Journal of Environmental Hydrology
ISSN 1058-3912


Electronic Journal of the International Association for Environmental Hydrology

JEH Volume 19 (2011), Paper 17    Posted July 29, 2011
FLUORIDES IN THE PHREATIC AQUIFER OF THE LOESS PLAIN, CORDOBA PROVINCE, ARGENTINA

M. Blarasin1
A. Cabrera1
F. Hildmann2
E. Matteoda1
F. Becher3
J. Giuliano3
L. Maldonado4

1Dpto. Geología, Univ. Nacional de Río Cuarto, Argentina
2Dpto. Geografía, Univ. Nacional de Río Cuarto, Argentina
3CONICET, Argentina
4FONCyT, Argentina


ABSTRACT
The natural occurrence of excessive quantities of dissolved fluorides in water has affected people’s health for centuries. The aim of this paper is to assess fluoride contents and the geochemical environment that determines their presence and distribution in the unconfined aquifer in Malena town and its surrounding rural area (Córdoba, Argentina). The area presents two hydrogeologic environments: one composed by loess sediments and another where fluvial and aeolian sediments are interstratified. The F - levels range between 1.53 mg/L and 8.75 mg/L, the lowest contents being related to paleochannels. The statistical multivariate analysis (cluster and principal components) showed two groups: one is composed of the majority of main ions, with a high correlation nucleus formed by electrical conductivity and Na+, which explains water mineralization. The other group is composed by F - - As - pH - HCO3 - , which validates the affinity of these two trace elements to high pH, alkaline solutions. The negative high correlation (R -0.82) found between F - and Ca2+ corroborates that in groundwater with low levels of Ca2+, high concentrations of F - in solution are stable. The results show the geomorphological and lithological control over the dissolved F - levels. The highest levels of F - are related to: textural characteristics of the aquifer in the aeolian environment (very fine sands-silts) that generate slow groundwater flow; the mineralogy (volcanic glass, amphibole, pyroxene, apatite, all possible fluorine sources); and the bicarbonate sodium groundwater type and high pH of the solution (>7.80). Numerous cases of dental fluorosis were found in children, youngsters, and adults from the study region.


Reference: M. Blarasin, A. Cabrera, F. Hildmann, E. Matteoda, F. Becher, J. Giuliano, and L. Maldonado. 2011. Fluorides in the phreatic aquifer of the loess plain, Cordoba Province, Argentina. Journal of Environmental Hydrology, Vol. 19, Paper 17.
CONTACT:
M. Blarasin
Univ. Nacional de Río Cuarto
Ruta 36 km 601
Río Cuarto
Argentina

E-mail: mblarasin@exa.unrc.edu.ar



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