首页|期刊导航|地质科技通报|CO2驱替对致密砂岩孔隙结构的影响:以鄂尔多斯盆地三叠系延长组长7段为例

CO2驱替对致密砂岩孔隙结构的影响:以鄂尔多斯盆地三叠系延长组长7段为例OA

Effect of CO2 flooding on the pore structure of tight sandstones:A case study of Chang 7 Member of Triassic Yanchang Formation in Ordos Basin

中文摘要英文摘要

CO2 驱替是提高致密油藏采收率的重要方法.CO2 注入地层与原位矿物发生反应,改变岩石的孔隙结构.但致密砂岩成岩作用复杂,需要明确不同填隙物特征的致密砂岩在CO2 驱替过程中的微观结构变化机制.利用CO2 驱替、铸体薄片、扫描电镜、核磁共振、X射线衍射等方法,研究CO2 驱替前后致密砂岩矿物成分和孔隙结构的变化.结果表明,致密填隙物复杂多样,以黏土矿物和方解石为主,不同填隙物分布差异明显.填隙物会影响致密砂岩的矿物结构和孔隙形态.CO2 驱替后致密砂岩孔隙度增量平均值为 0.55%、渗透率增加率平均值为21.59%、相对分选系数平均值仅降低 0.01,表明CO2 驱替会增加储集层的孔隙度和渗透率,但对孔隙结构非均质性影响微弱.CO2 驱替过程中长石和方解石被溶蚀,生成石英和黏土矿物沉淀.在黏土含量高的致密砂岩中,CO2溶蚀作用分散,新沉淀的矿物和从骨架颗粒剥落的黏土会堵塞孔隙,物性变化幅度小.在方解石含量高的致密砂岩中,碳酸会溶蚀大量方解石,形成新的储集空间和流动路径,显著改善致密砂岩物性.因此,CO2 驱替对不同填隙物特征致密砂岩的孔隙结构影响不同,CO2 驱替对方解石含量高致密砂岩的物性增加明显好于黏土含量高致密砂岩.研究成果可为致密砂岩油藏开发评价提供了新的思路.

[Objective]CO2 flooding is a crucial technology for enhancing oil recovery efficiency in tight oil reservoirs.CO2 injection reacts with in situ minerals in the formation,leading to changes in the pore structure of the rock.However,tight sandstones undergo complex diagenesis with significant differences in cement distribution,and it is therefore necessary to clarify the mechanisms of microstructural changes in tight sandstones with different cement characteristics during the CO2 flooding process.[Methods]In this study,CO2 flooding simulation experiments,cast thin sections analysis,scanning electron microscopy(SEM),nuclear magnetic resonance,and X-ray diffraction were adopted to investigate the changes in mineral composition and pore structures of tight sandstones before and after CO2 flooding.[Results]The results showed that the cements in tight sandstones were complex and diverse,mainly composed of clay minerals and calcite,with significant distribution differences among different cement types.Cements affected the mineralogical structure and pore morphology of tight sandstones.After CO2 flooding,the average porosity increment of tight sandstones reached 0.55%,the average permeability increase rate was 21.59%,and the average relative sorting coefficient decreased by only 0.01,indicating that CO2 flooding increased the porosity and permeability of the reservoir,but had a weak impact on the heterogeneity of the pore structure.During CO2 flooding,feldspar and calcite were dissolved,resulting in the precipitation of quartz and clay minerals.In tight sandstone with high clay content,CO2 dissolution was dispersed,and the newly precipitated minerals and clay detached from framework grains blocked pores,leading to minor changes in petrophysical properties.In tight sandstones with high calcite content,carbonic acid dissolved large amounts of calcite,creating new storage spaces and flow paths,significantly improving the petrophysical properties of tight sandstones.Therefore,CO2 flooding has different effects on the pore structure of tight sandstones with varying cement characteristics.CO2 flooding results in a much more significant improvement in the physical properties of tight sandstones with high calcite content than those with high clay content.[Conclusion]These results can provide new insights for the development and evaluation of tight sandstone reservoirs.

吴小斌;强小龙;张晓燕;李刚;解强旺;王伟

延安大学石油工程与环境工程学院,陕西 延安 716099中国石油长庆油田分公司第二采气厂,陕西 榆林 719000中国石油长庆油田分公司第二采气厂,陕西 榆林 719000中国石油长庆油田分公司第二采气厂,陕西 榆林 719000中国石油长庆油田分公司第二采气厂,陕西 榆林 719000榆林学院化学与化工学院,陕西 榆林 719000

天文与地球科学

CO2 驱替孔隙结构致密砂岩矿物成分鄂尔多斯盆地

CO2 floodingpore structuretight sandstonemineral compositionOrdos Basin

《地质科技通报》 2026 (2)

11-19,9

国家自然科学基金项目(42362023)陕西省教育厅青年创新团队项目(24JP21722RCYPJB0103)榆林市青年科技新星项目(2024-KJZG-QNXX-007)陕西省科技厅项目(2025JC-YBQN-4562025JC-YBMS-452)中国科学院洁净能源创新研究院-榆林学院联合基金项目(YLU-DNL Fund 2022012)

10.19509/j.cnki.dzkq.tb20240452

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