THE GRAVITY TIDAL EFFECT OF WATERHEAD IN A MODEL OF HORIZONTAL MULTILAYER CONFINED AQUIFER

Base on elastic theory and the principle of dynamics of ground water, the partial differential equations that show the relationship between the waterhead in a model of horizontal multilayer condined aquifer and the gravity tidal are established. After they are simplified and solved, the cjuantitative relationship between the gravity ridal effect of the water level in the well and the hydrogeology parameters of the aguifer is discussed.