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Estudo do nivel piezometrico por analise geoestatistica

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dc.contributor.authorSturaro, J. R.
dc.contributor.authorLandim, P. M B
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-27T05:11:10Z
dc.date.available2014-05-27T05:11:10Z
dc.date.issued1988-12-01
dc.description.abstract160 groundwater bores in the Ribeirao Preto region were used to study the behaviour of the piezometric surface of the Botucatu Formation aquifer by geostatistical methodology. The semi-variogram showed the following results: nugget = 50 m2; sill = 450 m2 and range = 4.5 km. The piezometric surface, obtained by punctual kriging in a 100 x 100 knot grid, revealed two lowered zones: one in a southwest to north-northeastern trend, indicating the groundwater flow north toward the Rio Pardo; and the other in the central part due to the high concentration of holes in the urban region of Ribeirao Preto city. -from English summaryen
dc.format.extent201-210
dc.identifier.citationGeociencas, v. 7, p. 201-210.
dc.identifier.lattes0131652346152784
dc.identifier.lattes7206664999934534
dc.identifier.scopus2-s2.0-0024253260
dc.identifier.urihttp://hdl.handle.net/11449/63879
dc.language.isopor
dc.relation.ispartofGeociencas
dc.rights.accessRightsAcesso restrito
dc.sourceScopus
dc.subjectgeostatistical method
dc.subjectgroundwater flow
dc.subjectpiezometric surface
dc.subjectBrazil, Rio Pardo
dc.titleEstudo do nivel piezometrico por analise geoestatisticapt
dc.title.alternativePiezometric surface study by geostatistics methodologyen
dc.typeArtigo
dspace.entity.typePublication
unesp.author.lattes0131652346152784
unesp.author.lattes7206664999934534
unesp.campusUniversidade Estadual Paulista (UNESP), Instituto de Geociências e Ciências Exatas, Rio Claropt
unesp.departmentGeologia Aplicada - IGCEpt

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Rio Claro - IGCE - Instituto de Geociências e Ciências Exatas