Abstract
Permeability and thermal conductivity of natural gas hydrate sediments were characterized using a microfocus X-ray computed tomography (CT) technique. The free-gas spaces, sand particles, and hydrates or ices were identified from the obtained three-dimensional X-ray CT images, from which continuous pore networks were identified. The absolute permeability of the sediment correlated well increased with the ratio of parallel to vertical directions of continuous pore numbers. This fact indicates that the pore network in sediment can be useful for assessment of permeability. In order to characterize the thermal conductivity of methane hydrate sediments, a homogenization method was applied to microfocus X-ray CT images. The thermal conductivity calculated from three dimensional X-ray CT images was good agreement to those measured by the hot disk method, when the thermal conductivity of sand particles is 0.5 W/mK. These results demonstrated that the microfocus X-ray CT imaging can be effective for studying material flow and thermo-mechanical properties of natural gas hydrate sediments.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
More From: Journal of the Japanese Association for Petroleum Technology
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.