Acid extraction of radionuclides from soil samples using autoclave decomposition

S. Salmenbayev, Ardak M. Miratova, R. Kenzhebaev
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Abstract

The specifics of the nuclear tests carried out on the territory of the former Semipalatinsk test site (STS) led to the emergence of various sites that differ in levels of radioactive contamination and radionuclide composition. This also led to a significant difference in the solubility of radioactive particles. Traditionally, the “Experimental Field” testing ground was characterized by the presence of sparingly soluble, vitrified particles, which was determined by the features inherent in ground tests of nuclear weapons, namely, the interaction of the high-temperature explosion region with soil particles. The presence of such sparingly soluble particles in the soil cover makes it impossible to use 6–8 М HCl and 7–8 М HNO 3 solutions which are most often used radiochemical analysis to determine the content of 90Sr and 239+240Pu. This paper considers methods for the acid extraction of anthropogenic radionuclides from soils of the STS using autoclaving. The aim of the research is to develop a method for the acid extraction of anthropogenic radionuclides from enlarged soil samples using autoclave decomposition. A blank soil sample was used to determine the optimal autoclave decomposition parameters; to test the acid extraction method, a soil sample was taken from the territory of the “experimental field” testing ground. The radionuclide 137Cs has been used as the most optimal indicator of acid extraction due to its strong fixation on clay and mineral soil particles and ease of detection by the gamma radiation. Autoclave decomposition has been carried out by dissolving the studied samples in a mixture of mineral acids (HCl, HNO3, HF, H2SO4). The specific activity of radionuclide has been determined on a BE3830 gamma spectrometer with a high-purity germanium detector (Canberra, USA), the amount of undecomposed soil residue has been determined gravimetrically (PA214C analytical balance, Ohaus, USA). The data obtained indicate that the most complete extraction of 137Cs occurs when using concentrated HF solutions (individually or in a mixture with other mineral acids). The degree of extraction of 137Cs varied from 85 to 100%. The worst results have been shown by the use of a mixture of acids 3HCl:HNO 3. In this case the degree of extraction of 137Cs did not exceed 20%. The efficiency of decomposition of soil samples weighing 10 g with a concentrated solution of HF at a temperature of 120 to 160 ºC was ≥95%.
用高压灭菌器分解从土壤样品中酸提取放射性核素
在前塞米巴拉金斯克试验场境内进行的核试验的具体情况导致出现了放射性污染程度和放射性核素组成不同的各种试验场。这也导致了放射性粒子溶解度的显著差异。传统上,"试验场"试验场的特点是存在难溶的玻璃化颗粒,这是由核武器地面试验固有的特征决定的,即高温爆炸区域与土壤颗粒的相互作用。由于土壤覆盖层中存在这种易溶颗粒,因此不可能使用6-8 М HCl和7-8 М hno3溶液,而这些溶液是最常用的放射化学分析方法,用于测定90Sr和239+240Pu的含量。本文研究了用高压灭菌法从化粪池土壤中酸萃取人为放射性核素的方法。本研究的目的是开发一种利用高压灭菌器分解从放大土壤样品中酸提取人为放射性核素的方法。采用空白土样确定最佳蒸压釜分解参数;为了测试酸萃取方法,从“试验田”试验场的领土上取了一个土壤样本。由于放射性核素137Cs对粘土和矿质土壤颗粒有很强的固定作用,而且易于被伽马辐射检测到,因此被用作酸萃取的最佳指示剂。通过将所研究的样品溶解在无机酸(HCl, HNO3, HF, H2SO4)的混合物中进行高压釜分解。放射性核素的比活度用BE3830伽马能谱仪和高纯度锗检测器(堪培拉,美国)测定,未分解土壤残留物的量用重量法测定(PA214C分析天平,奥豪斯,美国)。所获得的数据表明,当使用浓缩HF溶液(单独或与其他无机酸混合)时,可以最完全地提取137Cs。137Cs的萃取度为85% ~ 100%。使用3HCl: hno3这两种酸的混合物,结果最差。在这种情况下,137Cs的萃取度不超过20%。在120 ~ 160℃的温度下,HF浓溶液对重达10 g的土样的分解效率≥95%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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