Comparison of Quantitative X-ray Diffraction Mineral Analysis Methods

矿物 定量分析(化学) 结构精修 准确度和精密度 软件 计算机科学 衍射 矿物学 X射线晶体学 粉末衍射 生物系统 材料科学 地质学 化学 数学 统计 结晶学 物理 光学 色谱法 冶金 程序设计语言 生物
作者
Jingyun Xiao,Yougui Song,Yue Li
出处
期刊:Minerals [Multidisciplinary Digital Publishing Institute]
卷期号:13 (4): 566-566 被引量:12
标识
DOI:10.3390/min13040566
摘要

X-ray diffraction (XRD) analysis, as one of the most powerful methods, has been widely used to identify and quantify minerals in earth science. How to improve the precision of mineral quantitative analysis is still a hot topic. To date, several quantitative methods have been proposed for different purposes and accompanied by diverse software. In this study, three quantitative mineral analysis methods, including the reference intensity ratio (RIR), Rietveld, and full pattern summation (FPS) methods, are compared and evaluated to systematically investigate their accuracy and applicability. The results show that the analytical accuracy of these methods is basically consistent for mixtures free from clay minerals. However, there are significant differences in accuracy for clay-mineral-containing samples. In comparison, it seems that the FPS method has wide applicability, which is more appropriate for sediments. The Rietveld method has been shown to be capable of quantifying complicated non-clay samples with a high analytical accuracy; nevertheless, most conventional Rietveld software fails to accurately quantify phases with a disordered or unknown structure. The RIR method represents a handy approach but with lower analytical accuracy. Overall, the present results are expected to provide a potentially important reference for the quantitative analysis of minerals in sediments.
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