Figure 9. The Advanced Light Source at LBNL, and use of the Beamline 8.3.2 to derive by means of x-ray microtomography relative permeability and capillary pressure relationships of <strong>hydrate</strong>-bearing media based on pore structure data. SUMMARY We discuss the range of activities at Lawrence Berkeley National Laboratory in support of <strong>gas</strong> production from natural <strong>hydrate</strong>s. Numerical simulation of depressurization-induced <strong>gas</strong> production indicates that Class 1 and 2 <strong>hydrate</strong> deposits hold significant promise as potential energy sources because they can yield large <strong>gas</strong> volumes at high rates using conventional production technology. In Class 3 deposits, neither pure depressurization (when S H is sufficiently low to permit significant flow) nor thermal stimulation (when S H >70%, thus severely reducing permeability) results in commercially viable <strong>gas</strong> production. Class 4 deposits are not promising production targets. We developed a laboratory program (closely coordinated with the simulation studies) to obtain parameters and relationships describing the thermal, thermodynamic, hydraulic and kinetic properties of <strong>hydrate</strong>-bearing media that are important in predicting <strong>gas</strong> production. An important feature of the laboratory studies is the use of x-ray CT scanning and microtomography to describe the strong spatial and temporal heterogeneity of <strong>hydrate</strong>s in porous media. Finally, we discuss briefly the LBNL studies in support of field tests of <strong>gas</strong> production from <strong>hydrate</strong>s. ACKNOWLEDGMENT This work was supported by the Assistant Secretary for Fossil Energy, Office of Natural Gas and Petroleum Technology, through the National Energy Technology Laboratory, under the U.S. Department of Energy, Contract No. DE-AC03-76SF00098. The authors are indebted to John Apps and Dan Hawkes for their thorough review and their insightful comments. 62 New Energy Resources in the <strong>CCOP</strong> Region - Gas Hydrates and Coalbed Methane
REFERENCES Sloan, E.D., 1998, Clathrate Hydrates of Natural Gases, Marcel Dekker, Inc., New York, NY. Gupta, A., T. Kneafsey, G.J. Moridis, Y. Seol, M.B. Kowalsky, and E.D. Jr. Sloan, 2006 Methane <strong>hydrate</strong> thermal conductivity in a large heterogeneous porous sample, J. Phys. Chem. B, 10.1021/jp0619639 (LBNL-59088). Kneafsey, T., L. Tomutsa, G.J. Moridis, Y. Seol, B. Freifeld, C.E. Taylor and A. Gupta, Methane <strong>hydrate</strong> formation and dissociation in a core-scale partially saturated sand sample, In Press, J. Petr. Sci. Eng., (LBNL-59087, 2005). Moridis, G.J. and T.S. Collett, 2003, Strategies for <strong>gas</strong> production from <strong>hydrate</strong> accumulations under various geologic conditions, LBNL-52568, Lawrence Berkeley National Laboratory, Berkeley, CA. Moridis, G.J., T.S. Collett, S.R. Dallimore, T. Satoh, S. Hancock and B. Weatherhill, 2004, Numerical studies of <strong>gas</strong> production scenarios from several CH 4 -<strong>hydrate</strong> accumulations at the Mallik site, Mackenzie Delta, Canada”, J. Petr. Sci. Eng., Vol. 43, 219-238. Moridis, G.J., M.B. Kowalsky and K. Pruess, 2005a, TOUGH-Fx/HYDRATE v1.0 User’s Manual: A code for the simulation of system behavior in <strong>hydrate</strong>-bearing geologic media, LBNL-58950, Lawrence Berkeley National Laboratory, Berkeley, CA (2005). Moridis, G.J., M.B. Kowalsky and K. Pruess, 2005b, Depressurization-induced <strong>gas</strong> production from Class 1 <strong>hydrate</strong> deposits, SPE 97266, 2005 SPE Annual Technical Conference and Exhibition, Dallas, Texas, U.S.A., 9–12 October 2005. Moridis, G.J., Y. Seol and T. Kneafsey, 2005c, Studies of reaction kinetics of methane <strong>hydrate</strong> dissociation in porous media, Paper 1004, Proc. 5 th International Conf. on Gas Hydr., 21- 30 (LBNL-57298). Moridis, G.J., T.S. Collett, S.R. Dallimore, T. Inoue and T. Mroz, 2005d, Analysis and interpretation of the thermal test of <strong>gas</strong> <strong>hydrate</strong> dissociation in the JAPEX/JNOC/GSC Mallik 5L-38 <strong>gas</strong> <strong>hydrate</strong> production research well, Geological Survey of Canada, Bulletin 585, S.R. Dallimore and T. Collett, Eds., (LBNL-57296). Moridis, G.J. and M. Kowalsky, 2006, Gas production from unconfined Class 2 <strong>hydrate</strong> accumulations in the oceanic subsurface, Chapter 7, in Economic Geology of Natural Gas Hydrates, M. Max, A.H. Johnson, W.P. Dillon and T. Collett, Eds., Kluwer Academic/Plenum Publishers, 249-266 (LBNL-57299). Moridis, G.J. and E.D. Sloan, 2006, Gas production potential of disperse low-saturation <strong>hydrate</strong> accumulations in oceanic sediments, LBNL-52568, Lawrence Berkeley National Laboratory, Berkeley, CA. New Energy Resources in the <strong>CCOP</strong> Region - Gas Hydrates and Coalbed Methane 63
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Coordinating Committee for Geoscien
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Thematic Session on New Energy Reso
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CONTENTS Page OPENING REMARKS……
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OPENING REMARKS by Chen Shik Pei Di
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WELCOME ADDRESS by Tai-Sup Lee Pres
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- Page 102 and 103: REFERENCES Collett, T.S. and Kuuskr
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In the early stage of back-arc open
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PART II COALBED METHANE (CBM)
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Supply and demand infrastructure of
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Amisan, Jogyeri, Baegunsa, and Seon
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PROPERTIES OF ANTHRACITE The coals
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Table 4. Average chemical compositi
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CONCLUSIONS 1. Most of the coals em
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INTRODUCTION Coal (total reserves 2
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ีีีีีีีีี ั ิ
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RESULTS By Government: The outcomes
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The gas composition (12 samples ana
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Table 4. Coal Depth Interval Hole N
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The results of studies made on 11 c
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CONCLUSION CBM is still hoped to be
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The Government of Indonesia through
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The Berau basin is a major coal pro
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PP: CBM - 1 Rambutan (GOI Sponsor)
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Overview of Project for CO 2 Seques
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The organic geochemistry research g
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3.5 25 3.0 20 Ar(%) C O 2(%) 2.5 2
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20 8 10 0 6 δ13C of CO2(‰) -10 -
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Figure 1. Index map of Akabira Coal
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ORIGIN OF AKABIRA CBM In Akabira mi