Thermal conductivity of methane hydrate-bearing Ulleung Basin marine sediments: Laboratory testing and numerical evaluation

Young Jin Kim, Tae Sup Yun

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

The thermal conductivity of gas hydrate-bearing sediments is a key parameter used to evaluate the heat transfer process relevant to phase transformation during gas hydrate production and to assess heat flux properties within the hydrate stability zone. Relatively few thermal conductivity values for in-situ hydrate-bearing sediments and laboratory hydrate-bearing sediments have been reported for under saturated conditions with vertical effective stress. In this study, we used sandy sediments obtained during the Ulleung Basin Gas Hydrate Expedition 2 (UBGH2) Expedition in Korea to synthesize methane hydrate-bearing sediments with saline pore fluid. The transient plane source method was implemented to measure the thermal conductivity of specimens with variable gas hydrate saturations. The measured thermal conductivity was ~1.47W/m/K and was independent of hydrate saturation. Results from additional tests of ice- and water-unsaturated sediments were also compared to our findings. Both geometric mean and 3D thermal network models corroborated the experimentally measured thermal conductivities assuming expected physical properties.

Original languageEnglish
Pages (from-to)77-84
Number of pages8
JournalMarine and Petroleum Geology
Volume47
DOIs
Publication statusPublished - 2013 Nov 1

Fingerprint

thermal conductivity
hydrates
marine sediment
sediments
methane
gas hydrate
evaluation
basin
sediment
expeditions
saturation
gases
effective stress
heat flux
heat transfer
laboratory
physical property
Korea
ice
phase transformations

All Science Journal Classification (ASJC) codes

  • Oceanography
  • Geophysics
  • Geology
  • Economic Geology
  • Stratigraphy

Cite this

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