2021
DOI: 10.1007/s12665-021-09527-4
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Source of 226Ra in Ramsar spring water, Iran: implication of water–rock interaction and stable isotopes

Abstract: This study was carried out primarily to understand the hydrogeochemical processes controlling the 226 Ra anomalies in Ramsar area. Analyses revealed two types of water; 1) non-thermal Ca-HCO 3 type and 2) thermal Na-Cl type, mainly of meteoric and hydrothermal origin, respectively. Non-thermal springs have higher concentrations of U due to silicate weathering. Thermal springs are characterized by high concentrations of 226 Ra, As, Fe, Li, Cs, Rb, Sr, Ba, B, Br -, F -, NO 3 -, PO 4 3and SiO 2 resulting from hig… Show more

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