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COMBINED EXPERIMENTAL AND COMPUTATIONAL APPROACH TO PREDICT THE GLASS-WATER REACTION

机译:结合实验和计算方法预测玻璃水反应

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摘要

The use of mineral and glass dissolution rates measured in laboratory experiments to predict the weathering of primary minerals and volcanic and nuclear waste glasses in field studies requires the construction of rate models that accurately describe the weathering process over geologic timescales. Additionally, the need to model the long-term behavior of nuclear waste glass for the purpose of estimating radionuclide release rates requires that rate models be validated with long-term experiments. Several long-term test methods have been developed to accelerate the glass-water reaction [drip test, vapor hydration test, product consistency test B, and pressurized unsaturated flow (PUF)], thereby reducing the duration required to evaluate long-term performance. Currently, the PUF test is the only method that mimics the unsaturated hydraulic properties expected in a subsurface disposal facility and simultaneously monitors the glass-water reaction. PUF tests are being conducted to accelerate the weathering of glass and validate the model parameters being used to predict long-term glass behavior. A one-dimensional reactive chemical transport simulation of glass dissolution and secondary-phase formation during a 1.5-year-long PUF experiment was conducted with the Subsurface Transport Over Reactive Multiphases (STORM) code. Results show that parameterization of the computer model by combining direct benchscale laboratory measurements and thermodynamic data provides an integrated approach to predicting glass behavior over the length of the experiment. Over the 1.5-year-long test duration, the rate decreased from 0.2 to 0.01 g/(m2 -day) based on B release for low-activity waste glass LAWA44. The observed decrease is approximately two orders of magnitude higher than the decrease observed under static conditions with the SON68 glass (estimated to be a decrease by four orders of magnitude) and suggests that the gel-layer properties are less protective under these dynamic conditions.
机译:使用实验室实验中测量的矿物和玻璃溶解速率来预测野外研究中的主要矿物以及火山玻璃和核废玻璃的风化,需要构建速率模型,以准确描述地质时标上的风化过程。此外,为估算放射性核素释放速率而对核废玻璃的长期行为进行建模的需求要求使用长期实验对速率模型进行验证。已经开发了几种长期测试方法来加速玻璃水反应[滴水测试,蒸汽水化测试,产品稠度测试B和加压不饱和流量(PUF)],从而缩短了评估长期性能所需的时间。当前,PUF测试是唯一一种模拟地下处置设施中预期的不饱和水力特性并同时监控玻璃水反应的方法。 PUF测试正在进行中,以加快玻璃的耐候性并验证用于预测玻璃长期性能的模型参数。在长达1.5年的PUF实验中,使用次生反应下的地下传输(STORM)代码进行了玻璃溶解和第二相形成的一维反应性化学传输模拟。结果表明,通过结合直接实验室规模的实验室测量结果和热力学数据对计算机模型进行参数化,可以提供一种在整个实验过程中预测玻璃行为的综合方法。在为期1.5年的测试期间,基于低活性废玻璃LAWA44的B释放量,该速率从0.2 g /(m2 -day)降低至0.01 g /(m2 -day)。所观察到的降低比在静态条件下使用SON68玻璃观察到的降低大约高两个数量级(估计降低了四个数量级),这表明在这些动态条件下,凝胶层特性的保护性较低。

著录项

  • 来源
    《Nuclear Technology》 |2011年第1期|p.22-39|共18页
  • 作者

    E. M. PIERCE; D. H. BACON;

  • 作者单位

    Pacific Northwest National Laboratory, Energy and Environment Directorate P.O. Box 999, Richland, Washington 99352,Oak Ridge National Laboratory, Energy and Environmental Sciences Directorate 1 Bethel Valley Road, Oak Ridge, Tennessee 37831-6038;

    Pacific Northwest National Laboratory, Energy and Environment Directorate P.O. Box 999, Richland, Washington 99352;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    mineral and glass wea thering; aluminoborosilica te nuclear waste glass; modeling reactive chemical transport;

    机译:矿物质和玻璃湿环;铝硼硅和核废玻璃;模拟反应性化学传输;
  • 入库时间 2022-08-18 00:43:44

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