Quantitative analysis of pyrite in coal
β Scribed by Sidney S. Pollack
- Publisher
- Elsevier Science
- Year
- 1971
- Tongue
- English
- Weight
- 126 KB
- Volume
- 50
- Category
- Article
- ISSN
- 0016-2361
No coin nor oath required. For personal study only.
β¦ Synopsis
THE PURPOSE of this communication is to suggest a possible third method for the determination of pyrite in coal in addition to the British Standard methodr-s and the direct (or non-simultaneous) method 4-e. Burns7 found the former procedure to be unsatisfactory for the analysis of pyrite in Australian coals.
X-ray diffractionspg is a common technique for quantitative analysis of crystalline materials although it is usually used for measuring percentages greater than 5 to 10%. However, the low mass absorption coefficient of carbon permits the detection by x-ray diffraction of very small amounts of crystalline inorganic compounds admixed with carbon. Although I have no need for the determination of pyrite in coal, I prepared some mixtures to determine the approximate minimum detectable percentage of pyrite in activated carbon. Diffractometer traces of mixtures containing 1% and 0.4 % (less than 10 pm) pyrite in activated carbon are shown in Figure 1. If there were no impurities in coal with diffraction lines which superimposed on the strongest pyrite lines, possibly as little as 0.2% pyrite could be determined quantitatively.
π SIMILAR VOLUMES
## Letters to the Editor Table 1 Minerals studied and their reactions upon heating to 900Β°C Mineral Chemical formula Reactions Kaoiinite lllite Calcite Dolomite Quartz Gypsum Rutile Pyrite Siderite Al&~O~ofOf-fI~ Release of adsorbed water and dehydroxylation K~fAI,Fe)y(Mg,Fe)r.t$ixAlyOlo(OH)~ Rele
A thorough investigation into the British Standard method for the determination of pyritic sulphur has shown that it is not suitable for all Australian coals, and that instead, the direct or non-simultaneous method should be adopted. Determinations of the iron which is not extractable with nitric ac
X-ray Photoelectron Spectroscopy (XPS) was used to study mineral, synthetic and coalassociated pyrites, oxidized for various time intervals at low temperatures with humid air or oxygen. This was done to find out if XPS could detect, monitor and clarify pyrite surface-oxidative changes that influence