2021
DOI: 10.1016/j.isci.2021.102448
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Mechanical behaviors of hydrate-bearing sediment with different cementation spatial distributions at microscales

Abstract: Dispersed hydrate spatial distribution strengthens the sediment more significantly Dispersed hydrate spatial distribution steepens and thins the shear band Hydrate distribution seems to not affect the pore space evolution during shearing The cementation interfacial area evolution was calculated during shearing

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Cited by 24 publications
(8 citation statements)
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“…The H–S bond coordination number represents the number of individual hydrate particles bonding to sand particles and is used to characterize the area of the cemented interface between hydrate and sand particles. Therefore, the ability of hydrate particles to bear the load component is closely related to the area of the cemented interface between hydrate and sand particles . In addition, as shown in Figure , it is noteworthy that after an axial strain of 9%, the stress components borne by the individual hydrate particles decrease more for the cluster and cementing types and less for the prepatchy and patchy types.…”
Section: Resultsmentioning
confidence: 92%
See 1 more Smart Citation
“…The H–S bond coordination number represents the number of individual hydrate particles bonding to sand particles and is used to characterize the area of the cemented interface between hydrate and sand particles. Therefore, the ability of hydrate particles to bear the load component is closely related to the area of the cemented interface between hydrate and sand particles . In addition, as shown in Figure , it is noteworthy that after an axial strain of 9%, the stress components borne by the individual hydrate particles decrease more for the cluster and cementing types and less for the prepatchy and patchy types.…”
Section: Resultsmentioning
confidence: 92%
“…Therefore, the ability of hydrate particles to bear the load component is closely related to the area of the cemented interface between hydrate and sand particles. 71 In addition, as shown in Figure 13, it is noteworthy that after an axial strain of 9%, the stress components borne by the individual hydrate particles decrease more for the cluster and cementing types and less for the prepatchy and patchy types. This behavior will be explained by observing the deformation of cementing and patchy type hydrates during shearing.…”
Section: Resultsmentioning
confidence: 93%
“…For the hydrate nucleation process, a certain amount of free guest molecules must be evenly distributed with the water molecules, and the free energy of the guest and water molecules should be relatively low. Only under these conditions can be the nuclei of the hydrate crystals can stabilize and continue to grow [34][35][36][37]. However, because of its very low solubility in water, R141b cannot diffuse uniformly in water molecules [19].…”
Section: Characteristics Of Hydrate Formationmentioning
confidence: 99%
“…Natural gas hydrate is a kind of ice-like clathrate crystal formed at low temperature and high pressure. On the one hand, natural gas hydrate provides new energy for human development; on the other hand, it can easily cause pipeline blockage and other safety problems if it is generated in the oil and gas pipeline. The addition of surfactants as anti-agglomerants is an effective way to prevent small hydrate particles from aggregating into large particles and protect pipes from blockages. …”
Section: Introductionmentioning
confidence: 99%