[Analysis and Prediction of Soil Erosion Under Different Land Use Change Scenarios in Kuye River Basin Based on PLUS-CSLE Model].

Q2 Environmental Science
Yu-Chi Chen, Yuan He, Ahmd Ehab Talat, Jian Wang, Ze-Kang Cai
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Abstract

The distribution of land use types is a comprehensive reflection of natural conditions and human activities, which affects the process of runoff and sediment transport by changing the surface morphology, and then affects the process of soil erosion. Based on the land use data in the Kuye River Basin from 2010 to 2020, this study uses the PLUS model to predict the land use distribution in 2025 under three scenarios and evaluates the soil erosion intensity from 2010 to 2025 on CSLE model, so as to explore the impact of land use change on soil erosion. The results showed that: ① From 2010 to 2020, the land use distribution in the Kuye River Basin was dominated by grassland and farmland. The area of farmland and grassland decreased, while the construction land and unused land increased. The expansion of farmland and grassland was mainly affected by elevation, rainfall, and population, and the expansion of construction land was mainly because of human activities. ② The soil erosion intensities in 2010, 2015, and 2020 were 25.91, 22.82, and 27.58 t·(hm2·a)-1, respectively, showing a trend of first weakening and then rebounding. ③ The soil erosion intensities under the simulated natural development, ecological protection, and economic growth scenarios in 2025 were 25.62, 24.60, and 27.41 t·(hm2·a)-1. The ecological protection scenario was better for controlling the soil erosion. ④ The areas with the most soil erosion in the basin were mainly the grassland and farmland in the loess gully in the central and southern parts, as well as the degraded land around some industrial/mining concentration parts. To effectively reduce the soil erosion, increasing forest and grassland while reducing the farmland and industrial/mining zones is suggested. Notably, focus should be on bolstering the upkeep and preserving terraced farmlands.

基于PLUS-CSLE模型的库野河流域不同土地利用变化情景土壤侵蚀分析与预测[j]。
土地利用类型分布是自然条件和人类活动的综合反映,通过改变地表形态影响径流输沙过程,进而影响土壤侵蚀过程。基于2010 - 2020年库野河流域土地利用数据,采用PLUS模型预测2025年3种情景下的土地利用分布,并利用CSLE模型评价2010 - 2025年土壤侵蚀强度,探讨土地利用变化对土壤侵蚀的影响。结果表明:①2010 ~ 2020年,库掖河流域土地利用格局以草地和农田为主;耕地和草地面积减少,建设用地和未利用地面积增加。耕地和草地的扩张主要受海拔、降雨和人口的影响,建设用地的扩张主要受人类活动的影响。②2010年、2015年和2020年土壤侵蚀强度分别为25.91、22.82和27.58 t·(hm2·a)-1,呈现先减弱后反弹的趋势;③2025年自然开发、生态保护和经济增长情景下的土壤侵蚀强度分别为25.62、24.60和27.41 t·(hm2·a)-1。生态保护方案对控制水土流失效果较好。④流域水土流失最严重的地区主要是中南部黄土沟壑区的草地和农田,以及部分工矿集中区周边的退化土地。为有效减少水土流失,建议在减少农田和工矿区的同时增加森林和草地。值得注意的是,重点应放在加强梯田的维护和保护上。
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
环境科学
环境科学 Environmental Science-Environmental Science (all)
CiteScore
4.40
自引率
0.00%
发文量
15329
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