegetation and biological practices in the Yellow River source region were significantly better than that of the Yangtze River. Rainfall erosivity increased from northwest to southeast. Extreme rainfall can lead to a 3.86-fold difference in rainfall erosivity, and the annual distribution of rainfall significantly affects soil erosion rates. There were significant spatial differences and trends in soil erosion rates across different regions, with the central part of SRYYR still undergoing significant degradation. Conservation measures resulted in a 26.15% decrease in the B factor (vegetation and biological practice factor) in Zones II, V, VI, and VII, but the current state of vegetation cover in Zone VIII remains a concern (increase 9.23%). The condition of grassland erosion in the SRYYR region improved year by year, while arable land experienced a worsening trend, and the soil erosion rates in forests fluctuated within a certain range. The formation of erosion channels and sediment transport not only changes the landscape but also has profound impacts on water quality and downstream ecosystems.

气候-生态-水文区划视角下的长江黄河源区侵蚀演变
将土壤侵蚀与综合区划相结合,可以反映土壤侵蚀的空间分异,揭示土壤侵蚀变化的驱动力。本文采用Köppen气候分类和K-means无监督聚类分析方法,综合考虑植被、气候、径流和输沙等因素,将长江黄河源区划分为8个气候-生态-水文综合带。利用CSLE模型分析了各区域土壤侵蚀速率演变规律和极端降雨事件的影响。研究发现,长江东部源区和黄河北部源区侵蚀严重。黄河源区的植被和生物实践明显优于长江源区。降雨侵蚀力由西北向东南增加。极端降雨可导致降雨侵蚀力差异达3.86倍,年降雨量分布显著影响土壤侵蚀速率。不同区域的土壤侵蚀速率存在显著的空间差异和趋势,其中SRYYR中部仍处于明显的退化状态。采取保护措施后,II、V、VI和VII区植被B因子(植被和生物实践因子)下降了26.15%,但VIII区植被覆盖现状仍然令人关注(增加了9.23%)。SRYYR地区草地侵蚀状况逐年改善,耕地侵蚀状况呈恶化趋势,森林土壤侵蚀速率在一定范围内波动。侵蚀通道的形成和泥沙的搬运不仅改变了景观,而且对水质和下游生态系统产生了深远的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
European Journal of Soil Science
European Journal of Soil Science 农林科学-土壤科学
CiteScore
8.20
自引率
4.80%
发文量
117
审稿时长
5 months
期刊介绍: The EJSS is an international journal that publishes outstanding papers in soil science that advance the theoretical and mechanistic understanding of physical, chemical and biological processes and their interactions in soils acting from molecular to continental scales in natural and managed environments.
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