Permafrost Disturbance Impacts on Dissolved Ion Loads and Nitrogen Dynamics
Abstract:
Key differences in the impacts of slope disturbance on the fluvial export of major ions, and nitrogen from these headwater catchments were observed. The export of ions increased for all streams (disturbed and undisturbed) in response to deep thaw in warm years. However, the impact of physical disturbance was largely limited to increased ion concentrations late in the season when baseflow was driven by rainfall and soil water drainage. In contrast, nitrate (NO3-) concentrations were substantially affected by physical disturbance. A comparison of a disturbed and undisturbed catchment shows the two streams had similar concentrations of all dissolved N prior to slope failure, yet five years following failure, NO3- concentrations in the disturbed watershed were two orders of magnitude higher than in the undisturbed catchment. NO3- was especially high following late season rainfall and isotopic evidence shows that late season NO3-is not from rainfall but microbially produced (mineralized).
Results indicate that the impact of disturbance on ion and N loads is limited by discharge and hydrological connectivity of the disturbed areas, that the drainage of upper permafrost (soils below normal active layer depth) is the likely source of enhanced ion and mineralized NO3-, and that impacts are evident several years after disturbance.
