X-ray variance method to determine the domain size and lattice distortion of ground kaolinite samples
The variance method [WILSON, 1963] was applied to determine the changes in domain size and lattice distortion along the 001 direction in dry grinding experiments of Sedlec (Zettlitz) kaolinite samples. Very short grinding (3 min) already resulted in considerable lattice distortion, while change in d...
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Testületi szerző: | |
Dokumentumtípus: | Cikk |
Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1980
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Sorozat: | Acta mineralogica-petrographica
24 |
Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
Tárgyszavak: | |
Online Access: | http://acta.bibl.u-szeged.hu/24679 |
Tartalmi kivonat: | The variance method [WILSON, 1963] was applied to determine the changes in domain size and lattice distortion along the 001 direction in dry grinding experiments of Sedlec (Zettlitz) kaolinite samples. Very short grinding (3 min) already resulted in considerable lattice distortion, while change in domain size is of minor extent. A grinding of 30—40 min converted the medium crystallized Sedlec (Zettlitz) kaolinite into a substance which had an X-ray diffraction pattern similar to that of poorly crystallized kaolinited. |
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Terjedelem/Fizikai jellemzők: | 115-119 |
ISSN: | 0365-8066 |