Please use this identifier to cite or link to this item: http://repositorio.lnec.pt:8080/jspui/handle/123456789/1016582
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dc.contributor.authorMota, R.pt_BR
dc.contributor.authorMonteiro dos Santos, F. A.pt_BR
dc.date.accessioned2023-10-12T13:58:08Zpt_BR
dc.date.accessioned2023-11-21T11:01:13Z-
dc.date.available2023-10-12T13:58:08Zpt_BR
dc.date.available2023-11-21T11:01:13Z-
dc.date.issued2006-06pt_BR
dc.identifier.urihttps://repositorio.lnec.pt/jspui/handle/123456789/1016582-
dc.description.abstractPorosity and water saturation percent, or their product—the water content—are important parameters for most hydrogeologic studies. Geophysical methods, especially the resistivity method, are routinely applied to studying variations in these parameters at field scales. Resistivity is highly influenced by the presence of water in pore spaces and therefore well suited for studying fluids and saturation. Laboratory and field work are being correlatedpt_BR
dc.language.isoengpt_BR
dc.publisherThe leading edgept_BR
dc.rightsopenAccesspt_BR
dc.title2D sections of porosity and water saturation percent from combined resistivity and seismic surveys for hydrogeologic studiespt_BR
dc.typearticlept_BR
dc.description.pages735-737pppt_BR
dc.description.sectorDG/NGEApt_BR
dc.description.magazineThe leading edgept_BR
dc.contributor.peer-reviewedSIMpt_BR
dc.contributor.academicresearchersSIMpt_BR
dc.contributor.arquivoSIMpt_BR
Appears in Collections:DG/NGEA - Comunicações a congressos e artigos de revista



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