Ground-penetrating radar insight into a coastal aquifer: the freshwater lens of Borkum Island

dc.bibliographicCitation.firstPage519eng
dc.bibliographicCitation.issue2eng
dc.bibliographicCitation.journalTitleHydrology and earth system sciences : an interactive open-access journal of the European Geosciences Unioneng
dc.bibliographicCitation.lastPage531eng
dc.bibliographicCitation.volume17eng
dc.contributor.authorIgel, J.
dc.contributor.authorGünther, T.
dc.contributor.authorKuntzer, M.
dc.date.accessioned2022-03-03T06:28:17Z
dc.date.available2022-03-03T06:28:17Z
dc.date.issued2013
dc.description.abstractFreshwater lenses, as important resource for drinking water, are sensitive to climate changes and sea level rise. To simulate this impact on the groundwater systems, hydraulic subsurface models have to be designed. Geophysical techniques can provide information for generating realistic models. The aim of our work is to show how ground-penetrating radar (GPR) investigations can contribute to such hydrological simulations. In the pilot area, Borkum island, GPR was used to map the shape of the groundwater table (GWT) and to characterise the aquifer. In total, 20 km of constant offset (CO) profiles were measured with centre frequencies of 80 and 200 MHz. Wave velocities were determined by common midpoint (CMP) measurements and vertical radar profiling (VRP) in a monitoring well. The 80 MHz CO data show a clear reflection at the groundwater table, whereas the reflection is weaker for the 200 MHz data. After correcting the GPR water tables for the capillary rise, they are in good accordance with the pressure heads of the observation wells in the area. In the centre of the island, the groundwater table is found up to 3.5 m above sea level, however it is lower towards the coastline and marshland. Some local depressions are observed in the region of dune valleys and around pumping stations of the local water supplier. GPR also reveals details within the sediments and highly-permeable aeolian sands can be distinguished from less-permeable marine sediments. Further, a silt loam layer below the water table could be mapped on a large area. The reflection characteristics indicates scattered erosion channels in this layer that cause it to be an aquitard with some leakage. GPR provides a high resolution map of the groundwater table and insight into the stratigraphy of the sediments and their hydraulic properties. This is valuable complementary information to the observation of sparsely distributed monitoring wells as input to hydraulic simulation.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/8108
dc.identifier.urihttps://doi.org/10.34657/7148
dc.language.isoengeng
dc.publisherMunich : EGUeng
dc.relation.doihttps://doi.org/10.5194/hess-17-519-2013
dc.relation.essn1607-7938
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subject.ddc550eng
dc.subject.otherDistributed monitoringeng
dc.subject.otherGeophysical techniqueseng
dc.subject.otherGround Penetrating Radareng
dc.subject.otherGround penetrating radarseng
dc.subject.otherHydraulic simulationeng
dc.subject.otherHydrological simulationseng
dc.subject.otherReflection characteristicseng
dc.subject.otherVertical radar profilingeng
dc.subject.otherAquiferseng
dc.subject.otherClimate changeeng
dc.subject.otherGroundwater resourceseng
dc.subject.otherRadareng
dc.subject.otherRadar measurementeng
dc.subject.otherSea leveleng
dc.subject.otherSilteng
dc.subject.otherStratigraphyeng
dc.subject.otherSubmarine geologyeng
dc.subject.otherWatereng
dc.subject.otherWellseng
dc.subject.otherGround penetrating radar systemseng
dc.subject.otherbiostratigraphyeng
dc.subject.othercapillarityeng
dc.subject.othercarbon monoxideeng
dc.subject.otherclimate changeeng
dc.subject.othercoasteng
dc.subject.othercoastal aquifereng
dc.subject.otherdata seteng
dc.subject.otherdrinking watereng
dc.subject.otherground penetrating radareng
dc.subject.otherhydraulic propertyeng
dc.subject.otherhydrogeologyeng
dc.subject.othermarine sedimenteng
dc.subject.othermonitoringeng
dc.subject.othernumerical modeleng
dc.subject.otherpressure effecteng
dc.subject.otherpumpingeng
dc.subject.otherscatteringeng
dc.subject.othersea level changeeng
dc.subject.othersilty loameng
dc.subject.otherwater tableeng
dc.subject.otherBorkumeng
dc.subject.otherEast Frisian Islandseng
dc.subject.otherFrisian Islandseng
dc.subject.otherGermanyeng
dc.subject.otherLower Saxonyeng
dc.titleGround-penetrating radar insight into a coastal aquifer: the freshwater lens of Borkum Islandeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorLIAGeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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