Wetlands often form the transition zone between upland soils and watershed streams, however, stream-wetland interactions and hydrobiogeochemical processes are poorly understood. We measured changes in stream nitrogen (N) through one riparian wetland and one beaver meadow in the Archer Creek watershed in the Adirondack Mountains of New York State, USA from 1 March to 31 July 1996. In the riparian wetland we also measured changes in groundwater N. Groundwater N changed significantly from tension lysimeters at the edge of the peatland to piezometer nests within the peatland. Mean N concentrations at the peatland perimeter were 1Γ5, 0Γ5 and 18Γ6 Β΅mol L 1 for NH 4 C , NO 3 and DON (dissolved organic nitrogen), respectively, whereas peatland groundwater N concentration was 56Γ9, 1Γ5 and 31Γ6 Β΅mol L 1 for NH 4 C , NO 3 and DON, respectively. The mean concentrations of stream water N species at the inlet to the wetlands were 1Γ5, 10Γ1 and 16Γ9 Β΅mol L 1 for NH 4 C , NO 3 and DON, respectively and 1Γ6, 28Γ1 and 8Γ4 Β΅mol L 1 at the wetland outlet. Although groundwater total dissolved N (TDN) concentrations changed more than stream water TDN through the wetlands, hydrological cross-sections for the peatland showed that wetland groundwater contributed minimally to stream flow during the study period. Therefore, surface water N chemistry was affected more by in-stream N transformations than by groundwater N transformations because the in-stream changes, although small, affected a much greater volume of water.
Stream water N input-output budgets indicated that the riparian peatland retained 0Γ16 mol N ha 1 day 1 of total dissolved N and the beaver meadow retained 0Γ26 mol N ha 1 day 1 during the study period. Nitrate dominated surface water TDN flux from the wetlands during the spring whereas DON dominated during the summer. This study demonstrates that although groundwater N changed significantly in the riparian peatland, those changes were not reflected in the stream. Consequently, although in-stream changes of N concentrations were less marked than those in groundwater, they had a greater effect on stream water chemistry-because wetland groundwater contributed minimally to stream flow.