Kalsilite (K
2O⋅Al
2O
3⋅2SiO
2) which was not known to crystallize out of the three-component melt of K
2O, Al
2O
3, and SiO
2, was found to crystallize from the system K
2O-Al
2O
3-SiO
2-B
2O
3-RO, wherein B
2O
3 and RO acted as the minerallizer for kalsilite. The crystallizing regions of kalsilite and of orthorhombic kaliophilite and the glassifying region in the system were investigated.
The results obtained were as follows:
a) Mixtures in the region richer in SiO
2 than K
2O⋅2SiO
2 and not so aluminoferous were usually glassified.
b) Orthorhombic kaliophilite was crystallized from the melt which is poorer in B
2O
3 than K
2O⋅Al
2O
3⋅2SiO
2⋅0.3B
2O
3, whether associated with RO or not.
c) In the system of K
2O⋅Al
2O
3⋅2SiO
2-B
2O
3 the mixtures in the region richer in B
2O
3 than K
2O⋅Al
2O
3⋅2SiO
2⋅0.4B
2O
3 were easily glassified, while addition of RO caused the glassified region to change into the crystallizing region of kalsilite.
d) The larger was the radius of R
2+ ion, the more effectively it acted as minerallizer.
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