论文部分内容阅读
通过分析在山地丘陵区控制红层地下水富集的岩性、地质构造及地形地貌等主要地质因素,论证了红层地下水富集的水文地质特征,认为富水块段的形成通常并不是仅仅由某一因素单独决定的,而是岩性、地质构造及地形地貌等地质因素共同作用的结果,而这些因素的组合具有明显的规律性。进而根据水文地质及环境地质调查研究成果及丰富的实践经验,归纳总结了反映红层地下水富集的水文地质因素组合的基本规律。
By analyzing the main geologic factors such as lithology, geological structure and topography in the hilly area, the enrichment of hydrogeological features of groundwater in red beds is demonstrated. It is concluded that the formation of water-rich blocks is usually not only caused by A certain factor alone decided, but the result of geological factors such as lithology, geological structure and topography, and the combination of these factors has obvious regularity. Based on the research results of hydrogeological and environmental geology and abundant practical experience, the basic law of the combination of hydrogeological factors that reflect the enrichment of groundwater in red beds is summarized.