Introduction to Ceramics
Some notes taken from The Practical Potter: A Step-By-Step Handbook by Josie Washaw, and Marie at Potterycrafters.com
What exactly is clay? The chemistry explained:
Clay is a wonderful material for additive and subtractive sculpture. You can take a large piece and carve away at it, or you can join pieces, adding them together. Clay is great at mimicking other materials. You can paint it in many different ways. You can press it against different surfaces to make it look like wood, canvas, a piece of fruit, etc. There are countless ways to press, cut, and stamp the surface for a wide variety of textures. And you can use it in mold making to create artwork from other materials such as plaster and bronze. It is hard to overstate the importance of clay ceramics in human history. We've been using it to make pottery since at least 14,000 BC. Our first written texts were on clay tablets. Clay is used in industry and in bricks - millions of people rely on clay for the homes they live in.
There are many different types of clay, each with their own strengths and weaknesses. The three basic components of all clay are: The plastic (kaolinite), the flux (feldspar), and the filler (grog). You can altar the properties and color of your clay by adding and mixing these materials either in the dry stage as a powder, or in the plastic stage.
The Plastic:
The basic mineral in all clay is kaolinite (Al2O3·2SiO2·2H2O) (found in kaolin rocks), which is made up of approximately 40% alumina, 46% silica, and 14% water.
When kaolinite is mixed with water it becomes plastic, meaning malleable. You can manipulate it without it cracking. As it dries, it hardens, becoming delicate and brittle. When heated in a kiln, the kaolinite particles melt and fuse together, the water evaporates, some gases are released, and the resulting structure hardens and becomes much stronger.
The Flux:
Clay fluxes are mixed in to lower the melting point of the material, making it easier to melt and vitrify (to turn to a glass when heated). When cooled, flux helps strengthen the kaolin bonds that make the clay hard and resilient. The most common clay fluxes are potassium oxide and sodium oxide, both found in feldspars (some of the most common rocks in the Earth's crust). Calcium oxides are often used in ceramic glazes.
The Filler:
Grog (also called firesand and chamotte) is basically clay that's been fired at high temperature, and then ground up to a powder. It can be added to clay for two purposes. First, it reduces shrinkage (clay shrinks, as it dries). Secondly, shrinking too suddenly can result in "thermal shock" and cracking. Grog helps clay to dry evenly to reduce the chance of cracking, which is particularly important in raku firing, where the vessel changes temperature dramatically fast.
What are the different kinds of clay?
Two clay classifications are: primary and secondary (sedimentary)
Primary clays are very white, both before and after firing. They are still in the same place as their “mother rock”. They have large particles, and have little exposure to the atmosphere. These are extremely pure, fire at high temperatures, and are almost “non-plastic” so they are not good for hand modeling, but can be used with molds. Plasticity is what allows clay to hold its shape when soft. If a great deal of water is added, the clay loses its plasticity, turning into a sticky substance called “slip”. If the clay is too dry is also loses its plasticity and will be hard to work with . If your clay cracks as you bend it, add more water. Examples include porcelain (china clay).
Secondary clays have been transported away from their mother rock by wind and water erosion, and deposited according to the size of their particles, with the heaviest settling to the bottom. The finest particles settle in places where the water is stagnant. These clays are finer and more plastic, but contain impurities. These impurities change the clay’s color and lower the firing temperature. The more plastic a clay is, the more it absorbs water, increasing in volume. Clays with smaller particles will shrink more than clays with large particles. Examples include ball clays and earthenware clays.
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