Interlobate esker architecture and related hydrogeological features derived from a combination of high-resolution reflection seismics and refraction tomography, Virttaankangas, southwest Finland

dc.contributor.authorMaries Georgiana
dc.contributor.authorAhokangas Elina
dc.contributor.authorMäkinen Joni
dc.contributor.authorPasanen Antti
dc.contributor.authorMalehmir Allireza
dc.contributor.organizationfi=maantiede|en=Geography |
dc.contributor.organization-code1.2.246.10.2458963.20.17647764921
dc.converis.publication-id18109616
dc.converis.urlhttps://research.utu.fi/converis/portal/Publication/18109616
dc.date.accessioned2022-10-28T13:42:52Z
dc.date.available2022-10-28T13:42:52Z
dc.description.abstract<p>A novel high-resolution (2–4 m source and receiver spacing) reflection and refraction seismic survey was carried out for aquifer characterization and to confirm the existing depositional model of the interlobate esker of Virttaankangas, which is part of the Säkylänharju-Virttaankangas glaciofluvial esker-chain complex in southwest Finland. The interlobate esker complex hosting the managed aquifer recharge (MAR) plant is the source of the entire water supply for the city of Turku and its surrounding municipalities. An accurate delineation of the aquifer is therefore critical for long-term MAR planning and sustainable use of the esker resources. Moreover, an additional target was to resolve the poorly known stratigraphy of the 70–100-m-thick glacial deposits overlying a zone of fractured bedrock. Bedrock surface as well as fracture zones were confirmed through combined reflection seismic and refraction tomography results and further validated against existing borehole information. The high-resolution seismic data proved successful in accurately delineating the esker cores and revealing complex stratigraphy from fan lobes to kettle holes, providing valuable information for potential new pumping wells. This study illustrates the potential of geophysical methods for fast and cost-effective esker studies, in particular the digital-based landstreamer and its combination with geophone-based wireless recorders, where the cover sediments are reasonably thick.<br /></p>
dc.format.pagerange829
dc.format.pagerange845
dc.identifier.eissn1435-0157
dc.identifier.jour-issn1431-2174
dc.identifier.olddbid183824
dc.identifier.oldhandle10024/166918
dc.identifier.urihttps://www.utupub.fi/handle/11111/41686
dc.identifier.urlhttps://link.springer.com/article/10.1007/s10040-016-1513-9
dc.identifier.urnURN:NBN:fi-fe2021042716120
dc.language.isoen
dc.okm.affiliatedauthorMäkinen, Joni
dc.okm.affiliatedauthorAhokangas, Elina
dc.okm.discipline1171 Geosciencesen_GB
dc.okm.discipline1171 Geotieteetfi_FI
dc.okm.internationalcopublicationinternational co-publication
dc.okm.internationalityInternational publication
dc.okm.typeA1 ScientificArticle
dc.publisherSpringer Berlin Heidelberg
dc.publisher.countryGermanyen_GB
dc.publisher.countrySaksafi_FI
dc.publisher.country-codeDE
dc.relation.doi10.1007/s10040-016-1513-9
dc.relation.ispartofjournalHydrogeology Journal
dc.relation.issue3
dc.relation.volume25
dc.source.identifierhttps://www.utupub.fi/handle/10024/166918
dc.titleInterlobate esker architecture and related hydrogeological features derived from a combination of high-resolution reflection seismics and refraction tomography, Virttaankangas, southwest Finland
dc.year.issued2017

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