An examination is made of two aspects of beach ground water behaviour: (i) water table fluctuations in response to tidal forcing, and (ii) pressure propagation through a saturated sand bed under swash. Models and measurements of each are presented. It is found that a 1-D Boussinesq model of water table behaviour provides good predictions of observed water table fluctuations. Further field work is needed before a simple model of pressure propagation can be properly tested
The swash zone is the part of the beach that reaches from the limit of wave run-up until the limit o...
Beach groundwater is a complex and dynamic system interacting with tides, waves and swash. Groundwat...
Proceedings of the 11th International Coastal Symposium, Szczecin, PolandInternational audienceAs pa...
Field measurements of swash-induced hydraulic (pressure) gradients in the surface layers of a sand b...
Field and laboratory observations have shown that a relatively low beach groundwater table enhances ...
This paper describes field measurements of near-surface hydraulic gradients within a sandy beach dur...
Previous studies of swash-ground water interactions have given prominance to infiltration of swash a...
In this paper, simultaneous measurements of the instantaneous shoreline (swash front) and the respon...
The coupling of sandy beach aquifers with the swash zone in the vicinity of the water table exit poi...
Field and laboratory observations have shown that a relatively low beach groundwater table enhances ...
The coupling of sandy beach aquifers with the swash zone in the vicinity of the water table exit poi...
To incorporate groundwater infiltration/exfiltration in the description of swash zone sediment trans...
International audienceExperiments are carried out in a wave basin in order to study the swash-ground...
International audienceA groundwater model is developed to simulate flows under the swash zone of san...
The dominant hydrodynamic forcing and resulting sediment transport mechanisms in the swash zone are ...
The swash zone is the part of the beach that reaches from the limit of wave run-up until the limit o...
Beach groundwater is a complex and dynamic system interacting with tides, waves and swash. Groundwat...
Proceedings of the 11th International Coastal Symposium, Szczecin, PolandInternational audienceAs pa...
Field measurements of swash-induced hydraulic (pressure) gradients in the surface layers of a sand b...
Field and laboratory observations have shown that a relatively low beach groundwater table enhances ...
This paper describes field measurements of near-surface hydraulic gradients within a sandy beach dur...
Previous studies of swash-ground water interactions have given prominance to infiltration of swash a...
In this paper, simultaneous measurements of the instantaneous shoreline (swash front) and the respon...
The coupling of sandy beach aquifers with the swash zone in the vicinity of the water table exit poi...
Field and laboratory observations have shown that a relatively low beach groundwater table enhances ...
The coupling of sandy beach aquifers with the swash zone in the vicinity of the water table exit poi...
To incorporate groundwater infiltration/exfiltration in the description of swash zone sediment trans...
International audienceExperiments are carried out in a wave basin in order to study the swash-ground...
International audienceA groundwater model is developed to simulate flows under the swash zone of san...
The dominant hydrodynamic forcing and resulting sediment transport mechanisms in the swash zone are ...
The swash zone is the part of the beach that reaches from the limit of wave run-up until the limit o...
Beach groundwater is a complex and dynamic system interacting with tides, waves and swash. Groundwat...
Proceedings of the 11th International Coastal Symposium, Szczecin, PolandInternational audienceAs pa...