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Conventional sedimentation equilibrium experiments

Analysis of Mixed Associations from Conventional Sedimentation Equilibrium Experiments. In these experiments one measures a quantity Mieq (14, 28) instead of Mweq. The basic sedimentation equilibrium equation for each reactant is... [Pg.278]

The analysis of nonideal, mixed associations from conventional sedimentation equilibrium experiments is a very difficult matter, and at present seems to be an impasse. These difficulties arise because the redistribution of the reactants is combined with nonideal behavior. We can illustrate the difficulties with the following example. The equation for reactant A can be written as... [Pg.283]

The sedimentation equilibrium experiment requires much smaller volumes of solution, about 0.15 ml. With six-hole rotors and multichannel centerpieces (41) it is potentially possible to do fifteen experiments at the same time. For situations where the photoelectric scanner can be used one might (depending on the extinct coefficients) be able to go to much lower concentrations. Dust is no problem since the centrifugal field causes it to go to the cell bottom. For conventional sedimentation equilibrium experiments, the analysis of mixed associations under nonideal conditions may be virtually impossible. Also, sedimentation equilibrium experiments take time, although methods are available to reduce this somewhat (42, 43). For certain situations the combination of optical systems available to the ultracentrifuge may allow for the most precise analysis of a mixed association. The Archibald experiment may suffer some loss in precision since one must extrapolate the data to the cell extremes (rm and r6) to obtain MW(M, which must then be extrapolated to zero time. Nevertheless, all three methods indicate that it is quite possible to study mixed associations. We have indicated some approaches that could be used to overcome problems of nonideality, unequal refractive index increments, and unequal partial specific volumes. [Pg.289]

Two ultracentrifuge sedimentation equilibrium experiments were carried out with ribonuclease in aqueous solution. The first was run in a conventional 12-mm cell and the second was performed in a synthetic boundary cell. The schematic diagrams of the ultracentrifuge patterns are shown in the following ... [Pg.264]

The equilibrium sedimentation experiment of sample P was analyzed only by applying the computation-oriented expressions. The resulting f(M) was compared with the previously obtained f(M). From the curve of f(M) the average values were computed and compared with the values computed in the same way from individual distribution curves of fractions A, B, and C. These values were also compared with M values obtained in a conventional way from equilibrium sedimentation by applying Equation 2, and with M values determined from velocity sedimentation experiment, Equation 30 (see Table II). [Pg.236]


See other pages where Conventional sedimentation equilibrium experiments is mentioned: [Pg.273]    [Pg.283]    [Pg.273]    [Pg.283]    [Pg.86]    [Pg.186]    [Pg.186]    [Pg.128]    [Pg.1296]   
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