An Analytical Model for Water Evaporation During CO2 Injection for Geological Storage

T. Russell, P. Bedrikovetsky
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Abstract

Formation damage during CO2 injection into depleted gas or oil reservoirs, or in aquifers, is highly affected by connate water evaporation into injected gas. For example, precipitated salts accumulate into dried-up zone around the well. Dried rock liberates fine clay particles. The aim of the work is creation of an analytical model for connate water evaporation into injected CO2 during coreflood and injection in vertical well. The mathematical model considers non-equilibrium evaporation accounting for changing interfacial area. The interfacial area is derived separately from approximating the porous media as a sphere pack and from the averaging of individual water patches. The resulting model is solved analytically using the method of characteristics, permitting the calculation of the water saturation and vapour concentration profiles during the evaporation process. Finally, we match 5 laboratory tests, determine the typical form of evaporation interface, and upscale the results for injection well conditions. Tuning of laboratory data exhibits high agreement for 5 laboratory tests and allows for characterization of field-scale evaporation dynamics from laboratory testing. The total evaporation time is provided explicitly by the model, and a criterion is presented for determining whether evaporation occurs within finite time. This work provides key insights into the behaviour of CO2 injection wells and can contribute to producing explicit formulae to predict mobilisation of fine clays and precipitation of salts due to rock drying.
用于地质封存的二氧化碳注入过程中水蒸发的分析模型
在向枯竭气藏、油藏或含水层注入二氧化碳的过程中,注入气体中的涵养水蒸发会对地层造成严重破坏。例如,沉淀的盐分会积聚到油井周围的干涸区域。干燥的岩石会释放出细小的粘土颗粒。这项工作的目的是建立一个分析模型,用于分析在垂直井的岩心充注和注入过程中,涵养水蒸发到注入的二氧化碳中的情况。该数学模型考虑了非平衡蒸发,考虑了界面面积的变化。界面面积是通过将多孔介质近似为一个球包和平均单个水斑分别得出的。利用特征法对所得到的模型进行分析求解,从而计算出蒸发过程中的水饱和度和蒸汽浓度曲线。最后,我们匹配了 5 项实验室测试,确定了蒸发界面的典型形式,并将结果放大到注水井条件下。对实验室数据进行调整后,5 个实验室测试结果显示出高度一致,并可通过实验室测试确定实地尺度的蒸发动力学特征。模型明确提供了总蒸发时间,并提出了确定蒸发是否在有限时间内发生的标准。这项工作为了解二氧化碳注入井的行为提供了重要依据,并有助于制定明确的公式来预测岩石干燥引起的细粘土移动和盐分沉淀。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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