Quantitative elemental analysis of high silica bauxite using calibration-free laser-induced breakdown spectroscopy

被引:18
|
作者
Fahad, Muhammad [1 ]
Ali, Sajjad [2 ]
Shah, Khizar Hussain [3 ]
Shahzad, Asim [4 ]
Abrar, Muhammad [5 ]
机构
[1] COMSATS Univ Islamabad, Dept Elect & Comp Engn, Abbottabad Campus,Univ Rd, Abbottabad 22060, Pakistan
[2] Univ Peshawar, Dept Phys, MRL, Peshawar 25120, Pakistan
[3] COMSATS Univ Islamabad, Dept Chem, Abbottabad Campus,Univ Rd, Abbottabad 22060, Pakistan
[4] Cent S Univ, Sch Geosci & Infophys, Geosci Bldg, Changsha 410083, Hunan, Peoples R China
[5] Hazara Univ Mansehra, Dept Phys, Mansehra 21300, Pakistan
关键词
X ray diffraction - Laser induced breakdown spectroscopy - Aluminum - Atomic emission spectroscopy - Fourier transform infrared spectroscopy - Scanning electron microscopy - Calibration - Fluorescence spectroscopy - Spectrum analysis - Silica - Energy dispersive spectroscopy;
D O I
10.1364/AO.58.007588
中图分类号
O43 [光学];
学科分类号
070207 ; 0803 ;
摘要
Bauxite is a primary ore of aluminum. Precise information about bauxite mineralogical composition is challenging and crucial for efficient aluminum extraction and for the determination of its appropriateness for different industrial applications. For the qualitative and quantitative analysis of bauxite ore, we performed laser-induced breakdown spectroscopy (LIBS) in conjunction with x-ray diffraction (XRD), x-ray fluorescence spectroscopy (XRF), scanning electron microscopy coupled with energy dispersive x-ray spectroscopy (SEM-EDS), and Fourier transform infrared spectroscopy (FTIR). Analysis of the acquired optical emission spectrum revealed the presence of Si, Al, Fe, K, Ti, Ca, Mg, Na, Cr, and Sr. The plasma temperature and electron number density values estimated using Boltzmann plot and Stark-broadening line profile methods were 5600 K and 7.65 x 10(17) cm(-3), respectively. In the present study we show that a calibration-free LIBS method presents a powerful solution, enabling quantitative analysis of multi-element bauxite ore better than traditional analytical techniques. The bauxite quantification obtained using CF-LIBS under the assumption of local thermodynamic equilibrium and optically thin plasma was Si = 47.31%, Al = 31.90%, Fe = 16.54%, K = 2.45%, Ti = 1.64%, and Ca = 0.16%, and its comparison with the outcome from XRD, XRF, SEM-EDS, and FTIR not only assisted but potentially enhanced the mineralogical composition understanding of bauxite ore in the present study. (C) 2019 Optical Society of America
引用
收藏
页码:7588 / 7596
页数:9
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