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首页> 外文期刊>The journal of physical chemistry, B. Condensed matter, materials, surfaces, interfaces & biophysical >Entropy of Water in the Hydration Layer of Major and Minor Grooves of DNA
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Entropy of Water in the Hydration Layer of Major and Minor Grooves of DNA

机译:DNA主槽和副槽水化层中水的熵

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Transport properties(translational and rotational)of water in the two grooves of the B-DNA duplex are known to be different from those in the bulk.Here,we use a recently developed theoretical scheme to compute the entropies of water molecules in both of the grooves of DNA and compare them with that in the bulk.The scheme requires as input both translational and rotational velocity autocorrelation function(Cv(t)and C_(omega)(t),respectively)data.These velocity autocorrelation functions were computed from an atomistic MD simulation of a B-DNA duplex(36 base pairs long)in explicit water(TIP3P).The average values of the entropy of water at 300 K in both of the grooves of DNA(the TS value in the major groove is 6.71 kcal/mol and that in the minor groove is 6.41 kcal/mol)are found to be significantly lower than that in bulk water(the TS value is 7.27 kcal/mol).Thus,the entropic contribution to the free energy change(T DELTA S)of transferring a minor groove water molecule to the bulk is 0.86 kcal/mol and of transferring a major groove water to the bulk is 0.56 kcal/mol at 300 K,which is to be compared with 1.44 kcal/mol for melting of ice at 273 K.We also calculate the energy of interaction of each water molecule with the rest of the atoms in the system and hence calculate the chemical potential(Helmholtz free energy per water molecule,A = E - TS)in the different domains.The identical free energy value of water molecules in the different domains proves the robustness of the scheme.We propose that the configurational entropy of water in the grooves can be used as a measure of the mobility(or microviscosity)of water molecules in a given domain.
机译:众所周知,B-DNA双链体的两个凹槽中水的传输特性(平移和旋转)与整体中的不同。在这里,我们使用最近开发的理论方案来计算两个分子中水分子的熵。该方案需要分别输入平移和旋转速度自相关函数(Cv(t)和C_ω(t))数据作为输入,这些速度自相关函数由一个显性水(TIP3P)中B-DNA双链体(长36个碱基对)的原子MD模拟。两个DNA凹槽中300 K处水的熵平均值(主凹槽中的TS值为6.71) kcal / mol和小槽中的kcal / mol为6.41 kcal / mol),明显低于散装水中的TS(TS值为7.27 kcal / mol)。因此,熵对自由能变化的贡献(T DELTA)将次要凹槽水分子转移到本体上的S)为0.86 kcal / mol和在300 K下将主要沟槽水转移到主体的水为0.56 kcal / mol,与273 K下冰融化的1.44 kcal / mol进行比较。我们还计算了每种水相互作用的能量分子与系统中的其余原子结合,从而计算出不同域中的化学势(每个水分子的亥姆霍兹自由能,A = E-TS)。不同域中水分子的自由能值相同,证明了其鲁棒性我们提出,凹槽中水的结构熵可以用作给定域中水分子迁移率(或微粘度)的量度。

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