## Abstract We used hydrochemistry and environmental isotope data (Ξ΄^18^O, Ξ΄D, tritium, and ^14^C) to investigate the characteristics of river water, groundwater, and groundwater recharge in China's Heihe River basin. The river water and groundwater could be characterized as Ca^2+^ο£ΏMg^2+^ο£ΏHCO~3~^β^
Simulated groundwater interaction with rivers and springs in the Heihe river basin
β Scribed by Li-Tang Hu; Chong-Xi Chen; Jiu Jimmy Jiao; Zhong-Jing Wang
- Book ID
- 102861166
- Publisher
- John Wiley and Sons
- Year
- 2007
- Tongue
- English
- Weight
- 965 KB
- Volume
- 21
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.6497
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β¦ Synopsis
Abstract
Surface water and groundwater in the Heihe river basin of China are interconnected and the pattern of water resources exploitation has a direct effect on the interaction of groundwater and surface water, especially on a downstream oasis. A threeβdimensional groundwater flow simulation model with eight model layers was established to simulate the regional groundwater flow in the multilayered aquifer system and the interaction among the rivers, springs, and groundwater. The model was calibrated not only with historical water levels but also with the investigated baseflow and spring flux. The simulation results of the numerical model match reasonably well with the observed groundwater levels, baseflow to rivers, and spring flux. The numerical simulation also demonstrates that the hydraulic connection between the river and the aquifers has transferred from the coupling to decoupling at some reaches. It is suggested that there is a vital need to reduce groundwater withdrawal and to rationalize the use of both groundwater and surface water in order to maintain sustainable development in the study area. Copyright Β© 2007 John Wiley & Sons, Ltd.
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