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Updated: Nov 7, 2025

Sedimentation Equilibrium of a Small Oligomer-forming Membrane Protein: Effect of Histidine Protonation on Pentameric Stability
Published on: April 2, 2015
Quantifying the concentration dependence of sedimentation coefficients for globular macromolecules: a continuing
Donald J Winzor1, Vlad Dinu2, David J Scott2,3
1School of Chemistry and Molecular Biosciences, University of Queensland, Brisbane, Queensland 4072 Australia.
Early attempts to model radial dilution effects in sedimentation velocity experiments require higher precision than current analytical ultracentrifuges provide. For dilute systems, use average sedimentation coefficients related to mean plateau concentrations until optical systems improve.
Area of Science:
- Biophysical Chemistry
- Macromolecular Science
- Analytical Ultracentrifugation
Background:
- Sedimentation velocity experiments are crucial for characterizing macromolecular behavior.
- Accurate determination of the sedimentation coefficient (s) dependence on concentration (c) is vital for understanding molecular interactions and properties.
- Theoretical models for radial dilution effects in sedimentation velocity experiments have historically faced limitations due to experimental precision.
Purpose of the Study:
- To evaluate the feasibility of directly incorporating radial dilution effects into sedimentation coefficient calculations.
- To identify the simplest, most accurate method for quantifying linear s-c dependence in dilute systems using current analytical ultracentrifuge technology.
- To propose improvements for optical systems to enhance precision in sedimentation velocity experiments.
Main Methods:
- Retrospective analysis of theoretical models for radial dilution in sedimentation velocity experiments.
- Evaluation of precision requirements for concentration distributions in analytical ultracentrifugation.
- Assessment of standard c(s), g*(s), and G(s) analysis methods for determining average sedimentation coefficients.
Main Results:
- Early theoretical models require concentration distribution precision exceeding that of current analytical ultracentrifuge optical systems.
- For dilute systems, the simplest approach involves using an average sedimentation coefficient () corresponding to the mean plateau concentration () after radial dilution.
- The relationship between this average parameter and current descriptions of concentration dependence for sedimentation and translational diffusion coefficients was examined.
Conclusions:
- Directly incorporating radial dilution effects into sedimentation coefficient calculations is currently limited by experimental precision.
- The use of average sedimentation coefficients provides a practical method for analyzing dilute systems with existing technology.
- Significant improvements in analytical ultracentrifuge optical systems are necessary for more precise measurements and advanced theoretical modeling.
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