IMPACT OF HURRICANE IRENE AND TROPICAL STORM LEE ON RIPARIAN ZONE HYDROLOGY AND BIOGEOCHEMISTRY

Although riparian zones are well known to reduce nitrogen (N) and phosphorus (P) runoff to streams, they also have the potential to affect greenhouse gas (GHG: CO₂, N₂O, CH₄) fluxes to the atmosphere. Following large storms, soil biogeochemical conditions often become more reduced, especially in oxbow depressions and side channels, which can lead to hot moments of GHG production. Here, we investigate the impact of the remnants of Hurricane Irene and Tropical Storm Lee on riparian zone hydrology (water table: WT), and biogeochemistry (oxidation-reduction potential (ORP), dissolved oxygen (DO), NO₃^-, PO₄^3-, CO₂, N₂O, CH₄). Results indicate that large storms have the potential to reset WT levels for weeks to months. Overbank flooding at our site following Irene and Lee led to the infiltration of well-oxygenated water at depth (higher DO and ORP), while promoting the development of anoxic conditions within soil aggregates near the soil surface (increased N₂O and CH₄ fluxes). A short-term increase in CO₂ emission was observed following Irene at our site where aerobic respiration was water-limited. Over a two-year period, an oxbow depression exhibited higher WT, higher CH₄ fluxes (hot moment), higher CO₂ fluxes (seasonal), and lower NO₃^- concentrations (seasonal) than the rest of the riparian zone. However, neither Irene, nor Lee, nor the oxbow depression significantly impacted PO₄^3-. Dissolved organic carbon, ORP, and DO data illustrate the time-lag (> 20 years) between the creation of an oxbow depression and the development of more reducing conditions in spite of clear differences in RZ and oxbow WT dynamics.