涌泉洞位于九江县涌泉乡伏船山，是天然断层裂隙产生崩塌而形成的溶洞。
Located on Fuchuan Mountain, Yongquan Town, Jiujiang County, Yongquan Cave was shaped by the collapse of geological fault.
结果表明，随着建筑物荷载增大，断层裂隙向下方采空区方向扩展和贯通，造成了浅层地表水向深部采空区渗流汇集。
The results show that with the building loads increase, the propagation of cracks is extending from the top to the bottom of the goaf, and shallow groundwater seeps together into the deep goaf.
在此基础上，对断层导水裂隙的扩展规律进行了分析。
On this basis, the expanding regularity of fault cracks conducting water is analysed.
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