2011
DOI: 10.1016/j.marpetgeo.2010.11.007
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Particle size effect on the saturation of methane hydrate in sediments – Constrained from experimental results

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Cited by 73 publications
(48 citation statements)
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“…The data of Lu et al (2011b) indicate that silica surfaces interact with interstitial waters adjacent to the silica particles, making the affected water unavailable for hydrate formation. The data of Lu et al (2011b) indicate that silica surfaces interact with interstitial waters adjacent to the silica particles, making the affected water unavailable for hydrate formation.…”
Section: Laboratory Analyses Hydrates Saturating Sandsmentioning
confidence: 99%
“…The data of Lu et al (2011b) indicate that silica surfaces interact with interstitial waters adjacent to the silica particles, making the affected water unavailable for hydrate formation. The data of Lu et al (2011b) indicate that silica surfaces interact with interstitial waters adjacent to the silica particles, making the affected water unavailable for hydrate formation.…”
Section: Laboratory Analyses Hydrates Saturating Sandsmentioning
confidence: 99%
“…In hydrate, the force between water molecules and gas molecules is intermolecular force (van der Waals force) that is relatively weaker than the electrostatic force. Therefore, some of the water molecules will be tightly bounded on the particle surface so as to lose the chance to combine with gas molecule [50,51]. Besides, a large number of water molecules are gathered around ions and alienated from gas molecules because of hydration ion effect of chloride salt solution.…”
Section: (Gas + Liquid + Solid + Hydrate) Phase Equilibriummentioning
confidence: 99%
“…hydrate depends on water saturation, and the particle size of sand and clay concentration in sediments [14,[25][26].…”
Section: Vk Saw Et Al / Methane Hydrate Formation and Dissociationmentioning
confidence: 99%