ISSN:
1432-0789
Keywords:
Rhizosphere
;
Bacterial counts
;
Microbial biomass
;
N immobilization
;
Soil organic N
Source:
Springer Online Journal Archives 1860-2000
Topics:
Biology
,
Geosciences
,
Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
Notes:
Summary The effect of roots on microbial growth and N immobilization was investigated in a pot experiment with barley, Italian ryegrass, and white clover. We used a silty subsoil with a low soil organic matter content (0.16%C and 0.012%N), which allowed us to measure N immobilization as an increase in total soil organic N (planted versus unplanted). At sampling, the soil was easily removed from intact roots by gentle washing, with a negligible loss of root material. Plant growth and extra mineral N (in planted soil only) gave increased total counts (fluorescence microscopy) and viable counts (plate dilution) of bacteria, a higher proportion of larger cells, and increased viable counts as a percentage of total counts. Under monocots, 12–17% of the added fertilizer N was recovered as soil organic N. Although this N immobilization was attributed to microbial assimilation, less than 1/4 was actually recovered as microbial biomass N, as measured with the chloroform fumigation/N-extraction method or calculated from total bacterial counts. The white clover accumulated substantial amounts of N due to N2 fixation. However, microbial N immobilization represented only 3% of the total N accumulation, showing that the microorganisms obtained a smaller share of biologically fixed N2 than of the N applied as fertilizer. Extra additions of mineral N (monocots) enhanced microbial N assimilation, partly due to increased plant growth. The results also strongly indicated, however, that the microbial growth under monocots was N-limited in the latter part of the experiment and that fertilizer N had a direct effect on microbial growth. In the early phase of plant growth, N immobilization ranged from 33 to 58 mg N g-1 root C. This level of immobilization required a release of organic C into the soil representing a minimum of 60–100% of that found in intact roots.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/BF00341493
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