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Bacteria and fungi also break down woody tissues, stems, leaves and dead roots, turning them into nutrients for somebody in the soil.
Live and dead roots were distinguished according to Vogt and Perrson (1991).
Dead roots are an important stock to account for in productive below-ground ecosystems.
Only live roots were measured; dead roots were removed and discarded.
Dead organic matter in a forested ecosystem refers to non-living biomass including deadwood, litter, and root necromass (dead roots).
However, an accounting for decomposition of dead biomass, dead roots and irrigation can significantly increase the share of carbon emissions.
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Below ground stocks include: dead root, upper peat and deep peat.
(3) The model simulates the spatiotemporal dynamics of live root, dead root, live shoot, standing dead, and litter biomass and nutrients of individual plants.
The C stock types that have been identified and modeled for this application include: live wood, live leaf, live root, deadwood, leaf litter, dead root, and soil (peat).
They speculated that the main source of N2O emissions from soils planted with N2-fixing legumes during the vegetation period may be attributable to the N release from root exudates and/or from the decomposition of dead root residues.
An experiment with 32 1·0-m2plots, 16 with a previous Larrea tridentata (creosotebush) plant and 16 without, was designed to investigate the influence of dead root systems on the downward movement of water and chemical tracers in a Mojave Desert soil.
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