首页> 外文会议>International high-level radioactive waste management conference >SPECTROSCOPIC DETECTION OF HYDROGEN PEROXIDE GENERATED BY ALPHA RADIOLYSIS IN SOLUTION
【24h】

SPECTROSCOPIC DETECTION OF HYDROGEN PEROXIDE GENERATED BY ALPHA RADIOLYSIS IN SOLUTION

机译:溶液中α放射分解产生的过氧化氢的光谱检测

获取原文

摘要

During the long-term disposal of used nuclear fuel, the near-surface alpha dose remains significant long after beta and gamma doses decrease. Among the radiolysis products of water, hydrogen peroxide is a dominant oxidizing species, even under reducing or anaerobic conditions. In addition to oxidizing U(Ⅳ) to U(Ⅳ) in the fuel matrix, sufficient concentrations of hydrogen peroxide in solution may also stabilize uranyl peroxide phases such as studtite or metastudtite at the fuel surface. In order to predict the long-term behavior of nuclear materials, radiolysis models help bridge the gap between short-term bench-top experiments (e.g., 0-10 years) and long-term natural analogue studies (e.g., 10~6 years). Here, spectroscopic methods are used to measure the amount of hydrogen peroxide generated by the alpha radiolysis of water in the presence of dissolved Americium-241 for comparison with alpha radiolysis models. The colorless compound, titanyl sulfate (Ti(Ⅳ)OSO_4), complexes strongly with colorless H_2O_2 in solution, yielding absorption in the visible region (≈ 405 nm). Additionally, experiments here show that Ti(Ⅳ)OSO_4 peroxide complexes remain stable for months when solutions are refrigerated between measurements. Using a 1 cm path-length UV-Vis set-up, detection limits of mid 10~(-6) M H_2O_2 were achieved; coupling a longer path-length (5 m) cell to the UV- Vis detector allows for mid 10~(-7) M H_2O_2 detection limits. This range of values is of interest for comparison with equilibrium values predicted by alpha radiolysis models. In order to evaluate total hydrogen peroxide generation as a Junction of time, small aliquots of Am-241 nitrate solution (2.09 mM) are added to 0.5 M Ti(Ⅳ)OSO_4 solutions, sealed in a vial, and measured at different time points. For an equilibrium kinetics study, "time zero " is established for a series of samples and spectra are taken for each vial at specified time-points with indicator solution being added immediately prior to measurement. Factors such as temperature are evaluated for comparison with radiolytic models. This study is an example of alpha radiolysis product detection using a homogeneous (e.g., liquid / liquid rather than solid /liquid or ion-beam/liquid) approaches to dose generation.
机译:在长期使用过的核燃料期间,β和γ剂量减少很长时间后,近地表α剂量仍然很重要。在水的放射分解产物中,即使在还原或厌氧条件下,过氧化氢也是主要的氧化物质。除了将燃料基体中的U(Ⅳ)氧化成U(Ⅳ)外,溶液中足够浓度的过氧化氢还可以使燃料表面的过氧化铀酰相(如辉石或偏辉石)稳定。为了预测核材料的长期行为,放射分解模型有助于弥合短期台式实验(例如0-10年)和长期自然类似物研究(例如10〜6年)之间的差距。 。在这里,使用光谱学方法测量在溶解的Americium-241存在下由水的α辐射分解产生的过氧化氢的量,以便与α辐射分解模型进行比较。无色化合物硫酸氧钛(Ti(Ⅳ)OSO_4)与溶液中的无色H_2O_2强烈络合,在可见光区域(≈405 nm)吸收。此外,此处的实验表明,两次测量之间将溶液冷冻后,Ti(Ⅳ)OSO_4过氧化物配合物可保持稳定数月。使用1 cm光程的UV-Vis设置,检测限达到了10〜(-6)M H_2O_2的中值;将更长的光程(5 m)池与UV-Vis检测器耦合可以实现10〜(-7)M H_2O_2的中等检测极限。该值的范围对于与α放射分解模型预测的平衡值进行比较很有意义。为了评估总的过氧化氢生成时间,将少量等分试样的Am-241硝酸盐溶液(2.09 mM)添加到0.5 M Ti(Ⅳ)OSO_4溶液中,密封在小瓶中,并在不同的时间点进行测量。对于平衡动力学研究,为一系列样品建立“时间零”,并在指定的时间点为每个样品瓶获取光谱,并在测量前立即添加指示剂溶液。评估温度等因素,以便与辐射分解模型进行比较。这项研究是使用均质(例如液体/液体而不是固体/液体或离子束/液体)方法进行剂量生成的α放射分解产物检测的示例。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号