CO2 sequestration wells sealing evaluation model: Jimusar depression, China as an example

0 ENERGY & FUELS
Dian Wang , Jun Li , Wei Lian , Xianbo Liu , Juncheng Zhang , Han Xiao
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Abstract

Suitable geological sites for CO2 sequestration often contain numerous existing wellbores, which have been identified as high-risk locations for CO2 leakage. To investigate whether the pressure disturbances caused by CO2 injection have the potential to drive the propagation of micro-annulus in nearby wells, this paper develops and validates a numerical simulation program, taking the Jimusar Depression in China as a case study. The results indicate that the phenomenon of formation overpressure caused by CO2 injection occurs not only in the reservoir but also in the caprock. The pressure response of the caprock exhibits a lag, resulting in a dynamic inter-layer pressure difference, with a peak difference observed during the early stages of injection. As the distance from the injection well increases, the peak pressure difference decreases exponentially, with a maximum differential pressure of 1.33 MPa observed at well J172. The pressure difference around the well can drive fluid migration along the cement bonding surface, and excessive pressure differences can lead to changes in the stress state of the surface. When the stress state transitions from compression to tension, and the tensile stress exceeds the bonding strength, micro-annulus may propagate. When the cement curing shrinkage rate is zero, the minimum pressure difference for micro-annulus propagation at the cement-sheath formation interface in well J172 is 9.39 MPa, which is significantly higher than the peak formation pressure difference of 1.33 MPa around the well, indicating a low risk of micro-annulus propagation. The shrinkage of the cement upon curing will considerably lower the critical pressure for micro-annulus propagation. At a cement shrinkage rate of 0.15%, the propagation pressure for micro-annulus decreases to 1.0 MPa, indicating a higher risk of micro-annulus propagation. This study proposes a CO2 sequestration well sealing assessment program, which confirms that under unfavorable conditions, CO2 injection may induce the propagation of micro-annulus near the well. This research holds significant implications for the safety of wellbores at CO2 sequestration sites, as well as for monitoring CO2 plumes and pressure.
二氧化碳封存井密封性评估模型:以中国吉木萨尔凹陷为例
二氧化碳封存的合适地质地点通常包含大量现有井筒,这些井筒已被确定为二氧化碳泄漏的高风险地点。为了研究二氧化碳注入引起的压力扰动是否有可能导致微空洞在附近井中传播,本文以中国吉木萨尔凹陷为例,开发并验证了一个数值模拟程序。结果表明,二氧化碳注入引起的地层超压现象不仅发生在储层中,也发生在盖岩中。盖岩的压力响应表现出滞后性,导致层间动态压差,在注入初期观测到峰值压差。随着与注水井距离的增加,峰值压差呈指数下降,在 J172 井观测到的最大压差为 1.33 兆帕。注水井周围的压差会推动流体沿水泥粘结面迁移,过大的压差会导致粘结面的应力状态发生变化。当应力状态从压缩过渡到拉伸,且拉伸应力超过粘结强度时,可能会产生微空洞。当水泥固化收缩率为零时,J172 井水泥-地层鞘界面微空洞扩展的最小压差为 9.39 兆帕,明显高于该井周围 1.33 兆帕的地层峰值压差,表明微空洞扩展的风险较低。水泥固化后的收缩将大大降低微空洞扩展的临界压力。当水泥收缩率为 0.15%时,微空洞的扩展压力将降至 1.0 兆帕,表明微空洞扩展的风险较高。本研究提出了二氧化碳封存井密封评估方案,证实了在不利条件下,二氧化碳注入可能会诱发井附近微空洞的扩展。这项研究对二氧化碳封存地点的井筒安全以及二氧化碳羽流和压力监测具有重要意义。
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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