Virtual Probes of Mineral-Water Interfaces: The More Flops, the Better!

被引:12
|
作者
Stack, Andrew G. [1 ]
Gale, Julian D. [2 ,3 ]
Raiteri, Paolo [2 ,3 ]
机构
[1] Oak Ridge Natl Lab, Div Chem Sci, Oak Ridge, TN 37831 USA
[2] Curtin Univ, Nanochem Res Inst, Perth, WA 6845, Australia
[3] Curtin Univ, Dept Chem, Perth, WA 6845, Australia
基金
澳大利亚研究理事会;
关键词
simulation; molecular dynamics; calcite; barite; kinetics; AMORPHOUS CALCIUM-CARBONATE; MOLECULAR-DYNAMICS; CRYSTAL-GROWTH; AQUEOUS-SOLUTION; FREE-ENERGY; DISSOLUTION; EXCHANGE; SURFACE; ION; MECHANISMS;
D O I
10.2113/gselements.9.3.211
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
New approaches are allowing computer simulations to be compared quantitatively with experimental results, and they are also raising new questions about reactivity at mineral-water interfaces. Molecular simulations not only help us to understand experimental observations, they can also be used to test hypotheses about the properties of geochemical systems. These new approaches include rigorous calibration of simulation models against thermodynamic properties and atomic structure. They also encompass rare event theory methods that allow simulation of slow, complex mineral surface reactions. Here, we give an overview of how these techniques have been applied to simulate mineral-water interface structure, growth/dissolution mechanisms, and cluster formation.
引用
收藏
页码:211 / 216
页数:6
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