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Soil-associated ecosystem functions (e.g., erosion control, microbial activity) were strongly related to environmental plot conditions and the species richness of belowground organisms.
The two-dimensional distribution of flow patterns and their dynamic change due to microbial activity were investigated in naturally fractured chalk cores.
Results obtained in both 2001 and 2002 showed that microbial biomass and microbial activity were generally higher in organically than conventionally managed soils with CGT being most effective.
Organo-mineral associations from these hot spots of microbial activity were recovered from plant residues (free particulate organic matter, fPOM) as fine grained mineral fraction with a typically low C/N ratio.
In contrast to previous studies, we found that these metrics of microbial activity were not consistently stimulated by N additions; rather, added N was primarily immobilized by microbes resulting in decreased chloroform-labile C N ratios.
In the same way, the nutrient concentrations were very different in each species, as a result of the different patterns of foliar nutrient resorption: both nutrient concentrations and microbial activity were higher in the Qd litter than in the Qc litter.
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Microbial activity was measured as basal respiration.
Microbial activity was increased in M. scabrinodis mounds only.
A reliable and sensitive proxy for microbial activity is activity of extracellular enzymes (EEA).
Soil microbial activity was inhibited or not with sodium azide (NaN3).
Spatial patterns of soil microbial activity are central to understanding greenhouse gas dynamics in wetlands.
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