Snow Flake Yet Again

Glazes are fired at cone 6 in an electric kiln.

The kiln is cooled slowly, at a rate of 50 deg F an hour in the temperature interval 1850 to 1700.

It is then cooled 25 deg F an hour in the temperature interval 1700 deg F to 1650 deg F.

There is then a 1 hour hold at 1650 deg F.

We last saw snow flake glazes:

Snow Flake Continues

We saw an additional test of the first glaze in this series, hiAl_4X_2,

with summary seger formula:
total alkali metals .77
alkaline earths equally divided between CaO and MgO
Alumina .66
Silica 3.3
Titania .23

and tests of two variations.

hiAl_4V_4Y with the same bases (fluxes) and lower alumina and silica
hiAl_4X_2Y_1 with some CaO replaced by MgO

Additional tests of these two variations were not encouraging. Both the snow flakes and the rutile blue ground phase are present,
but only with tight control on glaze application thickness. A thick application is required for the presence of two distinct phases,
yet just a bit thicker application and either the glaze will crawl, or show unhealed blisters.

glaze hiAl_4X_2PSi

full view

glaze hiAl_4_2PSi on plate 5 inches in diameter

hiAl_4X_2PSi "is" the glaze hiAl_4X_2 with a small amount of additional silica.
I added 4 % silica to the glaze, which gave a 6 % increase in silica in the empirical formula.
The appearance of the glaze is virtually unchanged,
though if one examines the surface closely with 30x magnification
the craze pattern is coarser, i.e. the craze lines are spaced further apart,
giving hope that the additional silica strengthened the glaze.



glaze hiAl_4Z_0 and hiAl_4Z_1

Both of these glazes have nearly the same summary empirical formula as hiAl_4X_2:

total alkali metals .77
Alumina .66
Silica 3.3
Titania .23

hiAl_4X_2 has Li2O = .2, these glazes have Li2O = .14. the intent is that less Li2O would result in a glaze that had a broader firing range.

These two glazes differ only in the distribution of the CaO and MgO,
the first has equal CaO and MgO,
the balance shifts, the second has predominantly MgO.

Although neither glaze has sufficient "flocking" to be interesting as a "snow flake" glaze,
I found the difference produced by the shift between CaO and MgO intriguing.

full view

glaze hiAl_4Z_0 plate 5 inches in diameter

equal CaO and MgO



full view

glaze hiAl_4Z_1 plate 5 inches in diameter

MgO dominates alkaline earths

With a shift to a glaze with alkaline earths dominated by MgO, I observe a shift in color from pale blue to grey.
Additionally, the second glaze has a smoother surface and is translucent.



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