STRUTURAL CONTROLS ON BARREIRAS AQUIFER - PIRANGI

The regional structuring, outlined by the overall preferential directions NW, NE and W-W, revealed as exerting strong influence on a diverse array of aspects of the Barreiras Aquifer context. These influences were attested by several aspects, based on the analysis of geological, hydrogeological and...

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Published inÁguas subterrâneas (São Paulo, Brazil) Vol. 20; no. 1
Main Authors Leandson Roberto Fernandes de Lucena, Ernani Francisco da Rosa Filho, Eduardo Chemas Hindi
Format Journal Article
LanguageEnglish
Published Associação Brasileira de Águas Subterrâneas 01.11.2006
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Abstract The regional structuring, outlined by the overall preferential directions NW, NE and W-W, revealed as exerting strong influence on a diverse array of aspects of the Barreiras Aquifer context. These influences were attested by several aspects, based on the analysis of geological, hydrogeological and geo-electrical data, notably on the aquifer geometry, as witnessed by sudden variations of saturated thicknesses caused by faulting. Quantitative configuration of major transmissivities, resulting from local increase of these saturated thicknesses, was evidenced through statistical correlations carried out between exploitation flows and saturated thicknesses or extensions of filtering sections, where correlation coefficients up to 0.79 were obtained. The remaining influences of the structural framework of the Barreiras Aquifer include from a control of the underground flow to evidences on the potenciometric map, as expressed by sudden changes in spacing or inflexion of the equipotentials. In addition, quantification of permanent reserves was carried out in the area of the Pirangi River basin, taking into consideration variations in the aquifer geometry resulting from local structuring. Other aspects of regional implication were also addressed, among them the probability that some coastal line faults, particularly the distensional and transtensional ones, be associated to the formation of saltwater wedges.
AbstractList The regional structuring, outlined by the overall preferential directions NW, NE and W-W, revealed as exerting strong influence on a diverse array of aspects of the Barreiras Aquifer context. These influences were attested by several aspects, based on the analysis of geological, hydrogeological and geo-electrical data, notably on the aquifer geometry, as witnessed by sudden variations of saturated thicknesses caused by faulting. Quantitative configuration of major transmissivities, resulting from local increase of these saturated thicknesses, was evidenced through statistical correlations carried out between exploitation flows and saturated thicknesses or extensions of filtering sections, where correlation coefficients up to 0.79 were obtained. The remaining influences of the structural framework of the Barreiras Aquifer include from a control of the underground flow to evidences on the potenciometric map, as expressed by sudden changes in spacing or inflexion of the equipotentials. In addition, quantification of permanent reserves was carried out in the area of the Pirangi River basin, taking into consideration variations in the aquifer geometry resulting from local structuring. Other aspects of regional implication were also addressed, among them the probability that some coastal line faults, particularly the distensional and transtensional ones, be associated to the formation of saltwater wedges.
Author Leandson Roberto Fernandes de Lucena
Ernani Francisco da Rosa Filho
Eduardo Chemas Hindi
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Title STRUTURAL CONTROLS ON BARREIRAS AQUIFER - PIRANGI
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