Hydrogen chloride decay, defined as the deposition of hydrogen chloride from fire (and other) atmospheres onto surfaces, has been studied as a function of atmospheric humidity, of size or configuration of the apparatus used, of type of surface in the apparatus and of rate of air movement. This decay means that, in a static system with a sorptive surface, hydrogen chloride has a half-life of 3 min or less, before disappearing from the atmosphere. A simplified mechanism has been devised to identify reactions which simulate the processes involved in hydrogen chloride generation, transport and decay. Mathematical fitting of the hydrogen chloride concentration-time profiles obtained from a large-scale and two small-scale apparatuses was carried out. The "parameters" Downloaded from 106 calculated in this way have been used as a method for screening system variables and identifying dependencies.It has been found that several factors affect hydrogen chloride decay, viz.: (i) The presence of humidity in the atmosphere greatly accelerates decay.(ii) The type of surface exposed to hydrogen chloride will have a large effect in determining peak atmospheric concentrations and rates of decay, with sorptive surfaces being responsible for much more rapid decay than smooth surfaces.(iii) The level of air agitation will also influence hydrogen chloride decay, because of the effect on the rate of transport of the molecules to the reactive surfaces.This work has two important implications in terms of fire hazard: (a) The peak airborne concentrations of hydrogen chloride which will be encountered in a real fire scenario will be much lower than would have been predicted from the chlorine content of the fuel; furthermore, these concentrations may soon decrease to very low levels because of decay.(b) The majority of small-scale smoke toxicity tests use non-sorptive surface environments; they are likely, therefore, to exaggerate the toxicity of the combustion products of chlorine-containing materials such as poly(vinyl chloride).