water gushing point 在采掘过程中发生突水的位置或地点。 突水点主要受地质构造、岩石性质、水文地质条件和人为因素控制。通常发生在水源充足、径流条件好、水压力高的岩石破碎部位,或者构造薄弱点(如断裂带、褶皱轴部等)、溶洞、陷落柱及其附近,以及采矿冒落裂隙和巷道底鼓部位。
突水与构造密切相关,突水点最大涌水量与断层密度呈正相关关系。
Water inrush is closely related to the structures. Maximum water emission of water inrush point has positive correlation with fault density.
该系统不但实现了突水水源的点查询,还实现了突水空间分区。
The system has realized not only inquiring for water resource of inrush, but also spatial classification.
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