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. Since 1960s, Artificial Recharge has been adopted to control the geologicaldisaster of land subsidence in Shanghai. The water source to recharge to theconfined aquifer meet the Standard for Drinking Water Quality which comesfrom the Huangpu River or Yangtze River. Thinking the difference between theprimary environment of deep confined aquifer and the surface water, therecharge will exert an impact on the quality of groundwater in the deepconfined aquifer, as well as to obtain satisfactory effects of landsubsidence prevention.This paper focused on the change rules of the elementssuch as Cl based on long term tracking and monitoring data from oneartificial recharge testing field. And research the solute transportcharacteristics in deep confined aquifer during artificial recharge. On thebases of these analysis, this paper presented the degree and scope ofinfluence to deep confined aquifer in the process of artificial recharge.

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