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介导转运的物理化学机制。II. 渗透和等渗体积流。

The physico-chemical mechanism of mediated transport. II. Osmotic and isosmotic volume flow.

作者信息

Massaldi H A

出版信息

J Theor Biol. 1984 Sep 7;110(1):35-57. doi: 10.1016/s0022-5193(84)80014-4.

Abstract

The process of volume change of cells subject to osmotic shocks or isosmotic entrance of permeant solute is formulated on the basis of the accepted structure for the plasma membrane and a physico-chemical approach similar to that recently developed. The effect of relevant parameters is discussed and theoretical equilibrium values for the variables are calculated in connection with water and permeant solute permeability determinations. Although a sorption-diffusional mechanism for solute and/or water volume flow within the membrane is assumed in both cases, the kinetics of volume change is shown to be totally different between them. In the isosmotic process a fixed relationship, given by the total solute concentration, is shown to exist between the permeant solute and volume fluxes to the cell, thereby implying a definite value for the volume fraction of water in the migration pathway, higher than 90%. The bi-phase osmotic regulatory response caused by permeant solute is simulated on the basis of an osmotic and isosmotic processes in series, showing good agreement with general behavior. Finally, an explanation to the problem of volume flow and forces in connection with a diffusional mechanism in biological and artificial membranes, is presented.

摘要

基于公认的质膜结构和一种类似于最近发展起来的物理化学方法,阐述了细胞在渗透冲击或渗透性溶质等渗进入时的体积变化过程。讨论了相关参数的影响,并结合水和渗透性溶质渗透率的测定计算了变量的理论平衡值。尽管在这两种情况下都假定了溶质和/或水在膜内的吸附-扩散机制,但结果表明它们之间体积变化的动力学完全不同。在等渗过程中,渗透性溶质与细胞的体积通量之间存在由总溶质浓度给出的固定关系,这意味着迁移途径中水的体积分数有一个确定的值,高于90%。基于串联的渗透和等渗过程模拟了由渗透性溶质引起的双相渗透调节反应,与一般行为显示出良好的一致性。最后,对生物膜和人工膜中与扩散机制相关的体积流动和力的问题给出了解释。

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