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  2. Saturation diving - Wikipedia

    en.wikipedia.org/wiki/Saturation_diving

    The "saturation system", "saturation complex" or "saturation spread" typically comprises either an underwater habitat or a surface complex which includesof a living chamber, transfer chamber and submersible decompression chamber, [45] which is commonly referred to in commercial diving and military diving as the diving bell, [46] personnel ...

  3. Oxygen minimum zone - Wikipedia

    en.wikipedia.org/wiki/Oxygen_minimum_zone

    In OMZs oxygen concentration drops to levels <10 nM at the base of the oxycline and can remain anoxic for over 700 m depth. [7] This lack of oxygen can be reinforced or increased due to physical processes changing oxygen supply such as eddy-driven advection, [7] sluggish ventilation, [8] increases in ocean stratification, and increases in ocean temperature which reduces oxygen solubility.

  4. Marine biogenic calcification - Wikipedia

    en.wikipedia.org/wiki/Marine_biogenic_calcification

    This series of reactions governs the pH levels in the ocean and also dictates the saturation state of seawater, indicating how saturated or unsaturated the seawater is with carbonate ions. Consequently, the saturation state significantly influences the balance between the dissolution and calcification processes in marine biogenic calcifiers.

  5. Dead zone (ecology) - Wikipedia

    en.wikipedia.org/wiki/Dead_zone_(ecology)

    Ocean deoxygenation – Reduction of the oxygen content of the oceans Oxygen minimum zone – Zone in which oxygen saturation in seawater in the ocean is at its lowest Shutdown of thermohaline circulation – System of surface and deep currents in the Atlantic Ocean Pages displaying short descriptions of redirect targets

  6. Apparent oxygen utilisation - Wikipedia

    en.wikipedia.org/wiki/Apparent_oxygen_utilisation

    O 2 concentrations in the ocean have decreased since the 1980s. [2] Part of this decrease is due to increased ocean heat content (OHC) from global warming decreasing O 2 solubility. As solubility in surface oceans decreases, O 2 out gasses to the atmosphere. [3] Increased AOU is likely also contributing to declining ocean O 2 concentrations. [2]

  7. SEALAB - Wikipedia

    en.wikipedia.org/wiki/SEALAB

    Preliminary research work was undertaken by George F. Bond, who named the project after the Book of Genesis, which prophesised humans would gain dominion over the oceans. Bond began investigations in 1957 to develop theories about saturation diving.

  8. Aragonite sea - Wikipedia

    en.wikipedia.org/wiki/Aragonite_sea

    However, the sea level, temperature, and calcium carbonate saturation state of the surrounding system also determine which polymorph of calcium carbonate (aragonite, low-magnesium calcite, high-magnesium calcite) will form. [11] [12]

  9. Aquanaut - Wikipedia

    en.wikipedia.org/wiki/Aquanaut

    The term aquanaut derives from the Latin word aqua ("water") plus the Greek nautes ("sailor"), by analogy to the similar construction "astronaut".The word is used to describe a person who stays underwater, breathing at the ambient pressure for long enough for the concentration of the inert components of the breathing gas dissolved in the body tissues to reach equilibrium, in a state known as ...