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
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
To follow the survival of an introduced bacteria in the contaminated soil, TBPZ was transformed with a plasmid carrying a gene for kanamycin resistance and the lux CDABE operon from
We found that horizontal spatial variation in potential nitrate production, leaching of nitrate and nitrogen concentrations from non-pooled ®eld samples was higher than variation
We initiated a laboratory study to directly assess the in¯uence of soil organic matter content on potential nitrogen immobilization and turnover for soils collected from across
Microbial respiration of sieved forest ¯oor samples (i.e. respir- ation of soils without ®ne roots) collected in 1995 was signi®cantly greater in the hardwood control than the
