Characterisation and multifaceted anisotropy assessment of Corvio sandstone for geological CO2 storage studies

被引:15
作者
Falcon-Suarez, Ismael [2 ]
Canal-Vila, Jacobo [1 ,3 ]
Delgado-Martin, Jordi [1 ]
North, Laurence [2 ]
Best, Angus [2 ]
机构
[1] Univ A Coruna, Sch Civil Engn, Campus Elvina S-N, La Coruna 15071, Spain
[2] Univ Southampton, Natl Oceanog Ctr, Waterfront Campus,European Way, Southampton SO14 3ZH, Hants, England
[3] Ctr Tecnol Repsol Ctra, N-V Km 18, Mostoles 28935, Spain
基金
英国工程与自然科学研究理事会; 英国自然环境研究理事会;
关键词
Corvio sandstone; Weak anisotropy; Wave velocities; Strength; Permeability; CO2; storage; EOR; ELASTIC-WAVE VELOCITIES; ELECTRICAL-RESISTIVITY; ATTENUATION ANISOTROPY; PERMEABILITY EVOLUTION; TRANSPORT-PROPERTIES; CAPILLARY-PRESSURE; PORE GEOMETRY; ROCK PHYSICS; STRESS STATE; MODULI;
D O I
10.1111/1365-2478.12469
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present a comprehensive characterisation of the physical, mineralogical, geomechanical, geophysical, and hydrodynamic properties of Corvio sandstone. This information, together with a detailed assessment of anisotropy, is needed to establish Corvio sandstone as a useful laboratory rock-testing standard for well-constrained studies of thermo-hydro-mechanical-chemical coupled phenomena associated with CO2 storage practices and for geological reservoir studies in general. More than 200 core plugs of Corvio sandstone (38.1 and 50 mm diameters, 2:1 length-to-diameter ratio) were used in this characterisation study, with a rock porosity of 21.7 +/- 1.2%, dry density 2036 +/- 32 kg m(-3), and unconfined compressive and tensile strengths of 41 +/- 3.28 and 2.3 +/- 0.14 MPa, respectively. Geomechanical tests show that the rock behaves elastically between approximate to 10 and approximate to 18 MPa under unconfined conditions with associated Young's modulus and Poisson's ratio of 11.8 +/- 2.8 GPa and 0.34 +/- 0.01 GPa, respectively. Permeability abruptly decreases with confining pressure up to approximate to 10 MPa and then stabilises at approximate to 1 mD. Ultrasonic P- and S-wave velocities vary from about 2.8-3.8 km s(-1) and 1.5-2.4 km s(-1), respectively, over confining and differential pressures between 0.1 and 35 MPa, allowing derivation of associated dynamic elastic moduli. Anisotropy was investigated using oriented core plugs for electrical resistivity, elastic wave velocity and attenuation, permeability, and tracer injection tests. Corvio sandstone shows weak transverse isotropy (symmetry axis normal to bedding) of <10% for velocity and <20% for attenuation.
引用
收藏
页码:1293 / 1311
页数:19
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