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Sedimentation equilibrium in macromolecular solutions of arbitrary concentration. II. Two protein components

โœ Scribed by Ronald C. Chatelier; Allen P. Minton


Publisher
Wiley (John Wiley & Sons)
Year
1987
Tongue
English
Weight
894 KB
Volume
26
Category
Article
ISSN
0006-3525

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โœฆ Synopsis


Synopsis

Relations describing sedimentation equilibrium in solutions containing two macromolecular solute components are derived for the following cases: (1) two nonassociating proteins at arbitrary concentration, (2) one dilute self-associating protein in the presence of a second inert protein at arbitrary concentration, and (3) two proteins at arbitrary concentration that can associate to form a single heterocomplex of arbitrary composition. As in earlier work (R. C. Chatelier and A. P. Minton (1987) Bwpolymers, 26,507-524), the relations are obtained by using scaled particle theory to calculate the thermodynamic activity of each species present at a given radial distance in the centrifuge. The results of numerical simulations of sedimentation equilibrium are presented as the dependence of apparent molecular weights, or apparent weight-average molecular weights, upon solution composition. Semiempirical methods are presented, by means of which the weightaverage molecular weights of self-and heteroassociating proteins in highly nonideal solutions may be estimated from experimental data. It is found that the semiempirical methods yield reasonably accurate estimates of the true weight-average molecular weight over a broad range of experimental conditions, providing that the partial specific volumes of two components in a heteroassociating system do not differ by more than about 0.05 mL/g.


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Sedimentation equilibrium in macromolecu
โœ Ronald C. Chatelier; Allen P. Minton ๐Ÿ“‚ Article ๐Ÿ“… 1987 ๐Ÿ› Wiley (John Wiley & Sons) ๐ŸŒ English โš– 972 KB

## Synopsis Relations describing sedimentation equilibrium in solutions of self-associating macromolecules at arbitrary concentration are presented. These relations are obtained by using scaled-particle theory to calculate the thermodynamic activity of each species present at a given radial distan