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Gas hydrates: Unlocking the energy from icy cages
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10.1063/1.3216463
/content/aip/journal/jap/106/6/10.1063/1.3216463
http://aip.metastore.ingenta.com/content/aip/journal/jap/106/6/10.1063/1.3216463

Figures

Image of FIG. 1.
FIG. 1.

Gas clathrate hydrate water cavities: (a) pentagonal dodecahedron , (b) tetrakaidecahedron , (c) hexakaidecahedron , (d) irregular dodecahedron , and (e) icosahedron .

Image of FIG. 2.
FIG. 2.

Burning methane hydrate snowball on the grill (left, courtesy of P. Walz, MBARI, the Monterey Bay Aquarium Research Institute). Crystal structure of sI methane hydrate comprised of and cages with methane guest molecules in blue (right, Ref. 3).

Image of FIG. 3.
FIG. 3.

Schematic showing predicted sigma ranges (sigma is effectively the size of the molecule), where a sI to sII transition (thermodynamic) occurs in a binary system of two sI formers. Reprinted with permission from K. C. Hester, Ph.D. thesis, Colorado School of Mines, 2007.

Image of FIG. 4.
FIG. 4.

Cartoon of PVCap interacting with a partial hydrate cage.

Image of FIG. 5.
FIG. 5.

Raman cell showing the hydrate morphology: (a) before and (b) after the unexpected transformation. Reprinted with permission from J. M. Schicks, R. Naumann, J. Erzinger, K. C. Hester, C. A. Koh, and E. D. Sloan, J. Phys. Chem. B 110, 11468 (2006). Copyright © 2006, American Chemical Society.

Image of FIG. 6.
FIG. 6.

Very high pressure (0.3–2.1 GPa) structural changes in gas hydrates at room temperature. Numerical values (adjacent to square boxes) indicate transition pressures. Hexagonal (sH) and tetragonal (sT) hydrate phases are distinct from sH and sT hydrate structures found at normal pressures (Ref. 1. Reprinted with permission from H. Hirai, T. Tanaka, K. Kawamura, Y. Yamamoto, and Y. Yagi, J. Phys. Chem. Solids 65, 1555 (2005). Copyright © 2006, Elsevier.

Image of FIG. 7.
FIG. 7.

The locations of natural gas hydrate deposits on shore within and beneath the permafrost, and off shore along the continental margins. Reprinted with permission from K. Kvenvolden.

Image of FIG. 8.
FIG. 8.

Resource pyramids of arctic and oceanic hydrated deposits (left) and all other conventional resources (right) in the United States. Reprinted with permission from R. Boswell and T. Collett, 2006.

Image of FIG. 9.
FIG. 9.

Recovered cores containing gas hydrates from Arctic deposits from Mount Elbert, Alaskan North Slope (top left; reprinted with permission from R. Boswell and T. Collett, 2006) and the Mallik Well, MacKenzie Delta, Canada (bottom left; reprinted with permission from T. S. Collett, M. Riedel, J. R. Cochran, R. Boswell, P. Kumar, and A. V. Sathe, unpublished), and from an oceanic deposit in the Krishna-Godavari Basin, India (right; courtesy of M. R. Walsh, CSM).

Image of FIG. 10.
FIG. 10.

Hydrate production methods of depressurization (left), thermal stimulation (middle; for inhibitor injection, hot fluids can be replaced with methanol, glycols, or other chemicals), and exchange (right).

Image of FIG. 11.
FIG. 11.

Mallik2002 short-term production test showing the gas flare from gas produced from hydrate under the permafrost. Reprinted with permission from S. R. Dallimore, T. S. Collett, eds., Scientific Results from the Mallik 2002 Gas Hydrate Production Research Well Program. Copyright © 2005 by Scott Dallimore and Tim Collett.

Image of FIG. 12.
FIG. 12.

The effect of the hydrate formation method on the hydrate growth mechanism. The physical properties of hydrate-bearing sediment depend on the size and distribution of hydrate (black) relative to the sediment grains (gray). Redrawn with permission from W. F. Waite et al., in press.

Image of FIG. 13.
FIG. 13.

Physical (white and yellow hydrate, top) and chemical (Raman spectra: white hydrate) heterogeneities of hydrate mounds in Barkley Canyon. The white hydrate has components up to isobutane in all specimens. Reprinted with permission from K. C. Hester, Ph.D. thesis, Colorado School of Mines, 2007.

Tables

Generic image for table
Table I.

Structural properties of clathrate hydrates (Ref. 1).

Generic image for table
Table II.

Comparison of the mechanical, thermal, and physical properties of ice, sI, and sII hydrates (Ref. 1).

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/content/aip/journal/jap/106/6/10.1063/1.3216463
2009-09-24
2014-04-19
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752b84549af89a08dbdd7fdb8b9568b5 journal.articlezxybnytfddd
Scitation: Gas hydrates: Unlocking the energy from icy cages
http://aip.metastore.ingenta.com/content/aip/journal/jap/106/6/10.1063/1.3216463
10.1063/1.3216463
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