Morphology of methane hydrate host sediments

Keith W. Jones; Huan Feng; Stanmire Tomov; William J. Winters; Michael Eaton; Devinder Mahajan

Morphology of methane hydrate host sediments

Keith W. Jones, Huan Feng, Stanmire Tomov, William J. Winters, Michael Eaton, Devinder Mahajan

Earth and Environmental Studies

Research output: Contribution to journal › Article › peer-review

Abstract

The morphological features including porosity and grains of methane hydrate host sediments were investigated using synchrotron computed microtomography (CMT) technique. The sediment sample was obtained during Ocean Drilling Program Leg 164 on the Blake Ridge at water depth of 2278.5 m. The CMT experiment was performed at the Brookhaven National Synchrotron Light Source facility. The analysis gave ample porosity, specific surface area, mean particle size, and tortuosity. The method was found to be highly effective for the study of methane hydrate host sediments.

Original language	English
Pages (from-to)	30-32
Number of pages	3
Journal	American Chemical Society, Division of Petroleum Chemistry, Preprints
Volume	50
Issue number	1
State	Published - Feb 2005

Cite this

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abstract = "The morphological features including porosity and grains of methane hydrate host sediments were investigated using synchrotron computed microtomography (CMT) technique. The sediment sample was obtained during Ocean Drilling Program Leg 164 on the Blake Ridge at water depth of 2278.5 m. The CMT experiment was performed at the Brookhaven National Synchrotron Light Source facility. The analysis gave ample porosity, specific surface area, mean particle size, and tortuosity. The method was found to be highly effective for the study of methane hydrate host sediments.",

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AU - Eaton, Michael

AU - Mahajan, Devinder

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AB - The morphological features including porosity and grains of methane hydrate host sediments were investigated using synchrotron computed microtomography (CMT) technique. The sediment sample was obtained during Ocean Drilling Program Leg 164 on the Blake Ridge at water depth of 2278.5 m. The CMT experiment was performed at the Brookhaven National Synchrotron Light Source facility. The analysis gave ample porosity, specific surface area, mean particle size, and tortuosity. The method was found to be highly effective for the study of methane hydrate host sediments.

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Morphology of methane hydrate host sediments

Abstract

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