Petrophysical Analyses for Supporting the Search for a Claystone-Hosted Nuclear Repository

Joachim Strobel
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Abstract

The Bundesgesellschaft für Endlagerung mbH (BGE; “Federal Company for Radioactive Waste Disposal”) is responsible for identifying a repository site in Germany for the storage of high-level radioactive waste, ensuring the best possible safety for at least 1 million years (StandAG, 2017). The three-phase site selection process is currently in Step 2 of its Phase I. Around 90 potentially suitable sub-areas are evaluated via individual representative preliminary safety assessments. These sub-areas cover all types of potential containment rock: allochthonous and autochthonous rock salt, claystone, and crystalline rock. Such a comprehensive assessment is challenging for a host rock that covers vast areas like claystone or autochthonous salt. One of the steps towards estimating parameters for a site search process requires the analysis of numerous logs from the areas of interest and their vicinity. Unfortunately, computing these parameters is a much more complex problem than it seems. While gamma ray logs have been the petrophysicist’s workhorse for decades, they allow no quantification of clay properties. Nuclear magnetic resonance and neutron activation logs yield critical information but are scarce in old wells. Decades of research have given good algorithms for defining wet clay porosity from resistivity logs, but inverting those for porosity and tortuosity remains challenging. Another log-derived parameter is a formation’s homogeneity, which quantifies the jaggedness of a logging curve. A vertical variogram or variable filter technique can accomplish this.
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用于支持寻找粘土岩托管核储存库的岩石物理分析
Bundesgesellschaft für Endlagerung mbH(BGE;"联邦放射性废物处置公司")负责在德国确定一个用于贮存高放射性废物的贮存场址,以确保至少 100 万年的最佳安全性(StandAG,2017 年)。约 90 个潜在合适的子区域已通过具有代表性的单个初步安全评估进行了评估。这些子区域涵盖了所有类型的潜在安全壳岩石:同生和自生岩盐、粘土岩和结晶岩。对于像粘土岩或自生岩盐这样覆盖面积广阔的围岩来说,进行这样的全面评估具有挑战性。为估算矿址搜索过程中的参数,其中一个步骤需要对感兴趣区域及其附近的大量测井资料进行分析。遗憾的是,计算这些参数是一个比想象中复杂得多的问题。虽然伽马射线测井几十年来一直是岩石物理学家的工作工具,但它们无法量化粘土的特性。核磁共振和中子活化测井可提供关键信息,但在老井中却很少见。数十年的研究已经给出了从电阻率测井曲线中定义湿粘土孔隙度的良好算法,但将这些算法反演为孔隙度和曲折度仍然具有挑战性。另一个测井参数是地层的均质性,即测井曲线的锯齿度。垂直变异图或可变滤波技术可以实现这一目的。
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