Year:
2015
Authors:
Dylla, N. P.* , R. Fox and T. Fisher
Source:
ASLO Aquatic Sciences Meeting, Granada, Spain
Abstract:
Nitrous Oxide (N
20) is a potent greenhouse gas, and streams, rivers, and groundwater act as sources of N
20 to the atmosphere. Four streams were sampled in four agriculturally dominated watersheds in the Choptank River Basin. N
20 gas concentrations and stream parameters were measured to estimate N
20 flux to the atmosphere for comparison with N
20 fluxes estimated with the IPCC protocols. N
20 fluxes (F, µmol N
20-N m
-2 h
-1) were calculated using measured N
20-N concentrations (Cm, µmol N
20-N L
-1) in excess of atmospheric equilibrium (Ceq, µmol N
20-N L
-1) and a gas exchange coefficient k (m h
-1) (F = (Cm - Ceq) * k). Fluxes of N
20 ranged over 0.17-23.10 µmol N
20-N m-2 h-1 in the four watersheds, and were similar to those calculated using the IPCC protocols and also to N
20 fluxes from nearby agricultural fields. The IPCC flux estimates were not statistically different from the empirically derived fluxes (p > 0.05). This approach can potentially provide a quick method to estimate the role of gas fluxes from streams in watersheds. Also, sampling occurred during a storm event—N
20 levels decreased during the storm event, while DO levels increased—which suggests that the rainfall itself caused an increase in gas exchange.
Mentors:
Tom Fisher, Ph.D.
Students:
Nicholas Dylla, Elmhurst College