Hydrostratigraphy of the Bauru Group in São Paulo State, Brazil
Geophysical logs, ditch samples and cores of water wells drilled in São Paulo State, Brazil, allowed the identification and correlation of different hydrostratigraphics units and the evaluation of hydraulic potential of the Bauru Aquifer System (Mesozoic of Paraná Basin). Identified units were Caiuá...
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| Format: | Article |
| Language: | English |
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Associação Brasileira de Águas Subterrâneas
2005-06-01
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| Series: | Revista Águas Subterrâneas |
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| Online Access: | https://aguassubterraneas.abas.org/asubterraneas/article/view/8225 |
| _version_ | 1818153107273547776 |
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| author | Flávio de Paula e Silva Chang Hung Kiang Maria Rita Caetano-Chang |
| author_facet | Flávio de Paula e Silva Chang Hung Kiang Maria Rita Caetano-Chang |
| author_sort | Flávio de Paula e Silva |
| collection | DOAJ |
| description | Geophysical logs, ditch samples and cores of water wells drilled in São Paulo State, Brazil, allowed the identification and correlation of different hydrostratigraphics units and the evaluation of hydraulic potential of the Bauru Aquifer System (Mesozoic of Paraná Basin). Identified units were Caiuá, Santo Anastácio, Birigüi, Adamantina and Marília aquifers, and Pirapozinho and Araçatuba aquitards. The aquifer units were differentiated in terms of isoliths of relative apparent permeability, as very permeable and moderately permeable. The isolith maps contemplate directly the most favorable potential areas to water production. The isoliths of high apparent permeability sandstone of Caiuá and Santo Anastácio aquifers showed larger concentrated values in the southwest occurrence area of the Bauru Group. The areas with best hydraulic potential for Birigüi Aquifer are concentrated on elongated strip along the center of his occurrence area. Adamantina Aquifer showed moderate and high isoliths of apparent permeability distributed in parallel strips to south and north of Tietê River. Resistivity logs of Marília Aquifer contemplate mainly the intense carbonatic cementation of the lithologies, hindering the distinction between high and moderate apparent permeability of its sandstones. The static water storage of the Bauru Aquifer System is about 1.600 km³, distributed by the Caiuá (150 km³), Santo Anastácio (560 km³), Birigüi (15 km³), Adamantina (810 km³) and Marília (80 km³) aquifers. |
| first_indexed | 2024-12-11T14:05:21Z |
| format | Article |
| id | doaj.art-f97fcc810f524f848db8435d50ebaf1d |
| institution | Directory Open Access Journal |
| issn | 0101-7004 2179-9784 |
| language | English |
| last_indexed | 2024-12-11T14:05:21Z |
| publishDate | 2005-06-01 |
| publisher | Associação Brasileira de Águas Subterrâneas |
| record_format | Article |
| series | Revista Águas Subterrâneas |
| spelling | doaj.art-f97fcc810f524f848db8435d50ebaf1d2022-12-22T01:03:41ZengAssociação Brasileira de Águas SubterrâneasRevista Águas Subterrâneas0101-70042179-97842005-06-0119210.14295/ras.v19i2.82255641Hydrostratigraphy of the Bauru Group in São Paulo State, BrazilFlávio de Paula e SilvaChang Hung KiangMaria Rita Caetano-ChangGeophysical logs, ditch samples and cores of water wells drilled in São Paulo State, Brazil, allowed the identification and correlation of different hydrostratigraphics units and the evaluation of hydraulic potential of the Bauru Aquifer System (Mesozoic of Paraná Basin). Identified units were Caiuá, Santo Anastácio, Birigüi, Adamantina and Marília aquifers, and Pirapozinho and Araçatuba aquitards. The aquifer units were differentiated in terms of isoliths of relative apparent permeability, as very permeable and moderately permeable. The isolith maps contemplate directly the most favorable potential areas to water production. The isoliths of high apparent permeability sandstone of Caiuá and Santo Anastácio aquifers showed larger concentrated values in the southwest occurrence area of the Bauru Group. The areas with best hydraulic potential for Birigüi Aquifer are concentrated on elongated strip along the center of his occurrence area. Adamantina Aquifer showed moderate and high isoliths of apparent permeability distributed in parallel strips to south and north of Tietê River. Resistivity logs of Marília Aquifer contemplate mainly the intense carbonatic cementation of the lithologies, hindering the distinction between high and moderate apparent permeability of its sandstones. The static water storage of the Bauru Aquifer System is about 1.600 km³, distributed by the Caiuá (150 km³), Santo Anastácio (560 km³), Birigüi (15 km³), Adamantina (810 km³) and Marília (80 km³) aquifers.https://aguassubterraneas.abas.org/asubterraneas/article/view/8225Aqüífero Bauruhidroestratigrafiaperfis geofísicos |
| spellingShingle | Flávio de Paula e Silva Chang Hung Kiang Maria Rita Caetano-Chang Hydrostratigraphy of the Bauru Group in São Paulo State, Brazil Revista Águas Subterrâneas Aqüífero Bauru hidroestratigrafia perfis geofísicos |
| title | Hydrostratigraphy of the Bauru Group in São Paulo State, Brazil |
| title_full | Hydrostratigraphy of the Bauru Group in São Paulo State, Brazil |
| title_fullStr | Hydrostratigraphy of the Bauru Group in São Paulo State, Brazil |
| title_full_unstemmed | Hydrostratigraphy of the Bauru Group in São Paulo State, Brazil |
| title_short | Hydrostratigraphy of the Bauru Group in São Paulo State, Brazil |
| title_sort | hydrostratigraphy of the bauru group in sao paulo state brazil |
| topic | Aqüífero Bauru hidroestratigrafia perfis geofísicos |
| url | https://aguassubterraneas.abas.org/asubterraneas/article/view/8225 |
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