Simulation of Gas Production from Multilayered Hydrate-Bearing Media with Fully Coupled Flow, Thermal, Chemical and Geomechanical Processes Using TOUGH + Millstone. Part 1: Numerical Modeling of Hydrates

被引:0
作者
George J. Moridis
Alejandro F. Queiruga
Matthew T. Reagan
机构
[1] Texas A&M University,Petroleum Engineering Department
[2] Lawrence Berkeley National Laboratory,Energy Geosciences Division
来源
Transport in Porous Media | 2019年 / 128卷
关键词
Methane hydrates; Reservoir simulation; Geomechanics; Coupled processes;
D O I
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中图分类号
学科分类号
摘要
TOUGH + Millstone has been developed for the analysis of coupled flow, thermal and geomechanical processes associated with the formation and/or dissociation of CH4-hydrates in geological media. It is composed of two constituent codes: (a) a significantly enhanced version of the TOUGH + HYDRATE simulator, V2.0, that accounts for all known flow, physical, thermodynamic and chemical processes associated with the behavior of hydrate-bearing systems undergoing changes and includes the most recent advances in the description of the system properties, coupled seamlessly with (b) Millstone V1.0, a new code that addresses the conceptual, computational and mathematical shortcomings of earlier codes used to describe the geomechanical response of these systems. The capabilities of TOUGH + Millstone are demonstrated in the simulation and analysis of the system flow, thermal and geomechanical behavior during gas production from a realistic complex offshore hydrate deposit. In the first paper of this series, we discuss the physics underlying the T + H hydrate simulator, the constitutive relationships describing the physical, chemical (equilibrium and kinetic) and thermal processes, the states of the CH4+H2O\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\hbox {CH}}_4 + {\hbox {H}}_2 \hbox {O}$$\end{document} system and the sources of critically important data, as well as the mathematical approaches used for the development of the of mass and energy balance equations and their solution. Additionally, we provide verification examples of the hydrate code against numerical results from the simulation of laboratory and field experiments.
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页码:405 / 430
页数:25
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共 131 条
  • [1] Anderson BJ(2011)Regional long-term production modeling from a single well test, Mount Elbert gas hydrate stratigraphic test well Alaska North Slope. Mar. Pet. Geol. 28 493-501
  • [2] Kurihara M(1966)Properties of porous media affecting fluid flow ASCE J. Irrig. Drain Div. 6 61-679
  • [3] White MD(1988)Generalized multiparameter correlation for nonpolar and polar fluid transport properties Ind. Eng. Chem. Res. 27 671-384
  • [4] Moridis GJ(2008)Effective correlation of apparent gas permeability in tight porous media Transp. Porous Media 83 375-147
  • [5] Wilson SJ(2001)Determination of activation energy and intrinsic rate constant of methane gas hydrate decomposition Can. J. Chem. Eng. 79 143-41
  • [6] Pooladi-Darvish M(1954)The interrelation between gas and oil relative permeabilities Prod. Mon. 19 38-268
  • [7] Gaddipati M(1901)A numerical study of microscale flow behavior in tight gas and shale gas reservoir systems Wasserbewewegung durch boden. ZVDI 45 1781-3685
  • [8] Masuda Y(2011)Diffusion of halogenated hydrocarbons in helium: the effect of structure on collision cross sections Transp. Porous Media 90 253-397
  • [9] Collett TS(1969)A rapid accurate unsteady-state Klinkenberg parameter J. Phys. Chem. 73 3679-1653
  • [10] Hunter RB(1972)Kinetics of methane hydrate decomposition SPE J. 12 383-539