Gas Hydrates in Permafrost: Distinctive Effect of Gas Hydrates and Ice on the Geomechanical Properties of Simulated Hydrate‐Bearing Permafrost Sediments

Jinhai Yang, Aliakbar Hassanpouryouzband, Bahman Tohidi, Evgeny Chuvilin, Boris Bukhanov, Vladimir Istomin, Alexey Cheremisin

Research output: Contribution to journalArticle

Abstract

The geomechanical stability of the permafrost formations containing gas hydrates in the Arctic is extremely vulnerable to global warming and the drilling of wells for oil and gas exploration purposes. In this work the effect of gas hydrate and ice on the geomechanical properties of sediments was compared by triaxial compression tests for typical sediment conditions: unfrozen hydrate-free sediments at 0.3 °C, hydrate-free sediments frozen at −10 °C, unfrozen sediments containing about 22 vol% methane hydrate at 0.3 °C, and hydrate-bearing sediments frozen at −10 °C. The effect of hydrate saturation on the geomechanical properties of simulated permafrost sediments was also investigated at predefined temperatures and confining pressures. Results show that ice and gas hydrates distinctively influence the shearing characteristics and deformation behavior. The presence of around 22 vol% methane hydrate in the unfrozen sediments led to a shear strength as strong as those of the frozen hydrate-free specimens with 85 vol% of ice in the pores. The frozen hydrate-free sediments experienced brittle-like failure, while the hydrate-bearing sediments showed large dilatation without rapid failure. Hydrate formation in the sediments resulted in a measurable reduction in the internal friction, while freezing did not. In contrast to ice, gas hydrate plays a dominant role in reinforcement of the simulated permafrost sediments. Finally, a new physical model was developed, based on formation of hydrate networks or frame structures to interpret the observed strengthening in the shear strength and the ductile deformation.

Original languageEnglish
Pages (from-to)2551-2563
Number of pages13
JournalJournal of Geophysical Research: Solid Earth
Volume124
Issue number3
Early online date27 Feb 2019
DOIs
Publication statusPublished - Mar 2019

Fingerprint

permafrost
Gas hydrates
Permafrost
Ice
gas hydrate
hydrates
Hydrates
Sediments
sediments
ice
gases
sediment
Bearings (structural)
Methane
Shear strength
shear strength
effect
methane
oil exploration
ductile deformation

Keywords

  • gas hydrate
  • geomechanical properties
  • ice
  • microhydrate networks
  • sediments
  • triaxial shearing

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

Yang, Jinhai ; Hassanpouryouzband, Aliakbar ; Tohidi, Bahman ; Chuvilin, Evgeny ; Bukhanov, Boris ; Istomin, Vladimir ; Cheremisin, Alexey. / Gas Hydrates in Permafrost: Distinctive Effect of Gas Hydrates and Ice on the Geomechanical Properties of Simulated Hydrate‐Bearing Permafrost Sediments. In: Journal of Geophysical Research: Solid Earth. 2019 ; Vol. 124, No. 3. pp. 2551-2563.
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abstract = "The geomechanical stability of the permafrost formations containing gas hydrates in the Arctic is extremely vulnerable to global warming and the drilling of wells for oil and gas exploration purposes. In this work the effect of gas hydrate and ice on the geomechanical properties of sediments was compared by triaxial compression tests for typical sediment conditions: unfrozen hydrate-free sediments at 0.3 °C, hydrate-free sediments frozen at −10 °C, unfrozen sediments containing about 22 vol{\%} methane hydrate at 0.3 °C, and hydrate-bearing sediments frozen at −10 °C. The effect of hydrate saturation on the geomechanical properties of simulated permafrost sediments was also investigated at predefined temperatures and confining pressures. Results show that ice and gas hydrates distinctively influence the shearing characteristics and deformation behavior. The presence of around 22 vol{\%} methane hydrate in the unfrozen sediments led to a shear strength as strong as those of the frozen hydrate-free specimens with 85 vol{\%} of ice in the pores. The frozen hydrate-free sediments experienced brittle-like failure, while the hydrate-bearing sediments showed large dilatation without rapid failure. Hydrate formation in the sediments resulted in a measurable reduction in the internal friction, while freezing did not. In contrast to ice, gas hydrate plays a dominant role in reinforcement of the simulated permafrost sediments. Finally, a new physical model was developed, based on formation of hydrate networks or frame structures to interpret the observed strengthening in the shear strength and the ductile deformation.",
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Gas Hydrates in Permafrost: Distinctive Effect of Gas Hydrates and Ice on the Geomechanical Properties of Simulated Hydrate‐Bearing Permafrost Sediments. / Yang, Jinhai; Hassanpouryouzband, Aliakbar; Tohidi, Bahman; Chuvilin, Evgeny; Bukhanov, Boris; Istomin, Vladimir; Cheremisin, Alexey.

In: Journal of Geophysical Research: Solid Earth, Vol. 124, No. 3, 03.2019, p. 2551-2563.

Research output: Contribution to journalArticle

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AU - Hassanpouryouzband, Aliakbar

AU - Tohidi, Bahman

AU - Chuvilin, Evgeny

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AU - Istomin, Vladimir

AU - Cheremisin, Alexey

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