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・ Cycling at the 1932 Summer Olympics – Men's sprint
・ Cycling at the 1932 Summer Olympics – Men's tandem
・ Cycling at the 1932 Summer Olympics – Men's team pursuit
・ Cycling at the 1932 Summer Olympics – Men's team road race
・ Cycling at the 1936 Summer Olympics
・ Cycling at the 1936 Summer Olympics – Men's 1000m time trial
・ Cycling at the 1936 Summer Olympics – Men's individual road race
・ Cycling at the 1936 Summer Olympics – Men's sprint
・ Cycling at the 1936 Summer Olympics – Men's tandem
・ Cycling at the 1936 Summer Olympics – Men's team pursuit
・ Cycling at the 1936 Summer Olympics – Men's team road race
・ Cycling at the 1948 Summer Olympics
・ Cycling at the 1948 Summer Olympics – Men's 1000m time trial
・ Cycling at the 1948 Summer Olympics – Men's individual road race
・ Cycling at the 1948 Summer Olympics – Men's sprint
Cyclic salt
・ Cyclic sediments
・ Cyclic set
・ Cyclic sieving
・ Cyclic stress
・ Cyclic subspace
・ Cyclic succession
・ Cyclic surgery theorem
・ Cyclic symmetry in three dimensions
・ Cyclic voltammetry
・ Cyclic vomiting syndrome
・ Cyclic-guanylate-specific phosphodiesterase
・ Cyclic/collective pitch mixing
・ Cyclica
・ Cyclical alternating pattern


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Cyclic salt : ウィキペディア英語版
Cyclic salt
Cyclic salt is salt that is carried by the wind when it comes in contact with breaking waves. It is estimated that more than 300 million tons of cyclic salt is deposited on the Earth's surface each year, and it is considered to be a significant factor in the chlorine content of the Earth's river water.〔 Kostock, Dennis. (The Material Flow of Salt. ) (U.S. Department of the Interior, Bureau of Mines, Information Circular 9343, 1990), pg. 4. 〕〔Bulletin - United States Geological Survey, Issue 330. (Harvard: The Survey, 1908), 48. 〕 In general, cyclic salt deposits are lower at sites further inland and are most abundant along the shoreline, although this pattern varies depending on the given environmental conditions.〔Clarke, Frank Wigglesworth. "The data of geochemistry," in Issue 491 of U.S. Geological Survey Bulletin. (Government Printing Office, 1911), 138-139.〕
Use of the term "cyclic" refers to the cycle in which the salt moves from sea to land and is then washed by rainwater back to the sea. The salt (and other solid matter) cannot evaporate as water does. Instead it leaves the ocean surface in fine droplets of drop impacts or bubble bursts. Wave-crests and other turbulence form foam. When drops splash or bubbles burst, fine droplets of solute are ejected from the water or bubble surface into the air. Some of the droplets are small enough to allow the water to evaporate before it falls back into the sea, leaving in the air a mote of the solid residue light enough to stay suspended by Brownian motion and be carried away on the wind.
==See also==

*Edible salt
*Sodium chloride

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Cyclic salt」の詳細全文を読む



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