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Kinetic fractionation is a process that separates stable isotopes from each other by their mass during unidirectional processes.
Additional recommended knowledge
One naturally-occurring example of kinetic fractionation is the evaporation of seawater to form clouds. In this instance, isotopically-lighter water molecules (i.e., those with 16O) will evaporate slightly more easily than will the isotopically-heavier water molecules with 18O.
During the course of this process the oxygen isotopes are fractionated: the clouds become enriched with 16O, the seawater becomes enriched in 18O. Thus, rainwater is observed to be isotopically lighter than seawater.
Categories: Unit operations | Environmental isotopes
|This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Kinetic_fractionation". A list of authors is available in Wikipedia.|