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Para alcanzar el equilibrio osmótico, el agua se mueve a través de una membrana semipermeable para igualar la concentración a ambos lados. Este movimiento se determina por la concentración de los solutos a ambos lados de la membrana.
La presión osmótica se mide en unidades de osmoles (osm) o miliosmoles (mosm), que se refieren al número real de partículas con actividad osmótica.
La osmolalidad del líquido intracelular y del extracelular se mantiene entre 290 y 310 mosm en cada compartimiento.
Presión osmótica
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