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1.
Summary The influence of total nitrification to nitrate or partial nitrification to nitrite on the soil organic nitrogen status was examined. NH
4
+
–15N was added to the soil in the absence and the presence of NaClO3, respectively nitrapyrin. The first chemical inhibits only nitrate formation, the second inhibits total nitrification. The accumulation of nitrite nitrogen in the soil at levels up to 5 mg kg–1 increased the loss of nitrogen. Yet, it did not increase the binding of mineral nitrogen into soil organic matter, relative to the control soil. The data suggest that the biochemistry of the nitrite formation process, rather than the levels of nitrite ions formed, are of primary importance in the role of nitrification mediated nitrosation of soil organic matter. 相似文献
2.
A strategy for high cell density culture of heterotrophic microalgae with inhibitory substrates 总被引:5,自引:0,他引:5
Substrate inhibition is one of the major problems preventing high cell densities of microalgae in heterotrophic culture, so
the possibility of overcoming the problem by various culture techniques was examined. It was found that perfusion culture
may be the most appropriate technique for high cell densities in heterotrophic culture using inhibitory substrates. An experimental
example in which a hollow fibre cell recycle system (HFCRS) was employed to achieve high cell densities of Chlamydomonas reinhardtii on acetate under heterotrophic conditions of growth was demonstrated. The cell density in the HFCRS was much higher than
that reported in the literature for this species. 相似文献
3.
The N2O flux from the surface of grass-covered pots was only significant following grass maturing. Removal of the above-ground plant
material resulted in an immediate and long-lasting increase in N2O production in the soil. The results suggest that easily available organic matter from the roots stimulates the denitrification
when the plants are damaged. Grass cutting might therefore result in a marked nitrogen loss through denitrification. The quantitative
effect was equal in soil with and without succinate added. The size of the anaerobic zone around the roots is therefore sufficient
to allow for denitrification activity mediated by increased organic matter availability because of plant cutting. 相似文献
4.
Effect of simulated forest fire on the availability of N and P in mediterranean soils 总被引:4,自引:0,他引:4
The effect of soil burning on N and P availability and on mineralization and nitrification rates of N in the burned mineral
soil was studied by combustion of soils in the laboratory.
At a fire temperature of 600°C, there was a complete volatilization of NH4 and a significant increase of pH, from 7.6 in the unburned soil to 11.7 in the burned soil. Under such conditions ammonification
and nitrification reactions were inhibited. Less available P was produced immediately after the fire at 600°C, as compared
to P amount produced at 250°C. Burning the soils with plants caused a decrease in NH4-N and (NO2+NO3)-N concentrations in the soil as well as a reduction in ammonification and nitrification rates. Combustion of soil with plants
contributed additional available P to the burned soil.
The existence of a non-burned soil under the burned one played an important role in triggering ammonification and nitrification
reactions. 相似文献
5.
Soil N mineralization and nitrification in relation to nitrogen solution chemistry in a small forested watershed 总被引:6,自引:1,他引:5
Spatial variations in soil processes regulating mineral N losses to streams were studied in a small watershed near Toronto, Ontario. Annual net N mineralization in the 0–8 cm soil was measured in adjacent upland and riparian forest stands using in situ soil incubations from April 1985 to 1987. Mean annual rates of soil N mineralization and nitrification were higher in a maple soil (93.8 and 87.0 kg.ha–1) than in a pine soil (23.3 and 8.2 kg.ha–1 ). Very low mean rates of mineralization (3.3 kg.ha–1) and nitrification (3.4 kg.ha–1) were found in a riparian hemlock stand. Average NO3-N concentrations in soil solutions were 0.3–1.0 mg.L–1 in the maple stand and >0.06mg.L–1 in the pine stand. Concentrations of NO3–N in shallow ground water and stream water were 3–4× greater in a maple subwatershed than in a pine subwatershed. Rapid N uptake by vegetation was an important mechanism reducing solution losses of NO3–N in the maple stand. Low rates of nitrification were mainly responsible for negligible NO3–N solution losses in the pine stand. 相似文献
6.
Citrobacter freundii, Paracoccus denitrificans and Pseudomonas stutzeri were grown either singly or in mixed culture in anaerobic nitrate or nitrite limited chemostats with formate and/or succinate as electron donors and carbon sources. C. freundii reduced nitrate or nitrite stoichiometrically to ammonia. Maximum molar growth yields for nitrate (nitrite) were 15.3 (9.9) g/mol for C. freundii on formate with succinate as carbon source, 15.3 (9.5) g/mol for Ps. stutzeri on succinate and 32.3 (20.4) g/mol for Pa. denitrificans on succinate. The almost identical growth yields indicate that the ATP output of the anaerobic processes in the nitrate (nitrite) ammonifying organism and Ps. stutzeri are nearly the same. In mixed cultures with either Ps. stutzeri or Pa. denitrificans, C. freundii was the best competitor for nitrate. These results show that in anaerobic environments C. freundii may compete successfully with denitrifying organisms. 相似文献
7.
