This method can be used to calculate the transmissibility coefficient of 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 transmissibility coefficient of aquifer complies with the normal probability distribution.
结果表明，1）该含水层导水系数在空间上的变化服从正态概率分布；
3
The main factors affecting the well yield are the transmissivity and water yield coefficient of the aquifer as well as the permeability coefficient and thickness of the leaky layer.