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Chinese Academy of Sciences Institutional Repositories Grid
Influence of slope, flow rate, and thawed depth on soil detachment rate in partially thawed black soils

文献类型:期刊论文

作者Chen, Chao1,2; Lei, Tingwu1,2; Ban, Yunyun1,3
刊名JOURNAL OF HYDROLOGY
出版日期2021-12-01
卷号603页码:11
关键词Detachment rate Partially thawed soil Thawed soil depth Slope gradient Flow rate
ISSN号0022-1694
DOI10.1016/j.jhydrol.2021.127009
通讯作者Lei, Tingwu()
英文摘要The detachment rate of partially thawed frozen soil supplies data sets to compute the soil erodibility and critical shear strength in rill erosion model. This research aims to investigate the effect of slope gradient, flow rate, and thawed soil depth on detachment rate under partially thawed condition. The detachment rates of partially thawed soil rill were estimated under three thawed soil depths (1, 2, 5 cm), four slope gradients (5 degrees, 10 degrees, 15 degrees, 20 degrees), and three flow rates (1, 2, 4 L/min). They were then computed with the sediment concentrations measured along different slope lengths of 0.5, 1, 2, 3, 4, 5, 6, 7, 8 m. Results show that the detachment rates on a partially thawed soil slope as a function of rill length are piecewise functions, which initially maintain a constant value before decreasing exponentially with rill length. In the constant detachment rate section, the constant detachment rate increased with thawed soil depth. After the constant detachment rate section, it increased with slope gradient and flow rate but decreased with the increase in thawed soil depth. The detachment rate decreased fast with the increase in slope gradient and flow rate. The computed detachment rates fitted by stepwise functions produced high coefficient of determination, thereby indicating a good correlation of detachment rate with rill length. The parameters, critical rill length, constant detachment rate, potential detachment capacity, and reduction coefficient of detachment rate in the piecewise function were regressed with stepwise regression method. They determined the effects of those four parameters on detachment rate. The influence of flow rate on critical rill length and thawed soil depth on reduction coefficient of detachment rate was limited. The combined impacts of slope gradient and flow rate were positively related to those four parameters. This study quantified the effect of slope, flow rate, and thawed soil depth on detachment rate and help to quantify the soil detachment rate in cold region.
WOS关键词SEDIMENT TRANSPORT ; CONCENTRATED FLOW ; WATER EROSION ; RILL EROSION ; FREEZE-THAW ; FROZEN ; VELOCITY ; RUNOFF ; ERODIBILITY ; MODEL
资助项目National Natural Science Foundation of China[41230746] ; National Natural Science Foundation of China[51621061]
WOS研究方向Engineering ; Geology ; Water Resources
语种英语
WOS记录号WOS:000715326800004
出版者ELSEVIER
资助机构National Natural Science Foundation of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/167657]  
专题中国科学院地理科学与资源研究所
通讯作者Lei, Tingwu
作者单位1.China Agr Univ, Coll Water Resources & Civil Engn, Beijing 100083, Peoples R China
2.Chinese Acad Sci & Minist Water Resources, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China
3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
Chen, Chao,Lei, Tingwu,Ban, Yunyun. Influence of slope, flow rate, and thawed depth on soil detachment rate in partially thawed black soils[J]. JOURNAL OF HYDROLOGY,2021,603:11.
APA Chen, Chao,Lei, Tingwu,&Ban, Yunyun.(2021).Influence of slope, flow rate, and thawed depth on soil detachment rate in partially thawed black soils.JOURNAL OF HYDROLOGY,603,11.
MLA Chen, Chao,et al."Influence of slope, flow rate, and thawed depth on soil detachment rate in partially thawed black soils".JOURNAL OF HYDROLOGY 603(2021):11.

入库方式: OAI收割

来源:地理科学与资源研究所

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