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Figure 9
Crystallization of amorphous Cs-geopolymer to pollucite, observed in situ at 1398 ± 5 K. Evolution of crystalline phase content was observed with a time resolution of ∼2 min. Only a subset of the HTXRD patterns acquired is shown.

Journal logoJOURNAL OF
SYNCHROTRON
RADIATION
ISSN: 1600-5775
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