中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Quantification of upslope and lateral inflow impacts on runoff discharge and soil loss in ephemeral gully systems under laboratory conditions

文献类型:期刊论文

作者Xu, Ximeng1,2; Zheng, Fenli2,3,4; Wilson, Glenn V.5; Zhang, Xunchang J.6; Qin, Chao7; He, Xu2
刊名JOURNAL OF HYDROLOGY
出版日期2019-12-01
卷号579页码:13
ISSN号0022-1694
关键词Ephemeral gully tributaries Flow hydrodynamics Concentrated flow Rill erosion Flow path Soil texture
DOI10.1016/j.jhydrol.2019.124174
通讯作者Zheng, Fenli(flzh@ms.iswc.ac.cn)
英文摘要Overland flow through an ephemeral gully (EG) system integrates flow from upslope areas and lateral side slopes. Lateral overland inflow creates tributaries to the main EG channel for runoff and sediment discharge which exacerbates the EG erosion and local soil degradation. However, research concerning tributary formation by overland flow, especially contributions of overland upslope and lateral inflows to EG erosion, are still lacking. Thus, simulated rainfall and inflow experiments under two erosive rainfall intensities (50 and 100 mm h(-1)) and two typical slope gradients (15 degrees and 20 degrees) were conducted under representative lateral and upslope overland inflow conditions using an 8-m long, 2-m wide and 0.6-m deep soil pan. The results showed that upslope and lateral inflow both contributed to the runoff connectivity of the EG channel and lateral rills in the EG system. For these simulated conditions, upslope inflow contributions to total runoff and soil loss were 62-78% and 65-81%, respectively, while lateral inflow only contributed around 10%. The contribution differences could be attributed to flow hydrodynamic characteristics in that shear stress and stream power in the EG channel were 4.9-8.6 times greater than those on the lateral slopes. Lateral inflow was important to lateral rill formation, which contributed to imbricated landform and lateral gradient formation process, and consequently promoted runoff and sediment connectivity of the EG system. Soil erosion induced by concentrated flow in channels and sheet flow in interill areas coarsened soil textures, soil particles lager than 0.02 min increased 12.6% on average, which may contribute to reduction of local soil productivity. This work demonstrates the critical need of preventing both upslope and lateral drainage into EG channels.
WOS关键词EROSION PROCESSES ; LOESS PLATEAU ; SIZE-SELECTIVITY ; ERODED SEDIMENT ; DETACHMENT ; FLOW ; HIGHLANDS ; REGION ; DEGRADATION ; HILLSLOPES
资助项目National Key R&D Program of China[2016YFE0202900] ; National Natural Science Foundation of China[41571263] ; External Cooperation Program of Chinese Academy of Sciences[161461KYSB20170013]
WOS研究方向Engineering ; Geology ; Water Resources
语种英语
出版者ELSEVIER
WOS记录号WOS:000500371200071
资助机构National Key R&D Program of China ; National Natural Science Foundation of China ; External Cooperation Program of Chinese Academy of Sciences
源URL[http://ir.igsnrr.ac.cn/handle/311030/130390]  
专题中国科学院地理科学与资源研究所
通讯作者Zheng, Fenli
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China
2.Northwest A&F Univ, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China
3.Chinese Acad Sci, Inst Soil & Water Conservat, Yangling 712100, Shaanxi, Peoples R China
4.MWR, Yangling 712100, Shaanxi, Peoples R China
5.USDA ARS, Natl Sedimentat Lab, Oxford, MS 38655 USA
6.USDA ARS, Grazinglands Res Lab, El Reno, OK 73036 USA
7.Tsinghua Univ, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
推荐引用方式
GB/T 7714
Xu, Ximeng,Zheng, Fenli,Wilson, Glenn V.,et al. Quantification of upslope and lateral inflow impacts on runoff discharge and soil loss in ephemeral gully systems under laboratory conditions[J]. JOURNAL OF HYDROLOGY,2019,579:13.
APA Xu, Ximeng,Zheng, Fenli,Wilson, Glenn V.,Zhang, Xunchang J.,Qin, Chao,&He, Xu.(2019).Quantification of upslope and lateral inflow impacts on runoff discharge and soil loss in ephemeral gully systems under laboratory conditions.JOURNAL OF HYDROLOGY,579,13.
MLA Xu, Ximeng,et al."Quantification of upslope and lateral inflow impacts on runoff discharge and soil loss in ephemeral gully systems under laboratory conditions".JOURNAL OF HYDROLOGY 579(2019):13.

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来源:地理科学与资源研究所

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