Land use change from C3 grassland to C4 Miscanthus

effects on soil carbon content and estimated mitigation benefit after six years

Alessandro Zatta, John Clifton-Brown, Paul Robson, Astley Francis St John Hastings, Andrea Monti

Research output: Contribution to journalArticle

46 Citations (Scopus)

Abstract

To date, most Miscanthus trials and commercial fields have been planted on arable land. Energy crops will need to be grown more on lower grade lands unsuitable for arable crops. Grasslands represent a major land resource for energy crops. In grasslands, where soil organic carbon (SOC) levels can be high, there have been concerns that the carbon mitigation benefits of bioenergy from Miscanthus could be offset by losses in SOC associated with
land use change. At a site in Wales (UK), we quantified the relatively short-term impacts (6 years) of four novel Miscanthus hybrids and Miscanthus 9 giganteus on SOC in improved grassland. After 6 years, using stable carbon isotope ratios (13C/12C), the amount of Miscanthus derived C (C4) in total SOC was considerable (ca. 12%) and positively correlated to belowground biomass of different hybrids. Nevertheless, significant changes in SOC stocks (0–30 cm) were not detected as C4 Miscanthus carbon replaced the initial C3 grassland carbon; however, initial SOC decreased more in the presence of higher belowground biomass. We ascribed this apparently contradictory
result to the rhizosphere priming effect triggered by easily available C sources. Observed changes in SOC partitioning were modelled using the RothC soil carbon turnover model and projected for 20 years showing that there is no significant change in SOC throughout the anticipated life of a Miscanthus crop. We interpret our observations to mean that the new labile C from Miscanthus has replaced the labile C from the grassland and, therefore, planting Miscanthus causes an insignificant change in soil organic carbon. The overall C mitigation benefit is therefore not decreased by depletion of soil C and is due to substitution of fossil fuel by the aboveground biomass, in this instance 73–108 Mg C ha 1 for the lowest and highest yielding hybrids, respectively, after 6 years.
Original languageEnglish
Pages (from-to)360-370
Number of pages11
JournalGlobal Change Biology. Bioenergy
Volume6
Issue number4
Early online date12 Apr 2013
DOIs
Publication statusPublished - 1 Jul 2014

Fingerprint

Miscanthus
soil carbon
Land use
soil organic carbon
land use change
Organic carbon
mitigation
grasslands
grassland
organic carbon
Soils
Carbon
carbon
soil
Crops
energy crop
belowground biomass
energy crops
arable soils
Biomass

Keywords

  • bioenergy
  • grassland
  • Miscanthus
  • priming effect
  • roots
  • SOC
  • stable carbon isotope

Cite this

Land use change from C3 grassland to C4 Miscanthus : effects on soil carbon content and estimated mitigation benefit after six years. / Zatta, Alessandro; Clifton-Brown, John; Robson, Paul; Hastings, Astley Francis St John; Monti, Andrea.

In: Global Change Biology. Bioenergy, Vol. 6, No. 4, 01.07.2014, p. 360-370.

Research output: Contribution to journalArticle

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abstract = "To date, most Miscanthus trials and commercial fields have been planted on arable land. Energy crops will need to be grown more on lower grade lands unsuitable for arable crops. Grasslands represent a major land resource for energy crops. In grasslands, where soil organic carbon (SOC) levels can be high, there have been concerns that the carbon mitigation benefits of bioenergy from Miscanthus could be offset by losses in SOC associated withland use change. At a site in Wales (UK), we quantified the relatively short-term impacts (6 years) of four novel Miscanthus hybrids and Miscanthus 9 giganteus on SOC in improved grassland. After 6 years, using stable carbon isotope ratios (13C/12C), the amount of Miscanthus derived C (C4) in total SOC was considerable (ca. 12{\%}) and positively correlated to belowground biomass of different hybrids. Nevertheless, significant changes in SOC stocks (0–30 cm) were not detected as C4 Miscanthus carbon replaced the initial C3 grassland carbon; however, initial SOC decreased more in the presence of higher belowground biomass. We ascribed this apparently contradictoryresult to the rhizosphere priming effect triggered by easily available C sources. Observed changes in SOC partitioning were modelled using the RothC soil carbon turnover model and projected for 20 years showing that there is no significant change in SOC throughout the anticipated life of a Miscanthus crop. We interpret our observations to mean that the new labile C from Miscanthus has replaced the labile C from the grassland and, therefore, planting Miscanthus causes an insignificant change in soil organic carbon. The overall C mitigation benefit is therefore not decreased by depletion of soil C and is due to substitution of fossil fuel by the aboveground biomass, in this instance 73–108 Mg C ha 1 for the lowest and highest yielding hybrids, respectively, after 6 years.",
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