中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
A study of physico-geographical factors for formation of hyperconcentrated flows in the Loess Plateau of China

文献类型:期刊论文

作者Xu, JX
刊名GEOMORPHOLOGY
出版日期1998-08-01
卷号24期号:2-3页码:245-255
关键词Hyperconcentrated Flows Physico-geographical Factors Extreme Concentration Of Suspended Sediment Alternating Wind And Water Processes Loess Plateau Of China
文献子类Article
英文摘要Semi-arid climate, poor vegetation cover and highly erodible loess can be regarded as the main natural factors responsible for the formation of hyperconcentrated flows on the Loess Plateau, China. The degree to which the hyperconcentrated flows develop, especially their extreme suspended concentration, shows a significant areal differentiation. This is closely related to the grainsize composition of suspended sediment. An optimal grainsize composition of suspended sediment has been identified, which leads to the highest value of extreme concentration among different river basins. This optimal composition is related to the combination of three surface material types, i.e., loess, wind-blown sand and weathered bedrock, and it occurs as a result of seasonally alternating wind and water processes operating in this area. (C) 1998 Elsevier Science B.V. All rights reserved.
语种英语
WOS记录号WOS:000075010100007
出版者ELSEVIER SCIENCE BV
源URL[http://ir.igsnrr.ac.cn/handle/311030/68189]  
专题中国科学院地理科学与资源研究所
通讯作者Xu, JX
作者单位Chinese Acad Sci, Inst Geog, Beijing 100101, Peoples R China
推荐引用方式
GB/T 7714
Xu, JX. A study of physico-geographical factors for formation of hyperconcentrated flows in the Loess Plateau of China[J]. GEOMORPHOLOGY,1998,24(2-3):245-255.
APA Xu, JX.(1998).A study of physico-geographical factors for formation of hyperconcentrated flows in the Loess Plateau of China.GEOMORPHOLOGY,24(2-3),245-255.
MLA Xu, JX."A study of physico-geographical factors for formation of hyperconcentrated flows in the Loess Plateau of China".GEOMORPHOLOGY 24.2-3(1998):245-255.

入库方式: OAI收割

来源:地理科学与资源研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。