Geophysical investigation of a freshwater lens on the island of Langeoog, Germany – Insights from combined HEM, TEM and MRS data

dc.bibliographicCitation.firstPage231eng
dc.bibliographicCitation.journalTitleJournal of applied geophysicseng
dc.bibliographicCitation.lastPage245eng
dc.bibliographicCitation.volume136eng
dc.contributor.authorCostabel, Stephan
dc.contributor.authorSiemon, Bernhard
dc.contributor.authorHouben, Georg
dc.contributor.authorGünther, Thomas
dc.date.accessioned2022-03-07T05:47:58Z
dc.date.available2022-03-07T05:47:58Z
dc.date.issued2017
dc.description.abstractA multi-method geophysical survey, including helicopter-borne electromagnetics (HEM), transient electromagnetics (TEM), and magnetic resonance sounding (MRS), was conducted to investigate a freshwater lens on the North Sea island of Langeoog, Germany. The HEM survey covers the entire island and gives an overview of the extent of three freshwater lenses that reach depths of up to 45 m. Ground-based TEM and MRS were conducted particularly on the managed western lens to verify the HEM results and to complement the lithological information from existing boreholes. The results of HEM and TEM are in good agreement. Salt- and freshwater-bearing sediments can, as expected, clearly be distinguished due to their individual resistivity ranges. In the resistivity data, a large transition zone between fresh- and saltwater with a thickness of up to 20 m is identified, the existence of which is verified by borehole logging and sampling. Regarding lithological characterisation of the subsurface, the MRS method provides more accurate and reliable results than HEM and TEM. Using a lithological index derived from MRS water content and relaxation time, thin aquitard structures as well as fine and coarse sand aquifers can be distinguished. Complementing the existing borehole data with the lithology information estimated from MRS, we generate a map showing the occurrence of aquitard structures, which significantly improves the hydrogeological model of the island. Moreover, we demonstrate that the estimates of groundwater conductivity in the sand aquifers from geophysical data are in agreement with the fluid conductivity measured in the boreholes.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/8166
dc.identifier.urihttps://doi.org/10.34657/7205
dc.language.isoengeng
dc.publisherAmsterdam [u.a.] : Elsevier Scienceeng
dc.relation.doihttps://doi.org/10.1016/j.jappgeo.2016.11.007
dc.relation.essn1879-1859
dc.rights.licenseCC BY-NC-ND 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/eng
dc.subject.ddc620eng
dc.subject.ddc660eng
dc.subject.ddc550eng
dc.subject.otherClay mappingeng
dc.subject.otherFreshwater lenseng
dc.subject.otherHelicopter electromagneticseng
dc.subject.otherMagnetic resonance soundingeng
dc.subject.otherTransient electromagneticseng
dc.titleGeophysical investigation of a freshwater lens on the island of Langeoog, Germany – Insights from combined HEM, TEM and MRS dataeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorLIAGeng
wgl.subjectIngenieurwissenschafteneng
wgl.typeZeitschriftenartikeleng
Files
Original bundle
Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
Geophysical_investigation_of_a_freshwater.pdf
Size:
2.65 MB
Format:
Adobe Portable Document Format
Description: