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Sodium crustal abundance

Sodium, 22 700 ppm (2.27%) is the seventh most abundant element in crustal rocks and the fifth most abundant metal, after Al, Fe, Ca and Mg. Potassium (18 400 ppm) is the next most abundant element after sodium. Vast deposits of both Na and K salts occur in relatively pure form on all continents as a result of evaporation of ancient seas, and this process still continues today in the Great Salt Lake (Utah), the Dead Sea and elsewhere. Sodium occurs as rock-salt (NaCl) and as the carbonate (trona), nitrate (saltpetre), sulfate (mirabilite), borate (borax, kemite), etc. Potassium occurs principally as the simple chloride (sylvite), as the double chloride KCl.MgCl2.6H2O (camallite) and the anhydrous sulfate K2Mg2(S04)3 (langbeinite). There are also unlimited supplies of NaCl in natural brines and oceanic waters ( 30kgm ). Thus, it has been calculated that rock-salt equivalent to the NaCl in the oceans of the world would occupy... [Pg.69]


See other pages where Sodium crustal abundance is mentioned: [Pg.483]    [Pg.301]    [Pg.483]    [Pg.2519]    [Pg.472]    [Pg.942]    [Pg.448]    [Pg.90]    [Pg.942]    [Pg.450]    [Pg.166]    [Pg.1466]    [Pg.342]    [Pg.346]    [Pg.348]    [Pg.38]   
See also in sourсe #XX -- [ Pg.127 ]




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Crustal abundances

Sodium abundance

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