The velocity sedimentation of solutes consisting of a monomer in rapidly established equilibrium with a tetramer has been simulated using a realistic model and a digital computer. The results are compared with the no-diffusion treatments of the same systems and with the simulated experiments done previously for trimerizing solutes. In the absence of diffusion, most of the tetramerizing solutes examined would have produced bimodal sedimenting boundaries. When diffusion was taken into account, the tendency to exhibit bimodal gradient profiles was more obvious in monomer-tetramer systems than in comparable monomer-trimer systems. The characteristic boundary shapes predicted by the no-diffusion model were less seriously obscured by the presence of dimer in the monomer-tetramer case than in the monomer-trimer case. Diagnostically useful shoulders and subsidiary maxima persisted in the simulated schlieren patterns given by tetramerizing solutes with monomer molecular weights as low as 20,000. Hydrodynamic concentration dependence of the sedimentation coefficients of the various solute species did not greatly obscure the unusual structure of either the monomer-trimer or the monomer-tetramer gradient profiles.
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