2022
DOI: 10.1016/j.energy.2021.122526
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Mechanical properties and strength criterion of clayey sand reservoirs during natural gas hydrate extraction

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Cited by 27 publications
(14 citation statements)
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“…The relationship between strength parameters and hydrate saturation is shown in Figure . It can be seen from Figure that cohesion is positively correlated with hydrate saturation . With the increase in hydrate saturation, the cohesion increases rapidly at first and then slowly.…”
Section: Resultsmentioning
confidence: 80%
“…The relationship between strength parameters and hydrate saturation is shown in Figure . It can be seen from Figure that cohesion is positively correlated with hydrate saturation . With the increase in hydrate saturation, the cohesion increases rapidly at first and then slowly.…”
Section: Resultsmentioning
confidence: 80%
“…However, the subsidence speeds of the clayey‐silty samples accelerated greatly and were larger than those of the sandy ones during hydrate dissociation. The greater mechanical weakening and permeability increase for the clayey‐silty samples due to hydrate dissociation are the main reasons for this behavior 34,35 . Simultaneously, the effective stress continued to increase, speeding up subsidence during dissociation for both types of GHBSs.…”
Section: Results and Analysesmentioning
confidence: 96%
“…Please note that I, II, and III represent the stage before, during, and after hydrate dissociation, respectively hydrate dissociation are the main reasons for this behavior. 34,35 Simultaneously, the effective stress continued to increase, speeding up subsidence during dissociation for both types of GHBSs. With continuous depressurization, the samples were reconsolidated and gradually restored to stability under the increased effective stress.…”
Section: Subsidence Responsementioning
confidence: 96%
“…Hydrate dissociation releases large amounts of gas and water, the pore space is filled with water and gas, the pore pressure increases continuously, and the pore structure of the sediments is disrupted. The dissociation of hydrates results in the loss of cementation between soil particles, which will lead to the reduction of shear strength, and thus accelerate the deformation of seafloor sediments. , …”
Section: Shear Mechanismmentioning
confidence: 99%