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中国物理学会期刊

原位生长ZIF-8构筑岩石基多尺度孔隙结构以增强二氧化碳吸附与驱替性能

Construction of Rock-Based Multiscale Pore Structures via In Situ Growth of ZIF-8 for Enhancing CO2 Adsorption and Displacement Performance

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  • 大气二氧化碳(CO2)浓度持续升高使高效碳捕集、利用与封存(carbon capture, utilization and storage, CCUS)需求愈加迫切。尽管已将CO2注入深部咸水层和油气藏进行地质封存和提高石油采收率(enhanced oil recovery, EOR),但天然储层岩石有限的界面吸附能力和孔隙表面活性位点,使CO2在长期注入过程中仍存在迁移与泄漏风险。针对这一问题,本文提出在天然岩石(贝雷砂岩,BS)中原位生长金属有机框架材料(MOFs)(沸石咪唑酯框架-8,ZIF-8)纳米晶体,构建兼具天然骨架稳定性与微孔吸附功能的ZIF-8/BS复合多孔介质。形貌和相态分析表明,ZIF-8在BS表面实现了均匀负载并保持了完整的晶体结构。CO2吸附、N2吸附、压汞(MIP)和T2-T2弛豫交换结果显示,ZIF-8的引入使BS形成由微孔、介孔和大孔共同构成的多尺度孔隙结构;原位生长后的ZIF-8主要改变了孔隙表界面特征并引入微孔贡献,未削弱BS原有孔隙网络的连通性,并且将比表面积由1.8197 m2 g-1提高至25.4238 m2 g-1。在298 K、100 kPa下,ZIF-8/BS的CO2吸附量达到22.21 cm3 g-1 STP,显著高于BS的0.15 cm3 g-1 STP,且多次循环吸脱附后性能保持稳定。此外,进一步结合在线核磁共振(NMR)监测下的超临界二氧化碳(sc-CO2)-水/油驱替实验,ZIF-8/BS在水相和油相驱替过程中均表现出更优的残余流体迁移能力与驱替效率。相较于BS,ZIF-8/BS的残余水饱和度由43.18%降至32.34%,水驱效率由56.82%提高至67.66%;残余油饱和度由37.49%降至28.69%,驱油效率由62.51%提高至71.31%,有效降低了受表面力束缚的孔壁残余流体。研究表明,在天然岩石孔隙中原位引入MOF功能相,可在保持主体孔隙连通性的基础上实现CO2吸附增强与驱替改善的耦合作用,为CO2-EOR与CO2地质封存过程中储层孔隙界面功能化提供了新的研究思路。

     

    The continuous increase in atmospheric carbon dioxide (CO2) concentration has created an urgent demand for efficient carbon capture, utilization and storage (CCUS). Although CO2 has been injected into deep saline aquifers and oil and gas reservoirs for geological storage and enhanced oil recovery (EOR), the limited interfacial adsorption capacity and pore-surface active sites of natural reservoir rocks mean that CO2 still faces risks of migration and leakage during long-term injection. To address this issue, this study proposes the in situ growth of metal-organic framework (MOF) nanocrystals, specifically zeolitic imidazolate framework-8 (ZIF-8), within natural rock (Berea sandstone, BS), thereby constructing ZIF-8/BS composite porous media with both the structural stability of the natural rock framework and microporous adsorption functionality. Morphological and phase analyses show that ZIF-8 achieves uniform loading on the BS surface while maintaining an intact crystal structure. CO2 adsorption, N2 adsorption, mercury intrusion porosimetry (MIP), and T2-T2 relaxation exchange results show that the introduction of ZIF-8 enables BS to form a multiscale pore structure composed of micropores, mesopores, and macropores. The in situ grown ZIF-8 mainly modifies the pore-surface interfacial characteristics and introduces a micropore contribution, without weakening the connectivity of the original BS pore network, and increases the specific surface area from 1.8197 m2 g-1 to 25.4238 m2 g-1. At 298 K and 100 kPa, the CO2 uptake of ZIF-8/BS reaches 22.21 cm3 g-1 STP, which is significantly higher than that of BS, 0.15 cm3 g-1 STP, and remains stable after multiple adsorption-desorption cycles. In addition, supercritical CO2 (sc-CO2)-water/oil displacement experiments under online nuclear magnetic resonance (NMR) monitoring show that ZIF-8/BS exhibits improved residual-fluid migration capability and displacement efficiency during both water-phase and oil-phase displacement. Compared with BS, the residual water saturation of ZIF-8/BS decreases from 43.18% to 32.34%, and the water-displacement efficiency increases from 56.82% to 67.66%; the residual oil saturation decreases from 37.49% to 28.69%, and the oil-displacement efficiency increases from 62.51% to 71.31%, indicating that ZIF-8/BS can effectively reduce pore-wall residual fluids constrained by surface forces. Overall, the in situ introduction of an MOF functional phase into natural rock pores can achieve the coupled enhancement of CO2 adsorption and displacement performance while maintaining the connectivity of the main pore network, providing a new research strategy for reservoir pore-interface functionalization during CO2-EOR and CO2 geological storage.

     

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