“…Gasification and melting of organic wastes in an inert atmosphere, or with the addition of a substoichiometric amount of an oxidising agent, results in the production of combustible gaseous components, such as CO, H 2 , and CH 4 , and their contents in syngas (SG) are significantly affected by the waste composition and the boundary conditions of the thermal process (atmosphere type, operating pressure, temperature, time, etc.) [1,2,14]. Due to the high temperatures generated by a plasma arc, independently from the partial pressure of oxygen, the organic components of the waste decompose into simple gaseous compounds.…”