The primary object of the peat milling operation is to mill a layer of peat on the surface of the bog such that all of this layer (throughout the bog) dries to the required moisture content in the same time interval, so that it can all be harvested simultaneously. Peat type (and hence drying characteristics) vary considerably throughout a given bog, hence the depth of this milled layer should at any given location in the bog match the drying characteristics of the peat at this location. In order to do this, it is necessary to determine some measurable characteristic of peat, representative of the drying time, so this can be used to determine the milling depth. Field and laboratory experiments revealed that compressibility of milled peat is a good depth control characteristic because of its high correlation with the relative drying time of milled peat. For example a typical high density peat (compressibility of 12%) has a milling depth requirement of 21 mm compared with 9 mm for a low density peat (compressibility of 25%). Results indicate that the application of this method within the peat industry would give a 27% increase in dry matter yields per hectare and the variation of the moisture content of the harvested milled peat would be reduced from a standard deviation of 0·55 kg/kg to one of 0·22 kg/kg.