Overexploitation of groundwater in Cangzhou area has attracted wide attention.Different layers of the aquifer may be connected through wells,since most wells of the deep aquifer have screens in several layers.This stu...Overexploitation of groundwater in Cangzhou area has attracted wide attention.Different layers of the aquifer may be connected through wells,since most wells of the deep aquifer have screens in several layers.This study proved the existence of vertical flow through wells,calculated the flow velocity and quantity of vertical flow in wells with methods of both field measurement and numerical simulation.Further,the recharge of deep groundwater by vertical flow through wells was estimated.An annual recharge of 1.5×10~8-2.8×10~8 m^3 from the third aquifer to the forth aquifer in Cangzhou area was estimated,according to the in-well measurement by heat pulse flowmeter sonde.展开更多
文摘Overexploitation of groundwater in Cangzhou area has attracted wide attention.Different layers of the aquifer may be connected through wells,since most wells of the deep aquifer have screens in several layers.This study proved the existence of vertical flow through wells,calculated the flow velocity and quantity of vertical flow in wells with methods of both field measurement and numerical simulation.Further,the recharge of deep groundwater by vertical flow through wells was estimated.An annual recharge of 1.5×10~8-2.8×10~8 m^3 from the third aquifer to the forth aquifer in Cangzhou area was estimated,according to the in-well measurement by heat pulse flowmeter sonde.
