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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

For Wuxi soil, NH 4 Cl addition increased the mean CO 2 evolution rate in the ®rst incubation period ( P < 0.01) and the e€ect disappeared in the subsequent in- cubations+.

Our goal was to use chemical fractionation and carbohydrate analysis of the fractions (i) to determine quantitative and qualitative changes in soil organic matter following

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

The number of fast-growing total bacteria (a) and protozoa (b) around decomposing roots in soil microcosms with di€erent con- centrations of fenpropimorph: (a) Culturable bacteria

Although only a limited suite of ECM fungi has so far been investigated, it is clear that they produce (see later) a range of enzymatic activities similar to wood- rotting fungi,

Methane emission rates at di€erent time points during the vegetation of rice microcosms consisting of one rice plant each in a planting pot containing 1 kg rice soil.. Black