Nitrous oxide and methane fluxes vs. carbon, nitrogen and phosphorous burial in new intertidal and saltmarsh sediments

Abstract

Carbon (C), nitrogen (N) and phosphorous (P) burial rates were determined within natural saltmarsh (NSM) and ‘managed realignment’ (MR) sediments of the Blackwater estuary, UK. Methane (CH4) and nitrous oxide (N2O) fluxes were measured along with their ability to offset a portion of the C burial to give net C sequestration. C and N densities (Cρ and Nρ) of NSM sediments (0.022 and 0.0019gcm−3) are comparable to other UK NSM sediments. Less vegetationally developed MR sediments have lower Cρ and Nρ (0.012 and 0.0011gcm−3) while the more vegetationally developed sites possess higher Cρ and Nρ (0.023 and 0.0030gcm−3) than NSM. Both NSM and MR areas were small CH4 (0.10–0.40gm−2yr−1) and N2O (0.03–0.37gm−2yr−1) sources. Due to their large Global Warming Potentials, even these relatively small greenhouse gas (GHG) fluxes reduced the net C sequestration within MR marshes by as much as 49%, but by only 2% from NSM. Potential MR areas within the Blackwater estuary (29.5km2 saltmarsh and 23.7km2 intertidal mudflat) could bury 5478tCyr−1 and 695.5tN yr−1, with a further 476tNyr−1 denitrified. The saltmarsh MR would also sequester 139.4t Pyr−1. GHG fluxes would reduce the C burial benefit by 24% giving a C sequestration rate of 4174tCyr−1. Similar areas within the Humber estuary (74.95km2) could bury 3597tCyr−1 and 180tNyr−1, with a further 442tNyr−1 denitrified. GHG fluxes would reduce the C burial benefit by 31% giving a C sequestration rate of 2492t Cyr−1. Overall, MR sites provide sustainable coastal defence options with significant biogeochemical value and, despite being net sources of CH4 and N2O, can sequester C and reduce estuarine nutrient loads.