Directory UMM :Data Elmu:jurnal:S:Soil Biology And Chemistry:Vol32.Issue6.Jun2000:
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Our objective was to analyze the organic C content and stable C isotope ( 13 C) composition of whole soil and water soluble and microbial biomass fractions to determine the source
Carbon mineralization from whole soil (WS), soil plus heavy fraction (S+HF) and soil plus light fraction (S+LF) mixtures of dis- turbed (white bars) and minimally-disturbed (black
The uptake rates of methane in the uppermost layer of soil core samples from OFD1 and OFD2 were larger than those of the subsurface layer, and the largest consumption was observed
We hypothesized that manure-derived organic matter ®rst enters the soil primarily as particulate material, and during decomposition is transformed within the macro- aggregate
Dierences in catabolic evenness between pasture and other land-uses on matched soils were related to dierences in organic C pools (total organic C, microbial biomass C,
In general, plant material and to a lesser extent soil compaction influenced the dynamic processes in the soil affecting microbial activity and water stable aggregation. Higher
Measured and model-predicted average levels of microbial biomass C concentration and extracellular enzyme activity in soils with cereal rotation, with low-OM and high-OM organic
Measured and model-predicted average levels of microbial biomass C concentration and extracellular enzyme activity in soils with cereal rotation, with low-OM and high-OM organic
