Preliminary evidence of effects of Phragmites australis growth on N2O emissions by laboratory microcosms

Abstract

Abstract Denitrification has been found to play a significant role in the nitrogen (N) biogeochemical cycle of riparian wetland systems; however, there is little understanding of the role of emergent macrophytes in sediment denitrification. In this study, laboratory culture experiments were conducted to examine how Phragmites australis growth affected N 2 O emissions. Additionally, preliminary investigations into the variability of carbon and available NO 3 − –N fractions were conducted. The N 2 O emission rate was quantified based on the high-resolution N 2 O microprofiles in acetylene-inhibited sediment cores. Seasonal-dependence of N 2 O emission was remarkable throughout incubation of both P. australis rooted sediments and control with no P. australis , and increased significantly with biomass steady accumulation (p 2 O m −2 day −1 at day 180 (in late autumn) in the P. australis rhizosphere . Simultaneously, N 2 O emissions were more highly influenced by fine-root biomass, belowground biomass and plant height than total biomass, root activity and relative growth rate in the Spearman rank correlation model. More specifically, based on the strong and significant (p 2 O emission flux, the rapid transformation indicated that changes in the HWC (ranging from 720 to 3564 mg kg −1 ) with plant growth could reflect a 14-fold variation in N 2 O emissions during the growth stage, and that N 2 O emissions were highly dependent on fine-root biomass and its delivery of organic carbon. The ion exchangeable form NO 3 -N (IEF-NO 3 -N) in sediments was found to be the predominant transferable form involved in denitrification, while the iron-manganese oxide form NO 3 -N (IMOF-NO 3 -N) can be considered as a potential source of nitrogen for denitrification. This study highlights that emergent macrophyte communities dominate riparian ecosystem denitrification and that the metabolic mechanisms of emergent macrophytes can have positive feedbacks on the HWC fraction and available NO 3 -N combined with sediment components in rhizosphere sediments.