Divergent shift of normal alpine meadow exacerbated soil loss of hillslope alpine meadows based on field experiments

被引:2
|
作者
Ma, Yulei [1 ,2 ]
Liu, Yifan [1 ,2 ]
Ban, Yunyun [3 ]
Zhao, Jingxue [4 ,5 ]
Shi, Zhihua [2 ,6 ,7 ]
Wu, Gaolin [1 ,2 ,7 ]
机构
[1] Northwest A&F Univ, Inst Soil & Water Conservat, Coll Soil & Water Conservat Sci & Engn, State Key Lab Soil Eros & Dryland Farming Loess Pl, Yangling 712100, Shaanxi, Peoples R China
[2] Chinese Acad Sci & Minist Water Resource, Inst Soil & Water Conservat, Yangling 712100, Shaanxi, Peoples R China
[3] Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
[4] Lanzhou Univ, State Key Lab Herbage Improvement & Grassland Agro, Lanzhou 730000, Peoples R China
[5] Lanzhou Univ, Coll Ecol, Lanzhou 730000, Peoples R China
[6] Huazhong Agr Univ, Coll Resources & Environm, Wuhan 430070, Peoples R China
[7] CAS Ctr Excellence Quaternary Sci & Global Change, Xian 710061, Peoples R China
基金
中国国家自然科学基金;
关键词
Alpine meadow; Divergent shifts; Runoff; Soil erodibility; Soil loss; HYDRAULIC-PROPERTIES; WATER EROSION; RUNOFF; VEGETATION; IMPACT; CARBON; FLOW; ESTABLISHMENT; ERODIBILITY; GRASSLAND;
D O I
10.1016/j.iswcr.2023.11.007
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Global climate change and overgrazing are driving shifts in the plant composition of grassland communities, which may profoundly affect the function of grassland ecosystems in regulating runoff and soil erosion. Here, we examined the shift effects of normal hillslope alpine meadow to shrub and severely degraded meadow states on runoff and sediment generation under natural rainfall conditions, and determined the contributions of plant and soil properties changes to soil erodibility, runoff and sediment generation by in situ rainfall experiment and monitoring on the hillslope of Qinghai-Tibetan Plateau. The results showed that normal meadow shift into severely degraded meadow state, mean weight diameter, soil saturated hydraulic conductivity, soil cohesion and soil erodibility K-factor at the topsoil decreased by 70.3%, 73.1%, 80.3% and-13.1%, respectively, and when normal meadows shift into shrub meadow state, they reduced by 49.1%,-1.3%, 49.4%, and-8.3%, respectively. Runoff and soil loss signi ficantly changed by- 40.0% and 177.8% when normal meadow shifted into a severely degraded meadow state, while runoff and soil loss signi ficantly changed by + 65.0% and +77.8% when normal meadow shifted into a shrub meadow state. Our findings highlight that the two divergent shifts both increased soil loss compared to the normal hillslope alpine meadows. Overall, our results indicate that the divergent shifts of normal alpine meadows exacerbated soil erodibility and soil loss of hillslope alpine meadows. These results obtained here offer a novel perspective on the regulation of runoff and soil erosion in the alpine meadow ecosystem. (c) 2023 International Research and Training Center on Erosion and Sedimentation, China Water and Power Press, and China Institute of Water Resources and Hydropower Research. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd. This is an open access article under the CC BYNC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
引用
收藏
页码:565 / 577
页数:13
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