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  2. 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]

  3. 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]

  4. 11S globulin family - Wikipedia

    en.wikipedia.org/wiki/11S_globulin_family

    It is characterized by a hexamer (with hexagonal shape). Several residues are conserved among 11S family. Like other globulins, they are not completely digested and broken into amino acids and have the potential to bind to various proteins in the body and can exert effects independent of their amino acids constituents, even after consumption. [3]

  5. 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 ...

  6. 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

  7. Soil - Wikipedia

    en.wikipedia.org/wiki/Soil

    Once in the soil-plant system, most nutrients are recycled through living organisms, plant and microbial residues (soil organic matter), mineral-bound forms, and the soil solution. Both living soil organisms (microbes, animals and plant roots) and soil organic matter are of critical importance to this recycling, and thereby to soil formation ...

  8. Eukaryotic ribosome - Wikipedia

    en.wikipedia.org/wiki/Eukaryotic_ribosome

    Sedimentation coefficient 60 S 50 S Molecular mass ~2.0×10 6 Da ~1.3×10 6 Da Proteins 46 33 rRNAs 25/28 S rRNA (3354 nucleotides) 5 S rRNA (120 nucleotides) 5.8 S rRNA (154 nucleotides) 23S rRNA (2839 nucleotides) 5S rRNA (122 nucleotides) Small subunit Sedimentation coefficient 40 S 30 S Molecular mass ~1.2×10 6 Da ~0.7×10 6 Da Proteins 33 ...

  9. Proteasome - Wikipedia

    en.wikipedia.org/wiki/Proteasome

    The proteasome subcomponents are often referred to by their Svedberg sedimentation coefficient (denoted S). The proteasome most exclusively used in mammals is the cytosolic 26S proteasome, which is about 2000 kilodaltons (kDa) in molecular mass containing one 20S protein subunit and two 19S regulatory cap subunits. The core is hollow and ...

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