%0 Journal Article
%T Swash-groundwater dynamics in a sandy beach laboratory experiment
%+ Institut méditerranéen d'océanologie (MIO)
%+ ISMR
%+ Laboratoire des Écoulements Géophysiques et Industriels [Grenoble] (LEGI)
%A Sous, Damien
%A Lambert, Adrien
%A Rey, Vincent
%A Michallet, Hervé
%< avec comité de lecture
%Z MIO:13-048
%@ 0378-3839
%J Coastal Engineering
%I Elsevier
%V 80
%P 122-136
%8 2013-10-01
%D 2013
%R 10.1016/j.coastaleng.2013.05.006
%K swash zone
%K groundwater dynamics
%K sandy beach
%K pressure gradients
%K infragravity waves
%Z Sciences of the Universe [physics]/Ocean, Atmosphere
%Z Engineering Sciences [physics]/Mechanics [physics.med-ph]/Fluids mechanics [physics.class-ph]
%Z Physics [physics]/Mechanics [physics]/Fluid mechanics [physics.class-ph]Journal articles
%X Experiments are carried out in a wave basin in order to study the swash-groundwater interaction. A set of wave gauges and pressure sensors are used to monitor the free surface and groundwater dynamics. The study is based on the comparison of two selected cases which differ by the gravity and infragravity forcing conditions, the features of wave breaking in the surf zone, the presence of a standing wave attached to the beachface and the wave setup at the shoreline. Significant differences are observed in the response of the swash-groundwater system. The watertable overheight appears to be controlled by the amount of infragravity energy available at the shore. Cyclic beach drainage processes can be observed when the watertable is low. Significant time-averaged and time-resolved flows are observed into the sand, depending on the swash hydrodynamics. The presence of a gravity standing wave modulation attached to the shore is shown to affect swash and groundwater dynamics. Most of the pressure gradients observed under the swash zone are related to infiltration flows and are thus related to moderate increase of the sediment relative weight.
%G English
%L hal-00824276
%U https://hal.science/hal-00824276
%~ INSU
%~ UGA
%~ UNIV-TLN
%~ CNRS
%~ UNIV-GRENOBLE1
%~ UNIV-AMU
%~ INPG
%~ OSUG
%~ LEGI
%~ MIO
%~ OSU-INSTITUT-PYTHEAS
%~ GIP-BE
%~ TESTUPPA
%~ MIO-OPLC