The aim of our study was to identify interactions between the decomposition of aboveground litter and rhizosphere activity. The experimental approach combined the placement of labelled litter (δ13C=-37.9‰) with forest girdling in a 35-year-old Norway spruce stand, resulting in four different treatment combinations: GL (girdled, litter), GNL (girdled, no litter), NGL (not girdled, litter), and NGNL (not girdled, no litter). Monthly sampling of soil CO2 efflux and δ13C of soil respired CO2 between May and October 2002 allowed the partitioning of the flux into that derived from the labelled litter, and that derived from native soil organic matter and roots. The effect of forest girdling on soil CO2 efflux was detectable from June (girdling too...
The rhizosphere priming effect (RPE) is increasingly being considered to be an important regulator o...
The DIRT Experiment (Detritus Input and Removal Treatments) is a long-term study of controls on soil...
<p>1. Quantifying pathways and temporal dynamics of carbon (C) flux between plants and soil is...
The aim of our study was to identify interactions between the decomposition of aboveground litter an...
The aim of our study was to identify interactions between the decomposition of aboveground litter an...
The aim of our study was to identify interactions between the decomposition of aboveground litter an...
The aim of our study was to identify interactions between the decomposition of aboveground litter an...
The widespread use of forest litter as annual bedding in central Europe for many, centuries gave ris...
Background and aims: We determined the relationship between site N supply and decomposition rates wi...
1. Quantifying pathways and temporal dynamics of carbon (C) flux between plants and soil is critical...
1. Quantifying pathways and temporal dynamics of carbon (C) flux between plants and soil is critical...
The widespread use of forest litter as annual bedding in central Europe for many, centuries gave ris...
The stimulation of vegetation productivity in response to rising atmospheric CO 2 concentrations can...
There is a growing but inconclusive body of work on effects of litter-mixing on ecological processes...
Leaf and fine root litter decomposition is central to biogeochemical cycles in northern forest. I st...
The rhizosphere priming effect (RPE) is increasingly being considered to be an important regulator o...
The DIRT Experiment (Detritus Input and Removal Treatments) is a long-term study of controls on soil...
<p>1. Quantifying pathways and temporal dynamics of carbon (C) flux between plants and soil is...
The aim of our study was to identify interactions between the decomposition of aboveground litter an...
The aim of our study was to identify interactions between the decomposition of aboveground litter an...
The aim of our study was to identify interactions between the decomposition of aboveground litter an...
The aim of our study was to identify interactions between the decomposition of aboveground litter an...
The widespread use of forest litter as annual bedding in central Europe for many, centuries gave ris...
Background and aims: We determined the relationship between site N supply and decomposition rates wi...
1. Quantifying pathways and temporal dynamics of carbon (C) flux between plants and soil is critical...
1. Quantifying pathways and temporal dynamics of carbon (C) flux between plants and soil is critical...
The widespread use of forest litter as annual bedding in central Europe for many, centuries gave ris...
The stimulation of vegetation productivity in response to rising atmospheric CO 2 concentrations can...
There is a growing but inconclusive body of work on effects of litter-mixing on ecological processes...
Leaf and fine root litter decomposition is central to biogeochemical cycles in northern forest. I st...
The rhizosphere priming effect (RPE) is increasingly being considered to be an important regulator o...
The DIRT Experiment (Detritus Input and Removal Treatments) is a long-term study of controls on soil...
<p>1. Quantifying pathways and temporal dynamics of carbon (C) flux between plants and soil is...