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Molecular dynamics simulation of water in a contact with an iron pyrite FeS_2 surface

机译:与黄铁矿FeS_2表面接触的水的分子动力学模拟

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A strong adsorption of the water molecules to the pyrite surface is shown by a molecular dynamic simulation of the water-iron pyrite FeS_2 interface. Water molecules closest to the pyrite surface are bound by an electrostatic interaction to the iron atoms in grooves running parallel to one of the crystal axes. The grooves are about two atoms wide and are directed along (010) for the (001) surface. The position of the water-surface potential minimum and the energy of adsorption were determined by optimization for a single water molecule at the interface. At room temperature and normal density there are altogether three distinguishable layers of water above the surface. One is associated with the groove: one with H bonding to the sulphur atoms comprising the ridges separating the grooves, and the third with the soft wall boundary between the absorbed water layers and bulk region of water. Simulations were also used to explore the effect of a temperature range significant for geophysical studies.
机译:水-黄铁矿FeS_2界面的分子动力学模拟表明水分子对黄铁矿表面的强烈吸附。最靠近黄铁矿表面的水分子通过静电相互作用与平行于其中一个晶轴延伸的沟槽中的铁原子结合。凹槽大约两个原子宽,并且沿着(010)指向(001)表面。通过优化界面处的单个水分子,确定了水表面电势最小值的位置和吸附能。在室温和正常密度下,表面上方共有三层可区分的水层。一种与沟槽相关:一种与氢键结合到硫原子上,硫原子构成分隔沟槽的凸脊,第三种具有与吸收的水层和大部分水之间的软壁边界。还使用模拟来探索温度范围对地球物理研究的影响。

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