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Density Functional Theory Study of Ferrihydrite and Related Fe-Oxyhydroxides

机译:亚铁矿及其氢氧化铁的密度泛函理论研究

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The atomic and magnetic structure and thermodynamic stability of ferrihydrite (Fe5O8H) are calculated based on the structure recently proposed by Michel et al. (Science 2007, 316, 1726). Ferrihydrite stability is compared with that of the Fe-oxyhydroxide polymorphs goethite (a-FeOOH) and lepidocrocite (γ-FeOOH) and the oxide hematite (α-Fe2O3). The GGA+U method is employed to correct known errors in treating correlated d-electrons in Fe atoms. GGA+U yields smaller errors in calculated thermodynamic quantities relative to experiment as compared with a standard GGA functional for all of the Fe-oxyhydroxides studied. Good agreement is obtained between the DFT-predicted and experimental ferrihydrite structure when the effects of varying crystallinity and particle size are taken into account. The magnetic properties of ferrihydrite are modeled using a Heisenberg model parametrized with DFT-based magnetic coupling constants. The groundstate magnetic ordering of bulk ferrihydrite is predicted to be ferrimagnetic, with the Fe-site spins ordering with alternating alignment in layers stacked along the c-direction in the crystallographic unit cell. The groundstate is predicted to disorder to a paramagnetic structure at T_N = 250 K, undergoing a Neel transition. The enthalpy and Gibbs free energy of reaction of bulk crystalline ferrihydrite at 298.15 K are predicted to be ΔH~(298.15) _rxn)(Fe5O8H) = 6.4 kJ/(mol-Fe) and ΔG~(298.15) _(rxn)(Fe5O8H) = 6.9kJ/(mol-Fe), respectively, relative to bulk hematite and liquid water. The values demonstrate that fully crystalline ferrihydrite is metastable with respect to the formation of both hematite and goethite at 298.15 K but may be stabilized at small particle sizes due to favorably low surface formation energy. A simple surface energy model is used to predict the formation energy of ferrihydrite nanoparticles of arbitrary size, yielding results consistent with the observed formation energies for nanoparticle samples.
机译:铁水石(Fe5O8H)的原子和磁结构以及热力学稳定性是根据Michel等人最近提出的结构计算的(Science 2007, 316, 1726)。将铁水石的稳定性与Fe-氢氧化物多晶型针铁矿(a-FeOOH)和锂云母(γ-FeOOH)以及氧化物赤铁矿(α-Fe2O3)进行了比较。采用GGA+U方法纠正了处理Fe原子中相关d电子的已知错误。与所有研究的氢氧化铁的标准GGA泛函相比,GGA+U相对于实验计算的热力学量产生较小的误差。当考虑不同结晶度和粒径的影响时,DFT预测的铁水石结构与实验铁水石结构之间取得了良好的一致性。使用海森堡模型对铁水石的磁性进行建模,该模型参数化了基于DFT的磁耦合常数。预计块状亚铁石的基态磁序是亚铁磁性的,在晶体晶胞中,Fe-位自旋在沿c方向堆叠的层中交替排列。预计基态将在 T_N = 250 K 时无序为顺磁性结构,经历 Neel 跃迁。预测块状结晶铁水石在298.15 K时的反应焓和吉布斯自由能为ΔH~(298.15) _rxn)(Fe5O8H) = 6.4 kJ/(mol-Fe),ΔG~(298.15) _(rxn)(Fe5O8H) = 6.相对于块状赤铁矿和液态水,分别为 9kJ/(mol-Fe)。这些值表明,全结晶铁水石在298.15 K时相对于赤铁矿和针铁矿的形成都是亚稳态的,但由于表面形成能低,可以在小粒径下稳定。采用简单的表面能模型预测任意尺寸的亚铁水石纳米颗粒的形成能,得到的结果与观测到的纳米颗粒样品的形成能一致。

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