Methane
gas hydrate (MGH) is an important clean energy source.
In submarine continental margins, the main hydrate occurrence in the
sediment is the pore-filling type, and there is a huge difference
in the sediment particle shape. Thus, in this study, with a new algorithm
based on X-ray computed tomography (CT), 16 three-dimensional models
were reconstructed with different hydrate saturations and particle
shapes. Pore network modeling (PNM) was used to characterize the pore
space evolution, and the impacts of various hydrate saturations and
particle shapes on the other physical properties were studied using
PNM and the finite volume method (FVM). It is found that (1) when
both the sediment particle size and the hydrate saturation are certain,
the hydrate-bearing sediment (HBS) with rounder particles presents
a smaller average radius of the pore and throat, (2) when hydrate
saturation increases, the tortuosity appears as an upward trend and
the HBS with irregular particles presents a faster increased rate,
(3) when hydrate saturation becomes higher and higher, the permeability
of HBS emerges as a downward trend and the HBS with rounder particles
presents a lower permeability, (4) under the same hydrate saturation,
the HBS with rounder particles presents a higher apparent thermal
conductivity, and (5) the electrical conductivity of HBS will gradually
decrease as hydrate saturation increases, and the HBS with rounder
particles presents a lower electrical conductivity and a higher resistivity.