Geochemistry of natural chromium occurrence in a sandstone aquifer in Bauru Basin, Sao Paulo State, Brazil


Autoria(s): Bertolo, Reginaldo Antonio; Bourotte, Christine Laure Marie; Hirata, Ricardo; MARCOLAN, Leonardo; SRACEK, Ondra
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

20/10/2012

20/10/2012

2011

Resumo

Anomalous concentrations of Cr(VI) occur in groundwaters of the Adamantina Aquifer, in a large region in the western state of Sao Paulo, sometimes exceeding the potability limit (0.05 mg L(-1)). To identify the possible geochemical reactions responsible for the occurrence of Cr in groundwater in Urania, borehole rock samples were collected in order to carry out mineralogical and chemical analyses. In addition, multilevel monitoring wells were installed and groundwater samples were analyzed. Analyses of the borehole rock samples show the occurrence of a geochemical anomaly of Cr in the quartzose sandstones (average concentrations of 221 ppm). Chrome-diopside is one of the main minerals contributing to this anomaly, having an average Cr content of 1505 ppm. Sequential extraction experiments indicated weakly adsorbed Cr in the order of 0.54 ppm, and this quantity is enough to provide the Cr concentrations observed in groundwater. Groundwaters from the monitoring wells proved to be stratified, with the highest concentrations of Cr(VI) (0.13 mg L(-1)) being associated with high redox and pH values (over 10) and high concentrations of Na. Geochemical reactions that may explain the release of Cr from the solid phase to groundwater involve the release of Cr(III) from minerals (like chrome-diopside and Cr-Fe hydroxide), followed by oxidation of Cr(III) to Cr(VI), probably related to the reduction of Mn oxides present in the aquifer. Then cation exchange occurs and dissolution of carbonates which increases the pH of groundwater, resulting in the desorption and mobilization of Cr(VI) into groundwater. (C) 2011 Elsevier Ltd. All rights reserved.

FAPESP[97/13879-6]

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

FAPESP[98/15340-0]

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

FAPESP[05/60502-3]

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

CNPq[154492/2006-0]

Identificador

APPLIED GEOCHEMISTRY, v.26, n.8, p.1353-1363, 2011

0883-2927

http://producao.usp.br/handle/BDPI/30309

10.1016/j.apgeochem.2011.05.009

http://dx.doi.org/10.1016/j.apgeochem.2011.05.009

Idioma(s)

eng

Publicador

PERGAMON-ELSEVIER SCIENCE LTD

Relação

Applied Geochemistry

Direitos

restrictedAccess

Copyright PERGAMON-ELSEVIER SCIENCE LTD

Palavras-Chave #WESTERN MOJAVE DESERT #HEXAVALENT CHROMIUM #SEQUENTIAL EXTRACTION #TRACE-ELEMENTS #OXIDATION #MANGANESE #SOILS #GROUNDWATER #CALIFORNIA #CR(III) #Geochemistry & Geophysics
Tipo

article

original article

publishedVersion