𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Determination of low levels of quartz in calcium carbonates by x-ray diffractometry

✍ Scribed by N.J. Elton; P.D. Salt


Publisher
Elsevier Science
Year
1994
Tongue
English
Weight
898 KB
Volume
286
Category
Article
ISSN
0003-2670

No coin nor oath required. For personal study only.

✦ Synopsis


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) at the 0.1 wt.% level. The quarts in the samples is pre-concentrated by partial acid dissolution of the calcium carbonate, and careful attention is given to reproducible sample preparation of the resultant partial residues. Calibration is by an external standard with mass absorption corrections being applied to compensate for variations in sample chemistry. The presence of additional accessory minerals such as mica and feldspar can lead to problems due to overlapping diffraction peaks. These problems are discussed and the use and limitations of the short range profile fitting techniques employed in this method are described. The significance of particle statistics, counting statistics, and the variability associated with sample preparation in limiting the accuracy of quantification at low levels is also examined.


πŸ“œ SIMILAR VOLUMES


Determination of quartz in kaolins by x-
✍ N.J. Elton; P.D. Salt; J.M. Adams πŸ“‚ Article πŸ“… 1994 πŸ› Elsevier Science 🌐 English βš– 1018 KB

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

Qauntitative determination of quartz in
✍ Gary P. Tomaino πŸ“‚ Article πŸ“… 1994 πŸ› Elsevier Science 🌐 English βš– 444 KB

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