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Comparative analyzes among electrical resistivity tomography arrays in the characterization of flow structure in free aquifer

dc.contributor.authorMoreira, Cesar Augusto [UNESP]
dc.contributor.authorLapola, Marcelo Montenegro [UNESP]
dc.contributor.authorCarrara, Alan [UNESP]
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2018-11-26T16:32:26Z
dc.date.available2018-11-26T16:32:26Z
dc.date.issued2016-04-01
dc.description.abstractThis paper makes a comparative analysis between the Dipole-dipole, Wenner and Schlumberger arrays through electric resistivity tomography (ERT), about the sensitivity and resolution in the spatial characterization of infiltrating pollutants in septic tank and cone of depression in supply well, both contained in unconfined aquifer. Data acquisition consisted of electrical resistivity readings using five parallel lines with 105m long, electrode spacing and lines of 5m. The data from each line were subjected to 2D inversion and then interpolated to generate 3D blocks, which were extracted from a fixed resistivity isosurface (620 Omega.m), which enabled the modeling of volumes related to the flow structures. The results for the Dipole-dipole array allowed the modeling of the cylindrical structure associated to the supply well, and an isosurface deformation associated to the septic tank, but did not allow the modeling of the plume. The data for the Schlumberger array cannot allow for the cone recognition, but resulted in a drop shape model, associated to the septic tank and similar to a contamination plume. The Wenner array resulted in a model with structure in elongated keel format associated to the cone of depression, and another that is similar to the drop shape model, also associated to the septic tank. The comparative analysis shows that the Dipole-dipole array is recommended in works of modeling vertically integrated three-dimensional structures of high resistivity in the saturated zone. The Wenner and Schlumberger arrays are recommended for modeling vertically integrated three-dimensional structures of low resistivity in unsaturated zone, with emphasis on the Schlumberger array.en
dc.description.affiliationUniv Estadual Paulista, UNESP, Dept Appl Geol, Rio Claro Campus 24-A Ave,1515,POB 178, BR-13506900 Sao Paulo, SP, Brazil
dc.description.affiliationUniv Estadual Paulista, UNESP, Grad Phys, Rio Claro Campus 24-A Ave,1515,POB 178, BR-13506900 Sao Paulo, SP, Brazil
dc.description.affiliationUniv Estadual Paulista, UNESP, Grad Environm Engn, Geosci & Exact Sci Inst, Rio Claro Campus 24-A Ave,1515,POB 178, BR-13506900 Sao Paulo, SP, Brazil
dc.description.affiliationUnespUniv Estadual Paulista, UNESP, Dept Appl Geol, Rio Claro Campus 24-A Ave,1515,POB 178, BR-13506900 Sao Paulo, SP, Brazil
dc.description.affiliationUnespUniv Estadual Paulista, UNESP, Grad Phys, Rio Claro Campus 24-A Ave,1515,POB 178, BR-13506900 Sao Paulo, SP, Brazil
dc.description.affiliationUnespUniv Estadual Paulista, UNESP, Grad Environm Engn, Geosci & Exact Sci Inst, Rio Claro Campus 24-A Ave,1515,POB 178, BR-13506900 Sao Paulo, SP, Brazil
dc.format.extent119-129
dc.identifier.citationGeofisica Internacional. Mexico: Inst Geophysics Unam, v. 55, n. 2, p. 119-129, 2016.
dc.identifier.issn0016-7169
dc.identifier.lattes9086857312391080
dc.identifier.orcid0000-0002-6949-6679
dc.identifier.urihttp://hdl.handle.net/11449/161363
dc.identifier.wosWOS:000373316200003
dc.language.isoeng
dc.publisherInst Geophysics Unam
dc.relation.ispartofGeofisica Internacional
dc.relation.ispartofsjr0,312
dc.rights.accessRightsAcesso restrito
dc.sourceWeb of Science
dc.subjectDipole-dipole
dc.subjectSchlumberger
dc.subjectWenner
dc.subjectcontamination plume
dc.subjectcone of depression
dc.titleComparative analyzes among electrical resistivity tomography arrays in the characterization of flow structure in free aquiferen
dc.typeArtigo
dcterms.rightsHolderInst Geophysics Unam
unesp.author.lattes9086857312391080[1]
unesp.author.orcid0000-0002-6949-6679[1]
unesp.campusUniversidade Estadual Paulista (Unesp), Instituto de Geociências e Ciências Exatas, Rio Claropt
unesp.departmentFísica - IGCEpt
unesp.departmentGeologia Aplicada - IGCEpt

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