Directory UMM :Data Elmu:jurnal:S:Soil Biology And Chemistry:Vol32.Issue11-12.oct2000:
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These factors were: global fungal micro¯ora, the fungi producing phenoloxidases (PO + ), the activities of several phenoloxidases, hydrosoluble phenols, and temperature, humidity and
Unfortunately, nodule occupancy by the inoculated strains could not be studied by serol- ogy in the ®eld experiments, because of cross reactions among some of the strains used in
While the nitri®cation rates were very close for both soils at low water potentials, the partial pressures of acetylene required to inhibit nitri®cation were dier- ent (Table 1)..
The measurements of water content most often used by soil microbiologists are gravimetric water content ( W g), volumetric water content ( W v), percentage of water holding
results were reported from a temperate deciduous for- est (Edwards and Sollins, 1973) (>60% of total soil respiration originated from deeper mineral horizons) and boreal Canadian
Mechanisms for and causes of positive real priming eects for carbon (C) and nitrogen (N), caused by addition of dierent substances (PE=priming eect; MO=microorganisms;
The most rapid rates of degradation were observed in the inoculated Soakwaters (soil 4, Table 1) and Sheep Pens (soil 2, Table 1) samples whose organic matter contents were 0.3
Methane emission rates at dierent time points during the vegetation of rice microcosms consisting of one rice plant each in a planting pot containing 1 kg rice soil.. Black
