The variation of stress in the aquifer inversed is closer to practice by the tidal effect of the water level in a deep well than by the barometric effect.
利用井水位的固体潮效应反演含水层应力变化，比利用气压效应更接近实际情况。
The variation of stress in the aquifer inversed is closer to practice by the tidal effect of the water level in a deep well than by the barometric effect.
利用井水位的固体潮效应反演含水层应力变化，比利用气压效应更接近实际情况。
应用推荐