Studying the impact of reservoir temperature, water salinity and CO2 dryness on CO2 injectivity during geological CO2 sequestration

Parvin Ahmadi, F. Ahmaad, M. Aziz Rahman, S. Rezaei Gomari
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Abstract

Carbon capture and storage (CCS) is proved to be effective measure for reducing CO2 emissions. whilst the world still highly depends on the use of fossil fuel energy, this method is necessary for reaching the world’s 1.5 °C goal. Saline aquifers among all possible underground formations are most common targeted ones for CO2 storage due to their frequent presence, and large storage capacity. However, this storage option suffers from sufficient well injectivity to inject large volumes of CO2 at acceptable rates through a minimum number of wells. The injectivity impairment/reinforcement happens through mineral dissolution, fine particle movement, salt precipitation and hydrate formation (known so far). Each of these mechanisms will be more dominant in injectivity alteration at different distance from the injection point depending on reservoir pressure and temperature, formation water salinity, rock mineralogy, and flow rate of CO2 injection as well as its dryness. In this study we have chosen a commercial software Eclipse 300 together with an open-source code to investigate the impact of formation characteristics, CO2 -Brine-Rock interaction, pressure, temperature as well as injection rate on injectivity alteration. The goal for this work is to provide a workflow which can help predicting injectivity alteration using the existing tools. Simulation results show that permeability is affected severely by salt precipitation during CO2 injection. Combined static and dynamic parameter study demonstrate that the injection rate plays a crucial role in size and expansion of CO2 plume as well as growth rate of dry out zone length, amount of salt precipitation and length of equilibrium region. The higher the injection rate, the quicker activation of the capillary and gravity force which leads to drag more brine to near well-bore resulting in higher volume fraction of salt precipitation. However, low injection rate could result in smaller CO2 plume, shorter dry out zone and longer equilibrium region in term of distance from injection point. Thus, optimizing the injection rate regarding reservoir parameters i.e., temperature, pressure and in-situ salinity, will lead to higher storage capacity as well as well performance and maintenance.
研究地质封存过程中储层温度、水矿化度和CO2干燥度对CO2注入能力的影响
碳捕集与封存(CCS)已被证明是减少二氧化碳排放的有效措施。虽然世界仍然高度依赖化石燃料能源的使用,但这种方法对于达到世界1.5°C的目标是必要的。在所有可能的地下地层中,盐水含水层是最常见的二氧化碳储存目标,因为它们经常存在,而且储存能力大。然而,这种储存方式的缺点是,由于井的注入能力不足,只能通过最少的井,以可接受的速度注入大量的二氧化碳。注入性损伤/增强发生在矿物溶解、细颗粒运动、盐沉淀和水合物形成(目前已知)。根据油藏压力和温度、地层水矿化度、岩石矿物学、CO2注入流量及其干燥程度的不同,这些机制在距注入点不同距离处的注入能力变化中更为重要。在这项研究中,我们选择了商业软件Eclipse 300和一个开源代码来研究地层特征、CO2 -盐水-岩石相互作用、压力、温度和注入速度对注入性蚀变的影响。这项工作的目标是提供一个工作流程,可以帮助预测使用现有工具的注入性变化。模拟结果表明,注CO2过程中盐沉淀对渗透率影响较大。静态参数与动态参数相结合的研究表明,注入速率对CO2羽流的大小和扩张、干透区长度、盐沉淀量和平衡区长度的增长速度起着至关重要的作用。注速越高,毛管的激活和重力作用越快,导致更多的盐水被拖到井眼附近,从而导致更高的盐沉淀体积分数。然而,从注入点的距离来看,低注入速率会导致CO2羽流较小,干灭区较短,平衡区较长。因此,根据储层参数(即温度、压力和地层盐度)优化注入速率,将提高储层容量、提高油井性能和维护能力。
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