Dynamics of colloidal particles in ice

被引:15
|
作者
Spannuth, Melissa [1 ]
Mochrie, S. G. J. [2 ]
Peppin, S. S. L. [3 ]
Wettlaufer, J. S. [1 ,2 ,4 ,5 ]
机构
[1] Yale Univ, Dept Geol & Geophys, New Haven, CT 06520 USA
[2] Yale Univ, Dept Phys, New Haven, CT 06520 USA
[3] Univ Oxford, Math Inst, OCCAM, Oxford OX1 3LB, England
[4] Yale Univ, Program Appl Math, New Haven, CT 06520 USA
[5] NORDITA, SE-10691 Stockholm, Sweden
基金
美国国家科学基金会;
关键词
SOLIDIFICATION; SUSPENSIONS; DEPENDENCE; SCATTERING;
D O I
10.1063/1.3665927
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
We use x-ray photon correlation spectroscopy (XPCS) to probe the dynamics of colloidal particles in polycrystalline ice. During freezing, the dendritic ice morphology and rejection of particles from the ice created regions of high particle density, where some of the colloids were forced into contact and formed disordered aggregates. The particles in these high density regions underwent ballistic motion, with a characteristic velocity that increased with temperature. This ballistic motion is coupled with both stretched and compressed exponential decays of the intensity autocorrelation function. We suggest that this behavior could result from ice grain boundary migration. (C) 2011 American Institute of Physics. [doi:10.1063/1.3665927]
引用
收藏
页数:5
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