Correlating soil porosity and respective geological unit in Paraíba do sul Valley, Brazil: a geostatistical methodology proposal

dc.contributorUniversidade Estadual Paulista (Unesp)
dc.creatorCamarinha, Pedro Ivo Mioni [UNESP]
dc.creatorBernardes, George de Paula [UNESP]
dc.creatorTrannin, Isabel Cristina de Barros [UNESP]
dc.creatorSimoes, Silvio Jorge Coelho [UNESP]
dc.date2016-03-02T12:59:38Z
dc.date2016-03-02T12:59:38Z
dc.date2012
dc.date.accessioned2023-09-12T08:39:10Z
dc.date.available2023-09-12T08:39:10Z
dc.identifierhttp://www.abms.com.br/links/soilsandrocks/solos-e-rochas-vol35-n3.pdf
dc.identifierSoils & Rocks, v. 35, n. 3, p. 209-222, 2012.
dc.identifier1980-9743
dc.identifierhttp://hdl.handle.net/11449/135069
dc.identifier0554631424547411
dc.identifier7371537941854293
dc.identifier3526553928214195
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8784307
dc.descriptionThis manuscript aims proposing a methodology for correlating soil porosity to the respective geological units using geostatistical analysis techniques, including interpolation data by kriging. The site studied was in Lorena municipality, Paraíba do Sul Valley, southeastern Brazil. Specifically all studies were carried out within an area of 12 km2 located at Santa Edwirges farm. The database comprehended 41 soil samples taken at different geological and geomorphologic units at three different depths: surface, 50 cm and 100 cm depth. The geostatistical analyses results were correlated to a geological mapping specifically elaborated for the site. This mapping accounts for two different geological formations and a geological contact characterized by a shearing zone. The results indicate the existence of a significant relationship between the soil porosity and the respective geological units. The studies revealed that the residual soils from weathered granitic rocks tend to have higher porosities than the residual soils from weathered biotite gneiss rocks, while the soil porosity within the shearing zone is relatively un-sensitive to the respective geological formation. The spatial patterns observed were efficient to evaluate the relationship between the soil porosity, geology unit and the and geomorphology showing a good potential for correlating with others soil properties such as hydraulic conductivity, soil water retention curves and erosion potentials.
dc.descriptionUniversidade Estadual Paulista Júlio de Mesquita Filho, Departamento de Projetos e Construção Civil, Faculdade de Engenharia de Guaratinguetá, Guaratinguetá, Avenida Ariberto Pereira da Cunha, 333, Pedregulho, CEP 12516410, SP, Brasil
dc.descriptionUniversidade Estadual Paulista Júlio de Mesquita Filho, Departamento de Projetos e Construção Civil, Faculdade de Engenharia de Guaratinguetá, Guaratinguetá, Avenida Ariberto Pereira da Cunha, 333, Pedregulho, CEP 12516410, SP, Brasil
dc.format209-222
dc.languageeng
dc.relationSoils & Rocks
dc.relation0,133
dc.rightsAcesso restrito
dc.sourceCurrículo Lattes
dc.subjectGeostatistic
dc.subjectSampling
dc.subjectError prediction
dc.subjectPorosity map
dc.titleCorrelating soil porosity and respective geological unit in Paraíba do sul Valley, Brazil: a geostatistical methodology proposal
dc.typeArtigo


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