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  2. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    The two most prevalent ions in seawater are chloride and sodium. Together, they make up around 85 per cent of all dissolved ions in the ocean. Magnesium and sulfate ions make up most of the rest. Salinity varies with temperature, evaporation, and precipitation. It is generally low at the equator and poles, and high at mid-latitudes. [12]

  3. Sea - Wikipedia

    en.wikipedia.org/wiki/Sea

    In fact, the oceans teem with life and provide many varying microhabitats. [95] One of these is the surface film which, even though tossed about by the movement of waves, provides a rich environment and is home to bacteria, fungi, microalgae, protozoa, fish eggs and various larvae. [96]

  4. Hypersaline lake - Wikipedia

    en.wikipedia.org/wiki/Hypersaline_lake

    A hypersaline lake is a landlocked body of water that contains significant concentrations of sodium chloride, brines, and other salts, with saline levels surpassing those of ocean water (3.5%, i.e. 35 grams per litre or 0.29 pounds per US gallon).

  5. Seawater - Wikipedia

    en.wikipedia.org/wiki/Seawater

    In addition, sodium leached out of the ocean floor when the ocean formed. The presence of salt's other dominant ion, chloride, results from outgassing of chloride (as hydrochloric acid) with other gases from Earth's interior via volcanos and hydrothermal vents. The sodium and chloride ions subsequently became the most abundant constituents of ...

  6. Marine chemistry - Wikipedia

    en.wikipedia.org/wiki/Marine_chemistry

    The international community has agreed that restoring the chemistry of the oceans is a priority, and efforts toward this goal are tracked as part of Sustainable Development Goal 14. Due to the interrelatedness of the ocean, chemical oceanographers frequently work on problems relevant to physical oceanography , geology and geochemistry , biology ...

  7. Chlorine cycle - Wikipedia

    en.wikipedia.org/wiki/Chlorine_cycle

    Oceans are the largest source of chlorine in the Earth's hydrosphere. [2] In the hydrosphere, chlorine exists primarily as chloride due to the high solubility of the Cl − ion. [3] The majority of chlorine fluxes are within the hydrosphere due to chloride ions' solubility and reactivity within water systems. [2]

  8. Salinity - Wikipedia

    en.wikipedia.org/wiki/Salinity

    Salinity in rivers, lakes, and the ocean is conceptually simple, but technically challenging to define and measure precisely. Conceptually the salinity is the quantity of dissolved salt content of the water. Salts are compounds like sodium chloride, magnesium sulfate, potassium nitrate, and sodium bicarbonate which dissolve into ions. The ...

  9. Sea salt - Wikipedia

    en.wikipedia.org/wiki/Sea_salt

    Although the principal component is sodium chloride, the remaining portion can range from less than 0.2 to 22% of other salts. These are mostly calcium, potassium, and magnesium salts of chloride and sulfate with substantially lesser amounts of many trace elements found in natural seawater.