同位素示踪方法测定柴达木盆地西台盐湖地下卤水参数研究

Determining Hydrogeological Parameters of Subsurface Brine in the Xitai Saltlake of the Chaidamu Basin with Isotope Tracer Method

为了测定柴达木盆地西台吉乃尔盐湖地下水流速、流向,从而来计算该区的渗透系数,正确确定其渗透系数,无论对科学研究还是对生产开采,均有着重要的理论和现实意义。介绍同位素示踪方法测定该区地下水卤水流速,流向实验原理及结果,并对实验数据进行分析整理。

Correct estimate of hydrogeologic parameters has theoretical and practical significance for both scientific research and groundwater exploitation. This paper first introduces the principle of using isotope tracer method studying brine groundwater flow. The isotope dilution method was used to determine aquifer parameters, including flow velocity, direction and permeability of the groundwater in Xitai Salt Lake, Chaidam Basin. The experimental data were analyzed and reviewed accordingly.