本文介绍在各种采矿地质条件下,井壁透水性的观测结果及水流流入井筒的测量结果。阐明了目前确定及研究层流向紊流过渡方法的特征。介绍了作者用来研究岩石,建筑材料及矿山巷道模型渗透性的仪器。作者所进行的混凝土井壁模型的研究也证实了井壁的透水性。同时证实了水流通过井壁可以按层流或紊流方式流动。在线性流动范围内,导出了水流通过井壁速度的公式。 This article presents observations of borehole water permeability and the results of flow into the wellbore under various mining geological conditions. The characteristics of the method for determining and studying laminar turbulence transition are elucidated. Introduced the author used to study rock, building materials and mine roadway model permeability. The author’s study of the concrete borehole model also confirmed the water permeability of the borehole wall. At the same time, it is confirmed that the water flow through the shaft wall can flow in a laminar or turbulent manner. Within the linear flow range, the formula for the velocity of water flowing through the borehole wall is derived.