Use of hydrofluoric acid dissolution for the concentration of dickite and nacrite from kaolin deposits: An FTIR study

Clay Minerals

Volumn 37, Issue 3, 2002, Pages 559-570

  Fraser, A R ^a   Wilson, M J ^a   Roe, M J ^a   Shen, Z Y ^a  

^a SCOTTISH CROP RESEARCH INSTITUTE   (United Kingdom)

Author keywords

Dickite; Hydrofluoric acid; Infrared spectroscopy; Kaolinite; Nacrite

Indexed keywords

INFRARED SPECTROSCOPY; INORGANIC ACIDS; KAOLIN; SCANNING ELECTRON MICROSCOPY;

PARTICLE SIZE;

CLAY;

DICKITE; DISSOLUTION; HYDROFLUORIC ACID; KAOLINITE; NACRITE;

EID: 0036757667     PISSN: 00098558     EISSN: None     Source Type: Journal    
DOI: 10.1180/0009855023730058     Document Type: Article

References (14)

1. Depth-dependent transformation of kaolinite to dickite in sandstones of the Norwegian continental shelf
2. The infrared spectra of layer silicates
3. Kaoline from Warsaw geodes, Keokuk region, Iowa
4. Scan electron micrographs of kaolins collected from diverse environments of origin -1
5. Elevated dehydroxylation temperature of the Keokuk geode kaolinite - a possible reference mineral
6. Some phosphate minerals of soils
7. Mineralogy of kaolin clays from Pugu, Tanganyika
8. Attribution of the OH stretching bands of kaolinite
9. Infrared methods
10. Nacrite from the Southern Upland fault near Abington, Strathclyde, Scotland
11. Nacritic clay associated with the Jiangshan-Shaoxing deep fault in Zhejiang Province, China
12. Dickite from sandstones in Northern England and North Wales
13. Intercalation of water in kaolin minerals