Take two reservoirs separated by a semipermeable membrane that passes water and retains one neutral solute. Stipulate , and , equivalent to and . Treat both chemical solutions as dilute and ideal. These are invented model conditions, not measurements or recommended biological conditions.
For pressures measured at the same height beside the membrane, define . The model predicts
At , net water transfer favors A to B. At , the opposing pressure balances the osmotic pressure difference, giving zero net transfer with unequal concentrations. At , the sign reverses and net water transfer favors B to A, toward the more dilute reservoir. Raising pressure changes the total water potential, rather than changing the membrane into a one-way gate.
Figure 1.
Stipulated concentration and pressure conditions determine net water transfer
. Original computed comparison for ideal retained solute at , with A at and B at . The horizontal axis is ; the vertical axis is . Three marked cases show forward transfer, balance and reversed transfer. These are instantaneous reservoir conditions, not a time course or measured biological data; slope does not specify permeability or speed. Details.
Fixed concentrations require large maintained reservoirs or an instantaneous comparison. In a closed membrane osmometer, entering water causes dilution of the receiving chemical solution and changes its volume; the final balance must use final concentrations. A supported cell wall provides another way to develop the opposing pressure, as explained under turgor pressure.

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