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  2. Sedimentation coefficient - Wikipedia

    en.wikipedia.org/wiki/Sedimentation_coefficient

    The sedimentation coefficient is typically dependent on the concentration of the solute (i.e. a macromolecular solute such as a protein). Despite 80+ years of study, there is not yet a consensus on the way to perfectly model this relationship while also taking into account all possible non-ideal terms to account for the diverse possible sizes, shapes, and densities of molecular solutes. [2]

  3. Svedberg - Wikipedia

    en.wikipedia.org/wiki/Svedberg

    A laboratory ultracentrifuge. In chemistry, a Svedberg unit or svedberg (symbol S, sometimes Sv [a]) is a non-SI metric unit for sedimentation coefficients.The Svedberg unit offers a measure of a particle's size indirectly based on its sedimentation rate under acceleration (i.e. how fast a particle of given size and shape settles out of suspension). [1]

  4. Mason–Weaver equation - Wikipedia

    en.wikipedia.org/wiki/Mason–Weaver_equation

    where t is the time, c is the solute concentration (moles per unit length in the z-direction), and the parameters D, s, and g represent the solute diffusion constant, sedimentation coefficient and the (presumed constant) acceleration of gravity, respectively. The Mason–Weaver equation is complemented by the boundary conditions

  5. Lamm equation - Wikipedia

    en.wikipedia.org/wiki/Lamm_equation

    The first and second terms on the right-hand side of the Lamm equation are proportional to D and sω 2, respectively, and describe the competing processes of diffusion and sedimentation. Whereas sedimentation seeks to concentrate the solute near the outer radius of the cell, diffusion seeks to equalize the solute concentration throughout the cell.

  6. Sedimentation equilibrium - Wikipedia

    en.wikipedia.org/wiki/Sedimentation_equilibrium

    The advantage of using analytical sedimentation equilibrium analysis for Molecular Weight of proteins and their interacting mixtures is the avoidance of need for derivation of a frictional coefficient, otherwise required for interpretation of dynamic sedimentation. Sedimentation equilibrium can be used to determine molecular mass.

  7. Centrifugation - Wikipedia

    en.wikipedia.org/wiki/Centrifugation

    In order to investigate this phenomenon, a centrifuge with even higher speeds was needed, and thus the ultracentrifuge was created to apply the theory of sedimentation-diffusion. [24] The same molecular mass was determined, and the presence of a spreading boundary suggested that it was a single compact particle. [ 24 ]

  8. Clearing factor - Wikipedia

    en.wikipedia.org/wiki/Clearing_factor

    The K-factor is related to the sedimentation coefficient by the formula: = Where is the time to pellet a certain particle in hours. Since is a constant for a certain particle, this relationship can be used to interconvert between different rotors.

  9. Differential centrifugation - Wikipedia

    en.wikipedia.org/wiki/Differential_centrifugation

    Sedimentation depends on mass, shape, and partial specific volume of a macromolecule, as well as solvent density, rotor size and rate of rotation. The sedimentation velocity can be monitored during the experiment to calculate molecular weight. Values of sedimentation coefficient (S) can be calculated. Large values of S (faster sedimentation ...