The thermal decomposition temperature is the specific temperature at which a material begins to undergo chemical breakdown into simpler substances when subjected to heat, usually identified experimentally by the initial significant mass loss in a
thermogravimetric (TGA) curve. This marks the onset of observable chemical decomposition, where chemical bonds cleave solely due to
thermal energy. Since chemical reactions are essentially
always occurring, because molecules assume a
probability distribution of energies, there is no distinct temperature value at which decomposition spontaneously occurs. Therefore, the onset temperature is often used experimentally; this is the temperature at which a chemical reaction occurs at a measurable rate, and is thus highly dependent on the sensitivity of the corresponding instrument. The onset temperature can be calculated using
differential scanning calorimetry (DSC), which is also sensitive to the rate of heating. A higher rate of heating will often display a higher onset temperature due to further kinetic variables such as reaction order, activation energy, and autocatalytic behaviour. A simple substance (like
water) may exist in equilibrium with its thermal decomposition products, effectively halting the decomposition. The equilibrium fraction of decomposed molecules increases with the temperature. Since thermal decomposition is a kinetic process, the observed temperature of its beginning in most instances will be a function of the experimental conditions and sensitivity of the experimental setup. For a rigorous depiction of the process, the use of thermokinetic modeling is recommended. ==Examples==