Variation in the sediment deposition behind check-dams under different soil erosion conditions on the Loess Plateau, China

doi:10.1002/esp.4364

ISWC OpenIR > 水保所科研产出--SCI > 2018--SCI

	Variation in the sediment deposition behind check-dams under different soil erosion conditions on the Loess Plateau, China
	Yanhong Wei 1,2; Zhong He 1,2; Juying Jiao 1,2; Yujin Li 3; Yixian Chen 1,2; Hengkang Zhao 3; Jiao, JY (reprint author), Northwest A&F Univ, Inst Soil & Water Conservat, 26 Xinong Rd, Yangling 712100, Shaanxi, Peoples R China.
文章类型	Article
	2018
发表期刊	EARTH SURFACE PROCESSES AND LANDFORMS
ISSN	0197-9337
通讯作者邮箱	jyjiao@ms.iswc.ac.cn
卷号	43 期号:9 页码:1899-1912
摘要	To maintain a reasonable sediment regulation system in the middle reaches of the Yellow River, it is critical to determine the variation in sediment deposition behind check-dams for different soil erosion conditions. Sediment samples were collected by using a drilling machine in the Fangta watershed of the loess hilly-gully region and the Manhonggou watershed of the weathered sandstone hilly-gully (pisha) region. On the basis of the check-dam capacity curves, the soil bulk densities and the couplet thickness in these two small watersheds, the sediment yields were deduced at the watershed scale. The annual average sediment deposition rate in the Manhonggou watershed (702.0mm/(km(2)a)) from 1976 to 2009 was much higher than that in the Fangta watershed (171.6mm/(km(2)a)) from 1975 to 2013. The soil particle size distributions in these two small watersheds were generally centred on the silt and sand fractions, which were 42.4% and 50.7% in the Fangta watershed and 60.6% and 32.9% in the Manhonggou watershed, respectively. The annual sediment deposition yield exhibited a decreasing trend; the transition years were 1991 in the Fangta watershed and 1996 in the Manhonggou watershed (P < 0.05). In contrast, the annual average sediment deposition yield was much higher in the Manhonggou watershed (14011.1t/(km(2)a)) than in the Fangta watershed (3149.6t/(km(2)a)). In addition, the rainfalls that induced sediment deposition at the check-dams were greater than 30mm in the Fangta watershed and 20mm in the Manhonggou watershed. The rainfall was not the main reason for the difference in the sediment yield between the two small watersheds. The conversion of farmland to forestland or grassland was the main reason for the decrease in the soil erosion in the Fangta watershed, while the weathered sandstone and bare land were the main factors driving the high sediment yield in the Manhonggou watershed. Knowledge of the sediment deposition process of check-dams and the variation in the catchment sediment yield under different soil erosion conditions can serve as a basis for the implementation of improved soil erosion and sediment control strategies, particularly in semi-arid hilly-gully regions. Copyright (c) 2018 John Wiley & Sons, Ltd.
关键词	Dam-controlled Watershed Sedimentation Erosion Environment Sediment Yield Sediment Particle Size The Loess Plateau
学科领域	Physical Geography ; Geology
DOI	10.1002/esp.4364
收录类别	SCI
出版地	111 RIVER ST, HOBOKEN 07030-5774, NJ USA
语种	英语
WOS记录号	WOS:000437831300013
出版者	WILEY
项目资助者	National Key Research and Development Program of China [2016YFC0501604] ; National Key Research and Development Program of China [2016YFC0501604] ; National Science Foundation of China [41472156, 41371280] ; National Science Foundation of China [41472156, 41371280] ; Opening Fund of the State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau [A314021402-1809] ; Opening Fund of the State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau [A314021402-1809]
引用统计
文献类型	期刊论文
条目标识符	sbir.nwafu.edu.cn/handle/361005/8214
专题	水保所科研产出--SCI_2018--SCI
通讯作者	Jiao, JY (reprint author), Northwest A&F Univ, Inst Soil & Water Conservat, 26 Xinong Rd, Yangling 712100, Shaanxi, Peoples R China.
作者单位	1.Chinese Acad Sci, Inst Soil & Water Conservat, State Key Lab Soil Eros & Dryland Farming Loess P, Yangling, Shaanxi, Peoples R China 2.Minist Water Resources, Yangling, Shaanxi, Peoples R China 3.Northwest A&F Univ, Inst Soil & Water Conservat, 26 Xinong Rd, Yangling 712100, Shaanxi, Peoples R China 4.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Desert & Desertificat, Lanzhou, Gansu, Peoples R China
推荐引用方式 GB/T 7714	Yanhong Wei,Zhong He,Juying Jiao,et al. Variation in the sediment deposition behind check-dams under different soil erosion conditions on the Loess Plateau, China[J]. EARTH SURFACE PROCESSES AND LANDFORMS,2018,43(9):1899-1912.
APA	Yanhong Wei.,Zhong He.,Juying Jiao.,Yujin Li.,Yixian Chen.,...&Jiao, JY .(2018).Variation in the sediment deposition behind check-dams under different soil erosion conditions on the Loess Plateau, China.EARTH SURFACE PROCESSES AND LANDFORMS,43(9),1899-1912.
MLA	Yanhong Wei,et al."Variation in the sediment deposition behind check-dams under different soil erosion conditions on the Loess Plateau, China".EARTH SURFACE PROCESSES AND LANDFORMS 43.9(2018):1899-1912.

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