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 |
卷 | 20 |
期 | 2 |
页 | 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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