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| Titel |
Free and protected soil organic carbon dynamics respond differently to abandonment of mountain grassland |
| VerfasserIn |
S. Meyer, J. Leifeld, M. Bahn, J. Fuhrer |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1726-4170
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| Digitales Dokument |
URL |
| Erschienen |
In: Biogeosciences ; 9, no. 2 ; Nr. 9, no. 2 (2012-02-23), S.853-865 |
| Datensatznummer |
250006773
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| Publikation (Nr.) |
 copernicus.org/bg-9-853-2012.pdf |
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| Zusammenfassung |
Land-use change (LUC) and management are among the major driving forces of
soil carbon (C) storage. Abandonment of mountain grassland promotes
accumulation of aboveground biomass and litter, but related responses of soil
organic matter (SOM) dynamics are uncertain. To determine SOM-C turnover we
sampled 0–10 cm of soils in the European Alps along two land-use gradients (hay meadows, grazed
pastures and abandoned grasslands) of different management
intensity. A first land-use gradient was located at Stubai Valley (MAT: 3 °C, MAP: 1097 mm) in Austria and
a second at Matsch Valley (MAT: 6.6 °C, MAP: 527 mm) in Italy. We estimated C
input and decomposition rates of water-floatable and free particulate
organic matter (wPOM, fPOM <1.6 g cm−3) and
aggregate-occluded particulate and mineral-associated organic matter (oPOM
<1.6 g cm−3, mOM >1.6 g cm−3) using bomb radiocarbon.
In mountain grasslands average C turnover increased from roots (3 yr) < wPOM (5 yr) < fPOM (80 yr) < oPOM (108 yr) < mOM
(192 yr). Among SOM fractions the turnover of fPOM-C varied most in relation to management. Along both land-use gradients C input pathways shifted from root-derived
towards litter-derived C. The C input rates of both wPOM-C and fPOM-C were affected by land management at both sites. In contrast, oPOM-C and mOM-C dynamics
remained relatively stable in response to grassland abandonment. Carbon accumulation rates of free POM decreased strongly with time since LUC (10, 25 and 36 yr).
For wPOM-C, for example, it decreased from 7.4 > 2.2> 0.8 g C m−2 yr−1. At both sites, most C was sequestered in the first years after
LUC and free POM reached new steady state within 20–40 yr.
We conclude that w-and fPOM-C vs. oPOM-C dynamics respond differently to
grassland management change and thus POM does not represent a homogeneous SOM
fraction. Sequestered C is stored in the labile POM and not stabilized in the long-term.
Thus, it is unlikely that
abandonment, the dominant form of LUC in the European Alps, provides a
substantial net soil C sink. |
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