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Research on solute transport characteristics in the process of artificial recharge to control land subsidence in deep confined aquifer

机译：深入纳入含水层中土地沉降过程中溶质运输特性研究

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Since 1960s, Artificial Recharge has been adopted to control the geological disaster of land subsidence in Shanghai. The water source to recharge to the confined aquifer meet the Standard for Drinking Water Quality which comes from the Huangpu River or Yangtze River. Thinking the difference between the primary environment of deep confined aquifer and the surface water, the recharge will exert an impact on the quality of groundwater in the deep confined aquifer, as well as to obtain satisfactory effects of land subsidence prevention.This paper focused on the change rules of the elements such as Cl based on long term tracking and monitoring data from one artificial recharge testing field. And research the solute transport characteristics in deep confined aquifer during artificial recharge. On the bases of these analysis, this paper presented the degree and scope of influence to deep confined aquifer in the process of artificial recharge.
机译：自20世纪60年代以来，已采取人工补给以控制上海地地沉降地质灾害。 水源为受限含水层充电，符合来自黄浦江或长江的饮用水质量标准。 思考深层狭窄含水层和地表水的主要环境之间的差异，充值将对深入狭窄含水层的地下水质量产生影响，从而获得土地沉降预防效果。本文重点关注 根据一个人工充电测试字段的长期跟踪和监视数据，更改CL等元素规则。 并在人工补给过程中研究深层狭窄含水层的溶质运输特性。 在这些分析的基础上，本文介绍了人工补给过程中对深层狭窄含水层的影响程度和范围。

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