The geochemical facies of Hungarian thermal waters were the object of this study. Samples were separated into groups by relative ages (δ 18 O values). Mature and immature subgroups were formed on the basis of dissolved (semi)volatile organic compounds. The oldest (connate) waters form one group with a small number of samples. The subgroups containing different small molecular-sized soluble aromatics differ sharply in their chemical features (sodium, hydrogen carbonate, iodine, ammonium etc. content). The origin of the organic matter may differ in the subgroups as inferred by their different δ 18 O values and ten times greater halogen contents.Our results show that the decomposition of organic matter produces small molecular-sized aromatic compounds and also influences the amounts of inorganic components in thermal waters, through the increase of feldspar hydrolysis and carbonate dissolution.Key words: hydrogeochemistry, thermal waters, δ 18 O, organic matter, aromatic compounds
IntroductionThermal waters in the Pannonian Basin may contain high amounts of dissolved organic material.Humic substances and aromatic content of some tens of Hungarian thermal waters have been described qualitatively by Kárpáti et al. (1995Kárpáti et al. ( , 1996aKárpáti et al. ( ,b, 1999 Central European Geology, Vol. 52/3-4, pp. 269-285 (2009) DOI: 10.1556/CEuGeol.52.2009 Interaction
Magdolna HetényiUniversity of Szeged, Szeged According to these authors, the concentration of humic substances usually decreases and those of the aromatic compounds increases with increasing water temperature. The appearance of the different homologue series is temperaturedependent. Aromatic hydrocarbons appeared at a threshold temperature of 80°C, followed by phenols at ~90 °C, and in the hottest waters (>90 °C) fatty acids were identified. In the homologue series demethylation was associated with increasing temperature, leading to a decrease of the relative abundances of the higher molecular-sized members and a clear predominance of the compounds containing less carbon atoms.Recently Varsányi et al. (2002) discussed quantitatively the contribution of humic substances, acetate, propionate and aromatic compounds to organic material dissolved in thermal waters of SE Hungary, mostly south of the Kõrös River. Vetõ et al. (2004a) reported concentrations and isotopic composition of methane in thermal waters of SE Hungary and discussed pathways of bacterial methanogenesis.In an ongoing project, we are focusing on aromatic compounds but thermal waters taken from north of the Kõrös River and those from northern and southwestern parts of the country are also studied. In this communication we present the chemical and isotopic signatures of 38 thermal water samples. More than 500 aromatic compounds (PAHs, phenols, heteroaromatics) and relatively long carbon-chain fatty acids were found and identified in half of them. The water samples were grouped according to their oxygen isotope composition (δ 18 O value in ‰ VSMOW). The difference in the δ 18 O value can b...