Department of Nuclear Science and Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA.
J Am Chem Soc. 2011 Mar 2;133(8):2499-510. doi: 10.1021/ja107003a. Epub 2011 Feb 4.
We present the structural and dynamic nature of water ultraconfined in the quasi-two-dimensional nanopores of the highly disordered calcium-silicate-hydrate (C-S-H), the major binding phase in cement. Our approach is based on classical molecular simulations. We demonstrate that the C-S-H nanopore space is hydrophilic, particularly because of the nonbridging oxygen atoms on the disordered silicate chains which serve as hydrogen-bond acceptor sites, directionally orienting the hydrogen atoms of the interfacial water molecules toward the calcium-silicate layers. The water in this interlayer space adopts a unique multirange structure: a distorted tetrahedral coordination at short range up to 2.7 Å, a disordered structure similar to that of dense fluids and supercooled phases at intermediate range up to 4.2 Å, and persisting spatial correlations through dipole-dipole interactions up to 10 Å. A three-stage dynamics governs the mean square displacement (MSD) of water molecules, with a clear cage stage characteristic of the dynamics in supercooled liquids and glasses, consistent with its intermediate-range structure identified here. At the intermediate time scales corresponding to the β-relaxation of glassy materials, coincident with the cage stage in MSD, the non-Gaussian parameter indicates a significant heterogeneity in the translational dynamics. This dynamic heterogeneity is induced primarily because of the heterogeneity in the distribution of hydrogen bond strengths. The strongly attractive interactions of water molecules with the calcium silicate walls serve to constrain their motion. Our findings have important implications on describing the cohesion and mechanical behavior of cement from its setting to its aging.
我们介绍了水在高度无序的硅酸钙水合物(C-S-H)准二维纳米孔中极度受限的结构和动力学性质,C-S-H 是水泥的主要结合相。我们的方法基于经典分子模拟。我们证明了 C-S-H 纳米孔空间是亲水的,这主要是由于无序硅酸盐链上的非桥氧原子充当氢键受体位点,从而定向排列界面水分子的氢原子朝向钙-硅酸盐层。这种夹层空间中的水采用独特的多范围结构:在短程(可达 2.7 Å)下呈扭曲的四面体配位,在中程(可达 4.2 Å)下呈类似于密集流体和过冷相的无序结构,通过偶极-偶极相互作用保持空间相关性可达 10 Å。水分子的均方位移(MSD)受三阶段动力学控制,具有明确的笼状阶段,这是过冷液体和玻璃动力学的特征,与这里确定的中间范围结构一致。在对应于玻璃状材料β弛豫的中间时间尺度上,与 MSD 的笼状阶段一致,非高斯参数表明平移动力学存在显著的非均一性。这种动态异质性主要是由于氢键强度分布的异质性引起的。水分子与钙硅酸盐壁之间的强吸引力相互作用限制了它们的运动。我们的发现对描述水泥从凝固到老化过程中的内聚性和力学行为具有重要意义。