The hydrate morphology in sandy methane hydrate (MH)-bearing sediment (MHBS) is commonly classified as pore-filling, cementation, grain-coating and load-bearing. This paper presents a numerical investigation into the mechanical behaviour of coexistence-type MHBS using the discrete-element method (DEM). The coexistence type is represented as a combination of pore-filling and cementation types. For MHBS with a given MH saturation (S MH), the relative content of pore-filling and cementation is characterised by the cement ratio λ (λ = 0 means pure pore-filling and λ = 1 means pure cementation). A series of drained triaxial compression tests is simulated, and micromechanical variables such as bond breakage are examined. The results show that (a) the strength and dilatancy of the coexistence-type MHBS are higher when the cement ratio is larger. The normalised strength and secant modulus increase linearly with the cement ratio. (b) When the cement ratio increases, the critical-state line on the mineral void ratio e cr–ln p′ projection shifts towards a higher position and the bond breakage ratio is larger. (c) The shear stress of the coexistence-type MHBS with cementation is affected by the MH generation process due to the MH bond breakages.
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5 May 2023
Research Article|
August 14 2019
DEM simulation of coexistence type methane hydrate bearing sediments
Jun Liu, BEng;
Jun Liu, BEng
PhD research student
Department of Geotechnical Engineering, College of Civil Engineering, Tongji University, Shanghai, China
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Mingjing Jiang, PhD
Department of Civil Engineering, School of Civil Engineering, Tianjin University, Tianjin, China
(corresponding author: mingjing.jiang@tju.edu.cn)
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(corresponding author: mingjing.jiang@tju.edu.cn)
Publisher: Emerald Publishing
Received:
March 10 2019
Accepted:
August 13 2019
Online ISSN: 2051-803X
ICE Publishing: All rights reserved
2023
Environmental Geotechnics (2023) 10 (3): 206–217.
Article history
Received:
March 10 2019
Accepted:
August 13 2019
Citation
Liu J, Jiang M (2023), "DEM simulation of coexistence type methane hydrate bearing sediments". Environmental Geotechnics, Vol. 10 No. 3 pp. 206–217, doi: https://doi.org/10.1680/jenge.19.00066
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