在矿区或其他水文地质工程地质勘测中,含水层厚度H及坑、孔道最大涌水量Q_(max)都是一项重要的指标,也是大量勘探及多次试验所惟一觅求的指标。因为H、Q_(max)值能具体而定量地表明含水岩系的特征。然而直到现在为止,这一数值仍然必须依靠大量的钻 In mining or other hydrogeological engineering geological surveys, the thickness H of the aquifer and the maximum water inflow Q * (max) of the tunnels are both important indicators and also the only index for many exploration and multiple tests. Because of the H, Q_ (max) values ​​can be used to specify the characteristics of aquifer rocks in a specific and quantitative way. However until now, this number still had to rely on a large number of drills