Page 2: Research news on groundwater flow

Groundwater flow refers to the movement of water through the pore spaces and fractures of unsaturated and saturated geologic media, governed primarily by hydraulic gradients and the hydraulic properties of the aquifer. It is quantitatively described by Darcy’s law, which relates specific discharge to hydraulic conductivity and the gradient of hydraulic head, and by the groundwater flow equation, a partial differential equation combining Darcy’s law with conservation of mass. Groundwater flow processes control recharge, discharge, solute transport, and aquifer response to stresses such as pumping, and are analyzed using analytical solutions, numerical models, and field measurements of head, permeability, and storage parameters.

Seeping groundwater can be a hidden source of greenhouse gases

Scientists know that streams and rivers can contribute significant quantities of greenhouse gases to the atmosphere. One way these bodies of water come to contain greenhouse gases is via groundwater, which picks up carbon ...

NASA uses advanced radar to track groundwater in California

Where California's towering Sierra Nevada surrenders to the sprawling San Joaquin Valley, a high-stakes detective story is unfolding. The culprit isn't a person but a process: the mysterious journey of snowmelt as it travels ...

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