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首页> 外文期刊>International Journal of Greenhouse Gas Control >Continuum scale modelling of salt precipitation in the context of CO2 storage in saline aquifers with MRST compositional
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Continuum scale modelling of salt precipitation in the context of CO2 storage in saline aquifers with MRST compositional

机译:MRST成分的盐水含水量CO2贮藏中CO2储存背景下的盐水降水型连续模型

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摘要

Carbon capture and storage (CCS) would contribute considerably towards climate change mitigation, if it would be implemented on a very large scale; at many storage sites with substantial injection rates. Achieving high injection rates in deep saline aquifers requires a detailed assessment of injectivity performance and evaluation of the processes that alter the permeability of the near-well region. One of the most common forms of the injectivity loss in the context of CO2 storage in saline aquifers is salt precipitation driven by the evaporation of brine into the relatively dry injected CO2 stream. We present a novel compositional transport formulation based on overall-composition variables which models salt as a separate solid phase which could potentially form through two essentially different ways, i.e., kinetic or equilibrium. To model formation drying-out and subsequent halite-precipitation, an accurate and reliable fluid model ePC-SAFT, which can effectively account for ionic effects, is applied. In addition, a volume balance approach (i.e., depending on how far the salt saturation is from the solubility limit) is implemented to estimate solid saturation in a simulation cell. The resulting simulator is benchmarked against several well-known examples, with analytical solutions demonstrating the ability of the code to cover a variety of physical mechanisms. Finally, injection of dry CO2 into a brine-saturated core-scale domain is simulated and sensitivity analyses over various parameters are performed. We show that the new model is capable to quantitatively represent the physics of salt precipitation (for example salt self-enhancing) under different reservoir conditions.
机译:碳捕获和储存(CCS)将大大促进气候变化缓解,如果它将以大规模实施;在许多具有实质注射率的存储网站。在深盐含水层中实现高注射率需要详细评估再射性能和改变近孔区域渗透性的过程的评估。在盐水含水层的CO2储存中,在盐水含水层的上下文中最常见的重点损失之一是通过盐水蒸发到相对干燥的注入的CO 2流中的盐沉淀。我们提出了一种基于整体组成变量的新型成分转运制剂,其将盐作为单独的固相模拟,其可能通过两个基本上不同的方式形成,即动力学或平衡。为了模拟形成干燥和随后的半乳酸沉淀,应用可以有效地解释离子效应的精确且可靠的流体模型EPC-SAFT。另外,实现了体积平衡方法(即,根据盐饱和来自溶解度极限的距离)来实现以估计模拟单元中的固体饱和度。由此产生的模拟器与若干知名示例进行基准测试,分析解决方案表明代码涵盖各种物理机制的能力。最后,模拟将干CO2注入盐水饱和核心尺度域中,并在各种参数上进行敏感性分析。我们表明,在不同的储层条件下,新模型能够定量地代表盐沉淀(例如盐自增强)的物理学。

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