Quick Search:       Advanced Search
CHEN Ai-qing,XUE Yong,XU Hong-liu,LI Guo-wu.Assessment of Accuracy and Error Sources of the Rietveld Quantitative Phase Analysis Method in Mineral Contents of Evaporites[J].Rock and Mineral Analysis,2017,36(4):374-381
View Full Text   View/Add Comment   EndNote   BibTeX   Download reader
Assessment of Accuracy and Error Sources of the Rietveld Quantitative Phase Analysis Method in Mineral Contents of Evaporites
Received:August 02, 2016  Revised:July 20, 2017
DOI:10.15898/j.cnki.11-2131/td.201608020111
Key words: evaporite  Rietveld quantitative phase analysis  Rietveld refinement  sylvite
Author NameAffiliationE-mail
CHEN Ai-qing Key Laboratory of Mineralogy and Metallogeny, Chinese Academy of Sciences
Guangdong Provincial Key Laboratory of Mineral Physics and Materials Development
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
University of Chinese Academy of Sciences, Beijing 100049, China 
 
XUE Yong Beijing North Yanyuan Micro-structure Analysis and Testing Center, Beijing 100084, China xyly-299@163.com 
XU Hong-liu Testing Center of Hunan Nonferrous Geological Prospecting Institute, Changsha 410000, China  
LI Guo-wu School of Scientific Research, China University of Geosciences(Beijing), Beijing 100083, China  
Hits: 213
Download times: 349
Abstract:
      The Rietveld phase quantitative analysis (RQPA) method has been widely applied in geology. In the analysis of evaporite, the evaluation and error control of precision are important factors to improve the quality. The RQPA method was applied to simulated binary mixtures (halite and sylvite), ternary mixtures (halite, sylvite, and calcite), and geological samples (i.e., gypsum and sylvite samples). The contents of each mineral calculated by RQPA were compared with the results of chemical analytical data to evaluate the RQPA's accuracy and the main error sources were analyzed. The results show that the absolute errors between theoretical and calculated values are in the range of 0.4%-0.9% and 0.1%-1.2% for the binary and ternary mixtures, respectively. The mineral contents of geological samples matched very well with the results of the chemical analysis. The standard deviation of binary mixtures is 0.702 for 10 calculated results. The relative standard deviation of the same samples are 1.74%(KCl) and 1.17%(NaCl), respectively. The study indicates that the RQPA method is accurate in the quantitative analysis of mineral contents of evaporite rocks. The error sources arose mainly from the nature of the samples, sample preparation, measuring conditions, and refinement process. Due to the advantages of reducing the preferred orientation, not requiring pure samples, and high utilization of data, the RQPA method has a potentially extensive application in mineral exploration analysis, reserve evaluation, and industries of evaporites, when coupled with the chemical analysis method.