This method can be used to calculate the transmissibilitycoefficientof well aquifer by means of the oscillation curve of well water level instead of the recovery curve.
该方法不是用井水位的恢复曲线,而是用井水位的振荡曲线计算出水井含水层的导水系数。
2
The results shows that: 1, The spatial change of the transmissibilitycoefficientof aquifer complies with the normal probability distribution.