Estudo do nivel piezometrico por analise geoestatistica

dc.contributorUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-27T05:11:10Z
dc.date.accessioned2022-10-05T17:24:29Z
dc.date.available2014-05-27T05:11:10Z
dc.date.available2022-10-05T17:24:29Z
dc.date.created2014-05-27T05:11:10Z
dc.date.issued1988-12-01
dc.identifierGeociencas, v. 7, p. 201-210.
dc.identifierhttp://hdl.handle.net/11449/63879
dc.identifier2-s2.0-0024253260
dc.identifier0131652346152784
dc.identifier7206664999934534
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3914043
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 summary
dc.languagepor
dc.relationGeociencas
dc.rightsAcesso restrito
dc.sourceScopus
dc.subjectgeostatistical method
dc.subjectgroundwater flow
dc.subjectpiezometric surface
dc.subjectBrazil, Rio Pardo
dc.titleEstudo do nivel piezometrico por analise geoestatistica
dc.typeArtigo


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