GHG emissions

In addition to CO2 fluxes we also measured greenhouse gas (GHG) emissions, including nitrous oxide (N2O) and methane (CH4). However, N2O emissions were minimal during the first two years - as can be expected on nutrient (i.e. N) poor blanket bog - and only CH4 emissions were further investigated. Methane emissions were measured first only on non-vegetated peat areas (vegetation was removed and cut regularly) but measurements over vegetated areas were subsequently added to capture plant-mediated transport (PMT) impacts from vegetation, especially sedges, as well as oxidation potential from vegetation, especially Sphagnum. Moreover, methane flux measurement methodology adapted over time with availability of state-of-the-art analysers (moving from cover bog GC to LGR GHG and then to LiCor GHG analysers).

Static cover box for GHG emissions (CH4, N2O and CO2)

greenhouse gas analyzer provides continuous measurements above the Arctic Circle

NEW ultra-portable (what a joke !) LGR GHG analyser

LGR GHG analyser in action at Nidderdale

"Gas-Snake" in place on soil surface among grass

Soil GHG flux examples for all three sites (from left to right: July; October; December 2012):

Mossdale - wettest (top), Nidderdale - driest (mid) and Whitendale (bottom)

So far, the GHG fluxes revealed clear differences only for CO2 and CH4 (methane) fluxes between sites and less so for treatments (i.e. N2O emissions were very similar over the first three years and an average value of 0.03 nmol N2O m-2 s-1 or 0.035 g N2O m-2 yr-1 was used in any further GHG calculations; see below left). The annual methane emissions showed considerable inter-annual and general site variability and emissions also showed a huge difference in using mean (much higher) versus median (much lower) fluxes. Moreover, average annual methane emissions (below right) showed considerable management differences (uncut > mown > burnt), and revealed particularly high (median) emission peaks after or during very wet and warm years (i.e. 2015 - 2017) - notable this was similar to measurements reported for another UK blanket bog site (Moor House, NNR; contact: Prof Niall McNamara):

N2O emissions
Methane Site & Management

Combining the mean NEE budgets with the median CH4 and average N2O fluxes, we estimated the net GHG budget (based on their Global Warming Potential, GWP, over a 100 year time period) based on a transformation of CH4 into CO2eq = x 25 and N2O into CO2eq = x 298.

A key component of the GHG flux is methane. Notably, aerenchymous plants such as sedges act as 'vents' for methane, allowing methane to escape quickly from deeper, anoxic and methane producing (methanogenesis) peat layers to the atmosphere, thus avoiding access to methane oxidising bacteria (methanotrophy). We therefore also measured GHG (including methane) fluxes from plots with or without vegetation and assessed the percentage of sedges within each plot. This allowed us to correlate methane fluxes against %sedge cover and the overall plant mediated transfer (vegetated - peat) was 62%):
Methane bare vs vegetated Sites
Methane bare vs vegetated NW only

Above: Methane emissions were positively correlated with higher sedge cover (left) and Comparison of CH4 (methane) fluxes (in nmol m-2 s-1) using the Los Gatos UGGA analyser on uncut plots on either vegetation free (peat) or vegetated areas (regrown since heather cutting in 2013) for all three sites (centre) or for only Nidderdale and Whitendale (right)

Notably, GHG fluxes are higher from vegetated plots (NEE cut - regrown) versus vegetation free peat (GHG) plots, and the fast re-vegetation at Mossdale with sedges after mowing lead to much higher methane fluxes from mown plots than measured on burnt plots with much less regrowth overall. However, intact (uncut) plots also showed fairly high methane emissions, even under lower overall sedge cover (as it is Calluna dominated).

Below: GHG budgets were compared to those published by the IUCN UK Peatland initiative (left), and either with using the mean (centre) or the median (right) methane emissions:

net GHG mean
net GHG median

Finally, the average annual net GHG budgets were estimated over the project period for each site (Nidderdale, Mossdale, Whitendale) and management scenario (uncut, burnt, mown), which included accounting for average emissions from management (fuel for burning and mowing management; combustion loss and charcoal sequestration from biomass burning), assuming a 20 year management rotation. However, as values for global warming potential (GWP) are context dependent (see Allen et al., 2018: "Ambiguity arises because emissions of cumulative pollutants and [short-lived climate pollutants] (SLCPs) translate into impact on the planetary energy budget in fundamentally different ways: for cumulative pollutants like CO2, radiative forcing largely scales with the total stock (cumulative integral) of emissions to date, while for SLCPs like methane, it scales with the current flow (emission rate) multiplied by the SLCP lifetime"), we considered a range of GWPs. First, we adhered to the IPPC's 4th Assessment values based on the 100 year GWP (for methane and N2O), secondly, we considered the sustained GWP (SGWP; see Neubauer & Megonigal, 2015; Balcombe et al., 2018), this considers that the standard GWP does not adequately represent sustained ecosystem emissions of methane, thirdly, we also considered the SGWP for both, the 100 year and the 20 year time period (i.e. the latter much better representing the actual short-term climate effects, particularly of the short lived methane gas, and the need to achieve urgent reductions in atmospheric GHG emissions); all also considered (for very variable methane emissions) either using the overall median fluxes or the mean of the 8 annual median fluxes (i.e. for all plot replicates throughout a year):

IPPC Median Methane 100 years
IPCC Mean of Median Methane 100 years
Median Methane SGWP 100 years
Mean of Median Methane SGWP 100 years
Median SGWP 20 years
Mean of Median Methane SGWP 20 years

Above: Noticeable are the increasing net GHG emissions (see above tables) based on the various GWP options (from top to bottom: IPCC < SGWP 100 years < SGWP 20 years) and the overall higher net GHG emissions when using mean methane emissions of overall median emissions (left) vs. annual median fluxes (right) and from mowing over burning after 6 years of post-management. However, burning emissions also need to include the additional emissions from biomass combustion (about 90 tCO2eq m-2 yr-1), which is indicated also for charcoal C capture and mowing emissions.