Temporal changes in suspended sediment transport in a gullied loess basin: the lower Chabagou Creek on the Loess Plateau in China
文献类型：期刊论文
| 作者 | Fang, H. Y.1,2; Cai, Q. G.1; Chen, H.1; Li, Q. Y.3 |
| 刊名 | EARTH SURFACE PROCESSES AND LANDFORMS
 |
| 出版日期 | 2008-11-01 |
| 卷号 | 33期号:13页码:1977-1992 |
| 关键词 | Sediment Peak Peak Discharge Hysteresis Loop Hyperconcentrated Flow Chabagou Creek |
| ISSN号 | 0197-9337 |
| 产权排序 | Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc;Chinese Acad Sci, Grad Sch; Chinese Acad Sci, Yantai Inst Coastal Zone Res Sustainable Dev |
| 通讯作者 | Cai, QG, A11 Dalun Rd, Beijing 100101, Peoples R China |
| 文献子类 | Article |
| 英文摘要 | Suspended sediment dynamics are still imperfectly understood, especially in the loess hilly region on the Loess Plateau, with strong temporal variability, where few studies heretofore have been conducted. Using a dataset up to eight years long in the Lower Chabagou Creek, the variability in suspended sediment load at different temporal scales (within-flood variability, monthly-seasonal and annual) is analyzed in this paper. The results show that, on the within-flood scale, most of the sediment peaks lag behind peak discharges, implying that slope zones are the main sediment source area; independent of the occurring sequences of the peaks of sediment and discharge, all the events could present an anti-clock wise hysteresis loop resulting from the abundant material and the influence of hyperconcentrated flows on suspended sediment concentration. At monthly and seasonal scales, there is a 'store-release' process, i.e. sediment is prepared in winter, spring and late autumn, and exported in summer and early autumn. At the annual scale, the high variability in concentration and sediment yield are highly correlated with water yield, resulting from the number and magnitude of floods recorded yearly, and almost all the suspended load is transported during these events. Copyright (c) 2008 John Wiley & Sons, Ltd. |
| 学科主题 | Geography, Physical ; Geosciences, Multidisciplinary |
| URL标识 | 查看原文 |
| WOS关键词 | HYPERCONCENTRATED FLOWS ; DRAINAGE-BASIN ; RIVER BASINS ; FLOOD ; CATCHMENTS ; DYNAMICS ; DEPOSITS ; CHANNEL ; FLUXES ; STREAM |
| WOS研究方向 | Physical Geography ; Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000261083800004 |
| 资助机构 | National Grand Fundamental Research 973 Program of China [2007CB407207]; National Natural Science Foundation of China [30671721] |
| 公开日期 | 2011-07-05 |
| 源URL | [http://ir.yic.ac.cn/handle/133337/3587]  |
| 专题 | 烟台海岸带研究所_滨海湿地实验室 |
| 作者单位 | 1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing, Peoples R China 2.Chinese Acad Sci, Grad Sch, Beijing, Peoples R China 3.Chinese Acad Sci, Yantai Inst Coastal Zone Res Sustainable Dev, Yantai, Peoples R China |
| 推荐引用方式 GB/T 7714 | Fang, H. Y.,Cai, Q. G.,Chen, H.,et al. Temporal changes in suspended sediment transport in a gullied loess basin: the lower Chabagou Creek on the Loess Plateau in China[J]. EARTH SURFACE PROCESSES AND LANDFORMS,2008,33(13):1977-1992. |
| APA | Fang, H. Y.,Cai, Q. G.,Chen, H.,&Li, Q. Y..(2008).Temporal changes in suspended sediment transport in a gullied loess basin: the lower Chabagou Creek on the Loess Plateau in China.EARTH SURFACE PROCESSES AND LANDFORMS,33(13),1977-1992. |
| MLA | Fang, H. Y.,et al."Temporal changes in suspended sediment transport in a gullied loess basin: the lower Chabagou Creek on the Loess Plateau in China".EARTH SURFACE PROCESSES AND LANDFORMS 33.13(2008):1977-1992. |
入库方式： OAI收割
来源：烟台海岸带研究所
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