In 450BC, Greek philosopher Empedocles introduced the "standard model" of physics, in which everything consisted of four elements (earth, air, water, and fire) (above left), and two forces (attraction and repulsion); in 350 BC, Aristotle added to this a density model (above right), in which denser elements tend to rise; lighter elements fall; earth is the heaviest element (and the center of the universe); fire the lightest; burning (or combustion) was simply the movement of the elements to their natural inherent position. | In 790, Arabian chemist Geber introduced the “three principles” model of combustion, in which metals are formed of two elements: sulphur, ‘the stone which burns’, the principle of combustibility, and mercury, the principle of metallic properties; and the third principle salt, is what gives gives solidity. | In 1524, Swiss chemist Paracelsus introduced the “sulphur combustion model”, in which he adopted Aristotle’s version of the four element theory, but reasoned that they appeared in bodies as Geber’s three principles, such that mercury included the cohesive principle, so that when it left in smoke the wood fell apart; smoke represented the volatility (the mercury principle); the heat-giving flames represented flammability (sulphur); the remnant ash represented solidity (salt). |
In 1699, German chemist Johann Becher introduced the terra pinguis model of combustion, in which a fatty, oily material substance called“terra pinguis” was considered as the material of bodies that gives things the property of combustion. | In 1703, German chemist Georg Stahl, Becher's student, introduced the phlogiston model of combustion, in which in which heat was viewed as a fire-like element, having mass, called “phlogiston”, contained within combustible bodies and released during combustion. | In 1789, French chemist Antoine Lavoisier introduced the caloric model of combustion, in which the process of combustion was said to result in the release of weightless "caloric" particles, or rather that in every combustion there is a disengagement of the matter of heat (or igneous fluid) or of light. |