TY - JOUR
T1 - The effects of lateral variations in rock composition and texture on anhydrite caprock integrity of CO2 storage systems
AU - Hangx, S. J T
AU - Pluymakers, A. M H
AU - Ten Hove, A.
AU - Spiers, C. J.
PY - 2014
Y1 - 2014
N2 - We investigated the effect of rock texture and composition on the mechanical strength and volumetric behaviour of anhydrite-rich caprock. Conventional triaxial experiments were performed at 80°C, confining pressures of 1.5-35MPa and strain rates of ~10-5s-1, both dry and in the presence of fluids. We determined the failure envelope, and the effect of fluids upon it, for anhydrite displaying an equigranular texture consisting of euhedral grains. We observed a general pattern of increasing peak compressive strength with increasing confining pressure, consistent with a previous study on anhydrite from the same formation, which showed an irregular texture consisting of interlocking, acicular grains embedded in a fine-grained matrix. The peak strength of euhedral anhydrite was found to be 15-65% lower than that of acicular anhydrite. No chemical effects were observed for the fluids tested. Hydraulic fracturing experiments showed the tensile strength to be approximately 4MPa for euhedral and 6MPa for acicular anhydrite. We combined the failure envelopes with simple, analytical calculations on the effect of cooling on in-situ stress, showing that tensile caprock failure due to cooling would be unlikely for both types of anhydrite, assuming a hypothetical reservoir at a depth of 3800m. However, it should be noted that tensile failure may pose an issue for shallower reservoirs or weaker caprock formations.
AB - We investigated the effect of rock texture and composition on the mechanical strength and volumetric behaviour of anhydrite-rich caprock. Conventional triaxial experiments were performed at 80°C, confining pressures of 1.5-35MPa and strain rates of ~10-5s-1, both dry and in the presence of fluids. We determined the failure envelope, and the effect of fluids upon it, for anhydrite displaying an equigranular texture consisting of euhedral grains. We observed a general pattern of increasing peak compressive strength with increasing confining pressure, consistent with a previous study on anhydrite from the same formation, which showed an irregular texture consisting of interlocking, acicular grains embedded in a fine-grained matrix. The peak strength of euhedral anhydrite was found to be 15-65% lower than that of acicular anhydrite. No chemical effects were observed for the fluids tested. Hydraulic fracturing experiments showed the tensile strength to be approximately 4MPa for euhedral and 6MPa for acicular anhydrite. We combined the failure envelopes with simple, analytical calculations on the effect of cooling on in-situ stress, showing that tensile caprock failure due to cooling would be unlikely for both types of anhydrite, assuming a hypothetical reservoir at a depth of 3800m. However, it should be noted that tensile failure may pose an issue for shallower reservoirs or weaker caprock formations.
KW - Failure envelope
KW - Geomechanical testing
KW - Tensile strength
KW - Triaxial compression
KW - Zechstein formation
UR - http://www.scopus.com/inward/record.url?scp=84899070731&partnerID=8YFLogxK
U2 - 10.1016/j.ijrmms.2014.03.001
DO - 10.1016/j.ijrmms.2014.03.001
M3 - Article
AN - SCOPUS:84899070731
SN - 1365-1609
VL - 69
SP - 80
EP - 92
JO - International Journal of Rock Mechanics and Mining Sciences
JF - International Journal of Rock Mechanics and Mining Sciences
ER -