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本文通过对基岩水与孔隙水的比较分析，介绍了基岩水的分布、水动力学和水化学特征，指出了基岩水运动具有均位趋势、选择流动及汇流特性，得出了渗流理论不宜用于基岩水的结论。
Based on the comparative analysis of bedrock water and pore water, this paper introduces the distribution, hydrodynamics and hydrochemical characteristics of bedrock water. It is pointed out that the bedrock water movement has the trend of average trend, selective flow and confluence. It is concluded that the seepage theory should not be used The conclusion of water in bedrock.