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Large scale melt synthesis in an open crucible of Na-fluorohectorite with superb charge homogeneity and particle size
Sodium fluorohectorite Na 0.6[Mg 2.4Li 0.6]Si 4O 10F 2 was synthesized from the melt in an open glassy carbon crucible at 1265 °C under argon flow. A glass (Na 2O–Li 2O–SiO 2) precursor was used as a fluxing agent in order to maintain a low vapor pressure of volatile fluorides and sustain a low sili...
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Published in: | Applied clay science 2010-03, Vol.48 (1), p.39-45 |
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Main Authors: | , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Sodium fluorohectorite Na
0.6[Mg
2.4Li
0.6]Si
4O
10F
2 was synthesized from the melt in an open glassy carbon crucible at 1265
°C under argon flow. A glass (Na
2O–Li
2O–SiO
2) precursor was used as a fluxing agent in order to maintain a low vapor pressure of volatile fluorides and sustain a low silica activity, which inhibits the formation of silicon fluoride gases and promotes the fluorine solubility in the melt. To minimize the loss of volatile fluorine compounds the pre-synthesized alkali silicate glass was heated together with additional raw materials needed in a high frequency induction furnace rapidly from 800
°C up to 1265
°C and then kept at this temperature for a short period of time (15
min). The synthesis method can easily be scaled to batches larger than 1
kg. The Na
0.6-fluorohectorite obtained stands out by (i) phase purity as checked by X-ray powder diffraction (PXRD), (ii) a superb homogeneity of the charge density as demonstrated by stepwise hydration behavior followed by in-situ PXRD in a humidity chamber and the Lagaly method with alkylammonium exchange (
Mermut and Lagaly, 2001), (iii) a high cation exchange capacity (CEC) of 136
meq/100
g as determined by the copper complex ([Cu(trien)]
2+) method, and (iv) extreme lateral extensions with a median value of the particle size of 45
μm as measured by static laser light scattering (SLS) which was confirmed by scanning electron microscopy (SEM). |
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ISSN: | 0169-1317 1872-9053 |
DOI: | 10.1016/j.clay.2009.11.014 |