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渗透维里方程在低温生物学中的应用。

Application of the osmotic virial equation in cryobiology.

机构信息

Department of Chemical and Materials Engineering, University of Alberta, Edmonton, AB, Canada T6G 2V4.

出版信息

Cryobiology. 2010 Feb;60(1):30-42. doi: 10.1016/j.cryobiol.2009.07.011. Epub 2009 Aug 6.

Abstract

The multisolute osmotic virial equation is the only multisolute thermodynamic solution theory that has been derived from first principles and can make predictions of multisolute solution behaviour in the absence of multisolute solution data. Other solution theories either (i) include simplifying assumptions that do not take into account the interactions between different types of solute molecules or (ii) require fitting to multisolute data to obtain empirical parameters. The osmotic virial coefficients, which are obtained from single-solute data, can be used to make predictions of multisolute solution osmolality. The osmotic virial coefficients for a range of solutes of interest in cryobiology are provided in this paper, for use with concentration units of both molality and mole fraction, along with an explanation of the background and theory necessary to implement the multisolute osmotic virial equation.

摘要

多溶质渗透维里方程是唯一一种从第一原理推导出来的多溶质热力学溶液理论,可在没有多溶质溶液数据的情况下预测多溶质溶液的行为。其他溶液理论要么(i)包含简化假设,没有考虑不同类型溶质分子之间的相互作用,要么(ii)需要拟合多溶质数据以获得经验参数。由单溶质数据获得的渗透维里系数可用于预测多溶质溶液渗透压。本文提供了在低温生物学中感兴趣的一系列溶质的渗透维里系数,可与克分子浓度和摩尔分数的浓度单位一起使用,并解释了实施多溶质渗透维里方程所需的背景和理论。

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