Infrared spectroscopy and chemical degradation indicated several fulvic acid fractions from an iron-humus podzol capable of complexing and translocating metals. Acidic polysaccharides, some of them resembling pectic acid, were isolated in appreciable quantities. These are able to bind metals through carboxyl groups, but peptide components present in the polysaccharide fraction may provide alternative metal complexing centres. The high yield of acidextractable organic matter from the illuvial humus, together with its high content of carboxylic acid groups, make it likely that this fraction plays a major role in the translocation of metals. Phenolic compounds allegedly associated with this process were present in the fulvic acid solution in low amounts, and only in the extracts from the organic horizons.In trod u c tion THE term 'podzol' originally implied the occurrence of a bleached A2 layer below the surface horizons of the soil profile (Muir, 196 1). Wider definitions of the term include features which may be more obvious in the field, for example the existence of an ochreous B horizon containing translocated humus (cfi Romans, 1 970). The accumulation of humus in the B horizon, accompanied by relatively high concentrations of aluminium and iron, has been held t o indicate an organic complexation and translocation of mineral cations. Indeed, laboratory experiments involving leaf leachates (Bloomfield, 1970), and field studies on the composition of canopy drip and the movement of sub-surface soil water (Davies, 1 970) have demonstrated the feasibility of such hypotheses.Soil organic matter is also likely t o be important in this type of translocation, particularly the more soluble, lower molecular weight, fulvic acid fraction. Forsyth (1947) introduced a method of fractionating fulvic acid solutions based on adsorption of the mixtures on charcoal and the subsequent elution (by various solvents) of fractions A, B, C and D. The aim of the present study is to characterize these Forsyth fulvic acid fractions from a podzol under natural vegetation, using infrared spectroscopy and chemical degradation, and t o deduce whether they are capable of complexing and translocating metal ions. A preliminary account of this work has already beep given (Anderson, 1970).