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渗透动力学:VII. 分子与离子传输。

KINETICS OF PENETRATION : VII. MOLECULAR VERSUS IONIC TRANSPORT.

机构信息

Laboratories of The Rockefeller Institute for Medical Research.

出版信息

J Gen Physiol. 1934 Jan 20;17(3):469-80. doi: 10.1085/jgp.17.3.469.

Abstract

In some living cells the order of penetration of certain cations corresponds to that of their mobilities in water. This has led to the idea that electrolytes pass chiefly as ions through the protoplasmic surface in which the order of ionic mobilities is supposed to correspond to that found in water. If this correspondence could be demonstrated it would not prove that electrolytes pass chiefly as ions through the protoplasmic surface for such a correspondence could exist if the movement were mostly in molecular form. This is clearly shown in the models here described. In these the protoplasmic surface is represented by a non-aqueous layer interposed between two aqueous phases, one representing the external solution, the other the cell sap. The order of penetration through the non-aqueous layer is Cs > Rb > K > Na > Li. This will be recognized as the order of ionic mobilities in water. Nevertheless the movement is mostly in molecular form in the nonaqueous layer (which is used in the model to represent the protoplasmic surface) since the salts are very weak electrolytes in this layer. The chief reason for this order of penetration lies in the fact that the partition coefficients exhibit the same order, that of cesium being greatest and that of lithium smallest. The partition coefficients largely control the rate of entrance since they determine the concentration gradient in the non-aqueous layer which in turn controls the process of penetration. The relative molecular mobilities (diffusion constants) in the non-aqueous layer do not differ greatly. The ionic mobilities are not known (except for K(+) and Na(+)) but they are of negligible importance, since the movement in the non-aqueous layer is largely in molecular form. They may follow the same order as in water, in accordance with Walden's rule. Ammonium appears to enter faster than its partition coefficient would lead us to expect, which may be due to rapid penetration of NH(3). This recalls the apparent rapid penetration of ammonium in living cells which has also been explained as due to the rapid penetration of NH(3). Both observation and calculation indicate that the rate of penetration is not directly proportional to the partition coefficient but increases somewhat less rapidly. Many of these considerations doubtless apply to living cells.

摘要

在一些活细胞中,某些阳离子的穿透顺序与它们在水中的迁移率顺序相对应。这导致了这样一种观点,即电解质主要以离子形式通过原生质表面,而原生质表面的离子迁移率顺序应该与在水中发现的顺序相对应。如果这种对应关系能够得到证明,它也不能证明电解质主要以离子形式通过原生质表面,因为即使在分子形式下也可能存在这种对应关系。在本文所描述的模型中,这一点非常明显。在这些模型中,原生质表面由夹在两个水相之间的非水层表示,一个水相代表外部溶液,另一个水相代表细胞液。通过非水层的穿透顺序为 Cs > Rb > K > Na > Li。这将被认为是水中离子迁移率的顺序。然而,由于在该层中盐是非常弱的电解质,因此在非水层(在模型中用于表示原生质表面)中的运动主要以分子形式存在。这种穿透顺序的主要原因在于分配系数表现出相同的顺序,即铯的分配系数最大,锂的分配系数最小。分配系数在很大程度上控制着进入的速度,因为它们决定了非水层中的浓度梯度,而浓度梯度反过来又控制着穿透过程。在非水层中的相对分子迁移率(扩散常数)差异不大。离子迁移率是未知的(除了 K(+) 和 Na(+)),但它们不重要,因为在非水层中的运动主要以分子形式存在。它们可能遵循与水中相同的顺序,根据 Walden 法则。铵似乎比根据分配系数预期的更快进入,这可能是由于 NH(3) 的快速穿透。这让人想起了铵在活细胞中的快速穿透,这也被解释为 NH(3) 的快速穿透。观察和计算都表明,穿透速度与分配系数不是直接成比例的,而是增加得稍慢。这些考虑因素中的许多无疑适用于活细胞。

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