BEHAVIOUR OF URANIUM DURING PHOSPHATE ORE CALCINATION.

Mordechai Stein*, Avraham Starinsky, Yehoshua Kolodny

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

4 Scopus citations

Abstract

During industrial calcination of phosphate rock, uranium is mobilized with changes both in location and oxidation state. Fission track micromapping of uranium under the microscope has been employed to study the precise distribution of uranium within the samples. Oxidation state ratios of U(IV) to U(VI) were determined by chemical separation followed by delayed neutron activation. The calcination process was studied both in the laboratory and in a full-scale production kiln. It is shown that during calcination first carbonate-fluorapatite loses CO//2, and recrystallizes to fluorapatite. The recrystallization process intensifies with increasing temperature. Around 600 degree C all the uranium is oxidized to the hexavalent state. Migration of uranium in the apatite fragments initiates at 800 degree C. On increase of temperature to around 900 degree C, it forms uranium-rich phases in which it reaches 1-2%.

Original languageEnglish
Pages (from-to)834-847
Number of pages14
JournalJournal of chemical technology and biotechnology
Volume32
Issue number9
DOIs
StatePublished - 1982

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