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Geochemical effects of impurities in CO_2 on a sandstone reservoir

机译:杂质在砂岩水库CO_2中的地球化学作用

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In most cases, CO_2 captured from power plants or large industrial sources contains impurities. As purification of the stream is energy and cost intensive it is necessary to allow a certain level of impurities. The effects of impurities on (short- and long-term) geological storage are, however, uncertain. In this work, geochemical modelling with PHREEQC is performed to describe such effects on a sandstone reservoir (depleted gas field). The impact of two possible CO_2 streams, originating from pre-combustion and oxyfuel capture technology is investigated. The streams contain O_2, H_2, CO, H_2S, SO_2, and/or NO as potential chemically reactive components. H_2S, SO_2 and NO are computed to oxidize, thereby forming sulfuric or nitric acid, and decrease the pH of the formation water. A low pH of the brine may be the result of extensive dissolution and dissociation, and therefore accumulation in the brine phase, especially close to the injection well. The impact of impurities on fast reacting minerals (short-term effects) is predicted to be relatively insignificant, due to the low amount of brine generally present in a gas field. On the long-term (equilibrium stage), impurities cause a slightly different mineralogy compared to pure CO_2 injection. For the latter case a final increase in porosity of 3.5% is predicted whilst impurities (especially oxygen) could mitigate the porosity increase to zero due to the precipitation of minerals with higher molar volumes, like alunite and nontronite. Overall, the impurities do not seem to have a significant impact on the reservoir, even if accumulation in the brine takes place. The possible limiting effect of diffusion of impurities within the supercritical CO_2 towards the brine has not been taken into account, even though the effect could be relevant. It could delay the effect of the impurities due to retarded dissolution. Further research should focus on this issue. Also the spatial effects and effects on different reservoir types, cap rock and well cement need to be investigated.
机译:在大多数情况下,CO_2从发电厂或大型工业污染源捕获含有杂质。作为流的纯化是能量和成本密集的,需要以允许杂质的一定水平。杂质对(短期和长期)地质储存的影响,然而,不确定。在这项工作中,与PHREEQC地球化学模拟被执行以描述在砂岩储层(耗尽的气体场)这样的效果。两种可能的CO_2流的影响,从燃烧前和富氧燃烧捕捉技术起源进行了研究。流包含O_2,H_2,CO,硫化氢,二氧化硫和/或NO作为潜在的化学反应组分。硫化氢,二氧化硫和NO被计算以氧化,由此形成硫酸或硝酸,并降低地层水的pH值。盐水的低pH可以是广泛的溶解和离解,因此,在盐水相积累的结果,尤其是接近注入井。杂质对快速反应矿物(短期效应)的影响被预测为相对不显着,由于盐水通常存在于天然气田的低量。在长期(平衡段),杂质相比纯CO_2注射引起稍微不同的矿物学。对于后一种情况中的3.5%的孔隙率的最终增加,而杂质(尤其是氧气)的预测可以在孔隙率增加至零减轻由于具有较高的摩尔体积,如明矾石和绿脱石矿物的沉淀。总体而言,杂质似乎没有对水库一个显著的影响,即使堆积在盐水发生。朝盐水超临界CO_2中的杂质扩散的可能限制作用还没有被考虑到,尽管影响可能是相关的。这可能耽误的杂质的影响,由于智障溶解。进一步的研究应该关注这个问题。同样在不同的油藏类型,盖层和油井水泥的需求空间效果和效果进行调查。

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