Dissipation of overpressure into ambient mudrocks during geological carbon dioxide storage

Energy Procedia

Volumn 37, Issue , 2013, Pages 4457-4464

  Chang, Kyung Won ^a   Hesse, Marc A ^a   Nicot, Jean Philippe ^b  

^a UNIVERSITY OF TEXAS AT AUSTIN   (United States)

^b UNIVERSITY OF TEXAS AT AUSTIN   (United States)

Author keywords

Carbon dioxide storage; Mudrock; Overpressure; Post injection; Radius of review; Storage capacity

Indexed keywords

EID: 84898750333     PISSN: 18766102     EISSN: None     Source Type: Conference Proceeding    
DOI: 10.1016/j.egypro.2013.06.350     Document Type: Conference Paper

References (21)

1. 2storage capacities?, Oil & Gas Sci. Tech. Rev. IFP Energ. Nouvelles 2011; 66, p. 81-92.
2. Thornhill, J.T., T.E. Short, and L. Silka, Application of the area of review concept, Ground Water 1982; 20(1), p. 32-38.
3. Van der Kamp, G. and J.E. Gale, Theory of earth tide and barometric effect in porous formations with compressible grains, Water Resour. Res. 1983; 19(2), p. 538-544.
4. Green, D.H. and H.F. Wang, Specific storage as a poroelastic coefficient, Water Resour. Res. 1990; 26(7), p. 1631-1637.
5. Freeze, R.A. and J.A. Cherry, Groundwater, Prentice Hall; 1979.
6. Birkholzer, J.T., J.-P. Nicot, C.M. Oldenburg, Q. Zhou, S. Kraemer, and K. Bandilla, Brine flow up a well caused by pressure perturbation from carbon sequestration: Static and dynamic evolutions, Int. J. Greenh. Gas Cont. 2011; 5(4), p. 850-861.
7. Neuzil, C.E., How permeable are clays and shales?, Water Resour. Res. 1994; 30, p. 145-150.
8. Dewhurst, D.N., Y.L. Yang, and A.C. Aplin, Permeability and fluid flow in natural mudstones, in Muds Mudstones: Physical and fluid Flow Properties, edited by A.C. Aplin et al., Geol. Soc. Spec. Publ. 1999; 158, p. 23-43.
9. Domenico, P.A. and F.W. Schwartz, Physical and Chemical Hydrology, John Wiley & Sons Inc;1998.
10. Hovorka, S.D., C. Doughty, P.R. Knox, C.T. Green, K. Pruess, and S.M. Benson, Evaluation of brine-bearing sands of the Frio formation, Upper Texas Gulf Coast for geological sequestration of CO2, Conference Proceedings, In: First National Conference on Carbon Sequestration, NETL; 2001.
11. Hart, D.J., K.R. Bradbury, and D.T. Feinstein, The vertical hydraulic conductivity of an aquitard at two spatial scales, Ground Water 2006; 44(2), p. 201-211.
12. 2storage capacity in closed and semi-closed saline formations, Int. J. Greenh. Gas Con. 2008; 1(2), p. 626-639.
13. 2 storage in saline aquifers: A sensitivity study on the pressure response in stratified systems, Int. J. Greenh. Gas Con. 2009; 3(2), p. 181-194.
14. 2 as a greenhouse gas mitigation measure, Petrol. Geosci. 2009; 15, p. 59-73.
15. 2 sequestration operations, Energy Procedia 2009; 1(1), p. 4411-4418.
16. Chang, K.W., M.A. Hesse, and J.-P. Nicot, Reduction of lateral pressure propagation due to dissipation into ambient mudrocks during geological carbon dioxide storage, submitted to Water Resour. Res. (under revision).
17. Theis, C.V., The relationship between the lowering of the Piezometric surface and the rate and duration of discharge of a well using ground water storage, Trans. Am. Geophys. Union 1935; 16, p. 519-524.
18. Van Poolen, H., Radius of drainage and stabilization time equations, Oil Gas J. 1964; p. 138-146.
19. Talwani, P. and S. Acree, Pore pressure diffusion and the mechanism of reservoir-induced seismicity, Pure Appl. Geophys. 1984; 122(6), p.947-965.
20. 2in geological media in response to climate change, Environ. Geol. 2003; 44, p.277-289.
21. Michael, K., A. Golab, V. Shulakova, J. Ennis-King, G. Allison, S. Sharma, and T. Aiken, Geological storage of CO2 in saline aquifers - A review of the experience from existing storage operations, Int. J. Greenh. Gas Con. 2010; 5, p. 270-280.