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首页> 外文期刊>ACS Omega >Structural and Electronic Properties of Iron-Doped Sodium Montmorillonite Clays: A First-Principles DFT Study
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Structural and Electronic Properties of Iron-Doped Sodium Montmorillonite Clays: A First-Principles DFT Study

机译:铁掺杂蒙脱土钠粘土的结构和电子性质:第一性原理DFT研究

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摘要

First-principles calculations done via density functional theory were used to study the structural and electronic properties of sodium montmorillonite clay (Mt-Na+) of general formula MxAl3Si8O24H4Na·nH2O (Mx: Mg or Fe). The final position of the interlamellar sodium atom is found to be close to the oxygen atoms located on the upper surface of silica. Following Fe-Mt-Na+ system relaxation, with subsequent analysis of magnetic moment and magnetic states, the electroneutrality of the system established that both Fe2+ and Fe3+ oxidation states are possible to occur. The Mg2+-Mt-Na+ material shows a band gap energy greater than that of Fe2+-Mt-Na+ when iron is in the octahedral site. It is found that the valence-band maximum and the conduction-band minimum of iron-doped montmorillonite are both at the Γ-point, while it is at V → Γ for magnesium-doped montmorillonite. The calculated band gap from hybrid functional (HSE06) of Fe2+-Mt-Na+ is equal to 4.3 eV, exhibiting good agreement with experimental results obtained from ultraviolet–visible spectroscopy of the natural Mt-Na+ (Cloisite-Na+).
机译:通过密度泛函理论进行第一性原理计算,研究了通式为MxAl3Si8O24H4Na·nH2O(Mx:Mg或Fe)的钠蒙脱土(Mt-Na +)的结构和电子性能。发现层间钠原子的最终位置接近位于二氧化硅上表面的氧原子。在Fe-Mt-Na +系统松弛之后,通过随后的磁矩和磁态分析,该系统的电中性确定了Fe2 +和Fe3 +氧化态均可能发生。当铁位于八面体位置时,Mg2 + -Mt-Na +材料的带隙能大于Fe2 + -Mt-Na +的带隙能。发现掺铁蒙脱石的价带最大值和导带最小值均在Γ点,而掺镁蒙脱石的价带和导带最小值均在V→Γ。由Fe2 + -Mt-Na +的杂合功能(HSE06)计算得出的带隙等于4.3 eV,与从天然Mt-Na +(Cloisite-Na +)的紫外可见光谱获得的实验结果具有很好的一致性。

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