Directory UMM :Data Elmu:jurnal:S:Soil Biology And Chemistry:Vol32.Issue7.Jul2000:
Teks penuh
Dokumen terkait
We compared methane oxidation activity in laboratory incubations of samples from a podzolic soil pro®le to the microbial community structure of the soil, determined as the content
There are indications that an underlying process may be microorganisms which produce reactive chlorine that chemically degrades organic matter and facilitates degradation
For this, we ®tted two dierent temperature response func- tions to the laboratory incubation data, incorporated them into a simple carbon balance model (AndreÂn and KaÈtterer,
®eld soil slurry upon incubation under anoxic conditions: on the reduction of the electron acceptors nitrate, ferric iron, sulfate; on the production of CH 4 and CO 2 ; on the
Three intact soil cores (15 cm diameter) were col- lected on 21 May 1998 in PVC piping (25 cm deep) from each site; three additional soil samples from the H and mineral horizon
leguminosarum biovar viciae WSM710 grows rapidly on either glucose or fumarate as sole carbon source, but more slowly with histidine (Table 1).. Both pH values are above
If ergosterol is shown to be, and used as, an index of fungal area, and if sampling strategies are changed to minimise patchi- ness (the ``pedon'' used to obtain each replicate
sequently, ten adult worms ( Eisenia fetida ) were added to the pre-treated mixtures of aerobic and anaerobic sewage sludges, having a content of dry matter of about 40%; 0.5 kg (as
