Quantifying aquifer properties and freshwater resource in coastal barriers: A hydrogeophysical approach applied at Sasihithlu (Karnataka state, India)

dc.contributor.authorVouillamoz, J.-M.
dc.contributor.authorHoareau, J.
dc.contributor.authorGrammare, M.
dc.contributor.authorCaron, D.
dc.contributor.authorNandagiri, L.
dc.contributor.authorLegchenko, A.
dc.date.accessioned2026-02-05T09:35:05Z
dc.date.issued2012
dc.description.abstractMany human communities living in coastal areas in Africa and Asia rely on thin freshwater lenses for their domestic supply. Population growth together with change in rainfall patterns and sea level will probably impact these vulnerable groundwater resources. Spatial knowledge of the aquifer properties and creation of a groundwater model are required for achieving a sustainable management of the resource. This paper presents a ready-to-use methodology for estimating the key aquifer properties and the freshwater resource based on the joint use of two non-invasive geophysical tools together with common hydrological measurements. <br><br> We applied the proposed methodology in an unconfined aquifer of a coastal sandy barrier in South-Western India. We jointly used magnetic resonance and transient electromagnetic soundings and we monitored rainfall, groundwater level and groundwater electrical conductivity. The combined interpretation of geophysical and hydrological results allowed estimating the aquifer properties and mapping the freshwater lens. Depending on the location and season, we estimate the freshwater reserve to range between 400 and 700 L m??'2 of surface area (A± 50%). We also estimate the recharge using time lapse geophysical measurements with hydrological monitoring. After a rainy event close to 100% of the rain is reaching the water table, but the net recharge at the end of the monsoon is less than 10% of the rain. Thus, we conclude that a change in rainfall patterns will probably not impact the groundwater resource since most of the rain water recharging the aquifer is flowing towards the sea and the river. However, a change in sea level will impact both the groundwater reserve and net recharge. © Author(s) 2012.
dc.identifier.citationHydrology and Earth System Sciences, 2012, 16, 11, pp. 4387-4400
dc.identifier.issn10275606
dc.identifier.urihttps://doi.org/10.5194/hess-16-4387-2012
dc.identifier.urihttps://idr.nitk.ac.in/handle/123456789/26896
dc.subjectAquifer properties
dc.subjectCoastal area
dc.subjectCoastal barrier
dc.subjectDomestic supplies
dc.subjectElectrical conductivity
dc.subjectFresh water resources
dc.subjectGeophysical measurements
dc.subjectGeophysical tools
dc.subjectGroundwater models
dc.subjectGroundwater reserves
dc.subjectHuman communities
dc.subjectHydrogeophysical
dc.subjectKarnataka
dc.subjectPopulation growth
dc.subjectRain water
dc.subjectRainfall patterns
dc.subjectSpatial knowledge
dc.subjectSurface area
dc.subjectSustainable management
dc.subjectTransient electromagnetic soundings
dc.subjectUnconfined aquifers
dc.subjectWater tables
dc.subjectAquifers
dc.subjectElectric conductivity
dc.subjectEstimation
dc.subjectGeophysics
dc.subjectMagnetic resonance
dc.subjectPopulation statistics
dc.subjectPower quality
dc.subjectRain
dc.subjectRecharging (underground waters)
dc.subjectSea level
dc.subjectWater
dc.subjectGroundwater resources
dc.subjectcoastal zone
dc.subjectelectromagnetic method
dc.subjectgeophysical method
dc.subjectgroundwater resource
dc.subjecthydrological modeling
dc.subjectmonsoon
dc.subjectpopulation growth
dc.subjectrainwater
dc.subjectrecharge
dc.subjectsea level change
dc.subjectsustainable development
dc.subjectunconfined aquifer
dc.subjectwater management
dc.subjectwater quality
dc.subjectwater supply
dc.subjectwater table
dc.subjectIndia
dc.subjectSasihithlu
dc.titleQuantifying aquifer properties and freshwater resource in coastal barriers: A hydrogeophysical approach applied at Sasihithlu (Karnataka state, India)

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