Camarinha, Pedro Ivo Mioni [UNESP]Bernardes, George de Paula [UNESP]Trannin, Isabel Cristina de Barros [UNESP]Simoes, Silvio Jorge Coelho [UNESP]2016-03-022016-03-022012Soils & Rocks, v. 35, n. 3, p. 209-222, 2012.1980-9743http://hdl.handle.net/11449/135069This 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.209-222engGeostatisticSamplingError predictionPorosity mapArtigoAcesso restrito055463142454741173715379418542933526553928214195