论文部分内容阅读
黔中高原分水岭地区是我国典型的亚热带岩溶区，岩溶十分发育，地下径流成分的赋存、输移、补给和排泄等规律因岩层结构复杂而呈现独特性。对该地区的地下水资源评估通常多以水文地质法为主，水文学方法的应用尚属罕见。本文应用流域水文模型方法对该地区代表性流域的地下水资源规律和特性作了分析、评估，并与水文地质方法比较，成果基本一致。
The watersheds in the Central Guizhou Plateau are typical subtropical karst areas in China. Karst develops well. The occurrence, transport, recharge and discharge of underground runoff components are unique due to the complicated rock formation. The assessment of groundwater resources in the area is usually dominated by hydrogeological methods, and the application of hydrological methods is rare. In this paper, the laws and characteristics of groundwater resources in the representative basin of the region are analyzed and evaluated using the hydrological model of the watershed. Compared with the hydrogeological methods, the results are basically the same.