Abstract

We present a fully coupled thermo-hydro-mechanical formulation for the simulation of sediment deformation, fluid and heat transport and fluid/solid phase transformations occurring in methane hydrate geological systems. We reformulate the governing equations of energy and mass balance of the Code_Bright simulator to incorporate hydrate as a new pore phase. The formulation also integrates the constitutive model Hydrate-CASM to capture the effect of hydrate saturation in the mechanical response of the sediment. The thermo-hydraulic capabilities of the formulation are validated against the results from a series of state-of-the-art simulators involved in the first international gas hydrate code comparison study developed by the NETL-USGS. The coupling with the mechanical formulation is investigated by modeling synthetic dissociation tests and validated by reproducing published experimental data from triaxial tests performed in hydrate-bearing sands dissociated via depressurization. Our results show that the formulation captures the dominant mass and heat transfer phenomena occurring during hydrate dissociation and reproduces the stress release and volumetric deformation associated with this process. They also show that the hydrate production method has a strong influence on sediment deformation.

Highlights

  • Methane hydrates hold vast amounts of methane gas below the sea floor and in permafrost regions [1]

  • We reproduce the benchmark problem P2 proposed in the NETL-USGS first international gas hydrate code comparison study

  • Hydrate dissociation has a significant effect on the THM properties of MHBS and may cause its mechanical destabilization

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Summary

Introduction

Methane hydrates hold vast amounts of methane gas below the sea floor and in permafrost regions [1]. Current techniques for methane production from hydrate include thermal stimulation, depressurization, and inhibitor injection [6,7], among which, depressurization is deemed the most mature approach. These techniques perturb the thermodynamic and chemical conditions of the reservoir to destabilize the hydrate phase and force its dissociation into water and gas. Over the last 20 years, several numerical models have been proposed to simulate the behavior of gas hydrate reservoirs. Modeling efforts focused on evaluating the productivity of methane

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