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摘要: 常温下同一地区的地面水和地下水存在着一定的温度差异，这两种水体之间的渗透补给会使这种温差产生变化。本文提出的测温法就是基于这一变化特点，通过对山区河流水温的测量，推算出地下水向山区河流的排泄量，从而达到寻找地下水源，定量地评估地下水量的目的。Abstract: There is certain temperature difference between the surface water and groundwater in the same area in normal temperature.Percolation and supply between thes two kinds of water can make thes difference change.This paper proposed the surveying temperature in mountain area to deduce the drain volume from groundwater to river,and to search groundwater resoures and assess in quantity the groundwater.
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