2021
DOI: 10.1016/j.petlm.2021.10.010
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Microbial stabilisation and kinetic enhancement of marine methane hydrates in both deionised- and sea-water

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“…In the World Ocean, gas hydrates are most often discovered on continental slopes and shelves [8]. This is attributed to the accumulation of sediments with elevated content of organic matter, which is a source of thermogenic and microbial methane [9]. If there is a source of methane, marine gas hydrates are formed at a depth of over 320 m. The depth of the seafloor at which hydrates are formed depends on the bottom water temperature: the higher the temperature, the greater the sea depth is needed for hydrate formation [10].…”
Section: Introduction 1gas Hydratesmentioning
confidence: 99%
“…In the World Ocean, gas hydrates are most often discovered on continental slopes and shelves [8]. This is attributed to the accumulation of sediments with elevated content of organic matter, which is a source of thermogenic and microbial methane [9]. If there is a source of methane, marine gas hydrates are formed at a depth of over 320 m. The depth of the seafloor at which hydrates are formed depends on the bottom water temperature: the higher the temperature, the greater the sea depth is needed for hydrate formation [10].…”
Section: Introduction 1gas Hydratesmentioning
confidence: 99%