noun the process of heating a substance to a high temperature in order to bring about chemical changes, such as the removal of volatile components
In geology, calcination can refer to the natural process of heating rocks in the Earth's crust to release gases or change mineral structures.
In chemistry, calcination is the process of heating a substance to a high temperature but below its melting or fusing point to bring about thermal decomposition or phase transition, often used in the production of cement, lime, and other materials.
In archaeology, calcination can be used to analyze the composition of ancient materials and artifacts through controlled heating processes.
In metallurgy, calcination is used to remove volatile substances, water or carbon dioxide, from ores, to produce a more concentrated material for further processing.
In materials science, calcination is a common technique to modify the properties of materials by heating them to high temperatures in controlled environments.
Calcination is a process commonly used in chemistry to heat a substance to a high temperature in order to bring about a thermal decomposition, phase transition, or removal of a volatile fraction.
In metallurgy, calcination is used to remove volatile components from ores, such as carbonates, sulfates, or water, in order to prepare them for further processing.
Geologists may use calcination as a technique to study the thermal history of rocks and minerals, as heating a sample can provide information about its composition and properties.
In the field of ceramics, calcination is a crucial step in the production of ceramic materials, as it helps to remove organic impurities and improve the sintering process.
Archaeologists may encounter calcination when studying ancient pottery or other artifacts, as the firing process used to create these objects involves heating them to high temperatures.