Conversion from fluor- to hydroxyl-phlogopite in KOH solution

Synthetic fluor-phlogopite, KMg3Si3AlO10F2, was treated by KOH hydrothermal solution under the following conditions: a temperature range from 300 to 800°C, KOH concentration from 1 to 10M, and duration from 3 hours to 216 days under a constant external pressure of 100 MPa. Solid products were examin...

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Veröffentlicht in:Mineralogical Journal 1991, Vol.15(5), pp.190-202
Hauptverfasser: FUJITA, Taketoshi, SUGIMORI, Ken-ichiro, KOSUGI, Tetsushi, NAKAZAWA, Hiromoto
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container_end_page 202
container_issue 5
container_start_page 190
container_title Mineralogical Journal
container_volume 15
creator FUJITA, Taketoshi
SUGIMORI, Ken-ichiro
KOSUGI, Tetsushi
NAKAZAWA, Hiromoto
description Synthetic fluor-phlogopite, KMg3Si3AlO10F2, was treated by KOH hydrothermal solution under the following conditions: a temperature range from 300 to 800°C, KOH concentration from 1 to 10M, and duration from 3 hours to 216 days under a constant external pressure of 100 MPa. Solid products were examined by X-ray diffraction (XRD), scanning electron microscope (SEM) and electron microprobe analyzer (EPMA). The aqueous phase was chemically analyzed. In the entire range examined, (OH)-rich phlogopite was always produced in addition to the original F-phlogopite. The composition of the newly formed phlogopite varied with temperature and KOH concentration. The compositional gap between the two phlogopites was explained as an apparent immiscibility gap that appears in the temperature-composition section of the three parameter system of temperature, composition, and KOH concentration. The present study suggests practical conditions for the complete conversion from F- to OH-phlogopite as follows: [KOH]/[F-phlogopite]>8 and a temperature range of 500–600°C. SEM observations of the experimental products indicated that the F/OH exchange mechanism was not an ion exchange between solid and solution, but rather a dissolution and precipitation reaction in a KOH hydrothermal solution.
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Solid products were examined by X-ray diffraction (XRD), scanning electron microscope (SEM) and electron microprobe analyzer (EPMA). The aqueous phase was chemically analyzed. In the entire range examined, (OH)-rich phlogopite was always produced in addition to the original F-phlogopite. The composition of the newly formed phlogopite varied with temperature and KOH concentration. The compositional gap between the two phlogopites was explained as an apparent immiscibility gap that appears in the temperature-composition section of the three parameter system of temperature, composition, and KOH concentration. The present study suggests practical conditions for the complete conversion from F- to OH-phlogopite as follows: [KOH]/[F-phlogopite]&gt;8 and a temperature range of 500–600°C. 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Earth, ocean, space
Exact sciences and technology
Mineralogy
Silicates
title Conversion from fluor- to hydroxyl-phlogopite in KOH solution
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