Revisiting the modified Hvorslev formula to account for the dynamic process of streambed clogging: Field validation
Vasilevskiy, Peter Yu.2; Wang, Ping1; Pozdniakov, Sergey P.2; Davis, Paul3
刊名JOURNAL OF HYDROLOGY
2019
卷号568页码:862-866
关键词Surface-groundwater interaction Falling-head permeameter test Streambed hydraulic conductivity Streambed clogging Heihe River
ISSN号0022-1694
DOI10.1016/j.jhydrol.2018.11.034
通讯作者Wang, Ping(wangping@igsnrr.ac.cn)
英文摘要Estimating streambed hydraulic conductivity is particularly important in arid and semi-arid regions, where surface water infiltration from ephemeral dryland streams helps maintain riparian ecosystems. In situ permeameter tests are widely used to estimate the hydraulic conductivity of streambed sediments. Previous studies have demonstrated that one of the major factors controlling spatiotemporal variations in streambed hydraulic conductivity in such areas is streambed clogging by suspended sediments. Recently, a modified Hvorslev (1951) formula was theoretically proposed to account for the effect of streambed clogging on streambed hydraulic properties due to suspended particle sedimentation during falling-head tests. To validate the modified formula, fieldwork was conducted at five sites in the lower Heihe River, a typical intermittent river of north-western China, in September 2017. A simple PVC pipe with an inner diameter of 4 cm was used as a permeameter for the field tests. Both muddy river water and clean water were used to fill the permeameter to conduct comparative tests. To differentiate the interpretation of the field testing data obtained with clean water, the data obtained with muddy river water were analysed with an equation considering an iteratively increasing total hydraulic resistance of riverbed sediments due to the effects of riverbed clogging. The estimated vertical hydraulic conductivity for the top 0.3 m of riverbed sediments varied from 1 to 41 m/day. The proposed model was shown to accurately estimate the hydraulic conductivity of riverbed sediments using both clean and muddy water during slug tests.
资助项目National Natural Science Foundation of China[41671023] ; National Natural Science Foundation of China[41301025] ; National Natural Science Foundation of China-Russian Foundation for Basic Research (NSFC-RFBR) Programme[41811530084] ; National Natural Science Foundation of China-Russian Foundation for Basic Research (NSFC-RFBR) Programme[18-55-53025 GammaPhiEH_a] ; Chinese Academy of Sciences and Russia, Ukraine and Belarus
WOS关键词RIVERBED HYDRAULIC CONDUCTIVITY ; SPATIAL VARIABILITY ; GROUNDWATER ; HETEROGENEITY ; EXCHANGE ; WATER ; BANK
WOS研究方向Engineering ; Geology ; Water Resources
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000455694400068
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China-Russian Foundation for Basic Research (NSFC-RFBR) Programme ; Chinese Academy of Sciences and Russia, Ukraine and Belarus
内容类型期刊论文
源URL[http://ir.igsnrr.ac.cn/handle/311030/50479]  
专题中国科学院地理科学与资源研究所
通讯作者Wang, Ping
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, 11A Datun Rd, Beijing 100101, Peoples R China
2.Lomonosov Moscow State Univ, Dept Hydrogeol, GSP-1, Moscow 119899, Russia
3.EnviroLogic Inc, 736 Main St,Suite 5, Durango, CO 81301 USA
推荐引用方式
GB/T 7714
Vasilevskiy, Peter Yu.,Wang, Ping,Pozdniakov, Sergey P.,et al. Revisiting the modified Hvorslev formula to account for the dynamic process of streambed clogging: Field validation[J]. JOURNAL OF HYDROLOGY,2019,568:862-866.
APA Vasilevskiy, Peter Yu.,Wang, Ping,Pozdniakov, Sergey P.,&Davis, Paul.(2019).Revisiting the modified Hvorslev formula to account for the dynamic process of streambed clogging: Field validation.JOURNAL OF HYDROLOGY,568,862-866.
MLA Vasilevskiy, Peter Yu.,et al."Revisiting the modified Hvorslev formula to account for the dynamic process of streambed clogging: Field validation".JOURNAL OF HYDROLOGY 568(2019):862-866.
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