Alternate Names: Television Stone
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Ulexite is a natural source of boron, it is similar to colemanite mineral. These two minerals are the only practical sources of insoluble boron for glazes (other than frits). Ulexite one of the lowest melting non-lead ceramic minerals, it can form an ultra-gloss transparent glass at cone 06. Strangely this material does not appear to flux bodies nearly as well as one might expect.
Ulexite is a truly uncommon ceramic mineral in that it contains almost no alumina or silica, it is nothing but fluxing oxides. This mineral forms in unusual geologic circumstances and can be found in very few places in the world. The chemistry given here is theoretical, actual deposits will have lower boron content.
The popular mineral Gerstley Borate, used by potters for many decades is, is composed partly of ulexite. It was mined and stockpiled in the California desert many years ago. The last remaining stockpile is being ground, bagged and sold by Laguna Clay. Ulexite is available in small quantities for potters at Plainsman Clays.
While Ulexite melts well, it does have a very high LOI (that means that gases are generated during melting). For this reason it is not possible to produce ultra-clear glazes at low temperatures (as with frits). Notwithstanding this, by doing a double-soak firing it is possible to clear many more bubbles. Thinner glazes layer are also much more transparent.
Ulexite is available industrially from Turkey and Chile. It is used in the fiberglass industry as a melter but its potential has never been exploited to any extent in ceramic glazes.
These cone 04 glazes have the same recipe (a version of Worthington Clear sourcing B2O3 from Ulexite instead of Gerstley borate). While the one on the left is OK, the one on the right is great! Why? It has 10% added lead bisilicate frit. Of course, I would not recommend this, I am just demonstrating how well it melts. Still, we gasp at the thought of using lead while we thrive on unstable flux-deprived, glass-deprived and alumina-deprived base stoneware glazes with additions of toxic colorants like chrome and manganese!
90% Alberta Slip (which is a mix of half and half raw and calcine) and 10% Ulexite fired at cone 6. A dazzling fluid dark amber transparent. You could also do this using a high-boron frit.
Two clear glazes fired in the same slow-cool kiln on the same body with the same thickness. Why is one suffering boron blue (1916Q) and the other is not? Chemistry and material sourcing. Boron blue crystals will grow when there is plenty of boron (and other power fluxes), alumina is low, adequate silica is available and cooling is slow enough to give them time to grow. In the glaze on the left B2O3 is higher, crystal-fighting Al2O3 and MgO levels are alot lower, KNaO fluxing is alot higher, it has more SiO2 and the cooling is slow. In addition, it is sourcing B2O3 from a frit making the boron even more available for crystal formation (the glaze on the right is G2931F, it sources its boron from Ulexite).
These two glazes have the same chemistry but different recipes. The F gets its boron from Ulexite, and Ulexite has a high LOI (it generates gases during firing, notice that these gases have affected the downward flow during melting). The frit-based version on the right flows cleanly and contains almost no bubbles. At high and medium temperatures potters seldom have bubble issues with glazes. This is not because they do not occur, it is because the appearance of typical glaze types are not affected by bubbles (and infact are often enhanced by them). But at low temperatures potters usually want to achieve good clarity in transparents and brilliance in a colors, so they find themselves in the same territory as the ceramic industry. An important way to do this is by using more frits (and the right firing schedules).
Left: Worthington Clear cone 04 glaze (A) uses Gerstley Borate to supply the B2O3 and CaO. Right: A substitute using Ulexite and 12% calcium carbonate (B). The degree of melting is the same but the gassing of the calcium carbonate has disrupted the flow of B. Gerstley Borate gasses also, but does so at a stage in the firing that does not disrupt this recipe. However, as a glaze, B does not gel and produces a clearer glass. A further adjustment to source CaO from non-gassing wollastonite would likely improve it.
The ulexite in Gerstley Borate melts first, producing an opaque fired glass having the unmelted (and still gassing) particles of colemanite suspended in it. By 1750F the colemanite is almost melted also. Boron-containing frits, by contrast, begin softening at a much lower temperature and gradually spread and melt gradually. Not surprisingly they produce a more stable glaze (albeit often less interesting visually).
Low fire glazes must be able to pass the bubbles their bodies generate (or clouds of micro-bubbles will turn them white). This cone 04 flow tester makes it clear that although 3825B has a higher melt fluidity (it has flowed off onto the tile, A has not). And it has a much higher surface tension. How do I know that? The flow meets the runway at a perpendicular angle (even less), it is long and narrow and it is white (full of entrained micro-bubbles). Notice that A meanders down the runway, a broad, flat and relatively clear river. Low fire glazes must pass many more bubbles than their high temperature counterparts, the low surface tension of A aids that. A is Amaco LG-10. B is Crysanthos SG213 (Spectrum 700 behaves similar to SG13, although flowing less). However they all dry very slowly. Watch for a post on G2931J, a Ulexite/Frit-based recipe that works like A but dries on dipped ware in seconds (rather than minutes).
These are various different terra cotta clays fired to cone 04 (also a low fire white-buff fritted stoneware) with a recipe I formulated to source the same chemistry as the popular Worthington clear, but sourcing the B2O3 from Ulexite and a frit instead of Gerstley Borate (G2931B). All pieces are fired with a soak-soak-slow cool firing. Fit is good on all except a fritted terra cotta stoneware where it is shivering slightly (all were boil:ice tested). This outlines work I am doing to create an alternative recipe for the popular 50:30:20 GB:EPK:Silica recipe (Worthington clear) that uses Ulexite instead of Gerstley Borate (the later is notorious for turning glaze slurries into jelly!).
Out Bound Links
Details how to substitute Gerstley Borate for another boron source in the popular Floating Blue glaze recipe. The lesson demonstrates that the most practical way to deal with the GB issue is on a glaz...
This term is very generic, referring of course to frits that contain boron. Unfortunately that is 80-90% of available frits! Boron frits may have 1% boron or 50% boron. Even though the boron in the frit is no longer in the borax form it is still customary to refer to such as "borax frits". Since man...
In Bound Links
Colemanite, Calcium Borate, Borocalcite
The term 'boron' refers to the oxide B2O3. 'Borate materials' thus contain B2O3, they source it to glass-building during melting in the kiln. Boron is actually the potter's friend (because of his electronic-controller-equipped kiln) while as the same time it can be a scourge in industry (because the...
Here is how to completely fix Gerstley-Borate glaze recipes This outlines work I did to create an alternative transparent base glaze recipe in the popular 50:30:20 GB:Kaolin:Silica system (e.g. Wor...
The major borate minerals are Colemanite and Ulexite. The geology required for borates is found in very few places in the world (mainly southern California, Chile, Turkey, Argentina, Spain, Russia). B...