松散砂岩中的反应流:在地球固碳中的应用

Hongyan Yu, Yihuai Zhang, M. Lebedev, Zhenliang Wang, M. Verrall, S. Iglauer
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引用次数: 1

摘要

向含盐含水层注入二氧化碳(CO2)通常被认为是大规模储层的最佳选择,并且CO2可以提高采收率。在CO2注入初始阶段,孔隙结构和渗透率因细颗粒的释放、运移而发生变化,这对储层筛选和注入设计具有重要意义。因此,我们利用微ct岩心驱油仪对储层状态下未固结砂岩进行了原位活盐水注入前后的成像。结果表明,注盐后非固体高孔隙介质岩石孔隙结构发生明显变化,孔隙度仅略有增加。同时,活盐水冲刷后,石英中产生了许多裂缝。通过对微CT扫描图像的分析,量化比表面积,计算绝对渗透率。由于孔隙结构的改变可以提高CO2的渗透性,渗透率显著提高,特别是低渗透储层。这项研究的结果提供了湖相页岩力学特性的广泛特征,因此可以帮助优化水力压裂基础和提高天然气采收率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reactive Flow in Unconsolidated Sandstone: Application to Carbon Geosequestration
Carbon dioxide (CO2) inject to the saline aquifers are general considered as the best candidates for large-scale storage and CO2 enhance oil recovery. The pore structure and permeability are changed by the fines release, migration in the initial stage of CO2 injection, which is of great importance for reservoir screening and injection design requires adequate understanding. We thus imaged an unconsolidated sandstone at reservoir condition before and after live brine injection in situ with micro-CT core flooding apparatus. We conclude that the pore structure of the unsolid high pores media rock can be significantly changed after live brine injection, although the porosity just have a small increased. Meanwhile, many fractures are generated in the quartz after live brine flush away. Specific surface area are quantified from micro CT scan image analysis to calculate the absolute permeability. The permeability is significantly improved due to the pore structure change which can improve CO2 infectivity, especially low-permeability reservoirs. The results of this study present a broad characterization of the mechanical properties in lacustrine shale and can therefore help optimize hydraulic fractured fundamental and enhanced gas recovery.
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