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Impact of elevated CO2 on soil organic matter dynamics as related to changes in aggregate
turnover and residue quality. J. Six, A. Carpentier, C. van Kessel, R. Merckx, D. Harris, W.R. Horwath, and A. Lüscher.
Global Change Biology. Submitted (2000)
Increasing global atmospheric CO2 concentration can
potentially affect C cycling in terrestrial ecosystems. This study was conducted to assess the impact of elevated
CO2 concentration on soil organic matter and aggregate dynamics in Lolium perenne
and Trifolium repens pastures. Soil samples from a 6 year old "free air CO2
enrichment" (FACE) experiment were separated in four aggregate size classes (< 53, 53-250, 250-2000, and > 2000 µm).
Free light fraction (i.e. particulate organic matter (POM) outside of aggregates; free LF) and intra- aggregate-POM
(i.e. POM occluded within the aggregate structure; iPOM) were isolated. The distinct 13C-signature of the CO2 used to raise the ambient CO2
concentration in FACE allowed us to calculate proportions of recently incorporated C (< 6 yr) in the physically defined
soil fractions. Large and small macroaggregates (> 2000 µm and 250-2000 µm) were found to be 23%-60% more
enriched in new C compared to microaggregates (53-250 µm), confirming a hierarchical aggregate structure.
In addition, higher proportions of new C in macroaggregates under T. repens compared to L. perenne
indicate a faster macroaggregate turnover in T. repens. This faster macroaggregate turnover is hypothesized
to be a result of the higher residue quality (C:N ratio) of T. repens compared to L. perenne which would
reduce the potential of sequestering C under elevated CO2. In the L. perenne
soil, elevated CO2 did not increase total C, but led to: 1) a doubling of the amount
of large macroaggregates, 2) a 40% increase in total iPOM-C, and 3) a sequestration of C in microaggregates.
These observations indicate that the sequestration of iPOM-C and microaggregate-C induced by elevated CO2
in the low residue quality, L. perenne treatment, resulted from an increase in macroaggregation without a
change in macroaggregate turnover.
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