Dadarlat Voichita M, Post Carol Beth
Department of Medicinal Chemistry and Molecular Pharmacology, Markey Center for Structural Biology, Purdue Cancer Center, Purdue University, West Lafayette, IN, USA.
Biophys J. 2006 Dec 15;91(12):4544-54. doi: 10.1529/biophysj.106.087726. Epub 2006 Sep 22.
The experimental determination of protein compressibility reflects both the protein intrinsic compressibility and the difference between the compressibility of water in the protein hydration shell and bulk water. We use molecular dynamics simulations to explore the dependence of the isothermal compressibility of the hydration shell surrounding globular proteins on differential contributions from charged, polar, and apolar protein-water interfaces. The compressibility of water in the protein hydration shell is accounted for by a linear combination of contributions from charged, polar, and apolar solvent-accessible surfaces. The results provide a formula for the deconvolution of experimental data into intrinsic and hydration contributions when a protein of known structure is investigated. The physical basis for the model is the variation in water density shown by the surface-specific radial distribution functions of water molecules around globular proteins. The compressibility of water hydrating charged atoms is lower than bulk water compressibility, the compressibility of water hydrating apolar atoms is somewhat larger than bulk water compressibility, and the compressibility of water around polar atoms is about the same as the compressibility of bulk water. We also assess whether hydration water compressibility determined from small compound data can be used to estimate the compressibility of hydration water surrounding proteins. The results, based on an analysis from four dipeptide solutions, indicate that small compound data cannot be used directly to estimate the compressibility of hydration water surrounding proteins.
蛋白质压缩性的实验测定既反映了蛋白质的固有压缩性,也反映了蛋白质水化层中的水与本体水的压缩性差异。我们使用分子动力学模拟来探究球状蛋白质周围水化层的等温压缩性对带电、极性和非极性蛋白质 - 水界面的不同贡献的依赖性。蛋白质水化层中水的压缩性由带电、极性和非极性溶剂可及表面的贡献的线性组合来解释。当研究已知结构的蛋白质时,这些结果提供了一个将实验数据解卷积为固有贡献和水化贡献的公式。该模型的物理基础是球状蛋白质周围水分子的表面特异性径向分布函数所显示的水密度变化。与带电原子水化的水的压缩性低于本体水的压缩性,与非极性原子水化的水的压缩性略大于本体水的压缩性,而极性原子周围水的压缩性与本体水的压缩性大致相同。我们还评估了从小分子化合物数据确定的水化水压缩性是否可用于估计蛋白质周围水化水的压缩性。基于对四种二肽溶液的分析结果表明,小分子化合物数据不能直接用于估计蛋白质周围水化水的压缩性。