The flexibility of low molecular weight double-stranded DNA as a function of length. I. Light scattering measurements and the estimation of persistence lengths from light scattering, sedimentation and viscosity.

In the preceding paper are described the isolation and physical characterization of seven narrowly disperse fractions of calf thymus DNA in the molecular weight range 0.3 to 1.3 X 10(6) daltons. Herein, we have determined by light scattering the molecular weights and root mean square radii of these fractions in a solvent comprising 0.2 M NaCl, 2 mM EDTA, 2mM Na-PO4,pH7. Measurements were made in a modified Wippler-Scheibling photometer to a 20 degree lower limit of scattering angle on solutions rendered virtually dust-free by procedures described. The optical anisotropies of the DNA fractions were measured permitting the experimental molecular weights and root mean square radii to be corrected to their true values. From these values, with appropriate polydispersity corrections, we calculate a Kratky-Porod persistence length, a, of 54.0 +/- 5.6 nm which is invariant over the molecular range examined. From the sedimentation coefficients (preceding paper) and the theory of Yamakawa and Fujii, we calculate a to be 66 nm, a value found to apply equally well to several DNA samples of various origins whose sedimentation rates are known in themolecular weight range from about 4 X 10(4) to 10(8) daltons. Similarly, from the intrinsic viscosities and the theory of Yamakawa and Fujii, we calculate a to be 59 nm, which again adequately applies to a number of DNA samples whose viscosities have been measured by other workers in the molecular wieght range 3 X 10(5) to 10(8) daltons. The Flory-Mandelkern paramerter, beta, was found to vary with molecular weight in the manner predicted by the theory of Yamakawa and Fujii. The average value of a from the three sets of measurements is 60 +/- 6nm, which we believe applies to double-stranded DNA molecules, independent of chain length, over the whole range of molecular weights from which reliable data exist.

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