Physical properties of hydrate‐bearing sediments are often correlated with hydrate
saturation with little or no information on hydrate distribution uniformity in the specimens …

Fine‐grained sediments limit hydrate nucleation, shift the phase boundary, and hinder gas
supply. Laboratory experiments in this study explore different strategies to overcome these …

Based on the high-resolution industrial x-ray computerized tomography (X-CT), a dedicated
apparatus was developed to observe in-situ pore scale distribution of gas hydrate directly …

Sediment particles affect the phase behavior of gas hydrates, both by increasing the surface
energy where pore geometry forces hydrate crystals to attain high curvatures and through …

Hydrate-bearing sediments constitute complex hydrological systems, within which the pore
habit of hydrate significantly affects all physical properties. However, there is scarce pore …

Permeability is critical to understand gas production behavior from hydrate reservoirs. The
effects of particle size distribution and initial brine saturation on effective permeability of …

To study physical properties of methane gas hydrate‐bearing sediments, it is necessary to
synthesize laboratory samples due to the limited availability of cores from natural deposits. X …

The physical properties of gas hydrate‐bearing sediments depend on the volume fraction
and spatial distribution of the hydrate phase. The host sediment grain size and the state of …

Heterogenous distribution of gas hydrate in pores is the common characteristic of hydrate
formation at various experimental scales. In this work, in order to fill the gap of defining the …

Gas-hydrates are natural clean energy resources with significant potentials as the
alternative energy resources. Nevertheless, the formation, migration and dissolution of …