Massaldi H A, Borzi C H
J Theor Biol. 1984 Feb 21;106(4):537-57. doi: 10.1016/0022-5193(84)90006-7.
On the basis of the currently accepted model for the cell membrane structure, a physico-chemical model for mediated transport is developed and solved for the case of polar non-electrolyte migration through the cell membrane. The model considers the interstitial space defined by the transport protein subunits to be the migration pathway for polar solutes. A Langmuir-type adsorption equilibrium is assumed at the interfaces and a multicomponent diffusion mechanism of solute and water is postulated within the migration pathway, where the polar residues of the transport protein represent another component of the system. Membrane selectivity is governed by the adsorption constants, which are shown to affect strongly the kinetics of transport. Isosmotic transport and the volume change of the cell are important features incorporated in the model, which is shown to fulfill the peculiar properties of facilitated diffusion systems. It is concluded that the same type of pathway can be used for the transport of other polar solutes through existing or induced hydrophilic channels, for which a similar approach is suggested.
基于目前被广泛接受的细胞膜结构模型,我们建立了一个介导运输的物理化学模型,并针对极性非电解质通过细胞膜的迁移情况进行求解。该模型认为,由转运蛋白亚基界定的细胞间隙是极性溶质的迁移途径。假设在界面处存在朗缪尔型吸附平衡,并假定在迁移途径内溶质和水存在多组分扩散机制,其中转运蛋白的极性残基代表系统的另一个组分。膜的选择性由吸附常数决定,吸附常数被证明对运输动力学有强烈影响。等渗运输和细胞体积变化是该模型纳入的重要特征,该模型被证明能够满足易化扩散系统的特殊性质。得出的结论是,相同类型的途径可用于其他极性溶质通过现有或诱导的亲水通道的运输,并针对此提出了类似的方法。