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本文是在吉林西部白城地区进行地下水资源评价时,为了取得更多的点参数,根据该区水文地质条件和地下水的动态特征,经初步研究而提出的。 到目前为止,研究地下水流向集水构筑物的运动规律的一些主要理论公式都是以地下水流向井的水平运动为主要研究内容。并借助于抽水所产生的水位下降建立理论公式,确定水文地质参数。 本文试图讨论在由两个含水层(潜水含水层和下伏有不透水层的第一个半承压含水层)及其间的
In order to get more point parameters in the evaluation of groundwater resources in Baicheng area of western Jilin, this paper presents a preliminary study based on the hydrogeological conditions of the area and the dynamic characteristics of groundwater. So far, some major theoretical formulas for studying the movement of groundwater flowing to water-collecting structures have been based on the horizontal movement of groundwater flowing to the well as the main research content. And by virtue of the water level produced by pumping down to establish a theoretical formula to determine the hydrogeological parameters. This article attempts to discuss the role of the aquifer in two aquifers (the submerged aquifer and the underlying semi-confined aquifer under water) along with