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dc.contributor.authorHussain, Yawar-
dc.contributor.authorUagoda, Rogério Elias Soares-
dc.contributor.authorBorges, Welitom Rodrigues-
dc.contributor.authorNunes, José Gustavo da Silva-
dc.contributor.authorHamza, Omar-
dc.contributor.authorCondori, Cristobal-
dc.contributor.authorAslam, Khurram-
dc.contributor.authorDou, Jie-
dc.contributor.authorCárdenas-Soto, Martín-
dc.date.accessioned2021-06-16T16:17:12Z-
dc.date.available2021-06-16T16:17:12Z-
dc.date.issued2020-08-14-
dc.identifier.citationHUSSAIN, Yawar et al. The potential use of geophysical methods to identify cavities, sinkholes and pathways for water infiltration. Water, v. 12, n. 8, 2289, 2020. DOI: https://doi.org/10.3390/w12082289. Disponível em: https://www.mdpi.com/2073-4441/12/8/2289. Acesso em: 16 jun. 2021.pt_BR
dc.identifier.urihttps://repositorio.unb.br/handle/10482/41176-
dc.language.isoPortuguêspt_BR
dc.publisherMDPIpt_BR
dc.rightsAcesso Abertopt_BR
dc.titleThe potential use of geophysical methods to identify cavities, sinkholes and pathways for water infiltrationpt_BR
dc.typeArtigopt_BR
dc.subject.keywordGeofísica - metodologiapt_BR
dc.subject.keywordInfiltraçãopt_BR
dc.rights.license© 2020 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).pt_BR
dc.identifier.doihttps://doi.org/10.3390/w12082289pt_BR
dc.description.abstract1The use of geophysical characterization of karst systems can provide an economical and non-invasive alternative for extracting information about cavities, sinkholes, pathways for water infiltration as well as the degree of karstification of underlying carbonate rocks. In the present study, three geophysical techniques, namely, Ground Penetrating Radar (GPR), Electrical Resistivity Tomography (ERT) and Very Low Frequency Electromagnetic (VLFEM) methods were applied at three different locations in relation to fluvial karst, which is listed as an environmentally sensitive area in Rio Vermelho, Mambaí, Goiás, Brazil. In the data acquisition phase, the GPR, direct-current (DC) resistivity and VLFEM profiles were obtained at the three locations in the area. Data were analyzed using commonly adopted processing workflows. The GPR results showed a well-defined lithology of the site based on the amplitude of the signal and radar typologies. On the other hand, the inverted resistivity cross-sections showed a three-layered stratigraphy, pathways of water infiltration and the weathered structures in carbonate (Bambui group). The interpretation of VLFEM as contours of current density resulted from Fraser and Karous–Hjelt filters, indicated the presence of conductive structures (high apparent current density) that might be linked to the weathered carbonate and other conductive and resistive anomalies associated with the water-filled and dry cavities (cave), respectively. The results encourage the integrated application of geophysical techniques such as the reconnaissance for further detailed characterization of the karst areas.pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-4155-6764pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-9448-1313pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-5158-1947pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-6184-4085pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-5048-0423pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0001-5930-199Xpt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-6586-469Xpt_BR
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