8.1. Fundamentals#
As stated in section 1.1, pyrolysis describes the emission of gases from the solid material. It is the thermal decomposition of materials under inert atmosphere. Whereby thermal decomposition is defined as a process of extesive chemical species change caused by heat. The gases released from the solid may afterwards react with oxygen, this reaction is not part of the pyrolysis.
Studying pyrolysis with the TGA#
A thermogravimetric analyser (TGA) is often used to study pyrolysis. In a tga the mass of the sample is so small (usually between

Fig. 8.1 TGA#
In a TGA a small amount of sample mass is placed in a crucible. This crucible is placed in the TGA. During the measurement the device will heat with a specified heating rate (e.g.
Fig. 8.2 Mass loss curve from TGA data.#
Fig. 8.3 Mass loss rate curve from TGA data#
Arrhenius equation#
To describe a pyrolysis process Arrhenius equations are usually used. Suppose an amount of one specific material (X) is completly converted to gaseous fuel with one reaction. This pyrolysis reaction can than be described by a rate equation and the Arrhenius equation:
where
: activation energy : pre-exponential factor : reaction order
Modeling with FDS#
There are several ways to model pyrolysis in fds. The simplest way is to specify the heat release rate. In this case the pyrolising sample will be modeled as ejection of gaseous fuel from the surface.
However fds, also allows for more complex pyrolysis modelling. Every material described in the fds input file can undergo multiple reactions. The amount of reactions should be specified by N_REACTIONS
for every material. For every single reaction the reaction parameters, the created solid material, the released gas species, and others should be specified in the input file.
For each reaction the kinetic parameters need to be specified. The general evolution equation is given by:
where:
: rate of reaction at the tempeature T_s of the ith material undergoing the jth reaction : yield of production of material i by other reactions : density of the ith matierial of the layer : original density of the layer : local oxygen volume fraction