2022
DOI: 10.1016/j.ijrmms.2021.104958
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Validation of strongly coupled geomechanics and gas hydrate reservoir simulation with multiscale laboratory tests

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Cited by 12 publications
(15 citation statements)
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“…Sequential indicator simulation is a simulation method based on pixel [11] [12] [13]. By calculating the variation function of spatial attribute parameters, a stochastic reservoir model based on the variation function is established.…”
Section: Principle Of Sequential Indication Simulationmentioning
confidence: 99%
“…Sequential indicator simulation is a simulation method based on pixel [11] [12] [13]. By calculating the variation function of spatial attribute parameters, a stochastic reservoir model based on the variation function is established.…”
Section: Principle Of Sequential Indication Simulationmentioning
confidence: 99%
“…To date, only short-term production tests have been performed onshore in Alaska , and Canada , and offshore in Japan , and China, , which have produced encouraging results. Reservoir response modeling , suggests that gas production from methane hydrates increased during the first several years, which is in contrast to production from other resources, such as shale gas. , With the exclusion of the Arctic/Antarctic methane hydrate accumulations and with oceanic methane hydrates representing 99% of the total global methane hydrate resource, , the U.S. Department of Energy, Gulf of Mexico methane hydrate program is focused on the need for offshore reservoir characterization of coarse-grained methane hydrate reservoirs. , …”
Section: Methane Hydrates As a Massive Bridge Fuel Clean-energy Sourcementioning
confidence: 99%
“…As aforementioned, the total entropy variation δ Sl is then balanced in terms of the variations of the following: m J , T l , p l,J , and σ. In Equation (21), sl,J is the internal entropy for material l per unit mass of phase J, i.e., the specific entropy of phase J for the material.…”
Section: Mp Materials and Flow And Heat Constitutive Relationsmentioning
confidence: 99%
“…For Equation (21), note also that the volumetric strain term derived from γ l η l K l δσ l v (σ l v is the mean stress of material l) is negligible because the heat source induced by deformation is trivial considering the typical large heat capacity of rock. However, the heat can induce volume change as expressed in Equations ( 1) and (3); thus, the "one-way" coupling is still valid between heat and geomechanics, i.e., from heat to geomechanics only.…”
Section: Mp Materials and Flow And Heat Constitutive Relationsmentioning
confidence: 99%
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