Hypotonic

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In biology, a hypotonic cell environment is an environment with a lower concentration of solutes than the cytoplasm of the cell. In a hypotonic environment, osmosis causes water to have net flow into the cell, causing the swelling and expansion of the cell.

In summary, a hypertonic solution contains a higher concentration compared to the cell. Hypotonic means it has a lower concentration compared to the cell. Isotonic is in between where the concentration of the cell and the solution is in ratio.

Living in a Hypotonic Environment

Plants thrive in hypotonic environments. Their cells have rigid cell walls that prevent bursting. In fact, the pressure of the cytoplasm against the cell wall keeps the plant from wilting and losing its shape. This pressure is called turgor pressure. On the other hand, cells without cell walls will swell and, if the environment is sufficiently hypotonic, burst and die (referred to as cytolysis).

Some protists (such as Paramecium) counteract this with the use of contractile vacuoles that pump water rapidly out of the cell. Other organisms actually pump solutes out of the cell in order to lower the concentration gradient of the solute in the cell and hopefully create an isotonic environment.

The opposite of hypotonic is hypertonic, where the net movement of water is directed out of the cell into the environment; the intermediate state is called isotonic, where there is no net movement of water in and out of the cell.

See also

Template:Biochem-stubde:Hypoton es:Hipotónico fr:Hypotonique nl:Hypotoon pl:Roztwór hipotoniczny vi:Nhược trương zh:低滲