Fluoride content in drinking water supply in Sao Miguel volcanic island (Azores, Portugal)

被引:32
作者
Cordeiro, S. [2 ]
Coutinho, R. [1 ]
Cruz, J. V. [1 ]
机构
[1] Univ Azores, Dept Geosci, Ctr Volcanol & Geol Hazards Assessment, CVARG, P-9501801 Ponta Delgada, Portugal
[2] Camara Municipal Ponta Delgada, Municipal Serv Water & Sanitat, SMAS, P-9500246 Ponta Delgada, Portugal
关键词
Island hydrology; Volcanic aquifers; Water quality; Fluoride; Azores; FURNAS VOLCANO; GROUNDWATER; CHEMISTRY; FLUOROSIS; FRAMEWORK; POLLUTION; HAZARDS; SURFACE; ORIGIN; RIFT;
D O I
10.1016/j.scitotenv.2012.05.070
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
High fluoride contents in the water supply of the city of Ponta Delgada, located in the volcanic island of Sao Miguel (Azores, Portugal) have been reported. Dental fluorosis in Sao Miguel has been identified and described in several medical surveys. The water supply in Ponta Delgada consists entirely of groundwater. A study was carried out in order to characterize the natural F-pollution of a group of springs (30) and wells (3), that are associated to active central volcanoes of a trachytic nature. Two springs known for their high content in fluoride were sampled, both located in the central volcano of Furnas. The sampled waters are cold, ranging from slightly acidic to slightly alkaline (pH range 6.53-7.60), exhibiting a low electrical conductivity (springs range 87-502 mu S/cm: wells range 237-1761 mu S/cm), and are mainly from the Na-HCO3. Na-HCO3-Cl and Na-Cl-HCO3 water types. Results suggest two main trends of geochemical evolution: silicate weathering, enhanced by CO2 dilution, and seawater spraying. Fluoride contents range between 0.17 mg/L and 2 mg/L, and no seasonal variations were detected. Results in the sources of the water supply system are lower than those of the Furnas volcano, which reach 5.09 mg F/L, demonstrating the effect of F-rich gaseous emanations in this area. Instead, the higher fluoride contents in the water supply are mainly due to silicate weathering in aquifers made of more evolved volcanic rocks. (C) 2012 Elsevier B.V. All rights reserved.
引用
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页码:23 / 36
页数:14
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