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26 May 2020 Wave-driven Groundwater Flows in Sandy Beaches: A Richards Equation-based Model
Jean-Baptiste Clément, Damien Sous, Frédéric Golay, Mehmet Ersoy
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Abstract

Clément, J.-B.; Sous, D.; Golay, F. and Ersoy M., 2020. Wave-driven groundwater flows in sandy beaches: A Richards equation-based model. In: Malvárez, G. and Navas, F. (eds.), Global Coastal Issues of 2020. Journal of Coastal Research, Special Issue No. 95, pp. 1047–1051. Coconut Creek (Florida), ISSN0749-0208.

A groundwater model is developed to simulate flows under the swash zone of sandy beach. Variably saturated beach is described by Richards equation, which is solved by the Rivage code thanks to a discontinuous Galerkin method. The SWASH code is used to simulate wave propagation in nearshore waters and compute suitable boundary conditions at the beachface to force Richards equation. An idealized case is considered to investigate the beach groundwater response to the action of swash cycles associated with long IG-like waves: infiltration/ exfiltration, water table, hydraulic head and pore velocities are outlined. A good qualitative agreement is found with observations from experimental studies in the literature.

©Coastal Education and Research Foundation, Inc. 2020
Jean-Baptiste Clément, Damien Sous, Frédéric Golay, and Mehmet Ersoy "Wave-driven Groundwater Flows in Sandy Beaches: A Richards Equation-based Model," Journal of Coastal Research 95(sp1), 1047-1051, (26 May 2020). https://doi.org/10.2112/SI95-204.1
Received: 31 March 2019; Accepted: 13 February 2020; Published: 26 May 2020
KEYWORDS
forced coupling
groundwater
numerical modelling
seepage
swash zone
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