Physical-chemical characterization of uranium containing sediments

Q4 Agricultural and Biological Sciences
L. Závodsḱa, Eva Kosorínová, J. Lesńy, D. Bodiš
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引用次数: 1

Abstract

The presented paper is intended to study the chemical behaviour of combined geogenicanthropogenic uranium content in specific stream sediments. The sampling points have been chosen with respect to the natural conditions in the locality of groundwater outflow from a former uranium mine adit in Považský Inovec mountain range, near Kálnica village. Besides the total uranium determination and physical-chemical characterization of the relevant water- and sediment samples we carried out modified Tessier type sequential fractionation extractions of natural- and artificially contaminated sediment samples after time dependent agitation in air and in the atmosphere of argon. The obtained results have been compared with those fulfilled with montmorillonite K-10. The total uranium concentrations of the relevant groundwater samples as well as of stream sediments have been determined by ICP-MS using HP 4500. The determinations of uranium in extracts have been accomplished according STN757614, utilizing arsenazo III as a selective complex forming reagent for spectrophotometric determination of uranyl-ions at 650 nm. The total uranium concentration of the groundwater outflow and in the sediment taken in its immediate vicinity has been 31.75±0.35 μg dm-3 and 38.0±2.7 μg g-1 respectively. Unlike montmorillonit K-10, in which the carbonate-bound fraction of uranium after 1 week aeration and agitation in argon atmosphere represents 22.8% and 18.6% respectively, uranium in investigated sediments has been present predominantly in carbonate-bound fraction-reaching under similar conditions 38.6% and 26.6%, respectively.
含铀沉积物的物理化学特征
本文旨在研究特定水系沉积物中地质-人为联合铀含量的化学行为。采样点的选择参照了Kálnica村附近Považský Inovec山脉前铀矿坑道流出地下水地区的自然条件。除了对相关的水和沉积物样品进行总铀的测定和物理化学表征外,我们还对自然污染和人工污染的沉积物样品进行了改良的Tessier型顺序分馏提取,这些样品经过空气和氩气的时间依赖搅拌。所得结果与K-10蒙脱土的测定结果进行了比较。用hp4500等离子体质谱法测定了相关地下水样品和水系沉积物的总铀浓度。采用STN757614,偶氮胂ⅲ作为选择性络合物形成试剂,在650 nm处分光光度法测定了提取液中铀的含量。地下水出水口铀浓度为31.75±0.35 μg -3,附近沉积物铀浓度为38.0±2.7 μg -1。与monmonillonit K-10不同,在氩气中充气和搅拌1周后,铀的碳酸盐结合部分分别占22.8%和18.6%,所研究沉积物中的铀主要以碳酸盐结合部分存在,在类似条件下分别达到38.6%和26.6%。
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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来源期刊
Nova Biotechnologica et Chimica
Nova Biotechnologica et Chimica Agricultural and Biological Sciences-Food Science
CiteScore
0.60
自引率
0.00%
发文量
47
审稿时长
24 weeks
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