Abstract

1. The effect of pH on the buoyant density of the complexes of Ag + with DNA has been studied using 3H-labeled human DNA and several bacterial DNAs to determine the conditions necessary for the maximum resolution of compositional heterogeneity. In neutral Cs 2SO 4 density gradients, Ag + complexes with (G · C)-rich components are always denser than those with (A · T)-rich components, since (G · C)rich DNAs have a larger affinity for Ag + than (A · T)-rich DNAs and their complexes are denser than (A · T)-rich complexes. In alkaline ( pH > 9 ) Cs 2SO 4 gradients, the buoyant density of the Ag + · DNA complex is not a simple function of base composition. The Ag + affinity of (A · T)-rich DNA is larger than that of (G · C)-rich DNA but the density of a (G · C)-rich complex is larger. Thus the ordering of the buoyant density changes depends on the amount of added Ag +. 2. The problem of resolving the density heterogeneity within a tracer DNA, and minor components of DNA, is explored and useful fractionation techniques are developed.

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