THERMODYNAMICS AND EQUILIBRIUM SEDIMENTATION ANALYSIS OF THE CLOSE APPROACH OF DNA-MOLECULES AND A MOLECULAR ORDERING TRANSITION
THERMODYNAMICS AND EQUILIBRIUM SEDIMENTATION ANALYSIS OF THE CLOSE APPROACH OF DNA-MOLECULES AND A MOLECULAR ORDERING TRANSITION
复制标题
DOI:
10.1002/bip.1981.360200615
复制
发表时间:
1981-01-01
期刊:
影响因子:
2.9
通讯作者:
LERMAN, LS
中科院分区:
文献类型:
--
作者:
BRIAN, AA;FRISCH, HL;LERMAN, LS
Measurement of the equilibrium distribution of persistence length fragments of DNA in high concentration in the ultracentrifuge shows that the reduced osmotic pressure rises much faster than linearly. From analysis of the data in terms of the Zimm cluster integral, the net interactions between helices are apparently purely repulsive at all distances. A theoretical equation of state derived from scaled particle theory with 1 adjustable parameter is in excellent agreement with the experimental data if the salt concentration is not excessively low. The parameter represents the hard-core radius in a simplified approximation to the potential function for the electrostatic repulsion between helices. It value depends on the salt concentration, and it shrinks at high salt to a radius in close agreement with direct structural estimates. At a particular value of the osmotic pressure that is only slightly salt dependent, the solution undergoes a reversible transition to a denser, turbid, optically anisotropic phase. The relation between DNA volume fraction (including the electrostatic radius) at the transition point, and the effective asymmetry of the molecules as a function of salt, is in approximate correspondence with various theoretical treatments. The experimental function extrapolates to the correct limit for spherical particles. The work needed to bring DNA to a high concentration is estimated. The phase transition is evidently 1st order.