BIogeochemical Gradients and RADionuclide transport. BIGRAD

生物地球化学梯度和放射性核素传输。

• 批准号: NE/H006540/1
• 负责人: Steven Thornton
• 金额: $ 66.41万
• 依托单位: University of Sheffield
• 依托单位国家: 英国
• 项目类别: Research Grant
• 财政年份: 2010
• 资助国家: 英国
• 起止时间: 2010 至 无数据
• 项目状态: 已结题
• 来源: https://gtr.ukri.org/projects?ref=NE%2FH006540%2F1
• 关键词: BIogeochemical; Gradients; RADionuclide; transport.; BIGRAD

Over 50+ years of nuclear power generation and weapons development, the UK has created large quantities of radioactive wastes. In terms of total volume, the largest fraction (> 90 %) of the higher activity waste is Intermediate Level Waste (ILW). ILW does not produce heat but contains long-lived radioisotopes, and so cannot be disposed of near the Earth's surface. The Government has recently decided that the UK's ILW should be disposed of underground (200 - 1000 m) in a 'Geological Disposal Facility' (GDF). The safety of a GDF depends on slowing the return of radioactivity from the GDF to Earth surface. Understanding the processes which control the movement of radioactivity out of the GDF and to the rock and beyond is therefore critical. The UK's ILW is very diverse and includes discarded nuclear fuel, the metal containers used to hold fuel, as well as sludges and organic debris produced when processing these radioactive materials. The UK has treated many of these radioactive wastes by immobilising them in cement and a substantial fraction of ILW has now been cemented and awaits disposal. Once the wastes have been placed in the GDF, the intention is to backfill the remaining space with cement. No site has been identified for UK wastes as yet, but it is expected that the site will be under the water table and therefore be wet. This means that, after the waste is emplaced, the GDF will rewet as groundwater percolates through the wastes. Over a long time (from hundreds to millions of years) the ILW and its steel containers will degrade, and the cement will react with the groundwater to make it very alkaline. This is a design feature, as very alkaline, 'rusty' conditions are expected to make most radioactive components of the ILW very insoluble. However, this alkaline water will react with the rock around the repository to form a 'chemically disturbed zone' (CDZ). Up until now, no studies have examined the chemical, physical and biological development of this CDZ and how this affects the mobility of radioactive contaminants from the GDF. We have chosen to study four long-lived radionuclides, the fission product technetium as well as uranium, neptunium and plutonium all of which will be present over the long timescales relevant to the CDZ. In this project, we will try and understand how the CDZ will evolve over thousands to millions of years, so we can predict the movement of radioactivity through it, and help assess the safety of the GDF. To do this, we need to study the chemical, physical and biological changes which occur as the CDZ develops, and the way in which these different factors interact with each other. We will use experiments to understand these processes and, based on these, we will develop computer models to predict what will happen in the future. We have divided our work programme into three parts: 1 Geosphere Evolution, where we will examine rock and mineral interactions, and how water flow within the rock is affected by chemical and microbiological changes caused by the water from the GDF; 2 Radionuclide Form, Reaction and Transport, where we will examine the chemical form and solubility of radionuclides, their interactions with microorganisms, and with rock surfaces, and the potential for microscopic particles to carry radioactivity; 3 Synthesis and Application, where we will bring all the experimental results together and design, develop and test our computer model to examine radionuclide transport in the CDZ. To ensure we link the different parts of the project effectively, we have identified two 'cross cutting themes' (CCTs) - (i) biogeochemical processes in the CDZ; and (ii) predictive modelling of the CDZ, which will tie all the different pieces of work together. Our work will provide improved understanding of the controls on contaminant mobility across the CDZ, improve confidence in the safety of geological disposal, and hence assist the UK in the crucial task of disposing of radioactive wastes.

