Color in glazes containing Chrome Oxide

cone 10 oxidation

The Downfire profile

A half hour hold at 1750 deg F

A three hour hold at 1700 deg F

slow downfire at 25 deg F an hour in the interval 1700 deg F to 1650 deg F

A one hour hold at 1650 deg F

Clay body is a grolleg porcelain from Tacoma Clay Art Center.

We last saw the two glazes paperWhite_ZO_1 and paperWhite_ZO_3 in:

Chrome Colors

We noted that this pair of glazes had a prominent bright green phase.
I was curious to see the effect on the color of making these glazes matt without changing the composition of the bases,
so I added sufficient Alumina Hydroxide to produce an alumina matt. The fluxes (first column components of the empirical formula) are unchanged,
and there is a substantial shift in the colors.

paperWhite_ZO_3 with added alumina hydroxide in addition to the chrome oxide, is pinholed and likely underfired.

In a further exploration of the effect of the composition of the bases (fluxes) on the color of a glaze containing .25 %
chrome oxide I tested two glazes which differ only in the relative proportion of BaO and SrO.

In their respective empirical Formula's these two glaze have in common:

Alkali metals .44
Al2O3 .5
SiO2 3

The alkali metals are evenly split between K2O and Na2O
The alkaline earths are dominated by BaO and SrO:

paperWhite_ZP_0 has low BaO and high SrO with BaO .25, SrO .28.

paperWhite_ZP_1 has high BaO and low SrO with BaO .35, SrO .18.

The non test tiles are small bowls ~3 inches in diameter.



full view

paperWhite_ZO_1 with 0.2 % Chrome oxide

full view

paperWhite_ZO_1 with 0.2 % Chrome oxide and added alumina



full view

paperWhite_ZO_3 with 0.2 % Chrome oxide

full view

paperWhite_ZO_3 with 0.2 % Chrome oxide and added alumina



full view

paperWhite_ZP_0 with 0.2 % Chrome oxide



full view

paperWhite_ZP_1 with 0.2 % Chrome oxide



Commentary

Note that the addition of alumina to paperWhite_ZO_1 and to paperWhite_ZO_3 causes a striking color shift.

Equally, paperWhite_ZP_0 and paperWhite_ZP_1 show the effect of a change in balance between BaO and SrO, from turquoise to bright apple green.

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