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DNA orientation in shear flow
Author(s) -
Simonson Tomas,
Kubista Mikael
Publication year - 1993
Publication title -
biopolymers
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.556
H-Index - 125
eISSN - 1097-0282
pISSN - 0006-3525
DOI - 10.1002/bip.360330809
Subject(s) - ionic strength , persistence length , chemistry , ionic bonding , dna , shear (geology) , shear flow , velocity gradient , linear dichroism , crystallography , physics , circular dichroism , molecule , thermodynamics , materials science , aqueous solution , biochemistry , composite material , ion , organic chemistry
The linear dichroism (LD) has been measured for DNA molecules 239–164,000 base pairs long oriented in shear flow over a large range of velocity gradients (30–3,000 s −1 ) and ionic strengths (2–250 m M ). At very low gradients, the degree of DNA orientation increases quadratically with the applied shear as predicted by the Zimm theory [J. Zimm, (1956) Chemical Physics , Vol. 24, p. 269]. At higher gradients, the orientation of fragments ≥ 7 kilobase pairs (kbp) increases linearly with increasing shear, whereas the orientation of fragments ≥ 15 kbp shows a more complicated dependence. In general, the orientation decreases with increasing ionic strength throughout the studied ionic strength interval, owing to a decrease in the persistence length of the DNA. The effect is most dramatic at ionic strengths below 10 m M , and is more pronounced for longer DNA fragments. For fragments ≥ 15 kbp and velocity gradients ≥ 100 s −1 , the orientation can be adequately described by the empirical relation: LD r = –( k 1 ‐G)/( k 2 + G), where k 1 is a linear function of the square root of the ionic strength and k 2 depends on the DNA contour length. Since the DNA persistence length can be represented as a linear function of the reciprocal square root of the ionic strength [D. Porschke, (1991) Biophysical Chemistry , Vol. 40, p. 169], extrapolation of the empirical relation provides information about the stiffness of the DNA fibers. © 1993 John Wiley & Sons, Inc.