Dynamics of soil loss and sediment export as affected by land use/cover change in Koshi River Basin, Nepal
Yigez, Belayneh6,7; Xiong, Donghong5,7; Zhang, Baojun7; Belete, Marye4; Chalise, Devraj3; Chidi, Chhabi Lal2; Guadie, Awoke1; Wu, Yanhong5,7; Rai, Dil Kumar6,7
刊名JOURNAL OF GEOGRAPHICAL SCIENCES
2023-06-01
卷号33期号:6页码:1287-1312
关键词soil loss sediment export land use cover InVEST model Koshi River basin Google Earth Engine
ISSN号1009-637X
DOI10.1007/s11442-023-2130-x
英文摘要

How the dynamics in soil loss (SL) and sedimentation are affected by land use/cover change (LULCC) has long been one of the most important issues in watershed management worldwide, especially in fragile mountainous river basins. This study aimed to investigate the impact of LULCC on SL and sediment export (SE) in eastern regions of the Koshi River basin (KRB), Nepal, from 1990 to 2021. The Random Forest classifier in the Google Earth Engine platform was employed for land use/land cover (LULC) classification, and the Integrated Valuation Ecosystem Services and Trade-offs (InVEST) Sediment Delivery Ratio model was used for SL and SE modeling. The results showed that there was a pronounced increase in forest land (4.12%), grassland (2.35%), and shrubland (3.68%) at the expense of agricultural land (10.32%) in KRB over the last three decades. Thus, the mean SL and SE rates decreased by 48% and 60%, respectively, from 1990 to 2021. The conversion of farmland to vegetated lands has greatly contributed to the decrease in SL and SE rates. Furthermore, the rates of SL and SE showed considerable spatiotemporal variations under different LULC types, topographic factors (slope aspect and gradient), and sub-watersheds. The higher rates of SL and SE in the study area were observed mostly in slope gradient classes between 8 & DEG; and 35 & DEG; (accounting for 83%-91%) and sunny and semi-sunny slope aspects (SE, S, E, and SW) (accounting for 57%-65%). Although the general mean rate of SL presented a decreasing trend in the study area, the current mean SL rate (23.33 t ha(-1) yr(-1)) in 2021 is still far beyond the tolerable SL rate of both the global (10 Mg ha(-1) yr(-1)) and the Himalayan region (15 t ha(-1) yr(-1)). Therefore, landscape restoration measures should be integrated with other watershed management strategies and upscaled to hotspot areas to regulate basin sediment flux and secure ecosystem service sustainability.

资助项目Chinese Academy of Sciences (CAS) Overseas Institution Platform Project[131C11KYSB20200033]
WOS关键词LOESS PLATEAU ; MIDDLE MOUNTAINS ; CLIMATE-CHANGE ; COVER CHANGES ; EROSION ; ABANDONMENT ; CATCHMENT ; LANDSCAPE ; CHINA ; GIS
WOS研究方向Physical Geography
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:001013197500008
资助机构Chinese Academy of Sciences (CAS) Overseas Institution Platform Project
内容类型期刊论文
源URL[http://ir.imde.ac.cn/handle/131551/57555]  
专题成都山地灾害与环境研究所_山地灾害与地表过程重点实验室
通讯作者Xiong, Donghong
作者单位1.Arba Minch Univ, Coll Nat Sci, Dept Biol, Arba Minch 21, Ethiopia
2.Tribhuvan Univ, Cent Dept Geog, Kathmandu, Nepal
3.Mackay Area Prod Serv, 26135 Peak Downs Highway, Te Kowai, Qld 4740, Australia
4.Debre Tabor Univ, Dept Nat Resource Management, Debre Tabor 272, Ethiopia
5.CAS TU, Kathmandu Ctr Res & Educ, Branch Sustainable Mt Dev, Kathmandu 44613, Nepal
6.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
7.Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China
推荐引用方式
GB/T 7714
Yigez, Belayneh,Xiong, Donghong,Zhang, Baojun,et al. Dynamics of soil loss and sediment export as affected by land use/cover change in Koshi River Basin, Nepal[J]. JOURNAL OF GEOGRAPHICAL SCIENCES,2023,33(6):1287-1312.
APA Yigez, Belayneh.,Xiong, Donghong.,Zhang, Baojun.,Belete, Marye.,Chalise, Devraj.,...&Rai, Dil Kumar.(2023).Dynamics of soil loss and sediment export as affected by land use/cover change in Koshi River Basin, Nepal.JOURNAL OF GEOGRAPHICAL SCIENCES,33(6),1287-1312.
MLA Yigez, Belayneh,et al."Dynamics of soil loss and sediment export as affected by land use/cover change in Koshi River Basin, Nepal".JOURNAL OF GEOGRAPHICAL SCIENCES 33.6(2023):1287-1312.
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