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首页> 外文期刊>X-Ray Spectrometry: An International Journal >Utilization of standardless analysis algorithms using WDXRF and XRD for Egyptian iron ore identification
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Utilization of standardless analysis algorithms using WDXRF and XRD for Egyptian iron ore identification

机译:使用WDXRF和XRD的无标准分析算法识别埃及铁矿石

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On the basis of fundamental parameter approaches, the validity of standardless wavelength dispersive X-ray fluorescence (WDXRF) and X-ray powder diffraction algorithms was confirmed for analyzing Egyptian iron ore samples collected from two different locations, Aswan and Baharyia. The studied Egyptian iron ores represent different depositional environments and consequently exhibit variable mineralogical and chemical compositions. In the case of WDXRF analysis, the ground powders of iron ore samples were mixed and pressed with low contamination binder in a mass ratio of wax: sample=4: 0.9g at 120kN cm~(-2). A standardless method for quantitative WDXRF was employed, which requires accurate determination of the amount of organic material in the sample. On the basis of differential thermal analysis, a new method is introduced for the determination of loss of ignition. With the application of the proposed method and standardless quantitative analysis, results for 12 elements in iron ores were obtained: Fe, Mn, Mg, Si, Al, Ca, Na, K, S, Ba, Zn, and Cl. The reliability and precision of the adopted procedure were tested against a standard reference material 'Iron ore concentrate (SRM 690, NIST, USA)'. The quantitative analysis results of the certified reference material were found acceptable. Depending on the WDXRF results, the powder samples were directly introduced to X-ray powder diffraction goniometry, and the phase compositions were quantitatively determined by using a standardless analysis program based on Rietveld method. The main phases of all iron ore samples are the hematite and goethite, whereas other phases are found with varying ratios, namely quartz, nordstrandite, rhodochrosite, kaolinite, todorokit, bassanit, andydrite, and hydroxyapatite.
机译:在基本参数方法的基础上,证实了无标准波长色散X射线荧光(WDXRF)和X射线粉末衍射算法用于分析从两个不同地点(阿斯旺和巴哈里亚)收集的埃及铁矿石样品的有效性。所研究的埃及铁矿石代表不同的沉积环境,因此呈现出不同的矿物学和化学组成。在WDXRF分析的情况下,将铁矿石样品的粉碎粉末与低污染粘结剂混合,并在120kN cm〜(-2)下按蜡:样品= 4:0.9g的质量比压制。采用了无标准的WDXRF定量方法,该方法需要准确测定样品中有机物的量。在差热分析的基础上,引入了一种新的测定燃烧损失的方法。通过所提方法的应用和无标定量分析,获得了铁矿石中12种元素的结果:铁,锰,镁,硅,铝,钙,钠,钾,硫,钡,锌和氯。针对标准参考材料“铁精矿(SRM 690,NIST,美国)”对所采用程序的可靠性和精度进行了测试。经认证的参考物质的定量分析结果被认为是可以接受的。根据WDXRF结果,将粉末样品直接引入X射线粉末衍射测角法,并使用基于Rietveld方法的无标准分析程序对相组成进行定量测定。所有铁矿石样品的主要相均为赤铁矿和针铁矿,而其他相则以不同的比例存在,即石英,钠锰矿,菱锰矿,高岭石,托多洛基特,重锰铁矿,红闪石和羟基磷灰石。

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