单注井人工补给含水层对水力导电性的影响

Yanhui Dong, Pinge Zhao, Weibo Zhou
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引用次数: 2

摘要

人工补给含水层是提高地下水位、预防和补救过度开采造成的环境和地质问题的重要措施。在回灌过程中,由于物理和化学堵塞,回灌性能逐渐下降,水力导率降低。为了揭示回灌性能的变化,本文以单注井回灌为例,研究了水力导率的变化规律。在西安市南郊100 ~ 300m的承压含水层进行了承压回灌试验。结果表明:人工补给含水层的水力导电性随时间幂函数衰减,且小于抽水的水力导电性;单位时间补水量越小,水导率衰减越慢。单位时间回灌水量小的效果好于单位时间回灌水量大的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effect of artificial aquifer recharge on hydraulic conductivity using single injection well
Artificial aquifer recharge is an important measure to raise the groundwater level, prevent and remedy the environmental and geological problems caused by the over extraction. Because of the physical and chemical clogging, the performance of recharge decreased gradually and the hydraulic conductivity reduced during the recharging process. In order to reveal the changing of recharging performance, the paper took the single injection well recharge as an example to research the changing law of hydraulic conductivity. The recharge test with pressure was done in confined aquifer depth of 100 to 300m at the south suburbs of Xi'an. The results show that hydraulic conductivity of artificial aquifer recharge attenuated with time power function and was smaller than the hydraulic conductivity of pumping. When the quantity of water recharge per unit time was smaller, the attenuation of hydraulic conductivity was slower. The performance of small quantity of water recharge per unit time was better than the large.
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