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• Gas_hydrate_stability_zone abstract "Gas hydrate stability zone, abbreviated GHSZ, also referred to as hydrate stability zone, or HSZ, refers to a zone and depth of the marine environment at which gas hydrates naturally exist in the Earth's crust. Gas hydrate stability primarily depends upon temperature and pressure, however other variables such as gas composition and ionic impurities in water influence stability boundaries. The existence and depth of a hydrate deposit is often indicated by the presence of a bottom-simulating reflector (BSR). A BSR is a seismic reflection indicating the lower limit of hydrate stability in sediments due to the different densities of hydrate saturated sediments, normal sediments and those containing free gas.The upper and lower limits of the HSZ, as well as its thickness, depend upon the local conditions in which the hydrate occurs. The conditions for hydrate stability generally restrict natural deposits to polar regions and deep oceanic regions. In polar regions, due to low temperatures, the upper limit of the hydrate stability zone occurs at a depth of approximately 150 meters.1 The maximum depth of the hydrate stability zone is limited by the geothermal gradient. Along continental margins the average thickness of the HSZ is about 500m.1 The upper limit in oceanic sediments occurs when bottom water temperatures are at, or near 0° celsius, and at a water depth of approximately 300 meters.1 The lower limit of the HSZ is bounded by the geothermal gradient. As depth below seafloor increases, the temperature eventually becomes too high for hydrates to exist. In areas of high geothermal heat flow, the lower limit of the HSZ may become shallower, therefore decreasing the thickness of the HSZ. Conversely, the thickest hydrate layers and widest HSZ are observed in areas of low geothermal heat flow. Generally, the maximum depth of HSZ extension is 2000 meters below the earth’s surface.1,3 Using the location of a BSR as well as the pressure-temperature regimen necessary for hydrate stability, the HSZ may be used to determine geothermal gradients.2If processes such as sedimentation or subduction transport hydrates below the lower limit of the HSZ, the hydrate will become unstable and disassociate, releasing gas. This free gas may become trapped beneath the overlying hydrate layer forming gas pockets, or reservoirs. The pressure from the presence of gas reservoirs impacts the stability of the hydrate layer. If this pressure is substantially changed, the stability of the methane layer above will be altered and may result in significant destabilization and disassociation of the hydrate deposit. Landslides of rock or sediment above the hydrate stability zone may also impact the hydrate stability. A sudden decrease in pressure can release gasses, or destabilize portions of the hydrate deposit. Changing atmospheric and oceanic temperatures may impact the presence and depth of the hydrate stability zone; however to what extent is still uncertain. In oceanic sediments, increasing pressure due to a rise in sea level may offset some of the impact of increasing temperature upon the hydrate stability equilibrium.1".
• Gas_hydrate_stability_zone wikiPageID "44433500".
• Gas_hydrate_stability_zone wikiPageLength "4947".
• Gas_hydrate_stability_zone wikiPageOutDegree "15".
• Gas_hydrate_stability_zone wikiPageRevisionID "653926963".
• Gas_hydrate_stability_zone wikiPageWikiLink Biogeochemistry.
• Gas_hydrate_stability_zone wikiPageWikiLink Category:Hydrates.
• Gas_hydrate_stability_zone wikiPageWikiLink Celsius.
• Gas_hydrate_stability_zone wikiPageWikiLink Clathrate_hydrate.
• Gas_hydrate_stability_zone wikiPageWikiLink Gas_hydrate.
• Gas_hydrate_stability_zone wikiPageWikiLink Geothermal_gradient.
• Gas_hydrate_stability_zone wikiPageWikiLink Landslide.
• Gas_hydrate_stability_zone wikiPageWikiLink Landslides.
• Gas_hydrate_stability_zone wikiPageWikiLink Marine_environment.
• Gas_hydrate_stability_zone wikiPageWikiLink Meters.
• Gas_hydrate_stability_zone wikiPageWikiLink Metre.
• Gas_hydrate_stability_zone wikiPageWikiLink Ocean.
• Gas_hydrate_stability_zone wikiPageWikiLink Oceanic_crust.
• Gas_hydrate_stability_zone wikiPageWikiLink Pressure.
• Gas_hydrate_stability_zone wikiPageWikiLink Reflection_seismology.
• Gas_hydrate_stability_zone wikiPageWikiLink Sediment.
• Gas_hydrate_stability_zone wikiPageWikiLink Sedimentation.
• Gas_hydrate_stability_zone wikiPageWikiLink Sediments.
• Gas_hydrate_stability_zone wikiPageWikiLink Seismic_reflection.
• Gas_hydrate_stability_zone wikiPageWikiLink Subduction.
• Gas_hydrate_stability_zone wikiPageWikiLink Temperature.
• Gas_hydrate_stability_zone wikiPageWikiLinkText "gas hydrate stability zone".
• Gas_hydrate_stability_zone wikiPageWikiLinkText "stability zone".
• Gas_hydrate_stability_zone hasPhotoCollection Gas_hydrate_stability_zone.
• Gas_hydrate_stability_zone wikiPageUsesTemplate Template:Reflist.
• Gas_hydrate_stability_zone subject Category:Hydrates.
• Gas_hydrate_stability_zone comment "Gas hydrate stability zone, abbreviated GHSZ, also referred to as hydrate stability zone, or HSZ, refers to a zone and depth of the marine environment at which gas hydrates naturally exist in the Earth's crust. Gas hydrate stability primarily depends upon temperature and pressure, however other variables such as gas composition and ionic impurities in water influence stability boundaries.".
• Gas_hydrate_stability_zone label "Gas hydrate stability zone".
• Gas_hydrate_stability_zone sameAs m.012blbm_.
• Gas_hydrate_stability_zone sameAs Q19904034.
• Gas_hydrate_stability_zone sameAs Q19904034.
• Gas_hydrate_stability_zone wasDerivedFrom Gas_hydrate_stability_zone?oldid=653926963.
• Gas_hydrate_stability_zone isPrimaryTopicOf Gas_hydrate_stability_zone.