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Artificial groundwater recharge, II. Rectangular recharging area
Journal of Hydrology, 1975Abstract The nonlinear, partial-differential equation characterizing the unsteady flow in an unconfined aquifer receiving uniform vertical recharge from a rectangular spreading basin is solved numerically. The method of solution consists of the alternating-direction implicit scheme with an inhomogeneous grid spacing.
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1988
Groundwater recharge is usually considered a process of water movement downward through the saturated zone under the forces of gravity or in a direction determined by the hydraulic conditions. In a broader sense the process of recharge is more complicated.
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Groundwater recharge is usually considered a process of water movement downward through the saturated zone under the forces of gravity or in a direction determined by the hydraulic conditions. In a broader sense the process of recharge is more complicated.
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2009
Principal aspects of groundwater use and recharge are reviewed in the {perspective} of achieving sustainable groundwater development, i.e. avoiding groundwater degradation. The analysis concerns both major aquifers and well fields and minor aquifers of local importance, such as in islands.
Luis Santos Pereira +2 more
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Principal aspects of groundwater use and recharge are reviewed in the {perspective} of achieving sustainable groundwater development, i.e. avoiding groundwater degradation. The analysis concerns both major aquifers and well fields and minor aquifers of local importance, such as in islands.
Luis Santos Pereira +2 more
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Quantification of Groundwater Recharge
Hydrogeologists should understand how groundwater recharges aquifers, the methods available for quantifying this component of the water budget, and the strengths and weaknesses of the different methods. Understanding the sources of recharge can be important for predicting the impacts of land use change and climate change on groundwater resources and ...Peter Cook, Philip Brunner
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