Data from: Afforestation-related fertilisation quickly turns barren cutaway peatland into a carbon dioxide sink

Energy peat extraction has declined rapidly in Europe in recent years,
leaving thousands of hectares of land requiring after-use management and
planning. A popular after-use option, afforestation, is understudied, and
there is a limited understanding of its overall effect on greenhouse gas
(GHG) and energy exchange. In this study, we present a multi-year record
of eddy covariance fluxes of carbon dioxide (CO2), energy fluxe,s and
surface albedo, chamber measurements of methane (CH4) and (N2O), and
estimates of lateral carbon (C) losses from dissolved organic carbon (DOC)
measurements from a cutaway peatland in Finland during the first three
years of afforestation. The site was fertilised with wood ash, and
2-year-old Scots pine (Pinus sylvestris) saplings were planted. Wild
vegetation emerged at the site in the first summer after fertilisation.
Satellite-derived leaf area index data showed clear year-on-year increase,
and there was good agreement with changes in CO2 fluxes over the full
study period. The albedo of the site increased with plant cover annually,
resulting in negative radiative forcings and net CO2-equivalent (CO2-eq)
removals. After being a source of CO2 in the first year (144 ± 20
g CO2‑C m−2 yr−1), the site transitioned to a
sink for the next two study years (−36 ± 12 and −19
± 19 g CO2‑C m−2 yr−1).
Annual fluxes of CH4 and N2O were small but not negligible. Net annual C
losses stopped after one year, where DOC losses offset CO2 uptake, and the
afforestation resulted in a mean change in the annual net ecosystem C
balance of 172 g C m−2 yr−1 and radiative
balance of −688 g CO2‑eq m−2 yr−1 over a
100-year time horizon. Cutaway peatlands typically remain long-term
sources of C if abandoned, and our results indicate that the afforestation
process can rapidly revegetate barren peatlands and halt net C losses.