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Experimental Study on Dispersion of Unconfined Aquifer in a Site of Jilin City

机译:吉林市某地无限制含水层扩散的试验研究

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摘要

Dispersion parameter is an important parameter for the establishment of groundwater solute transport model.The dispersion test uses sodium chloride as a tracer,which was conducted in a site in Jilin City.The standard curve comparison method was used to solve the dispersion parameters of the aquifer under the natural flow field.The test results show that under the natural flow field,the longitudinal dispersion of unconfined aquifer in Jilin City is 0.400m,and the transverse dispersion is 1.933×10-5~6.557×10-3m;while the longitudinal dispersion coefficient is 0.246m2/d,the transverse dispersion coefficient is 1.191×10-5~4.039×10-3m2/d.The above results can provide an important parameter basis for the establishment of groundwater solute transport model,the accurate prediction of temporal and spatial variation of pollutant concentration in groundwater and the formulation of groundwater pollution prevention and control scheme.
机译:分散参数是建立地下水溶质运输模型的重要参数。分散试验使用氯化钠作为示踪剂,其在吉林市的部位进行。标准曲线比较方法用于解决含水层的分散参数在自然流动场下。测试结果表明,在自然流场下,吉林市非整合含水层的纵向分散为0.4亿,横向分散体为1.933×10-5〜6.557×10-3m;而纵向分散系数为0.246m2 / d,横向分散系数为1.191×10-5〜4.039×10-3m2 / d。上述结果可以为建立地下水溶质运输模型提供重要参数基础,准确预测时间地下水污染物浓度的空间变化及地下水污染防治方案的配制。

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