经过50多年的核能发电和武器研发，英国产生了大量的放射性废物。就总体积而言，较高活性废物的最大比例(&gt；90%)是中级废物(ILW)。ILW不产生热量，但含有寿命长的放射性同位素，因此不能在地球表面附近处置。英国政府最近决定，应将英国的ILW处置在地下(200-1000米)的“地质处置设施”(GDF)中。GDF的安全性取决于减缓放射性从GDF返回地球表面的速度。因此，了解控制放射性从GDF移动到岩石和更远的过程是至关重要的。英国的ILW非常多样化，包括废弃的核燃料、用于存放燃料的金属容器，以及在处理这些放射性材料时产生的污泥和有机碎片。英国已经通过将这些放射性废物固定在水泥中来处理它们中的许多，而ILW的很大一部分现在已经被胶结起来，等待处置。一旦废物被放置在GDF中，其目的是用水泥回填剩余的空间。到目前为止，还没有为英国垃圾确定地点，但预计该地点将在地下水位之下，因此是潮湿的。这意味着，在垃圾就位后，GDF将随着地下水渗入垃圾而重新湿润。经过很长一段时间(从数百年到数百万年)，ILW及其钢质容器会降解，水泥会与地下水发生反应，使其变得非常碱性。这是一个设计特点，因为非常碱性、生锈的条件预计会使ILW中的大多数放射性成分非常不能溶解。然而，这些碱性水会与储存库周围的岩石发生反应，形成一个化学扰动区(CDZ)。到目前为止，还没有研究检查这个CDZ的化学、物理和生物发展，以及这如何影响来自GDF的放射性污染物的迁移。我们选择研究四种长寿命放射性核素，裂变产物氚以及铀、钚和钚，所有这些都将存在于与CDZ相关的长时间尺度上。在这个项目中，我们将尝试和了解CDZ将如何在数千到数百万年的时间里进化，这样我们就可以预测放射性物质在其中的移动，并帮助评估GDF的安全性。要做到这一点，我们需要研究CDZ发展过程中发生的化学、物理和生物变化，以及这些不同因素相互作用的方式。我们将利用实验来了解这些过程，并在此基础上开发计算机模型来预测未来会发生什么。我们的工作方案分为三个部分：1地圈演化，在那里我们将研究岩石和矿物的相互作用，以及岩石内的水如何受到来自GDF的水造成的化学和微生物变化的影响；2放射性核素的形成、反应和运输，我们将在其中研究放射性核素的化学形态和溶解性、它们与微生物和岩石表面的相互作用，以及微观粒子携带放射性的可能性；3合成和应用，我们将把所有实验结果汇集在一起，并设计、开发和测试我们的计算机模型，以检查放射性核素在CDZ的输送。为了确保我们有效地将项目的不同部分联系起来，我们确定了两个“横向主题”(CCT)--(I)CDZ中的生物地球化学过程；(Ii)CDZ的预测建模，这将把所有不同的工作联系在一起。我们的工作将使我们更好地了解CDZ对污染物迁移的控制，提高对地质处置安全的信心，从而帮助英国完成处置放射性废物的关键任务。

项目成果

Rock alteration in alkaline cement waters over 15 years and its relevance to the geological disposal of nuclear waste

• DOI: 10.1016/j.apgeochem.2014.08.003
• 发表时间: 2014-11
• 期刊: Applied Geochemistry
• 影响因子: 3.4
• 作者: Elizabeth B. A. Moyce;C. Rochelle;K. Morris;A. Milodowski;Xiaohui Chen;S. Thornton;J. Small;S. Shaw

Mathematical model of coupled dual chemical osmosis based on mixture-coupling theory

• DOI: 10.1016/j.ijengsci.2018.04.010
• 发表时间: 2018-08
• 期刊: International Journal of Engineering Science
• 影响因子: 6.6
• 作者: Xiaohui Chen;S. Thornton;W. Pao

A long-term experimental study of the reactivity of basement rock with highly alkaline cement waters: Reactions over the first 15 months

基岩与高碱性水泥水反应性的长期实验研究：前 15 个月的反应

• DOI: 10.1180/minmag.2016.080.056
• 发表时间: 2018
• 期刊: Mineralogical Magazine
• 影响因子: 2.7
• 作者: Rochelle C

Unsaturated hydro-mechanical-chemical constitutive coupled model based on mixture coupling theory: Hydration swelling and chemical osmosis

• DOI: 10.1016/j.ijengsci.2016.04.010
• 发表时间: 2016-07-01
• 期刊: INTERNATIONAL JOURNAL OF ENGINEERING SCIENCE
• 影响因子: 6.6
• 作者: Chen, XiaoHui;Pao, William;Small, Joe
• 通讯作者: Small, Joe

Geochemical modelling of multimineral evolution for a 15-month experiment

为期 15 个月的实验的多矿物演化地球化学模型

• DOI: 10.1680/jenge.19.00081
• 发表时间: 2023
• 期刊: Environmental Geotechnics
• 影响因子: 2.2
• 作者: Baqer Y