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Characterization and disequilibrium cases of radioelements in some Syrian hot waters
The radioactive and physical characteristics of Syrian hot waters were studied. The concentration of uranium, its daughters and the ^sup 234^U/^sup 238^U-activity ratios in the hot waters were measured by gamma and alpha ray spectroscopy. The ^sup 234^U/^sup 238^U-activity ratios showed that uranium...
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Published in: | Environmental earth sciences 2003-05, Vol.44 (1), p.78-84 |
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description | The radioactive and physical characteristics of Syrian hot waters were studied. The concentration of uranium, its daughters and the ^sup 234^U/^sup 238^U-activity ratios in the hot waters were measured by gamma and alpha ray spectroscopy. The ^sup 234^U/^sup 238^U-activity ratios showed that uranium in Syrian hot waters are in an equilibrium state. Some anomalous observations of these ratios were explained by former leaching of the uranium from Cretaceous phosphates by underground water. Also, the results showed that the temperature of the studied hot waters was independent of the contained radioelements. The temperature of hot waters is explained by the passing of these waters near the hot spot or by the relationship between the geological deposit of the aquifer rocks and the waters rather than the contents of the radioelements.[PUBLICATION ABSTRACT] |
doi_str_mv | 10.1007/s00254-002-0737-2 |
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The concentration of uranium, its daughters and the ^sup 234^U/^sup 238^U-activity ratios in the hot waters were measured by gamma and alpha ray spectroscopy. The ^sup 234^U/^sup 238^U-activity ratios showed that uranium in Syrian hot waters are in an equilibrium state. Some anomalous observations of these ratios were explained by former leaching of the uranium from Cretaceous phosphates by underground water. Also, the results showed that the temperature of the studied hot waters was independent of the contained radioelements. 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The concentration of uranium, its daughters and the ^sup 234^U/^sup 238^U-activity ratios in the hot waters were measured by gamma and alpha ray spectroscopy. The ^sup 234^U/^sup 238^U-activity ratios showed that uranium in Syrian hot waters are in an equilibrium state. Some anomalous observations of these ratios were explained by former leaching of the uranium from Cretaceous phosphates by underground water. Also, the results showed that the temperature of the studied hot waters was independent of the contained radioelements. The temperature of hot waters is explained by the passing of these waters near the hot spot or by the relationship between the geological deposit of the aquifer rocks and the waters rather than the contents of the radioelements.[PUBLICATION ABSTRACT]</description><subject>Aquifers</subject><subject>Cretaceous</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. 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subjects | Aquifers Cretaceous Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Exact sciences and technology Freshwater Geochemistry Groundwater Hydrogeology Hydrology. Hydrogeology Isotope geochemistry Isotope geochemistry. Geochronology Leaching Pollution, environment geology Radioactivity Uranium |
title | Characterization and disequilibrium cases of radioelements in some Syrian hot waters |
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