Patterns of stable S isotopes in a forested catchment as indicators for biological S turnover

Despite intensive biogeochemical research during the last thirty years, the relative importance of biological S turnover for the overall SO₄^2– budget of forested catchments remains uncertain. The objective of the present study was (i) to gain new insight into the S cycle of theLehstenbach catchment (Northeastern Bavaria, Germany) through the analysis of stable isotopes of S and (ii) to differentiate between sites which are hot spots for SO₄^2– reduction and sites where mineralization and adsorption/desorption processes are more important. The ³⁴S values and SO₄^2– concentrations of soil solutions, throughfall and groundwater at four different sites as well as runoff of the catchment were measured. The relatively low variability of ³⁴S in throughfall and bulk precipitation was in contrast to the high temporal and spatial variability of ³⁴S in the soil solution. Sulfate in the soil solution of upland sites was slightly depleted in³⁴S compared to input values. This was most likely due to S mineralization. Sulfate in the soil solution from wetland soils was clearly enriched in³⁴S, indicating dissimilatory SO₄^2– reduction. The observed spatial and temporal patterns of³⁴S turnover and SO₄^2– concentrations might explain the overall balanced S budget of the catchment. At a time of decreasing anthropogenic deposition SO₄^2– is currently released from upland soils. Furthermore, mineralization of organic S may contribute to SO₄^2– release. Wetland soils in the catchment represent a sink for SO₄^2– due to dissimilatory SO₄^2– reduction.