Coupled Effects of Capillary Pressure and Relative Permeability on Gas Production Behavior During Hydrate Depressurization

Capillary pressure and relative permeability are two key factors governing gas–water two-phase flow during hydrate depressurization; however, their relative contributions to gas production and the coupling mechanisms remain poorly understood. In this study, a unified and consistent framework has been developed to examine the coupled effects of capillary pressure and relative permeability for gas–water flow during hydrate depressurization. More specifically, an empirical relationship based on the van Genuchten (VG) model has been obtained for the entry pressure P0 and the shape parameter m, together with their representative ranges, by regressing the capillary pressure data from hydrate-bearing sediments collected from the public domain. Then, a numerical model was constructed to quantify the individual and coupled effects of capillary pressure and relative permeability on gas production in a target hydrate formation. The simulations employed fixed P0 values and prescribed relative permeability curves, without dynamically updating during hydrate dissociation. Across the compiled datasets, P0 is found to decrease inversely with pore radius and increase as a power-law function with hydrate saturation, whereas m exhibits considerable scatter in both sand-dominated (0.62–0.82) and silt-dominated (0.52–0.85) sediments. Within the tested VG model, parameter ranges, and Shenhu reservoir conditions, capillary pressure primarily suppresses local gas migration by enhancing water retention, with its limited impact on gas production, while cumulative gas production is overestimated without considering capillary pressure. In contrast, relative permeability plays a dominant role in hydrate production by directly controlling gas and water flow capacity and influencing pressure propagation. This study clarifies the relative roles and coupling mechanisms of capillary pressure and relative permeability during hydrate depressurization and provides a practical basis for selecting van Genuchten parameters and conducting flow-function sensitivity analyses in hydrate-bearing reservoirs.

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Publication Details

Journal
Journal of Marine Science and Engineering
Published
2026-10-30
DOI
https://doi.org/10.3390/jmse14212034
Primary Topic
Methane Hydrates and Related Phenomena
Type
article
Field-Weighted Citation Impact
0.00

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article

Coupled Effects of Capillary Pressure and Relative Permeability on Gas Production Behavior During Hydrate Depressurization

Chunsheng Ji, Dan Zhao, Daoyong Tony Yang, Pengqi Liu et al.
1 links
Journal of Marine Science and Engineering
Methane Hydrates and Related Phenomena
article

Coupled Effects of Capillary Pressure and Relative Permeability on Gas Production Behavior During Hydrate Depressurization

Chunsheng Ji, Dan Zhao, Daoyong Tony Yang, Pengqi Liu, Wei Zhang, Yurong Jin
article en

Abstract

Capillary pressure and relative permeability are two key factors governing gas–water two-phase flow during hydrate depressurization; however, their relative contributions to gas production and the coupling mechanisms remain poorly understood. In this study, a unified and consistent framework has been developed to examine the coupled effects of capillary pressure and relative permeability for gas–water flow during hydrate depressurization. More specifically, an empirical relationship based on the van Genuchten (VG) model has been obtained for the entry pressure P0 and the shape parameter m, together with their representative ranges, by regressing the capillary pressure data from hydrate-bearing sediments collected from the public domain. Then, a numerical model was constructed to quantify the individual and coupled effects of capillary pressure and relative permeability on gas production in a target hydrate formation. The simulations employed fixed P0 values and prescribed relative permeability curves, without dynamically updating during hydrate dissociation. Across the compiled datasets, P0 is found to decrease inversely with pore radius and increase as a power-law function with hydrate saturation, whereas m exhibits considerable scatter in both sand-dominated (0.62–0.82) and silt-dominated (0.52–0.85) sediments. Within the tested VG model, parameter ranges, and Shenhu reservoir conditions, capillary pressure primarily suppresses local gas migration by enhancing water retention, with its limited impact on gas production, while cumulative gas production is overestimated without considering capillary pressure. In contrast, relative permeability plays a dominant role in hydrate production by directly controlling gas and water flow capacity and influencing pressure propagation. This study clarifies the relative roles and coupling mechanisms of capillary pressure and relative permeability during hydrate depressurization and provides a practical basis for selecting van Genuchten parameters and conducting flow-function sensitivity analyses in hydrate-bearing reservoirs.

Journal of Marine Science and EngineeringVol. 14(21)
University of Regina (CA), Hainan University (CN), Guangzhou Marine Geological Survey (CN), State Key Laboratory of Marine Resource Utilization in South China Sea (CN)
National Natural Science Foundation of China, Natural Sciences and Engineering Research Council of Canada
Openalex Percentile: Top 24%
Methane Hydrates and Related Phenomena
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