SLIDE 8 XRD Diffractogram Analysis
Position [°2Theta] 10 20 30 40 500 1000 Illite Illite ; Illite Fluorapatite; Anhydrite Hematite; Il Fluorapatite; Anhyd Fluorapatite; Anhydrite Fluor Fluorapatite; He Fluorapatite; Illite Illite Fluorapatite; He CC 1100°C 100ms Air
1100°C 100ms Air
Position [°2Theta] 10 20 30 40 500 1000 Mullite, syn Quartz $GA Fluorapatite, syn Hematite Mullite, syn Quartz $GA Mullite, syn Fluorapatite, syn Mullite, syn; Fluorapatite, syn; Hematite Fluorapatite, syn Mullite, syn Fluorapatite, syn; Hematite Mullite, syn Mullite, syn; Quartz $GA; Fluorapatite, syn; Hematite CC 1100°C 350ms Air
1100°C 350ms Air With increasing residence time, the following occurs:
- The structure of the clays are
destroyed.
- Mullite forms.
- There are other changes also.
We can semi-quantify the percentage
- f a mineral phase by measuring the
area of its main peak. But we need to identify all of the minerals present. h w Area = h x width at half maximum height (FWHM) Therefore given sufficient temperature and time this hard mineral forms.