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Atomistic simulations of calcite nanoparticles and their interaction with water

机译:方解石纳米粒子及其与水相互作用的原子模拟

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Molecular dynamics (MD) simulations have been used to study the stability of calcite nanoparticles ranging in size from 18 to 324 f.u., both in vacuo and in the presence of explicit water molecules. In vacuo, the smallest particles become highly disordered during the MD simulation due to rotation and translation of the undercoordinated CO32- anions at the edges of the particles. As the nanoparticle size increases, the influence of the fully coordinated bulk ions begins to dominate and long-range order is seen both in the Ca-C pair distribution functions and in the degree of rotational order of the CO32- anions. However, when explicit water is added to the system, the molecules in the first hydration layer complete the coordination shell of the surface ions, preserving structural order even in the smallest of the nanoparticles. Close to particle surface, the structure of the water itself shows features similar to those seen close to planar periodic (10 < over bar > 1 < over bar > 4) surfaces, although the molecules are far less tightly bound.
机译:分子动力学(MD)模拟已被用于研究方解石纳米粒子在真空中和存在明显水分子的情况下的稳定性,尺寸从18至324 f.u.不等。在真空中,最小的粒子在MD模拟过程中会由于粒子边缘处配位不足的CO32-阴离子的旋转和平移而变得高度无序。随着纳米颗粒尺寸的增加,完全配位的整体离子的影响开始占主导地位,并且在Ca-C对分布函数和CO32-阴离子的旋转顺序中都可以看到远距离有序。但是,当向系统中添加明确的水时,第一水合层中的分子会完成表面离子的配位壳,即使在最小的纳米颗粒中也能保持结构顺序。接近粒子表面,水本身的结构显示出与接近平面周期性表面(10 1 4)的表面相似的特征,尽管分子之间的结合远不那么紧密。

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