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运用离散数学的图理论进行裂隙岩体裂隙网络连通性研究，建立了裂隙岩体初始裂隙网络渗流的离散数值模型．这一模型从根本上突破了经典的均质渗流理论．
The discrete mathematics graph theory is used to study the connectivity of fractured rock mass fissures, and a discrete numerical model of fissured rock mass initial fissure network seepage is established. This model fundamentally broke through the classical homogeneous seepage theory.