Mineralization of trace levels of [14C]-phenol by heterotrophic microorganisms was quantified at 4 sites along a river continuum in southwestern Virginia. Significant phenol mineralization rates were detected in surface sediment and seston samples at all sites from August 1985 through May 1986. Phenol degradation was strongly affected by season (ANOVA; P < 0.0001). From a baseline rate in August (range: 1.19 × 10-5 to 897 × 10-4 mg phenol mineralized mg AFDW-1 h-1) phenol mineralization rose to a yearly maximum in October (range: 1.21 × 10-4 to 1.16 × 10-3 mg phenol mineralized mg AFDW-1 h-1) despite decreasing stream temperatures. This autumnal peak in phenol degradation was attributed to the pulsed input of allochthonous detritus, especially leaf litter, which contains substantial quantities of phenols and related compounds. Although phenol mineralization was significant in these streams, phenols were metabolized at much slower rates than more labile compounds present in the dissolved organic matter (DOM) pool. Estimates of turnover rates for three major components of DOM revealed that glucose and glutamate turnover rates (0.064–0.140 h-1 mg sediment AFDW-1 and 0.140–0.610 h-1 mg sediment AFDW-1, respectively) were, respectively, 2.2–4.7 × and 9.6–16.9 × greater than phenol turnover rates (0.015–0.064 h-1 mg sediment AFDW-1). Although the relatively low rates of utilization of refractory phenolic materials suggest that these compounds may accumulate and become more prevalent components of the DOM pool, phenol concentrations at the 4 study sites remained below detectable levels (i.e., < 1 g 1-1) throughout the study. Consequently, it seems that although phenolic materials are metabolized more slowly than labile DOM, phenols are degraded at rates which preclude accumulation in the water column. 相似文献
8.
M. R. Tredici M. C. Margheri L. Giovannetti R. de Philippis M. Vincenzini 《Plant and Soil》1988,110(2):199-206
The cyanobiont ofCycas circinalis (identified asNostoc sp.) was isolated and its heterotrophic metabolism was studied in free culture under nitrogen-fixing conditions. Morphology, growth rate, nitrogenase activity, biochemical composition, efficiency of assimilation of organic carbon and molecular nitrogen were determined under different conditions of energy and carbon supply. The study has revealed the high potential of the heterotrophic metabolism in this symbiotic cyanobacterium. Although low rates of metabolic activities were attained under heterotrophic conditions, the efficiencies of organic carbon utilization (0.48 g cell-carbon per g glucose-carbon in chemoheterotrophy, from 0.65 to 0.74 under photoheterotrophy) and of N2 assimilation (35.0 mg N2 fixed per g glucose used in chemoheterotrophy, from 58.3 to 61.9 under photoheterotrophy) displayed by this organism were among the highest ever found in diazotrophically grown microorganisms. The isolate fromC. circinalis was able to grow indefinitely in the dark under nitrogen-fixing conditions, maintaining a well balanced biosynthetic activity and the capacity to resume photosynthetic metabolism quickly. The significance of the heterotrophic potential of this symbioticNostoc is discussed. 相似文献
9.
A. J. M. Stams H. W. G. Booltink I. J. Lutke-Schipholt B. Beemsterboer J. R. W. Woittiez N. van Breemen 《Biogeochemistry》1991,13(3):241-255
To demonstrate the contribution of atmospheric ammonium to soil acidification in acid forest soils, a field study with13N-ammonium as tracer was performed in an oak-birch forest soil. Monitoring and analysis of soil solutions from various depths on the13N-ammonium and15N-nitrate contents, showed that about 54% of the applied15N-ammonium was oxidized to nitrate in the forest floor. Over a period of one year about 20% of the15N remained as organic nitrogen in this layer. The percentage15N enrichment in ammonium and nitrate were in the same range in all the forest floor percolates, indicating that even in extremely acid forest soils (pH < 4) nitrate formation from ammonium can occur. Clearly, atmospheric ammonium can contribute to soil acidification even at low soil pH. 相似文献
10.
Balamani Bezbaruah 《Journal of biosciences》1983,5(3):267-278
Nitrification following ureolysis in soil samples from tea growing soils (pH 4.5–5.5) was found to be chiefly due to the activity
of heterotrophic bacteria belonging to generaBacillus, Arthrobacter, Sporosarcina, Micrococcus, Clostridium, Pseudomonas andProteus. A correlation between the intensity of ureolytic activity of organisms in a given soil sample and the yield levels of tea
was observed. In culture media the increase in the quantity of NH
4
+
-N indicating ureolysis was not accompanied by proportional increase in biomass. Ureolysis and nitrification in sterile soil
sample inoculated with the isolates improved through amendment of organic carbon to the soil. 相似文献