Andreoli T E, Troutman S L
J Gen Physiol. 1971 Apr;57(4):464-78. doi: 10.1085/jgp.57.4.464.
The present experiments were designed to evaluate the effective thickness of the unstirred layers in series with native and porous (i.e., in the presence of amphotericin B) lipid bilayer membranes and, concomitantly, the respective contributions of membranes and unstirred layers to the observed resistances to the diffusion of water and nonelectrolytes between aqueous phases. The method depended on measuring the tracer permeability coefficients for the diffusion of water and nonelectrolytes (P(DDi), cm sec(-1)) when the aqueous phase viscosity (eta) was increased with solutes having a unity reflection coefficient, such as sucrose or dextran. The effective thickness of the unstirred layers (alpha(t), cm) and the true, or membrane, permeability coefficients for diffusion of water and nonelectrolytes (P(mmi), cm sec(-1)) were computed from, respectively, the slope and intercept of the linear regression of 1/P(DDi) on eta. In both the native and porous membranes, alpha(t) was approximately 110 x 10(-4) cm. The ratio of P(f), the osmotic water permeability coefficient (cm sec(-1)) to P(mmH2O) was 1.22 in the native membranes and 3.75 in the porous membranes. For the latter, the effective pore radius, computed from Poiseuille's law, was approximately 5.6 A. A comparison of P(mmi) and P(DDi), indicated that the porous membranes accounted for 16, 25, and 66% of the total resistance to the diffusion of, respectively, H(2)O, urea, and glycerol, while the remainder was referable to the unstirred layers.
本实验旨在评估与天然脂质双分子层膜和多孔脂质双分子层膜(即存在两性霉素B的情况下)串联的未搅拌层的有效厚度,并同时评估膜和未搅拌层对观察到的水和非电解质在水相之间扩散阻力的各自贡献。该方法依赖于测量当水相粘度(η)因具有单位反射系数的溶质(如蔗糖或右旋糖酐)而增加时,水和非电解质扩散的示踪剂渗透系数(P(DDi),cm sec⁻¹)。未搅拌层的有效厚度(α(t),cm)以及水和非电解质扩散的真实或膜渗透系数(P(mmi),cm sec⁻¹)分别根据1/P(DDi)对η的线性回归的斜率和截距计算得出。在天然膜和多孔膜中,α(t)均约为110×10⁻⁴ cm。在天然膜中,渗透水渗透系数(cm sec⁻¹)P(f)与P(mmH₂O)的比值为1.22,在多孔膜中为3.75。对于后者,根据泊肃叶定律计算出的有效孔径约为5.6 Å。P(mmi)和P(DDi)的比较表明,多孔膜分别占H₂O、尿素和甘油扩散总阻力的16%、25%和66%,而其余部分归因于未搅拌层。