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The osmotic gradient across biological membranes refers to the difference in solute concentration between two solutions separated by a semipermeable membrane. This gradient drives the movement of water (osmosis) from regions of lower solute concentration (higher water potential) to regions of higher solute concentration (lower water potential), aiming to equalize solute concentrations on both sides of the membrane. It is crucial for maintaining cell turgor, volume, and overall homeostasis. Imbalances can lead to pathological states.
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