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- W2392145440 abstract "Groundwater in the Quaternary aquifers is one of the major sources of water supply for domestic uses in the Minle Piedmont Plain,northwestern China. Groundwater flow and renewability are controlled by the buried faults. The present work discusses the groundwater recharge,renewal and effects of the buried faults on groundwater renewability by using the environmental isotopes. The results indicate that (1) the groundwater in the Minle Piedmont Plain is recharged from infiltration of river water and local precipitation,and about 89% of groundwater is recharged from river while about 11% of groundwater recharge is received from local precipitation; (2) the groundwater renewability decreases from the upstream to the downstream,and the groundwater turnover time ranges from 20~30 years at the upstream to more than 50 years at the downstream; (3) the buried faults in the Minle Piedmont Plain slow down the velocity of groundwater flow." @default.
- W2392145440 created "2016-06-24" @default.
- W2392145440 creator A5046017431 @default.
- W2392145440 date "2010-01-01" @default.
- W2392145440 modified "2023-09-26" @default.
- W2392145440 title "Groundwater recharge and renewal in the Minle Piedmont Plain of the Heihe River Basin" @default.
- W2392145440 hasPublicationYear "2010" @default.
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