Numerical modelling of internal erosion during hydrate dissociation based on multiphase mixture theory. (4th December 2019)

• Record Type: Journal Article
• Authors: Akaki, Toshifumi; Kimoto, Sayuri
• Is Part Of: International journal for numerical and analytical methods in geomechanics. Volume 44:Number 2(2020)
• Page Start: 327
• Page End: 350
• Publication Date: 2019-12-04
• Subjects: internal erosion -- methane hydrate -- multiphase mixture theory; Soil mechanics -- Mathematics -- Periodicals; Rock mechanics -- Mathematics -- Periodicals; 624.1510151
• DOI: 10.1002/nag.3023
• Languages: English
• ISSNs: 0363-9061

Abstract

Summary: It has been reported that sand production, which is a simultaneous production of soil particles along with gas and water into a production well, forced to terminate the operation during the world's first offshore methane production test from hydrate‐bearing sediments in the Eastern Nankai Tough. The sand production is induced by internal erosion, which is the detachment and migration of soil particles from soil skeleton due to seepage flow. The inflow of the eroded soil particles into the production well leads to damage of the production devices. In the present study, a numerical model to predict the chemo‐thermo‐mechanically coupled behavior including internal erosion during hydrate dissociation has been formulated based on the multiphase mixture theory. In the proposed model, the internal erosion is expressed as mass transition of soil particles from soil skeleton to the fluidized soil particles. Since the internal erosion is considered to depend on the soil particle size, mass of soil particles are divided into several groups that have different representative particle diameters, and the constitutive equations for the onset condition and the mass transition rate of the internal erosion are formulated for each group. Also, transportation of soil particles in the liquid phase is formulated for each particle size group in the proposed model. Finally, a simulation of the methane gas production from the hydrate‐bearing sediment by depressurization method is presented, and the internal erosion and the dissociation behavior are discussed.