类co2酸岩蚀变不同阶段拉吾石灰岩输运特性

G. Radilla, M. Kacem, J. Lombard, M. Fourar
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引用次数: 6

摘要

自2005年以来,法国国家研究机构支持了几个旨在选择、验证和实施法国二氧化碳储存地质地点的科学项目。本文中介绍的工作是在gecarbonininjection项目中进行的,旨在研究位于巴黎盆地的碳酸盐深盐水含水层对地质二氧化碳储存的适用性。为了进行几种岩石物理和输运表征,选择了一种与含水层岩石相似的地质模拟物。测量参数包括固有渗透率、惯性系数、Klinkenberg系数、相对渗透率以及色散系数和分层系数等输运性质。Lavoux石灰石样品的特征是原始状态和经过CO2样酸岩蚀变阶段。结果表明,孔隙度、渗透率和惯性系数变化明显,相对渗透率、分散系数和分层系数几乎没有变化。这些结果意味着在Dogger地层中注入二氧化碳的过程中,二氧化碳的注入能力将保持甚至提高。然而,为了证实这一观察结果,需要进行额外的实验和建模工作,考虑到潜在的精细迁移。由于这些细小的位移,渗透率可能会发生变化。
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Transport Properties of Lavoux Limestone at Various Stages of CO2-Like Acid-Rock Alteration
Since 2005, the French National Research Agency supports several scientific projects intended to select, validate and implement a geological site for CO2 storage in France. The work presented in this paper was carried out within the Geocarbone-Injectivity project, aimed to study the suitability of a carbonate deep saline aquifer located in the Paris basin for a geological CO2 storage. A geological analog to the aquifer rock was chosen in order to perform several petrophysical and transport characterizations. Measured parameters were intrinsic permeability, inertia coefficient, Klinkenberg coefficient, relative permeabilities and transport properties such as the dispersion coefficient and the stratification factor. Samples of Lavoux limestone were characterized in their original state and also after a phase of CO2 -like acid-rock alteration. Results show sensible changes in porosity, permeability and inertia coefficient and almost no change in relative permeabilities, dispersion coefficient and stratification coefficient. These results mean that the CO2 injectivity would be maintained and even enhanced during its injection in the considered Dogger formation. Nevertheless, to confirm this observation, additional experimental and modeling work should be performed, taking into account the potential fine migration. A permeability alteration could be expected due to these fine displacements.
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