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chemocline

   Also found in: Wikipedia 0.01 sec.
chemocline [′kē·mə‚klīn]
(hydrology)
The transition in a meromictic lake between the mixolimnion layer (at the top) and the monimolimnion layer (at the bottom).


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The few dissolved sulfates that wash in are consumed by chemical reactions that occur within the chemocline, the thin layer of water that separates the oxygenated surface waters from the anoxic depths.
This sulfide usually changes into a benign sulfate salt when the dissolved gas encounters oxygen to flourish at an underwater boundary called a chemocline.
A boundary called a chemocline separates freshwater at the surface from deeper, denser fluids containing dissolved minerals and gases.
 
 
 
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