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在泉水水文地质勘察工作中,计算泉水流量的衰减方程具有重要的意义。利用它的计算结果,不仅可以判断地下水流态性质、水动力场特征并且可以进一步计算泉域范围内含水层区域性的贮水系数、渗透系数等重要的水文地质参数。在我国南方亚热带和热带岩溶地区,地下水以管道流为主,当年雨季补给的地下水,当年旱季基本可
In spring hydrogeological exploration work, the calculation of spring flow attenuation equation is of great significance. Using its calculation results, not only can the nature of groundwater flow state and hydrodynamic field be judged, but also important hydrogeological parameters such as water storage coefficient and permeability coefficient can be further calculated. In southern China’s subtropical and tropical karst areas, the groundwater is dominated by plumbing, then recharge the groundwater during the rainy season, then the basic dry season