“The edge of the sea is a strange and beautiful place.” ― Rachel Carson
Chemical Composition of Seawater & Ocean Chemistry
- water is the "universal solvent" dissolving at least 57 of the 92 elements found in nature.
- most natural elements and the compounds they form are found in the seas as dissolved solids, or solutes.
- seawater = solution/concentration of dissolved solids = salinity
- oceans remain homogenous mixture = ratio of individual salts remain unchanged, despite minor fluctuations in overall salinity.
- ocean chemistry = complex exchanges of seawater, the atmosphere, minerals, bottom sediments, and living organisms.
- mineral-rich water enter the ocean through hydrothermal (hot water) vents in the ocean floor.
- uniformity of seawater = complementary chemical reactions and continuous mixing - ocean basins interconnect, and water circulates among them.
- seven elements account for more than 99% of the dissolved solids in seawater = chlorine, sodium, magnesium, sulphur, calcium, potassium, and bromine.
- seawater also contain dissolved gases = carbon dioxide, nitrogen, and oxygen. Also contain suspended and dissolved organic matter, and a multitude of trace elements.
- Average salinity - 3.5% (% parts per hundred) / worldwide 3.4% to 3.7%, attributable to atmospheric conditions above the water and to volume of freshwater inflows.
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