Dynamics of water in LiCl and CaCl2 aqueous solutions confined in silica matrices:: A backscattering neutron spectroscopy study

被引:52
作者
Mamontov, E. [1 ]
Cole, D. R. [2 ]
Dai, S. [2 ]
Pawel, M. D. [3 ]
Liang, C. D. [2 ]
Jenkins, T. [4 ,5 ]
Gasparovic, G. [4 ,5 ]
Kintzel, E. [1 ]
机构
[1] Oak Ridge Natl Lab, Spallat Neutron Source, Oak Ridge, TN 37831 USA
[2] Oak Ridge Natl Lab, Div Chem Sci, Oak Ridge, TN 37831 USA
[3] Oak Ridge Natl Lab, Ctr Nanophase Mat Sci Div, Oak Ridge, TN 37831 USA
[4] Natl Inst Stand & Technol, NIST Ctr Neutron Res, Gaithersburg, MD 20899 USA
[5] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA
基金
美国国家科学基金会;
关键词
water; confinement; dynamics; neutron scattering;
D O I
10.1016/j.chemphys.2008.05.019
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
Backscattering neutron spectroscopy was used to probe the dynamics of water molecules in LiCl and CaCl2 aqueous solutions confined in 2.7, 1.9, and 1.4 nm diameter pores of various silica matrices. The pore size of 2.7 nm was found to be sufficiently large for the confined liquids to exhibit characteristic traits of bulk behavior, such as a freezing-melting transition and a phase separation. On the other hand, none of the fluids in the 1.4 nm pores exhibited a clear freezing-melting transition; instead, their dynamics at low temperatures gradually became too slow for the nanosecond resolution of the experiment. The greatest suppression of water mobility was observed in the CaCl2 solutions, which suggests that cation charge and perhaps the cation hydration environment have a profound influence on the dynamics of the water molecules. Quasielastic neutron scattering measurements of pure H2O and 1 m LiCl-H2O solution confined in 1.9 nm pores revealed a dynamic transition in both liquids at practically the same temperature of 225-226 K, even though the dynamics of the solution at room temperature appeared to slow down by more than an order of magnitude compared to the pure water. The observation of the dynamic transition in the solution suggests that this transition may be a universal feature of water governed by processes acting on the local scale, such as a change in the hydrogen bonding. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:117 / 124
页数:8
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