Natural revegetation of bog pools after peatland restoration involving ditch blocking: the influence of pool depth and implications for carbon cycling

Throughout the last two centuries peatlands have been subject to extensive drainage, typically through
the digging of ditches. Ecosystem restoration now focusses on damming or infilling these ditches to
increase biodiversity and to provide a range of ecosystem services such as carbon sequestration and
water provision. We surveyed 60 bog pools created following ditch blocking (alone) on a blanket bog
in north Wales. Eighteen months after restoration the mean total pool vegetation cover was 76%. There
was a strong negative relationship between pool depth and Eriophorum cover (r2 = 0.74), and a weaker
positive relationship between depth and Sphagnum cover (r2 = 0.35). Observations showed that pools had
been colonised by various invertebrate species. Pool dissolved organic carbon (DOC) concentrations were
not connected to pool vegetation, suggesting that catchment-scale processes drive DOC. Other studies
have shown that Eriophorum generates large methane fluxes, and that Sphagnum can act as a methane
sink. Therefore we recommend that pools should be deeper than 0.5 m to give the greatest carbon benefit,
whilst noting that this is unlikely to significantly affect DOC fluxes.