Numerical Determination of the Optimized Shape of Salt Caverns for Gas Storage

Document Type : Research Article

Authors

Dept. of Mining and Metallurgy/ Yazd University

10.17383/S2251-6565(15)940911-X

Abstract

Using salt caverns is one of the most developed methods for fluid hydrocarbon storage. Certainty of caverns stability and simultaneously having an economical working gas ratio, are important factors that rarely have been considered in Iran. Considering salt rock characteristics and high overburden, the gravitational stress can be assumed dominant. In situ stress acts as an external pressure and causes cavern convergence. Since conventional rock supports e.g. shotcrete, rock bolt, etc. are not applicable in the salt caverns; the cavern stability can only be achieved by an internal pressure caused by the gas inside the cavern. The paper deals with salt cavern stability analysis for gas storage. Specific geometrical and geotechnical properties (with the general properties of salt domes located in the Southwest of Iran) have been modeled by Phase2 and FLAC3D softwares. Geometrical and mechanical modeling of these caverns in finite difference and finite element in desired depth, determined the minimum and maximum gas pressure for cavern stability and working gas pressure was calculated as well. Comparison of these results implies that carrot shape cavern is more economical.

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[1] Höffler, F., & Kübler, M. (2007). Demand for storage of natural gas in northwestern Europe: Trends 2005–30. Energy Policy, 35(10), 5206-5219
[2] Energy Information Administration; (2002); “The Basic of Underground Natural Gas Storage”.  U.S. Energy Information Administration.
[3] Veil, J. A. (1997). Costs for Off-Site Disposal of Nonhazardous Oil Field Wastes: Salt Caverns Versus other Disposal Methods. ARGONNE NATIONAL LAB IL ENVIRONMENTAL ASSESSMENT AND INFORMATION SCIENCES DIV.
[4] U.S. Department of Energy; Argonne National Laboratory. (2010). “Argonne Home-Environmental Science Division -Programs/Projects”
http://www.ead.anl.gov/titan_rutile.htm; pp. 1-2.
[5] Thoms, R. L., & Gehle, R. M. (2000). A brief history of salt cavern use. In The 8th World Salt Symposium.[S. l.]: Elsevier (Vol. 2, pp. 207-214).
[6] Arbent, M. (2001). “Environmental geology”. Translated by Hormozi, Ahmad. Tehran Univestiy Publication Center.
[7] Warren, J. K. (2006). Evaporites: sediments, resources and hydrocarbons. Springer Science & Business Media.
[8] Veil, J. A. (2000); “Salt cavern & their use for disposal of oil field wastes”, By Argonne National Laboratory for the U.S. Department of Energy.
[9] Istvan, J. A., Evans, L. J., Weber, J. H., & Devine, C. (1997). Rock mechanics for gas storage in bedded salt caverns. International Journal of Rock Mechanics and Mining Sciences, 34(3), 142-e1.
[10] Staudtmeister, K., & Rokahr, R. B. (1997). Rock mechanical design of storage caverns for natural gas in rock salt mass. International Journal of Rock Mechanics and Mining Sciences, 34(3), 300-e1.
[11] Heusermann, S., Rolfs, O., & Schmidt, U. (2003). Nonlinear finite-element analysis of solution mined storage caverns in rock salt using the LUBBY2 constitutive model. Computers & structures, 81(8), 629-638.
[12] Huang, X., & Xiong, J. (2011). Numerical simulation of gas leakage in bedded salt rock storage cavern. Procedia Engineering, 12, 254-259.
[13] Berest, P., Brouard, B., Karimi-Jafari, M., & Van Sambeek, L. (2007). Transient behavior of salt caverns—interpretation of mechanical integrity tests. International Journal of Rock Mechanics and Mining Sciences, 44(5), 767-786.
[14] Bahroudi, A., Talbot, C. J. (2008). “Shapes and timing of structures in Hormouz salt in the Zagros basin”, Hans Ramberg Tectonic Laboratory, Department of Earth science, Uppsala University.
[15] Jackson, M. P. I., Cornelius, R. R., Craig, C. H., Gansser, A., Stocklin, J, Talbot, C. J. (1990). “Salt Diapirs of the Great Kavir, Central Iran”, Geological Society of American.
[16] Hampson, G., Lonergan, L., Sepehr, M., Bahroudi, A. (2005). “Sedimentological and stratigraphic record of salt diapir evolution, Southern Iran”, Department of Earth Science and Engineering , Imperial College.
[17] Rocscience Incorporation. (2005). Phase 2 Manual.
[18] DeVries, K. L.; Mellegard, K. D.; Callahan, G. D. (2002). “Salt Damage Criterion Proof-of-Concept Research Final Report”, Rapid City, South Dakota, pp. 1-20.
[19] DeVries K. L.; Mellegard K. D., Callahan G. D. (2003); “Cavern design using a salt damage criterion: proof-of-concept research final report. In: Proceedings of the SMRI spring meeting”, Houston, 1-18.
[20] Itasca Consulting Group, Inc. (2005). “FLAC 3D Fast Lagrangian Analysisof Continua in 3Dimensions”. Ver. 3.00 User’s Manual. Minneapolis: Itasca.
[21] Lee, B.; Kesler, M. (1975). “A Generalized Thermodynamic Correlation Based on Three-parameter Corresponding States”.  AIChE J., 21(3), 510-527.
[22] Sonntag, R. E., Borgnakke, C., Van Wylen, G. J., & Van Wyk, S. (1998). Fundamentals of thermodynamics (Vol. 6). New York: Wiley.