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本文应用同位素技术,结合含水岩组水文地质结构特征的分析及地下水动力学方法的年龄计算,揭示了河北平原京津以南地区深层地下水的形成规律,得出了深层地下水资源补给能力及承受开采能力很低的结论,这为今后深层地下水资源的合理开发利用提供了重要依据。
Based on the analysis of hydrogeological structure characteristics of aquifer and the calculation of the age of groundwater hydrodynamics, isotope techniques are used to reveal the formation of deep groundwater in the area south of Beijing and Tianjin in the Hebei Plain. The deep groundwater resources replenishment ability and undergoing mining Low-capacity conclusion, which provides an important basis for the rational development and utilization of deep groundwater resources in the future.