Peat decomposability in managed organic soils in relation to land use, organic matter composition and temperature

Organic soils comprise a large yet fragile carbon (C) store in the global C cycle. Drainage, necessary for agriculture and forestry, triggers rapid decomposition of soil organic matter (SOM), typically increasing in the order forest 

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Bibliographic Details
Published in:Biogeosciences 2018-02, Vol.15 (3), p.703-719
Main Authors: Bader, Cédric, Müller, Moritz, Schulin, Rainer, Leifeld, Jens
Format: Article
Language:English
Subjects:
Accumulation
Agricultural land
Agricultural management
Agriculture
Analysis
Bulk density
Carbon
Carbon dioxide
Carbon dioxide emissions
Carbon dioxide flux
Climate change
Composition
Controlled conditions
Correlation analysis
Crop residues
Decomposition
Emissions
Field tests
Fluxes
Forest soils
Forestry
Forests
Grasslands
Hydrology
Incubation period
Land use
Land use management
Mineralization
Moisture content
Organic carbon
Organic matter
Organic soils
Peat
Peatlands
Pollution monitoring
Polyphenols
Ratios
Soil
Soil characteristics
Soil density
Soil management
Soil organic matter
Soil temperature
Soil water
Soil water composition
Soils
Temperature
Topsoil
Weather
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Description
Summary:Organic soils comprise a large yet fragile carbon (C) store in the global C cycle. Drainage, necessary for agriculture and forestry, triggers rapid decomposition of soil organic matter (SOM), typically increasing in the order forest 
ISSN:1726-4189
1726-4170
1726-4189
DOI:10.5194/bg-15-703-2018