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Theory of boundary spreading in velocity ultracentrifugation of polydisperse solutes
Author(s) -
Fujita Hiroshi
Publication year - 1969
Publication title -
biopolymers
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.556
H-Index - 125
eISSN - 1097-0282
pISSN - 0006-3525
DOI - 10.1002/bip.1969.360070106
Subject(s) - chemistry , sedimentation coefficient , analytical ultracentrifugation , constant (computer programming) , distribution (mathematics) , sedimentation , thermodynamics , boundary (topology) , diffusion , plot (graphics) , analytical chemistry (journal) , mathematical analysis , chromatography , physics , ultracentrifuge , mathematics , statistics , enzyme , paleontology , biochemistry , sediment , computer science , programming language , biology
Under the assumptions that the rectangular approximation to the sector‐shaped cell is valid and that both the sedimentation coefficient s and the diffusion coefficient D are independent of concentration, asymptotic solutions to the boundary spreading equation for velocity ultracentrifugation of polydisperse solutes have been derived for three cases: case A, D = constant for all s ; case B, sD = constant; case C, \documentclass{article}\pagestyle{empty}\begin{document}$ \sqrt {sD} = {\rm constant} $\end{document} . Case A is the situation treated by all of the previous authors but supposed to be unrealistic for ordinary macromolecular solutes. Cases B and C may be associated with synthetic polymers under theta conditions and globular proteins in aqueous media, respectively. The solutions obtained have been used to explore the theoretical background of the empirical Gralén method for evaluating the distribution of s from sedimentation boundary curves, with special interest in the behavior of a plot for S versus 1/ t . Here S is the value of s for a fixed value of the apparent integral distribution of s and t is the time of centrifugation. It was found that when the distribution of s is Gaussian‐like and fairly narrow, this plot becomes linear over a more extended range of t in the order case B > case C > case A.