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Tritium Distribution in Soil in the Area of 'Atomic' Lake near the Semipalatinsk Test Site

机译:亚麻岛附近“原子”湖区土壤中土壤分布

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摘要

Data on concentrations and distribution of tritium in soils of the "Atomic" Lake excavation explosion area of Semipalatinsk Nuclear Test Site (Kazakhstan, East Kazakhstan oblast) are discussed. The concentrations of tritium in surface soil horizons and in soil profiles have been determined in the bulk soil samples and in different particle-size fractions. Tritium concentration in soils reaches 240 000 Bq/kg. A correlation has been found between tritium and europium concentrations in soils. Presumably, tritium formation is controlled by two mechanisms. One of them is the neutron activation process, i.e., nuclear reactions with lithium, boron, and nitrogen isotopes present in the soil; the other mechanism is related to the capture of tritium that was initially in the charge of mineral particles formed upon condensation from the red-hot explosion zone.
机译:讨论了“原子”湖挖掘爆炸区土壤浓度和分布的数据,讨论了亚马逊人克核试验网站(哈萨克斯坦,东哈萨克斯坦州)。 在散装土壤样品和不同的粒度级分中,确定了表面土壤视野和土壤曲线中的氚的浓度。 土壤中的氚浓度达到240 000 bq / kg。 在土壤中氚和铕浓度之间发现了相关性。 据推测,氚形成由两种机制控制。 其中一个是中子活化过程,即用锂,硼和土壤中存在的核反应; 其他机制与捕获氚最初是在从红热爆炸区的冷凝中形成的矿物颗粒的捕获有关。

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