Naturally occurring calcium carbonates often have a complex accessory mineralogy. Quartz is a common associate, typically present at concentrations < 1 wt.%. A method is described whereby x-ray powder diffractometry may be used to quantify quartz in such samples to better than f 0.01 wt.% (la error)
Determination of quartz in kaolins by x-ray powder diffractometry
โ Scribed by N.J. Elton; P.D. Salt; J.M. Adams
- Publisher
- Elsevier Science
- Year
- 1994
- Tongue
- English
- Weight
- 1018 KB
- Volume
- 286
- Category
- Article
- ISSN
- 0003-2670
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โฆ Synopsis
Depending upon their origin, naturally occurring kaolins contain various accessory minerals including micas, feldspars and quartz. These minerals may be partially removed, but rarely eliminated, by refining. When determining quartz by x-ray diffractometry, serious problems are encountered even with refined kaolins due to overlapping peaks from micas, feldspars and kaolinite itself. This paper discusses the peak overlap and other problems and describes how optimisation of sample preparation and diffractometer parameters, together with the use of profile fitting techniques permits the determination of crystalline quartz in bulk samples to f 0.015 wt.% (lo absolute) at the 0.1 wt.% level. A detailed examination of the errors involved in the analysis shows that counting and particle statistics are the most important error sources. For the samples examined in this study, counting statistics is the major contributor to the observed 15% relative error. Preliminary results on the use of a laboratory air classifier to generate "large" respirable dust samples from bulk powders for quartz analysis are given.
๐ SIMILAR VOLUMES
A detection limit of 0.05% quartz in calcitic and dolomitic carbonate and talc matrices is dependent upon significant counting time for optimal signal to noise ratio, utilization of peak area counts, absence of significant interfering phase(s), a known blank ( < 0.05%) for each matrix, statistically