Current methods for determining inorganic sulphur (S) in aerated mineral so
il horizons often result in underestimates. To overcome this defect we deve
loped a new method combining a batch extraction with 0.5 m NH4F solution at
a soil:solution ratio of 1:5 with a subsequent analysis of the mobilized S
O42- by ion chromatography. The ammonium fluoride extraction enables us to
characterize inorganic sulphate in non-calcareous forest soils. It is more
efficient than conventional procedures in which inorganic S is extracted wi
th phosphate or bicarbonate solution. In contrast to the extraction with st
rongly alkaline reagents (NaOH, KOH, LiOH), the NH4+-NH3 buffer system in N
H4F prevents the pH of the suspension from exceeding 9.0 and thus the undes
ired conversion of organic S into SO42- by auto-oxidation and hydrolysis of
ester sulphate. In a comparison we demonstrated that the inorganic S in si
x German forest soils is underestimated by up to 50% or 200 kg S ha(-1) in
the uppermost 60 cm, if it is assessed by extraction with 0.016 m KH2PO4 or
0.5 m NaHCO3 instead of 0.5 m NH4F. Conversely, the pool of ester sulphate
is overestimated almost threefold.