Study on CO2 Injection in Tight Sandstone Gas Reservoirs to Enhance Recovery and Burial Mechanism

IF 4.3 3区 化学 Q2 CHEMISTRY, MULTIDISCIPLINARY
Yulong Zhang*, Xiaolan Teng, Wenya Zhai, Wei Shi, Yaobo Liu, Yuan Liu and Xiao Wang, 
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Abstract

To study the mechanism of CO2 injection in tight sandstone gas reservoirs for enhanced recovery and geological storage, we conducted experimental studies based on the reservoir conditions in West Sichuan. These studies focused on the properties of CO2 and CH4, their adsorption and diffusion under high temperature and high pressure, the interactions of CO2 with tight sandstone and formation water, and the displacement efficiency of the CO2 injection in long core samples. The results show that under reservoir conditions, the adsorption capacity of CO2 in tight sandstone is nearly four times higher than that of CH4, and its diffusion capacity is also four times higher. This enables CO2 to replace adsorbed CH4 through competitive adsorption. Due to the greater density of CO2 compared to CH4, gravitational differentiation causes CO2 to sink below CH4, pushing CH4 upward in the reservoir. This process facilitates the sequestration of CO2 and enhances the recovery of natural gas. Additionally, CO2 injection dissolves feldspar and calcite in dense sandstone minerals, generating kaolinite, iron dolomite, and chlorite. The dissolution effect exceeds precipitation, leading to an increase in permeability by 73.25 to 91.15% and an increase in porosity by 0.65 to 0.72%. This improves the reservoir’s seepage characteristics, reduces the minimum flow pressure of liquids in the pores, decreases water-phase trapping damage, and ultimately increases gas recovery. This study provides technical guidance for the efficient development of tight sandstone gas reservoirs and geological storage of CO2.

致密砂岩气藏注CO2提高采收率及埋藏机理研究
为研究致密砂岩气藏CO2注入提高采收率和地质封存机理,结合川西地区储层条件进行了实验研究。这些研究主要集中在CO2和CH4的性质、高温高压下的吸附和扩散、CO2与致密砂岩和地层水的相互作用以及长岩心样品中CO2注入的驱油效率等方面。结果表明,在储层条件下,致密砂岩对CO2的吸附能力是CH4的近4倍,其扩散能力也是CH4的4倍。这使得CO2通过竞争性吸附取代被吸附的CH4。由于CO2的密度大于CH4,重力分异导致CO2下沉到CH4以下,推动储层中CH4向上。这一过程有利于二氧化碳的封存,提高了天然气的采收率。此外,二氧化碳的注入溶解了致密砂岩矿物中的长石和方解石,生成高岭石、铁白云石和绿泥石。溶蚀作用大于沉淀作用,渗透率增加73.25 ~ 91.15%,孔隙度增加0.65 ~ 0.72%。这改善了储层的渗流特性,降低了孔隙中液体的最小流动压力,减少了水相圈闭损害,最终提高了天然气采收率。该研究为致密砂岩气藏高效开发和CO2地质封存提供了技术指导。
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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来源期刊
ACS Omega
ACS Omega Chemical Engineering-General Chemical Engineering
CiteScore
6.60
自引率
4.90%
发文量
3945
审稿时长
2.4 months
期刊介绍: ACS Omega is an open-access global publication for scientific articles that describe new findings in chemistry and interfacing areas of science, without any perceived evaluation of immediate impact.
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