journal article·2002-11

Determination of structural disorder degree using an XRD profile fitting procedure. Application to Czech kaolins

M Chmielová, Z Weiss

Applied Clay Science· Volume 22· Issue 1-2
Publisher page

Abstract

Diffractions of (02, 11) band are very sensitive to the structural defects in kaolinite structure. Therefore, the empirical relation based on weighting peak intensity ratio of 0 2 0, 1 1̄ 0, and 1 1 1̄ (1 1̄ 1̄) reflections was used to estimate the degree of disorder in kaolinite samples collected from different Czech Republic kaolin deposits. X-ray diffraction (XRD) profiles taken from <5 μm fraction of kaolinite samples were used for determination of peak intensities I(1 1̄ 0), I(1 1 1̄), I(1 1̄ 1̄), I (0 2 0) and full width at half maximum (FWHM) values using profile fitting and decomposition procedure. The weighting intensity ratio index (WIRI) WIRI =1− exp {−[w 1 I(1 1 ̄ 0)+w 2 I(1 1 1 ̄ )+w 3 I(1 1 ̄ 1 ̄ )]/[w 4 I(0 2 0)]} was calculated. The w 1, w 2, w 3, and w 4 weight values are the reciprocal values of FWHM for 1 1̄ 0, 1 1 1̄, 1 1̄ 1̄, and 0 2 0 reflections, respectively. According the WIRI values (theoretically ranging from 0 to 1), three groups of kaolinite samples can be recognized: (I) one sample with high degree of structural order (0.70<WIRI<1.00), (II) two samples with medium degree of structural order (0.40<WIRI≤0.70), and (III) five samples with low degree of structural order (0.00<WIRI≤0.40). The WIRI values obtained were compared with Hinckley (HI) and Aparicio–Galán–Ferrell (AGFI) indices and very good relations were found between them.
Source: expertdata · Quality: candidate unverified · Source record ↗

Research context

OpenAlex topics: Clay minerals and soil interactions · Soil and Unsaturated Flow · Geochemistry and Geologic Mapping

SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.

References (14)

Show source-provided references
1. Mineralogical interference on kaolinite crystallinity index measurements10.1346/CCMN.1999.0470102 ↗
2. A new kaolinity crystallinity index from mathematical modelling of XRD data
3. Stacking faults in kaolin-group minerals in the light of real structural features10.1346/CCMN.1989.0370402 ↗
4. Correlation between the most frequently used XRD crystallinity indices for kaolinite: their accuracy and reproducibility
5. Variability in “crystallinity” values among the kaolin deposits of the coastal plain of Georgia and South Carolina
6. A method of quantitative mineralogical analysis of rocks from their elementary chemical analysis
7. Kužel · 1991
8. Determination of structural defects in phyllosilicates by X-ray powder diffraction: I. Principle of calculation of the diffraction phenomenon10.1346/CCMN.1977.0250609 ↗
9. Determination of structural defects in phyllosilicates by X-ray powder diffraction: II. Nature and proportion of defects in natural kaolinites10.1346/CCMN.1977.0250610 ↗
10. An expert system for the structural characterization of kaolinite10.1180/claymin.1990.025.3.01 ↗
11. The Hinckley index for kaolinites10.1180/claymin.1988.023.3.02 ↗
12. Stacking faults in the kaolin-group minerals: defect structures of kaolinite10.1346/CCMN.1989.0370302 ↗
13. Über das Verhalten von kaolinitit bei hohen Drücken
14. Stoch · 1974 · 186