Chronic atmospheric reactive N deposition has breached the N sink capacity of a northern ombrotrophic peatbog increasing the gaseous and fluvial N losses

Research output: Contribution to journalArticlepeer-review

Authors

  • Fotis Sgouridis
  • Christopher A. Yates
  • Charlotte E.M. Lloyd
  • Ernesto Saiz
  • Daniel N. Schillereff
  • Sam Tomlinson
  • Jennifer Williamson

Colleges, School and Institutes

External organisations

  • University of Bristol
  • Keele University
  • King’s College London
  • UK Centre for Ecology and Hydrology

Abstract

Peatlands play an important role in modulating the climate, mainly through sequestration of carbon dioxide into peat carbon, which depends on the availability of reactive nitrogen (Nr) to mosses. Atmospheric Nr deposition in the UK has been above the critical load for functional and structural changes to peatland mosses, thus threatening to accelerate their succession by vascular plants and increasing the possibility of Nr export to downstream ecosystems. The N balance of peatlands has received comparatively little attention, mainly due to the difficulty in measuring gaseous N losses as well as the Nr inputs due to biological nitrogen fixation (BNF). In this study we have estimated the mean annual N balance of an ombrotrophic bog (Migneint, North Wales) by measuring in situ N2 + N2O gaseous fluxes and also BNF in peat and mosses. Fluvial N export was monitored through a continuous record of DON flux, while atmospheric N deposition was modelled on a 5 × 5 km grid. The mean annual N mass balance was slightly positive (0.7 ± 4.1 kg N ha−1 y−1) and varied interannually indicating the fragile status of this bog ecosystem that has reached N saturation and is prone to becoming a net N source. Gaseous N losses were a major N output term accounting for 70% of the N inputs, mainly in the form of the inert N2 gas, thus providing partial mitigation to the adverse effects of chronic Nr enrichment. BNF was suppressed by 69%, compared to rates in pristine bogs, but was still active, contributing ~2% of the N inputs. The long-term peat N storage rate (8.4 ± 0.8 kg N ha−1 y−1) cannot be met by the measured N mass balance, showing that the bog catchment is losing more N than it can store due its saturated status.

Bibliographic note

Funding Information: The authors wish to acknowledge and thank staff at the UK Centre for Ecology & Hydrology (Bangor), who deployed and maintained instream optical sensors and Dwr Cymru Welsh Water (DCWW) for allowing access to the data. This research draws upon published datasets available through the Environmental Information Data Centre (hosted by UKCEH), funded under the Natural Environment Research Council (NERC) Macronutrient Cycles Programme. Stage discharge data along with the sampling and analysis of instream chemical variables were conducted under ‘Turf 2 Surf’ project (NERC; NE/J011991/1). Measurements of N 2 and N 2 O along with atmospheric deposition data were funded under the LTLS project (NERC; NE/J011541/1, NE/J011533/1 and NE/J011703/1 respectively). A special thanks goes to Edward Tipping and Hannah Toberman who carried out all the sampling and analysis in peat cores collected in the Migneint. Publisher Copyright: © 2021 The Authors

Details

Original languageEnglish
Article number147552
Number of pages11
JournalScience of the Total Environment
Volume787
Early online date15 May 2021
Publication statusPublished - 15 Sep 2021

Keywords

  • N isotopes, Atmospheric N deposition, Biological nitrogen fixation, Denitrification, DON, Peatbog

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