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Microbial mobilization and immobilization of soil nitrogen

Åt var och en efter behov - mikrobiell produktion och konsumption av oorganiskt kväve
Författare:
Publiceringsår: 2004
Språk: Engelska
Sidor: 104
Dokumenttyp: Doktorsavhandling
Förlag: Per Bengtson, Ekologihuset, 223 62 Lund,
Additional info: Article: I. Bengtsson, G., Bengtson, P., and Månsson, K.F. 2003. Gross nitrogen mineralization-, immobilization-, and nitrification rates as a function of soil C/N ratio and microbial activity. Soil Biology and Biochemistry 35, 143-154. Article: II. Bengtson, P., Bengtsson, G., and Falkengren-Grerup, U. Relieving substrate limitation – soil moisture and temperature determine gross N transformation rates. (Submitted) Article: III. Bengtson, P., Falkengren-Grerup, U., and Bengtsson, G. Spatial distribution of gross N transformation rates and plants – A reciprocal relationship. (Submitted) Article: IV. Månsson, K.F., Bengtson, P., Bengtsson, G., and Falkengren-Grerup, U. Competition for nitrogen – litter leachate favours microorganisms at the expense of plants. (Manuscript) Article: V. Bengtson, P. and Bengtsson, G. Rapid turnover of DOC in temperate forest soils accounts for increased CO2 production at elevated temperature. (Manuscript) Article: VI. Bengtson, P. and Bengtsson, G. Bacterial immobilization and remineralization of N at different growth rates and N concentrations. (Manuscript)

Sammanfattning

Microorganisms in forest ecosystems normally recycle nitrogen (N), such that gaseous losses and leaching are limited. Mobilization of organic N, including microbial N, and immobilization of inorganic N, especially NH4+, are the quantitatively most important N transformation processes. Various factors influence their rates, e.g. the amount of carbon and nitrogen, temperature, moisture, and the microbial biomass and activity. The factors are adressed in the thesis with the ambition to suggest mechanistic explanations for their influence on nitrogen mobilization and immobilization rates.

The mineralization and immobilization rates are not dependent on the concentration of carbon or nitrogen per se, but rather on the microbial biomass and its activity. This may invalidate the use of first order kinetics to describe mobilization and immobilization rates. Earlier claims that mineralization and immobilization rates are dependent on the concentration of carbon and nitrogen may have overseen the dependence of the microbial biomass on the soil organic matter content. Moisture, temperature, and the quality of the utilized organic matter appear to determine the activity of the microorganisms.

Mobilization of microbially bound N seem to occur mainly as a result of predation and drying-rewetting cycles, since microorganisms have an efficient intracellular recycling of nitrogen, especially at low ammonium concentrations. Thus, mobilization and remineralization of microbial nitrogen by other processes than predation and drying-rewetting cycles is likely to occur only when conditions promote high growth rates, i.e. when microorganisms are not substrate limited and temperature and moisture conditions are favourable.

The main factors determining microbial mobilization and immobilization of soil N are therefore the size of the microbial biomass, its activity, and the quality of the growth substrate. Those three factors in turn seem to be dependent on soil SOM content, predation, drying-rewetting cycles, temperature, and soil water content.

Disputation

2004-06-04
10:15
Blå Hallen, Ecology Building
  • Stephen C Hart

Nyckelord

  • Earth and Environmental Sciences
  • Ecology
  • Ekologi
  • growth rate
  • microbial activity
  • respiration
  • assimilation
  • immobilization
  • Nitrogen
  • mineralization

Övriga

  • Microbial Ecology
  • ISBN: 91-7105-210-0
  • ISRN: SE-LUNDBDS/NBKE-04/1034+104pp

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