By Charles E. Taylor, Jonathan T. Kwan
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Extra resources for Advances in the Studies of Gas Hydrates
A well is located in the center of the reservoir that has a radius of 200 m, and is producing gas at a constant bottomhole pressure (BHP) of 4000 kPa from the free gas zone. The permeability of the rock is 20 md, and the relative permeability and capillary pressure functions are depicted in Figure 5 and 6, respectively. The saturation of the phases in the reservoir and the other Figure 4. Initial pressure, temperature and saturation in the reservoir. Effect of Conductive and Convective Heat Flow 49 Figure 5.
A Mass Transport Limited Model for the Growth of Methane and Ethane Gas Hydrates”, Chem. , 49, pp. 1131. 1994. 8. , Bishnoi, P. : “Induction Phenomena in Gas Hydrate Nucleation”, Chem. Eng. , 49, pp. 2075–2084, 1994. 9. Makogon, Y. : “Gas Hydrates- Conclusion: Experiments Illustrate Hydrate Morphology, Kinetics”, OGJ, February 12, 2001. 10. Makogon, Y. : “Gas Hydrates as a Resource and a Mechanism for Transmission”, Proceedings of the SPE annual technical conference and exhibition held in San Antonio, Texas, 29 September-2 October, 2002.
6, Ch. 24, pp. 789–824. 8. Kittel, C. Thermal Physics; Wiley: New York, 1969). 9. Pomeransky, A. ; and Belosludov, V. R. In Architecture of Supramolecular Systems: Trends and Developments, Russian-French Workshop, Program and abstracts; Inst. of Inorg. : Novosibirsk, 2001, pp. 30–31. 10. Klauda, J. ; and Sandler, S. I. Chem. Eng. , 2003, 58, 27. 11. van Hinsberg, M. G. E. PhD Thesis; Univ. of Amsterdam, 1994. 12. Pomeransky, A. ; Belosludov, V. ; and Inerbaev, T. M. This book, p. 130. This page intentionally left blank 3 Phenomenological Modeling of Hydrate Formation and Dissociation Maria Carolina Gonzalez Chacin, Richard G.