Measurement of the absorptive efficiency of ferric oxide is made by passing a measured volume of air containing a known low concentration of H2S through the sample at a known constant velocity, and measuring the residual HzS which has not been extracted. This last measurement is carried out by passing the air through a paper impregnated with silver nitrate, and measuring the opticaL transmission density of the stain formed. Concentrations are calculated from the sulphide stain densities and the volumes of air passed through the papers. The calibration technique forms the basis of a method of measurement of trace amounts of H2S in the atmosphere, and is unaffected by the presence of SOz.