Based on model calculations,
32 in fluid transporting epithelia there is approximate balance between osmotic and hydrostatic pressures. To provide an intuitive understanding of why this is so, consider the factors generating transmembrane water flow:
where
um (cm/s) is the transmembrane water flow velocity,
Lm (cm/s/mm Hg) is the membrane hydraulic conductivity, Δ
cm (moles/cm
3) is the transmembrane osmotic difference, and Δ
pm (mm H
g) is the transmembrane hydrostatic pressure difference. In the absence of a hydrostatic pressure, if
Lm becomes very large, water flow velocity increases but not proportionally, because increases in
um wash away solute, reducing Δ
cm. The theoretical maximum limit for
um is termed isotonic transport,
34 and it occurs when the transported solution has the same osmolarity as that of the bathing medium (
c0 moles/cm
3). The osmolarity of the transported solution is given by
jm/
um (moles/cm
3), where
jm (moles/cm
3) is transmembrane salt flux. Hence the transmembrane water flow velocity is limited by:
Combining the above two equations gives:
The small parameter
ε = (
jm/
c0)/(RT
c0Lm) can be thought of as the ratio of membrane salt to water permeability. Where experimental data are available (reviewed in Mathias and Wang
34),
ε ≈ 10
−3. Assume
c0 = 300 mM and Δ
pm = 0, then a transmembrane osmotic gradient of a little less than Δ
cm = 0.3 mM would generate near isotonic transport. However, if a pressure of 335 mm Hg is present in the cell, then Δ
pm/RT = 16.75 mM and for the above inequality to hold, Δ
cm would have to be close to 17 mM. Thus, the experimental observation that membrane water permeability is much larger than salt permeability implies hydrostatic pressure will be approximately balanced by osmotic pressure and transmembrane water flow velocity will be approximately independent of pressure, insofar as transmembrane salt transport is independent of pressure. Transmembrane salt transport depends on Nernst potentials, intracellular voltage and membrane conductances, and should not appreciably change when pressure develops.