中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Effects of subsequent rainfall events with different intensities on runoff and erosion in a coarse soil

文献类型:期刊论文

作者Quanjiu Wang; Yafei Wang; Wei You; Jun Fan; Mu Jin; Xiubin Wei; Fan, J (reprint author), Northwest A&F Univ, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China.
刊名CATENA
出版日期2018
卷号170页码:100-107
ISSN号0341-8162
关键词Rain Simulator Soil Loss Infiltration The Loess Plateau
DOI10.1016/j.catena.2018.06.008
文献子类Article
英文摘要A deeper understanding of the hydrological response to subsequent rains would be useful in the prediction of runoff production for planning vegetation restoration and assessing flood risks. We used subsequent rains to study the role of rain intensity and antecedent soil moisture content (ASMC) on runoff and erosion for coarse soil of the semiarid Loess Plateau in China. The study used a rain simulator in a field planted with alfalfa (Medicago sativa), which is widely grown for animal feed to develop livestock operations, reduce soil erosion, and improve soil fertility/quality. A slope of 18% was selected because most of the land with slopes < 18% in the region is used for cropland. We tested three rain intensities (20, 40, and 60 mm h(-1), corresponding to low, moderate, and high intensities, respectively) with five successive rains (an initial and four subsequent rains) in triplicate. We quantified the changes of runoff depth (RD), sediment yield (SY), and sediment concentration (SC) over time and then analyzed the relationships between ASMC and runoff in 0-50 cm soil layers for all 45 simulated rains. Runoff commencement time (RCT) was shorter, the runoff coefficient (RC) was larger, and runoff was higher for the moderate and high intensities than the low intensity. Intermittency and the characteristics of the sequential rains also influenced these processes. A general linear model identified significant effects of rain sequence and intensity on RCT, RD, RC, SY, and SC (P < 0.01), but their interaction did not have a significant effect on RCT and SY. An exponential fit between ASMC and RC was best for the 0-10 cm and 10-20 cm layer (R-2 = 0.38, P < 0.000), and R-2 decreased from the 0-20 cm to the 30-40 cm layers. Soil moisture content (SMC) was an important factor controlling runoff, and the sequential rains led to high runoff and sediment transport, because runoff from storms on highly permeable soils is controlled by the saturation of the topsoil horizon and is more dependent on initial conditions.
学科主题Geology ; Agriculture ; Water Resources
出版地PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000441681500009
资助机构National Natural Science Foundation of China [41571130082, 41571224] ; National Natural Science Foundation of China [41571130082, 41571224] ; Western Youth Scholar of the Chinese Academy of Sciences [XAB2015A03] ; Western Youth Scholar of the Chinese Academy of Sciences [XAB2015A03] ; National Natural Science Foundation of China [41571130082, 41571224] ; National Natural Science Foundation of China [41571130082, 41571224] ; Western Youth Scholar of the Chinese Academy of Sciences [XAB2015A03] ; Western Youth Scholar of the Chinese Academy of Sciences [XAB2015A03]
源URL[http://ir.iswc.ac.cn/handle/361005/8174]  
专题水保所科研产出--SCI_2018--SCI
通讯作者Fan, J (reprint author), Northwest A&F Univ, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China.
作者单位Northwest A&F Univ, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling 712100, Shaanxi, Peoples R China
推荐引用方式
GB/T 7714
Quanjiu Wang,Yafei Wang,Wei You,et al. Effects of subsequent rainfall events with different intensities on runoff and erosion in a coarse soil[J]. CATENA,2018,170:100-107.
APA Quanjiu Wang.,Yafei Wang.,Wei You.,Jun Fan.,Mu Jin.,...&Fan, J .(2018).Effects of subsequent rainfall events with different intensities on runoff and erosion in a coarse soil.CATENA,170,100-107.
MLA Quanjiu Wang,et al."Effects of subsequent rainfall events with different intensities on runoff and erosion in a coarse soil".CATENA 170(2018):100-107.

入库方式: OAI收割

来源:水土保持研究所

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