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• W2097053622 abstract "Abstract We investigate the response of a laboratory aquifer submitted to artificial rainfall, with an emphasis on the early stage of a rain event. In this almost two-dimensional experiment, the infiltrating rainwater forms a groundwater reservoir which exits the aquifer through one side. The resulting outflow resembles a typical stream hydrograph: the water discharge increases rapidly during rainfall and decays slowly after the rain has stopped. The Dupuit–Boussinesq theory, based on Darcy’s law and the shallow-water approximation, quantifies these two asymptotic regimes. At the early stage of a rainfall event, the discharge increases linearly with time, at a rate proportional to the rainfall rate to the power of ${textstyle frac{3}{2}}$ . Long after the rain has stopped, it decreases as the squared inverse of time (Boussinesq, C. R. Acad. Sci. , vol. 137, 1903, pp. 5–11). We compare these predictions with our experimental data." @default.
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• W2097053622 date "2014-10-20" @default.
• W2097053622 modified "2023-10-01" @default.
• W2097053622 title "Response of a laboratory aquifer to rainfall" @default.
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• W2097053622 doi "https://doi.org/10.1017/jfm.2014.590" @default.
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