Structural dynamics of supercooled water from quasielastic neutron scattering and molecular simulations

被引:154
|
作者
Qvist, Johan [1 ]
Schober, Helmut [2 ]
Halle, Bertil [1 ]
机构
[1] Lund Univ, SE-22100 Lund, Sweden
[2] Inst Max Von Laue Paul Langevin, F-38042 Grenoble 9, France
来源
JOURNAL OF CHEMICAL PHYSICS | 2011年 / 134卷 / 14期
基金
瑞典研究理事会;
关键词
KINETIC GLASS-TRANSITION; LIQUID WATER; SELF-DIFFUSION; TEMPERATURE-DEPENDENCE; RELAXATION PROCESSES; JUMP DIFFUSION; HYDROGEN-BOND; MODEL; MOTIONS; REORIENTATION;
D O I
10.1063/1.3578472
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
One of the outstanding challenges presented by liquid water is to understand how molecules can move on a picosecond time scale despite being incorporated in a three-dimensional network of relatively strong H-bonds. This challenge is exacerbated in the supercooled state, where the dramatic slowing down of structural dynamics is reminiscent of the, equally poorly understood, generic behavior of liquids near the glass transition temperature. By probing single-molecule dynamics on a wide range of time and length scales, quasielastic neutron scattering (QENS) can potentially reveal the mechanistic details of water's structural dynamics, but because of interpretational ambiguities this potential has not been fully realized. To resolve these issues, we present here an extensive set of high-quality QENS data from water in the range 253-293 K and a corresponding set of molecular dynamics (MD) simulations to facilitate and validate the interpretation. Using a model-free approach, we analyze the QENS data in terms of two motional components. Based on the dynamical clustering observed in MD trajectories, we identify these components with two distinct types of structural dynamics: picosecond local (L) structural fluctuations within dynamical basins and slower interbasin jumps (J). The Q-dependence of the dominant QENS component, associated with J dynamics, can be quantitatively rationalized with a continuous-time random walk (CTRW) model with an apparent jump length that depends on low-order moments of the jump length and waiting time distributions. Using a simple coarse-graining algorithm to quantitatively identify dynamical basins, we map the Newtonian MD trajectory on a CTRW trajectory, from which the jump length and waiting time distributions are computed. The jump length distribution is Gaussian and the rms jump length increases from 1.5 to 1.9 angstrom as the temperature increases from 253 to 293 K. The rms basin radius increases from 0.71 to 0.75 angstrom over the same range. The waiting time distribution is exponential at all investigated temperatures, ruling out significant dynamical heterogeneity. However, a simulation at 238 K reveals a small but significant dynamical heterogeneity. The macroscopic diffusion coefficient deduced from the QENS data agrees quantitatively with NMR and tracer results. We compare our QENS analysis with existing approaches, arguing that the apparent dynamical heterogeneity implied by stretched exponential fitting functions results from the failure to distinguish intrabasin (L) from interbasin (J) structural dynamics. We propose that the apparent dynamical singularity at similar to 220 K corresponds to freezing out of J dynamics, while the calorimetric glass transition corresponds to freezing out of L dynamics. (C) 2011 American Institute of Physics. [doi:10.1063/1.3578472]
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页数:20
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