Serial permeability barriers to water transport in human placental vesicles

Summary Microvillous vesicles were prepared from term human placenta by shearing, differential centrifugation and Mg²⁺ precipitation. Vesicles were purified further on a sucrose density gradient producing two bands with densities of 1.16 to 1.18 g/ml (C1) and 1.13 to 1.15 g/ml (C2). The C2 fraction, which had a 24-fold enrichment of alkaline phosphatase and a three-fold reduction in Na⁺, K⁺-ATPase activity compared to homogenates, was used to measure osmotic water (P _f ) permeability.P _f was measured from the time course of scattered light intensity following exposure of vesicles to specified gradients of impermeant solutes.P _f decreased from 3.0×10^–3 to 0.6×10^–3 cm/sec with increasing gradient size (65 to 730mm; 23°C). Four possible causes of this behavior were examined theoretically and experimentally: an unstirred layer, saturation of water transport, large changes in the vesicle surface area with changes in volume and a structural restriction to vesicle volume change. The measured dependence ofP _f on gradient size and the effect of the channel-forming ionophore gramicidin onP _f fit best to the theoretical dependences predicted by a structural restriction mechanism. This finding was supported by experiments involving the effects onP _f of increased solution viscosity, initial vesicle volume, the magnitude of transmembrane volume flow, and the effects of gradient size on activation energy (E _a) forP _f . The decreasedP _f resulting from a structural restriction limiting vesicle volume change was modeled mathematically as a second barrier in series with the vesicle membrane.E _a measured using a 250-mm inwardly directed sucrose gradient was 5.4±0.6 kcal/mol (T>27°C) and 10.0±0.6 kcal/mol (T<27°C).E _a above 27°C is in the range normally associated with transmembrane passage of water via aqueous channels. Water transport was not inhibited byp-chloromercuribenzenesulfonate.