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This research presents artificial recharge of freshwater in Belgian coastal dunes, highlighting processes, hydrochemistry, and ecological implications. Extraction, infiltration, groundwater flow, and water types are analyzed, emphasizing low-mineralization source water. Various data and modeling methods are employed to demonstrate the positive effects on drawdowns and ecological restoration. Key reactions like carbonate dissolution are identified in the mixing of recharged water with existing dune water.
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Artificial Recharge of Fresh Water in the Belgian Coastal Dunes Alexander Vandenbohede, Luc Lebbe and Emmanuel Van Houtte Research Unit Groundwater Modelling Ghent University, Belgium Intermunicipal Water Company of the Veurne region (IWVA)
Infiltration of 2.5 million m³/year Extraction of 3.5 million m³/year Very low mineralisation of source water for recharge: 50 mg/l Extraction wells surrounding ponds
Borehole measurements Sedimentological data Head observations Chemical data Tracer test 3D density dependent flow transport modelling MOCDENS3D – Visual MOCDENS3D Hydrochemistry Hydrosomes (water bodies) Important processes
Replacement of dune water with recharged water
Conclusions • More water is extracted – less water dune water is extracted • Positive effects on drawdowns • Natural groundwater flow is partially restored • Ecological implications
Conclusions • Extracted water is mix of artificial recharged water and dune water • Extracted water is mix of water with a large spectrum of residence times (30 days to 5 years)
Conclusions • Source water for artificial recharge is of very low mineralisation 50 mg/l vs 500 mg/l for dune water • Distinct water types: dune water, extracted water, recharge water, recharged water in aquifer • Most important reactions: carbonate dissolution • consumption of oxygen/nitrate • oxidation of sulphide minerals