X-Ray Peak Profile Analysis of Materials M1 and M2 by Williamson-Hall and Size-Strain Plot Methods

IF 0.6 Q4 MATERIALS SCIENCE, MULTIDISCIPLINARY
Lalmi Khier, Lakel Abdelghani, D. Maouche
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Abstract

Received: 21 September 2020 Accepted: 10 March 2021 In this work, we have studied the Kaolin M1 and M2 by the X-ray diffraction method, and we have focused on mullite phase which is the main phase present in common in both products. An update of the program of the method of Stokes was carried out, it was necessary to the microstructural analysis. The completed version is less sensitive to the choice by excess of the number of coefficients of Fourier with regard to the effect of truncation and the office plurality of the errors. The determination of the symmetry of the cell of the principal phase (mullite) in the studied fritted Kaolins was carried out. In Kaolin M1, the size of crystallites of the dominant phase varies between 80 to 170 Å. In Kaolin M2, the size of the crystalline grains of mullite varies between 100 to 400 Å. The size of crystallites was confirmed by the joint method of Williamson-Hall. A distribution of sizes of crystallites was carried out. It shows a dominance of the size of approximately 140 Å for the principal phase of Kaolin M1 and a dominance of the size of approximately 230 Å for the same principal phase of Kaolin M2. By the study of the profiles of line by DRX, it appears very clearly that the principal phase of the various sintered Kaolins, mullite, is free from internal microstrains. It is the case of the mixtures fritted not only at low temperature (1100°C) during 1 hour but also the case of the mixtures of the type ‘chamotte’ cooks with 1350°C during very long times.
用Williamson-Hall和尺寸-应变图方法分析材料M1和M2的x射线峰形
在这项工作中,我们用x射线衍射方法研究了高岭土M1和M2,我们重点研究了莫来石相,这是两种产品共同存在的主要相。对斯托克斯法的程序进行了更新,以满足微观结构分析的需要。对于截断的影响和误差的复数度,完成后的版本对傅里叶系数数目的选择不太敏感。对所研究的烧结高岭土中主相(莫来石)的细胞对称性进行了测定。在高岭土M1中,优势相的晶粒大小在80 ~ 170 Å之间。在高岭土M2中,莫来石晶粒的大小在100到400之间Å。用Williamson-Hall联合法确定了晶体的大小。对晶体的大小进行了分析。结果表明,高岭土M1主相的优势尺寸约为140 Å,高岭土M2主相的优势尺寸约为230 Å。通过DRX线谱的研究,可以清楚地看到,各种烧结高岭土的主相莫来石不存在内部微应变。这种混合物不仅在低温下(1100°C)在1小时内凝固,而且在1350°C下长时间烹饪的“chamotte”类型混合物的情况也是如此。
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来源期刊
Annales De Chimie-science Des Materiaux
Annales De Chimie-science Des Materiaux 工程技术-材料科学:综合
CiteScore
1.70
自引率
25.00%
发文量
33
审稿时长
>12 weeks
期刊介绍: The ACSM is concerning the cutting-edge innovations in solid material science. The journal covers a broad spectrum of scientific fields, ranging all the way from metallurgy, semiconductors, solid mineral compounds, organic macromolecular compounds to composite materials. The editorial board encourages the submission of original papers that deal with all aspects of material science, including but not limited to synthesis and processing, property characterization, reactivity and reaction kinetics, evolution in service, and recycling. The papers should provide new insights into solid materials and make a significant original contribution to knowledge.
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