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• W2024200625 endingPage "18" @default.
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• W2024200625 abstract "This paper reviews current understanding of the physics of bubbles in soft (unlithified), cohesive sediments, certainly in the top 100 m from the sediment–water interface, but likely much deeper. Experimental evidence, primarily CT scans and internal pressure records, indicate that near-surface bubbles grow by elastically compressing and fracturing these sediments, which results in thin, irregular disks of gas. These data do not suggest either plastic or fluid behavior on the part of the bulk sediment. In addition there is no hint of capillary invasion of gas into the pores of fine-grained sediments. The growth rate of an elastic-fracturing, disk-shaped, bubble can vastly exceed that of a spherical bubble, depending on the eccentricity of the bubble. This effect results from the far more favorable surface-to-volume ratio of flattened bubbles. The initial rate of rise of bubbles in cohesive sediments also appears to be governed by a fracture process, which is driven by pseudo-buoyancy. The rate of bubble rise could be controlled by various possible mechanisms, but only the predictions from a visco-elastic-fracture propagation model seem to produce rise velocities that are not ballistic (<m s−1) and unobserved for bubbles leaving sediments. Bubbles can repeatedly utilize the same fracture path to rise to the surface and incomplete annealing of the path between subsequent bubbles greatly facilitates this process. Experimental evidence demonstrates that a rising bubble can deviate from its path to the surface if it encounters a “zone” of sediment with lower lateral fracture toughness; such a bubble will begin to move in a lateral direction, but stall because pseudo-buoyancy is no longer operative. Subsequent bubbles will do the same and accumulate in the low fracture-toughness zone. This explains the occurrence of shallow sub-seafloor domes of gas, and modeling of this process predicts only modest over-pressures in such structures." @default.
• W2024200625 created "2016-06-24" @default.
• W2024200625 creator A5080315848 @default.
• W2024200625 date "2012-12-01" @default.
• W2024200625 modified "2023-10-18" @default.
• W2024200625 title "The physics of bubbles in surficial, soft, cohesive sediments" @default.
• W2024200625 cites W1484744561 @default.
• W2024200625 cites W1545459481 @default.
• W2024200625 cites W1601006326 @default.
• W2024200625 cites W1675602030 @default.
• W2024200625 cites W1932868995 @default.
• W2024200625 cites W1963673176 @default.
• W2024200625 cites W1964057727 @default.
• W2024200625 cites W1965111125 @default.
• W2024200625 cites W1965536791 @default.
• W2024200625 cites W1967004426 @default.
• W2024200625 cites W1970299714 @default.
• W2024200625 cites W1972594000 @default.
• W2024200625 cites W1974363385 @default.
• W2024200625 cites W1974474590 @default.
• W2024200625 cites W1976279268 @default.
• W2024200625 cites W1978269183 @default.
• W2024200625 cites W1978846254 @default.
• W2024200625 cites W1984305821 @default.
• W2024200625 cites W1984668486 @default.
• W2024200625 cites W1986905165 @default.
• W2024200625 cites W1988976069 @default.
• W2024200625 cites W1994789837 @default.
• W2024200625 cites W2003764813 @default.
• W2024200625 cites W2006217228 @default.
• W2024200625 cites W2008798992 @default.
• W2024200625 cites W2012594298 @default.
• W2024200625 cites W2015521079 @default.
• W2024200625 cites W2018744948 @default.
• W2024200625 cites W2019377904 @default.
• W2024200625 cites W2022057155 @default.
• W2024200625 cites W2024454038 @default.
• W2024200625 cites W2025408056 @default.
• W2024200625 cites W2025980935 @default.
• W2024200625 cites W2027060408 @default.
• W2024200625 cites W2032901749 @default.
• W2024200625 cites W2035444882 @default.
• W2024200625 cites W2036473987 @default.
• W2024200625 cites W2042308565 @default.
• W2024200625 cites W2042864207 @default.
• W2024200625 cites W2051156910 @default.
• W2024200625 cites W2055942616 @default.
• W2024200625 cites W2062230312 @default.
• W2024200625 cites W2063836334 @default.
• W2024200625 cites W2065941285 @default.
• W2024200625 cites W2070237959 @default.
• W2024200625 cites W2071677280 @default.
• W2024200625 cites W2076827910 @default.
• W2024200625 cites W2077072906 @default.
• W2024200625 cites W2077674450 @default.
• W2024200625 cites W2082360872 @default.
• W2024200625 cites W2082873400 @default.
• W2024200625 cites W2090725111 @default.
• W2024200625 cites W2091287422 @default.
• W2024200625 cites W2091633031 @default.
• W2024200625 cites W2093072505 @default.
• W2024200625 cites W2093265611 @default.
• W2024200625 cites W2094957705 @default.
• W2024200625 cites W2097794260 @default.
• W2024200625 cites W2099181667 @default.
• W2024200625 cites W2102094391 @default.
• W2024200625 cites W2103248013 @default.
• W2024200625 cites W2112168108 @default.
• W2024200625 cites W2116660506 @default.
• W2024200625 cites W2119083643 @default.
• W2024200625 cites W2122767962 @default.
• W2024200625 cites W2126687317 @default.
• W2024200625 cites W2126722579 @default.
• W2024200625 cites W2128824444 @default.
• W2024200625 cites W2130407161 @default.
• W2024200625 cites W2135285641 @default.
• W2024200625 cites W2137860033 @default.
• W2024200625 cites W2139196973 @default.
• W2024200625 cites W2147209350 @default.
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• W2024200625 cites W2157672147 @default.
• W2024200625 cites W2160986314 @default.
• W2024200625 cites W2163302248 @default.
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• W2024200625 doi "https://doi.org/10.1016/j.marpetgeo.2012.07.002" @default.
• W2024200625 hasPublicationYear "2012" @default.
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