首页> 外文期刊>International Journal of Greenhouse Gas Control >Brine migration resulting from CO2 injection into saline aquifers - an approach to risk estimation including various levels of uncertainty.
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Brine migration resulting from CO2 injection into saline aquifers - an approach to risk estimation including various levels of uncertainty.

机译:注入盐水中的CO 2 导致盐水迁移-一种风险评估方法,包括各种不确定性。

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摘要

Comprehensive risk assessment is a major task for large-scale projects such as geological storage of CO2. Basic hazards are damage to the integrity of caprocks, leakage of CO2, or reduction of groundwater quality due to intrusion of fluids. This study focuses on salinization of freshwater aquifers resulting from displaced brine. Quantifying risk on the basis of numerical simulations requires consideration of different kinds of uncertainties and this study considers both, scenario uncertainty and statistical uncertainty. Addressing scenario uncertainty involves expert opinion on relevant geological features such as caprock properties, faults, and distinct geological layers. This is considered in this work by 6 different scenarios having different characteristic geological features. On the other hand, Monte Carlo methods are a classical approach to address statistical uncertainty. This is not feasible for large-scale 3D models including complex physics. Therefore, we apply a model reduction based on arbitrary polynomial chaos expansion combined with probabilistic collocation method. It is shown that, dependent on data availability, both types of uncertainty can be equally significant. The presented study provides estimates of the risk of brine discharge into freshwater aquifers due to CO2 injection into geological formations and resultant salt concentrations in the overlying drinking water aquifers.
机译:综合风险评估是诸如CO 2 的地质封存等大型项目的一项主要任务。基本危害是破坏盖层的完整性,CO 2 的泄漏或由于流体的侵入而导致的地下水质量下降。这项研究的重点是盐水置换引起的淡水含水层的盐碱化。在数值模拟的基础上量化风险需要考虑各种不确定性,本研究同时考虑了情景不确定性和统计不确定性。解决方案的不确定性涉及专家对相关地质特征(例如盖层性质,断层和独特的地质层)的看法。在这项工作中,通过具有不同特征地质特征的6种不同方案来考虑这一点。另一方面,蒙特卡洛方法是解决统计不确定性的经典方法。对于包括复杂物理的大规模3D模型,这是不可行的。因此,我们应用基于任意多项式混沌展开结合概率搭配方法的模型约简。结果表明,取决于数据的可用性,两种类型的不确定性可能同样重要。提出的研究提供了由于向地层中注入CO 2 而导致的盐水排放到淡水含水层中的风险以及上层饮用水含水层中盐浓度的估计。

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