Natural occurrence of hexavalent chromium in a sedimentary aquifer in Urania, State of Sao Paulo, Brazil

被引:44
作者
Bourotte, Christine [1 ]
Bertolo, Reginaldo [1 ]
Almodovar, Marta [2 ]
Hirata, Ricardo [1 ]
机构
[1] Univ Sao Paulo, Inst Geociencias, BR-05508080 Sao Paulo, Brazil
[2] Companhia Tecnol Saneamento Ambiental Estado Sao, CETESB, BR-05459900 Sao Paulo, Brazil
来源
ANAIS DA ACADEMIA BRASILEIRA DE CIENCIAS | 2009年 / 81卷 / 02期
基金
巴西圣保罗研究基金会;
关键词
chromium; groundwater; aquifer; natural contamination; OXIDATION; GROUNDWATER; ADSORPTION; CR(III); SOILS; WATER;
D O I
10.1590/S0001-37652009000200009
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Anomalous concentrations of hexavalent chromium have been detected in groundwater of the Adamantina Aquifer in at least 54 municipalities located in the northwestern region of the State of Sao Paulo, southeast Brazil, occasionally exceeding the permitted limit for human consumption (0.05 mg.L-1). An investigation was conducted in the municipality of Urania, where the highest concentrations of chromium were detected regionally. It was defined that the origin of this contamination is natural, since high concentrations of chromium were detected in aquifer sandstones (average of 221 ppm) and also in pyroxenes (6000 ppm), one of the main heavy minerals found in the sediments. Besides, no other possible diffuse or point sources of contamination were observed in the study area. Stratification of groundwater quality was observed and the highest concentrations of Cr6+ were detected at the base of the aquifer (0.12 mg.L-1), where groundwater shows elevated values for redox potential (472.5 mV) and pH (8.61). The origin of Cr6+ in water may be associated with the weathering of pyroxene (augite), followed by the oxidation of Cr3+ by manganese oxides. The highest concentrations of Cr6+ are probably related to desorption reactions, due to the anomalous alkaline pH found in groundwater at the base of the aquifer.
引用
收藏
页码:227 / 242
页数:16
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