A Geomechanical Model for Gas Hydrate Bearing Sediments Incorporating High Dilatancy, Temperature, and Rate Effects

Zhou, Bohan; Sanchez, Marcelo; Oldecop, Luciano; Santamarina, J. Carlos

doi:10.3390/en15124280

Title: A Geomechanical Model for Gas Hydrate Bearing Sediments Incorporating High Dilatancy, Temperature, and Rate Effects

Journal Article · Fri Jun 10 00:00:00 EDT 2022 · Energies

DOI:https://doi.org/10.3390/en15124280· OSTI ID:1872116

Zhou, Bohan; Sanchez, Marcelo;

;

The geomechanical behavior of methane hydrate bearing sediments (MHBS) is influenced by many factors, including temperature, fluid pressure, hydrate saturation, stress level, and strain rate. The paper presents a visco-elastoplastic constitutive model for MHBS based on an elastoplastic model that incorporates the effect of hydrate saturation, stress history, and hydrate morphology on hydrate sediment response. The upgraded model is able to account for additional critical features of MHBS behavior, such as, high-dilatancy, temperature, and rate effects. The main components and the mathematical formulation of the new constitutive model are described in detail. The upgraded model is validated using published triaxial tests involving MHBS. The model agrees overly well with the experimental observations and is able to capture the main features associated with the behavior of MHBS.

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Research Organization:: Texas A & M Univ., College Station, TX (United States)

Sponsoring Organization:: USDOE Office of Fossil Energy (FE)

Grant/Contract Number:: FE0013889

OSTI ID:: 1872116

Alternate ID(s):: OSTI ID: 1981139

Journal Information:: Energies, Journal Name: Energies Vol. 15 Journal Issue: 12; ISSN 1996-1073

Publisher:: MDPI AGCopyright Statement

Country of Publication:: Switzerland

Language:: English

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