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首页> 外文期刊>Applied radiation and isotopes: including data, instrumentation and methods for use in agriculture, industry and medicine >Uranium disequilibrium as a hydrological aid in studying the salinization processes in the Southeastern Coastal Plain of Israel.
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Uranium disequilibrium as a hydrological aid in studying the salinization processes in the Southeastern Coastal Plain of Israel.

机译:铀不平衡作为水文研究,用于研究以色列东南沿海平原的盐碱化过程。

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摘要

Saline waters, of unknown origin, have been encountered in the basal portions of the phreatic Coastal Plain aquifer of Israel. (234)U/(238)U disequilibrium was used to trace their origin to the evaporate layers within the Saqiye aquiclude, the most saline, and the warmest (up to 42 degrees C) waters are also those that have the highest uranium concentrations combined with low (234)U/(238)U activity ratios, derived as the ascending brines traverse underlying uranium-rich Senonian phosphorites, in secular equilibrium along fault conduits.
机译:在以色列的水下沿海平原含水层的基部遇到了来源不明的盐水。 (234)U /(238)U不平衡用于追踪其起源于萨奇耶含水层内的蒸发层,盐分最多,最温暖(最高42摄氏度)的水也是铀浓度最高的水(234)U /(238)U活度比低,是由于上升的盐水沿断层导管在世俗平衡中穿越了富铀的Senonian亚磷矿。

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