Please use this identifier to cite or link to this item: http://hdl.handle.net/1843/52111
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dc.creatorLucas de Queiroz Sallespt_BR
dc.creatorPaulo Henrique Ferreira Galvãopt_BR
dc.creatorLuiz Rogério Bastos Lealpt_BR
dc.creatorRicardo Galeno Fraga de Araujo Pereirapt_BR
dc.creatorCarlos Gleidson Campos da Purificaçãopt_BR
dc.creatorFernando Verassani Laureanopt_BR
dc.date.accessioned2023-04-17T22:29:37Z-
dc.date.available2023-04-17T22:29:37Z-
dc.date.issued2018-
dc.citation.volume77pt_BR
dc.citation.issue16pt_BR
dc.citation.spage1pt_BR
dc.citation.epage11pt_BR
dc.identifier.doihttps://doi.org/10.1007/s12665-018-7769-8pt_BR
dc.identifier.issn1866-6280pt_BR
dc.identifier.urihttp://hdl.handle.net/1843/52111-
dc.description.resumoThe morphological evolution of the karstic systems is associated with a set of physical and chemical processes, triggered by the dissolution of the rocks, related to percolation of groundwater and surface water, which consequently open underground voids and carve out peculiar forms of relief. Due to environmental and geotechnical aspects, this system is naturally more fragile and vulnerable than other natural systems and, therefore, has increasingly received the attention of the scientific community over the past decades. The objective of the study was to delimit zones with varying degrees of susceptibility for collapses and subsidence of sinkholes in the municipality of Iraquara, Chapada Diamantina (BA), Brazil, and to understand their geological and morphological determinant factors. Geological data, karst phenomenon map, and visual analysis in the field were used to categorize zones with different types of susceptibilities to the nucleation of new sinkholes based on a Hazard Index. This index was defined from the sum of geological hazard factors, lineament density, and sinkhole density. The areas that presented the highest susceptibility for terrain collapse and subsidence corresponded to regions where carbon‑ ate rocks outcrop, with high density of photolineaments and 2.62 sinkholes/km2. Processes associated with terrain collapse and subsidence in karst areas consisted of a combination of various factors, hindering precise predictions. However, zones of different types of susceptibilities to terrain collapse and subsidence can be delimited when the relationships between these processes and their factors are understood. The Hazard Index proposed does not provide quantitative values for the probability of hazard susceptibility, but rather indicates areas that are more susceptible to terrain subsidence and collapse.pt_BR
dc.languageporpt_BR
dc.publisherUniversidade Federal de Minas Geraispt_BR
dc.publisher.countryBrasilpt_BR
dc.publisher.departmentIGC - DEPARTAMENTO DE GEOLOGIApt_BR
dc.publisher.initialsUFMGpt_BR
dc.relation.ispartofEnvironmental Earth Sciencespt_BR
dc.rightsAcesso Abertopt_BR
dc.subjectKarstpt_BR
dc.subjectCarbonate rockspt_BR
dc.subjectChapada Diamantinapt_BR
dc.subjectCollapse and subsidencept_BR
dc.subjectBrazilpt_BR
dc.subject.otherBrasilpt_BR
dc.subject.otherRochas carbonáticaspt_BR
dc.titleEvaluation of susceptibility for terrain collapse and subsidence in karst areas, municipality of Iraquara, Chapada Diamantina (BA), Brazilpt_BR
dc.typeArtigo de Periódicopt_BR
dc.url.externahttps://link.springer.com/article/10.1007/s12665-018-7769-8pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-7912-3323pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0001-7183-0368pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0003-4015-3370pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0003-3913-3735pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0001-5268-3999pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0003-0674-4070pt_BR
Appears in Collections:Artigo de Periódico



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