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低孔低渗储层CO2封存迁移规律——以鄂尔多斯盆地为例OA

Migration law of CO2 storage in low-porosity and low-permeability reservoirs:Taking Ordos Basin as an example

中文摘要英文摘要

[研究目的]为丰富鄂尔多斯盆地低孔低渗枯竭油气藏储层碳封存的研究,计划实施每年10万t的地质储存(CCS)项目.共21 口注气井,平均每口井注气速率0.15 kg/s.[研究方法]拟选取鄂尔多斯盆地延长组长6油层作为目标储层,封存层平均孔隙度在7%~12%,平均渗透率在0.1~5 mD.从渗流力学、多相流体力学、计算流体力学等相关学科的基础理论出发,构建均质与非均质两种地质概念模型.通过数值模拟对比分析CO2在不同地质条件下的封存特点、流体迁移规律及相态转化机制,并结合矿场实践的实际情况,研究CO2低孔低渗储层封存的特点、流体迁移和输运的特性以及相关物理现象.[研究结果]超临界CO2灌注期间地层原有的压力平衡被打破,注入井周围地层压力迅速上升.均质模型压力呈均匀辐射状扩散,而非均质模型受渗透率级差影响,压力波前呈现显著的各向异性与"阶梯状"分布特征.CO2停注后地层压力又会逐渐趋于稳定;在均质模型中CO2呈"舌状"聚集带的状态聚集在储层顶部且侧向分布范围不断扩大.而在非均质模型中,表现出明显的"黏性指进"与边缘锯齿状特征.[结论]对比模拟注气期CO2平均迁移速度0.0157 m/d和水力压裂后矿场实践注气期CO,平均迁移速度7.35 m/d,发现对鄂尔多斯盆地低孔低渗储层先期进行水力压裂能够大大加快CO2的迁移速率,提高注入能力.

[Objective]To enrich the research on carbon storage in low-porosity and low-permeability depleted hydrocarbon reservoirs in the Ordos Basin,a carbon capture and storage(CCS)project with an annual capacity of 100,000 tons is planned.The project involves 21 injection wells,each with an average injection rate of 0.15 kg/s.[Methods]The Chang 6 oil layer of the Yanchang Formation in the Ordos Basin is selected as the target reservoir,characterized by an average porosity of 7%-12%and an average permeability of 0.1-5 mD.Based on the fundamental theories of percolation mechanics,multiphase fluid dynamics,and computational fluid dynamics,both homogeneous and heterogeneous conceptual geological models were constructed.Numerical simulations were employed to comparatively analyze the CO2 storage characteristics,fluid migration laws,and phase-transition mechanisms under different geological conditions.Furthermore,in combination with field practices,the study investigates the specific features of CO2 storage in low-porosity and low-permeability reservoirs,the behaviors of fluid migration and transport,and related physical phenomena.[Results]During supercritical CO2 injection,the initial formation pressure equilibrium is disrupted,leading to a rapid pressure increase around the injection wells.In the homogeneous model,the pressure diffuses uniformly in a radial pattern.Conversely,in the heterogeneous model,the pressure front exhibits significant anisotropy and"stepped"distribution characteristics due to permeability contrast.Following the cessation of injection,the formation pressure gradually stabilizes.In the homogeneous model,CO2 forms a"tongue-like"accumulation zone at the top of the reservoir,with its lateral distribution continuously expanding.In contrast,the heterogeneous model exhibits pronounced"viscous fingering"and jagged edge characteristics.[Conclusions]A comparison between the simulated average CO2 migration velocity during the injection period(0.0157 m/d)and the field-measured velocity following hydraulic fracturing(7.35 m/d)reveals that pre-treating the low-porosity and low-permeability reservoirs in the Ordos Basin with hydraulic fracturing significantly accelerates CO2 migration and enhances injection capacity.

汪锋;戴世鑫;朱伟;胡盼;宫玉菲

湖南科技大学资源环境与安全工程学院,湖南湘潭 411201湖南科技大学资源环境与安全工程学院,湖南湘潭 411201||湖南科技大学煤炭资源清洁利用与矿山环境保护湖南省重点实验室,湖南湘潭 411201湖南科技大学资源环境与安全工程学院,湖南湘潭 411201湖南科技大学资源环境与安全工程学院,湖南湘潭 411201中国矿业大学(北京)地球科学与测绘工程学院,北京 100083

天文与地球科学

CO2地质封存低孔低渗延长组油气勘查工程鄂尔多斯

CO2geological storagelow-porosity and low-permeabilityYanchang Formationoil and gas exploration engineeringOrdos

《中国地质》 2026 (2)

476-490,15

国家重点研发计划项目(2018YFB0605503,2018YFC0807801)和国家自然科学基金项目(51804112)联合资助. Supported by National Key Research and Development Program of China(No.2018YFB0605503,No.2018YFC0807801),and National Natural Science Foundation of China(No.51804112).

10.12029/gc20200710001

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