Citation Information

  • Title : Unexpected stimulation of soil methane uptake as emergent property of agricultural soils following bio-based residue application.
  • Source : Global Change Biology
  • Publisher : Wiley-Blackwell
  • Volume : 21
  • Issue : 10
  • Pages : 3864-3879
  • Year : 2015
  • DOI : 10.1111/gcb.12974
  • ISBN : 1354-1013
  • Document Type : Journal Article
  • Language : English
  • Authors:
    • Ho,A.
    • Reim,A.
    • Kim SangYoon
    • Meima-Franke,M.
    • Termorshuizen,A.
    • Boer,W. de
    • Putten,W. H. van der
    • Bodelier,P. L. E.
  • Climates: Marintime/Oceanic (Cfb, Cfc, Cwb).
  • Cropping Systems: Conservation cropping systems.
  • Countries: Netherlands.

Summary

Intensification of agriculture to meet the global food, feed, and bioenergy demand entail increasing re-investment of carbon compounds (residues) into agro-systems to prevent decline of soil quality and fertility. However, agricultural intensification decreases soil methane uptake, reducing, and even causing the loss of the methane sink function. In contrast to wetland agricultural soils (rice paddies), the methanotrophic potential in well-aerated agricultural soils have received little attention, presumably due to the anticipated low or negligible methane uptake capacity in these soils. Consequently, a detailed study verifying or refuting this assumption is still lacking. Exemplifying a typical agricultural practice, we determined the impact of bio-based residue application on soil methane flux, and determined the methanotrophic potential, including a qualitative (diagnostic microarray) and quantitative (group-specific qPCR assays) analysis of the methanotrophic community after residue amendments over 2 months. Unexpectedly, after amendments with specific residues, we detected a significant transient stimulation of methane uptake confirmed by both the methane flux measurements and methane oxidation assay. This stimulation was apparently a result of induced cell-specific activity, rather than growth of the methanotroph population. Although transient, the heightened methane uptake offsets up to 16% of total gaseous CO 2 emitted during the incubation. The methanotrophic community, predominantly comprised of Methylosinus may facilitate methane oxidation in the agricultural soils. While agricultural soils are generally regarded as a net methane source or a relatively weak methane sink, our results show that methane oxidation rate can be stimulated, leading to higher soil methane uptake. Hence, even if agriculture exerts an adverse impact on soil methane uptake, implementing carefully designed management strategies (e.g. repeated application of specific residues) may compensate for the loss of the methane sink function following land-use change.

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