黄赭石的XRD、TEM、EPR、IR及非线性光学研究

S. LakshmiReddy, U. Reddy, T. RavindraReddy, A. Thomas, R. RamaSubbaReddy, R. Frost, T. Endo
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引用次数: 7

摘要

本文研究了印度安得拉邦库达帕区Vempalli mandal的黄赭石矿物。化学分析表明,Fe2O3=4.22 wt%, TiO2=0.64 wt%。用x射线衍射(XRD)进行了结构表征。XRD结果表明,样品中存在针铁矿(Fe2O3)和石英。其中针铁矿是主要成分。其晶胞为正交晶胞,a=4.14, b=10.0, c=3.03A。利用傅里叶红外光谱研究了结构中金属离子周围的配体。透射电镜分析表明,该矿物由针状氧化铁纳米颗粒和石英组成,呈四面体和八面体层状。EPR结果表明,晶胞中含有Fe(III),其g值分别为4.19和2.13。FTIR性能是由于存在硅酸盐和羟基阴离子作为配体。使用z -扫描进行的非线性光学测量揭示了材料中存在强非线性光学限制,表明在激光安全装置中的潜在应用。
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XRD, TEM, EPR, IR and Nonlinear Optical Studies of Yellow Ochre
Yellow ochre mineral obtained from Vempalli mandal, Cuddapah district, Andhra Pradesh of India is investigated in the present work. Its chemical analysis indicate that Fe2O3=4.22 wt% and TiO2=0.64 wt%. Structural characterization is performed using X-ray diffraction (XRD). XRD results suggest that goethite (Fe2O3) and quartz are present. Among them goethite is the major constituent. Its unit cell is orthorhombic with a=4.14, b=10.0, c=3.03A. The ligands around the metal ion present in the structure are investigated using FTIR spectroscopy. Internal structure studied using TEM suggests that the mineral consists of needle shaped iron oxide nano particles and quartz formed as tetrahedral and octahedral layers. EPR results indicate that the unit cell of the crystal contains Fe(III), and its g values are found to be 4.19 and 2.13. FTIR properties are due to the presence of silicate and hydroxyl anions as ligands. Nonlinear optical measurements carried out using Z-scan reveal the presence of strong nonlinear optical limiting in the material, indicating potential applications in laser safety devices.
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