Abstract
The problem of methane hydrate decomposition in a reservoir saturated with a gas and hydrate mixture is investigated numerically. The results of the numerical simulation and an analytic solution obtained in the linear approximation are compared. It is shown that for high-permeability rocks the convective heat transfer in the near-well space of the reservoir predominates over the conductive transfer. This makes the use of intra-well heaters ineffective. It is found that an increase in the reservoir and well pressures and a decrease in the permeability suppress the formation of an extended hydrate dissociation region. Critical diagrams of existence of the frontal decomposition regime are constructed.
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Translated from Izvestiya Rossiiskoi Academii Nauk, Mekhanika Zhidkosti i Gaza, No. 4, 2006, pp. 127–134.
Original Russian Text Copyright © 2006 by Vasil’ev, Popov, and Tsypkin.
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Vasil’ev, V.I., Popov, V.V. & Tsypkin, G.G. Numerical investigation of the decomposition of gas hydrates coexisting with gas in natural reservoirs. Fluid Dyn 41, 599–605 (2006). https://doi.org/10.1007/s10697-006-0078-z
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DOI: https://doi.org/10.1007/s10697-006-0078-z