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Structural and Electronic Properties of Iron-DopedSodium Montmorillonite Clays: A First-Principles DFT Study

机译:铁掺杂的结构和电子性质蒙脱土钠粘土:DFT研究的首要原理

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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:利用密度泛函理论进行了第一性原理计算,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 + 系统弛豫之后,随后对磁矩和磁态进行分析,系统的电子中性确定了Fe 2 + 和Fe 可能会发生3 + 氧化态。 Mg 2 + -Mt-Na + 材料的带隙能大于Fe 2 + -Mt-Na + (当铁位于八面体位置时)。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。 Fe 2 + -Mt-Na + 的杂合功能(HSE06)计算出的带隙等于4.3 eV,与紫外可见实验结果吻合良好天然Mt-Na + (Cloisite-Na + )的光谱学。

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