Cited by 148Soil Carbon and Nitrogen DynamicsSoil erosion and sediment transportSoil Geostatistics and Mapping

Storage and turnover of carbon in grassland soils along an elevation gradient in the Swiss Alps

LEIFELD, JENS, ZIMMERMANN, MICHAEL, FUHRER, JÜRG, CONEN, FRANZ·2009·Global Change Biology

Abstract

Amount, composition, and rate of turnover of soil organic carbon (SOC) in mountainous cold regions is largely unknown, making predictions of future responses of this carbon (C) to changing environmental conditions uncertain. We hypothesized increasing amounts and declining turnover times of soil organic matter (SOM) under permanent grassland with increasing elevation and decreasing temperature. Samples from an irrigated transect in the Swiss Alps (880 to 2200 m elevation, mean annual temperatures +8.9 to +0.9 °C) were analyzed. Soil C stocks ranged from 49 to 96 t C ha −1 (0–20 cm) and were not related to elevation, though the highest site stored least C. Particulate organic carbon (POC) increased significantly with elevation and accounted for > 80% of the total soil C at 2200 m (0–5 cm). Mean residence times (MRTs) of POC computed by means of radiocarbon dating were in the order of years to decades and were positively related to elevation in the topsoil. At higher elevations, the estimated total C flux through the soil profile mainly depended on this fraction. MRT of mineral‐associated matter ranged from decades to centuries and was not systematically related to elevation, but positively related to the soil mineral surface area and it increased with soil depth. Turnover rates from simulations with the soil C model RothC exceeded those from 14 C measurements by a factor of 1.7–3.3 which suggests that C dynamics at these sites is overestimated by the model. Size of model pools and amount of C in soil fractions were only weakly correlated, thereby challenging previously postulated hypotheses concerning the correspondence of pools and fractions for grasslands at higher elevations.

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Crossref · 10.1111/j.1365-2486.2008.01782.x

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  • Simulations were greatly improved when decomposition rates were calibrated using labelled C measurements and applied to experimental evidence for poplar litter.

    “Simulations were greatly improved when decomposition rates were calibrated using labelled C measurements [173–175] and applied to the experimental evidence presented for poplar litter [78, 109].”

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Authors
LEIFELD, J., ZIMMERMANN, M., FUHRER, J., & CONEN, F.
Affiliations
  • Agroscope (CH)
  • University of Edinburgh (GB)
  • University of Basel (CH)
Corresponding author
LEIFELD, JENS
Venue
Global Change Biology
Publisher
Wiley
Published
2009-02-06
Volume
15
Issue
3
Pages
668-679
ISSN
  • 1354-1013 (ISSN-L)
  • 1365-2486
OpenAlex
W2139449145
Cited by
148
References
40
Citations by year
2026: 9 · 2025: 16 · 2024: 21 · 2023: 13 · 2022: 8 · 2021: 8 · 2020: 6 · 2019: 8 · 2018: 4 · 2017: 8 · 2016: 6 · 2015: 7 · 2014: 4 · 2013: 9 · 2012: 5
FWCI
8.12
Type
journal article
Language
en
Open access
closed
Locations
  • Global Change Biology (publishedVersion)
  • ResearchOnline - JCU (James Cook University) (submittedVersion)
Funders
Bundesamt für Umwelt
Topics
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil erosion and sediment transport
  • Physical Sciences › Environmental Science › Environmental Engineering › Soil Geostatistics and Mapping
Keywords
soil organic carbon, carbon turnover, elevation gradient, permanent grassland, particulate organic carbon, mean residence time, radiocarbon dating, mineral-associated organic matter, soil carbon stocks, soil carbon flux, RothC model, Swiss Alps

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