The results shows that: 1, The spatial change of the transmissibilitycoefficient 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；
2
This method can be used to calculate the transmissibilitycoefficient of well aquifer by means of the oscillation curve of well water level instead of the recovery curve.