中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Estimation of groundwater residence time and recession rate in watershed of the Loess Plateau

文献类型:SCI/SSCI论文

作者Zhu R. R. ; Zheng H. X. ; Liu C. M.
发表日期2010
关键词baseflow recession constant residence time Wudinghe River hydrograph recession base-flow new-york
英文摘要Groundwater residence time is an important indicator of hydrological cycle and essential for water resources development and utilization In this paper, groundwater residence time in non-flood season, flood season and water year has been determined from daily streamflow hydrograph of ten hydrological stations in Wudinghe River Basin located in the middle reaches of the Yellow River Basin. Results have showed that: baseflow recession constant in Wudinghe River Basin ranges from 0 72 to 0 94 with a larger recession rate in flood season than that in non-flood season. Spatially, the recession rate of baseflow in loess area is the biggest, but is the smallest in the sandy area. The half-residence time of groundwater varies from 1.8 to 45.5 days while overall residence time of groundwater is between 34 and 342 days in different sub-basins of the Wudinghe River Basin. The annual average overall residence time of groundwater decreases from 117 days in the upper reaches to 73 days in the lower reaches.
出处Journal of Geographical Sciences
20
2
273-282
收录类别SCI
语种英语
ISSN号1009-637X
源URL[http://ir.igsnrr.ac.cn/handle/311030/22204]  
专题地理科学与资源研究所_历年回溯文献
推荐引用方式
GB/T 7714
Zhu R. R.,Zheng H. X.,Liu C. M.. Estimation of groundwater residence time and recession rate in watershed of the Loess Plateau. 2010.

入库方式: OAI收割

来源:地理科学与资源研究所

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