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  2. Artificial seawater - Wikipedia

    en.wikipedia.org/wiki/Artificial_Seawater

    Artificial seawater (abbreviated ASW) is a mixture of dissolved mineral salts (and sometimes vitamins) that simulates seawater. Artificial seawater is primarily used in marine biology and in marine and reef aquaria , and allows the easy preparation of media appropriate for marine organisms (including algae , bacteria , plants and animals ).

  3. Marine chemistry - Wikipedia

    en.wikipedia.org/wiki/Marine_chemistry

    Modern chemical oceanography began as a field with the 1872–1876 Challenger expedition, led by the British Royal Navy which made the first systematic measurements of ocean chemistry. The chemical analysis of these samples providing the first systematic study of the composition of seawater was conducted by John Murray and George Forchhammer ...

  4. Marine biogenic calcification - Wikipedia

    en.wikipedia.org/wiki/Marine_biogenic_calcification

    The decreasing saturation of seawater with respect to calcium carbonate, associated with ocean acidification, a result of increased carbon dioxide (CO 2) absorption by the oceans, poses a significant threat to marine calcifiers. As CO 2 concentrations in seawater rise, a decrease in pH and a reduction in carbonate ion concentrations in seawater ...

  5. Seawater - Wikipedia

    en.wikipedia.org/wiki/Seawater

    Seawater, or sea water, is water from a sea or ocean. On average, seawater in the world's oceans has a salinity of about 3.5% (35 g/L, 35 ppt, 600 mM). This means that every kilogram (roughly one liter by volume) of seawater has approximately 35 grams (1.2 oz) of dissolved salts (predominantly sodium ( Na +

  6. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    This process is known as thermohaline circulation. In the Earth's polar regions ocean water gets very cold, forming sea ice. As a consequence the surrounding seawater gets saltier, because when sea ice forms, the salt is left behind. As the seawater gets saltier, its density increases, and it starts to sink.

  7. Salinity - Wikipedia

    en.wikipedia.org/wiki/Salinity

    The chemical properties of some of these forms depend on temperature and pressure. ... (an exception is when artificial seawater is ... but changes in ocean ...

  8. Sea salt aerosol - Wikipedia

    en.wikipedia.org/wiki/Sea_salt_aerosol

    Sea salt aerosols are mainly constituted of sodium chloride (NaCl), but other chemical ions which are common in sea water, such as K +, Mg 2+, Ca 2+, SO 4 2− and so on, can also be found. A recent study revealed that sea salt aerosols also contain a substantial amount of organic matter.

  9. TEOS-10 - Wikipedia

    en.wikipedia.org/wiki/TEOS-10

    TEOS-10 (Thermodynamic Equation of Seawater - 2010) is the international standard for the use and calculation of the thermodynamic properties of seawater, humid air and ice. It supersedes the former standard EOS-80 (Equation of State of Seawater 1980). [ 1 ]