Experimental Examination on Nitrous Oxide Accumulation during Nitrification in a Freshwater Lake
The N2O production during nitrification was studied in Lake Kizaki by vertical observations and two incubation experiments. The apparent N2O production (ΔN2O), the difference between observed and atmospheric-equilibrium concentration, was highly correlated with apparent oxygen consumption (-ΔO2), in...
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Published in | Japanese Journal of Limnology (Rikusuigaku Zasshi) Vol. 51; no. 4; pp. 237 - 248 |
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Format | Journal Article |
Language | English |
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The Japanese Society of Limnology
01.01.1990
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ISSN | 0021-5104 1882-4897 |
DOI | 10.3739/rikusui.51.237 |
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Abstract | The N2O production during nitrification was studied in Lake Kizaki by vertical observations and two incubation experiments. The apparent N2O production (ΔN2O), the difference between observed and atmospheric-equilibrium concentration, was highly correlated with apparent oxygen consumption (-ΔO2), in situ NO3- concentration and the amount of NH4+ decrease with time, indicating that N2O was produced by the nitrification process. In a long-term in situ incubation, simultaneous accumulations of NO3- and N2O were observed, the amounts of which were comparable to the in situ changes, suggesting their in situ productions. Both NO3- and N2O productions were greatly enhanced by an NH4+ enrichment after the emergence of nitrification activity. From both vertical observations and long-term in situ incubations, the yield of N2O relative to NO3- production was estimated to be about 0.1% during the active nitrification period. But thereafter, the obtained yields were appreciably higher. Another incubation experiment also showed that N2O production was delayed several days compared to NO3- production, indicating that N2O production was accelerated in the late phase of nitrification. The physiological state of nitrifiers was suggested to be of some importance for such phenomena. Nitrapyrin, a specific inhibitor of nitrification, was found not to be very effective for N2O formations in contrast with NO3- productions completely inhibited, suggesting a possibility of some N2O sources other than autotrophic nitrification. |
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AbstractList | The N2O production during nitrification was studied in Lake Kizaki by vertical observations and two incubation experiments. The apparent N2O production (ΔN2O), the difference between observed and atmospheric-equilibrium concentration, was highly correlated with apparent oxygen consumption (-ΔO2), in situ NO3- concentration and the amount of NH4+ decrease with time, indicating that N2O was produced by the nitrification process. In a long-term in situ incubation, simultaneous accumulations of NO3- and N2O were observed, the amounts of which were comparable to the in situ changes, suggesting their in situ productions. Both NO3- and N2O productions were greatly enhanced by an NH4+ enrichment after the emergence of nitrification activity. From both vertical observations and long-term in situ incubations, the yield of N2O relative to NO3- production was estimated to be about 0.1% during the active nitrification period. But thereafter, the obtained yields were appreciably higher. Another incubation experiment also showed that N2O production was delayed several days compared to NO3- production, indicating that N2O production was accelerated in the late phase of nitrification. The physiological state of nitrifiers was suggested to be of some importance for such phenomena. Nitrapyrin, a specific inhibitor of nitrification, was found not to be very effective for N2O formations in contrast with NO3- productions completely inhibited, suggesting a possibility of some N2O sources other than autotrophic nitrification. Nitrous oxide production during nitrification in a freshwater lake was verified from the close correlations of apparent N sub(2)O production Delta N sub(2)O) against apparent oxygen consumption (- Delta O sub(2)), in situ NO sub(3) super(-) concentration and NH sub(4) super(+) decrease with time, and from the stimulation by NH sub(4) super(+) and the inhibition by nitrapyrin of N sub(2)O production during lake water incubations. The N sub(2)O yield relative to NO sub(3) super(-) production was about 0.1% during the active nitrification period. But thereafter, N sub(2)O production continued with higher yields, due presumably to physiological change of nitrifiers. |
Author | YOH, Muneoki |
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References_xml | – reference: SAGI, T. (1966) : Determination of ammonia in sea water by the indophenol method and its application to the coastal and offshore waters. Oceanogrl. Mag., 18 : 43-51. – reference: YOSHIDA, N., H. MORIMOTO, M. HIRANO, I. KOIKE, S. MATSUO, E. WADA, T. SAINO and A. HATTORI (1989) : Nitrification rates and 15N abundances of N2O and NO3- in the western North Pacific. Nature, 342 : 895-897. – reference: YOSHIDA, T. and M. ALEXANDER (1970) : Nitrous oxide formation by Nitrosomonas europaea and heterotrophic microorganisms. Soil Sci. Soc. Amer. Proc., 34 : 880-882. – reference: BREMNER, J. M. and A. M. BLACKMER (1978) : Nitrous oxide : emission from soils during nitrification of feritilizer nitrogen. Science, 199 : 295-296. – reference: BLACKMER, A. M., J. M. BREMNER and E. L. SCHMIDT (1980) : Production of nitrous oxide by ammonia-oxidizing chemoautotrophic microorganisms in soil. Appl. Environ. Microbiol., 40 : 1060-1066. – reference: TAKAHASHI, M., T. Y0SHI0KA and Y. SAIJ0 (1982) : Nitrogen metabolism in Lake Kizaki, Japan. III. Active nitrification in early summer. Arch. Hydrobiol., 93 : 272-286. – reference: MCCARTHY, J. J., W. KAPLAN and J. L. NEVINS (1984) : Chesapeake Bay nutrient and plankton dynamics. 2. Sources and sinks of nitrite. Limnol. Oceanogr., 29 : 84-98. – reference: HAHN, J. (1981) : Nitrous oxide in the oceans, p. 191- 240. In C. C. Delwiche (ed.), Denitrification, Nitrification, and Atmospheric Nitrous Oxide, 10. John Wiley & Sons. – reference: YOH, M., H. Terai and Y. SAIJ0 (1988a) : A preliminary study on N2O production through nitrification in Lake Kizaki. Jpn. J. Limnol., 49 : 43-46. – reference: CLINE, J. D., D. P. WISEGARVER and K. KELLYHANSEN (1987) Nitrous oxide and vertical mixing in the equatorial Pacific during the 1982-1983 El Nino. Deep - Sea Res., 34 : 857-873. – reference: COHEN, Y. and L. I. GORDON (1979) : Nitrous oxide production in the ocean. J. Geophys. Res., 84 ; 347-353. – reference: GOODROAD, L. L. and D. R. KEENEY (1984) : Nitrous oxide production in aerobic soils under varying pH, temperature and water content. Soil Biol. Biochem., 16 : 39-43. – reference: YOSHINARI, T. (1976) : Nitrous oxide in the sea. Mar. Chem., 4 : 189-202. – reference: GOREAU, T. J., W. A. KAPLAN, S. C. WOFSY, M. B. M C ELROY, F. W. VALOIS and S. W. WATSON (1980) : Production of NO2- and N2O by nitrifying bacteria at reduced concentrations of oxygen. Appl. Environ. Microbiol., 40 : 526-532. – reference: Technicon Industrial Method (1972) : Nitrate and nitrite in water and seawater. Method No.158-71W/A. – reference: COHEN, Y. and L. I. GORDON (1978) : Nitrous oxide in the oxygen minimum of the eastern tropical North Pacific : evidence for its consumption during denitrification and possible mechanisms for its production. Deep Sea Res., 25 : 509-524. – reference: Y0SHI0KA, T. and Y. SAIJ0 (1985) : Active nitrification in the hypolimnion of Lake Kizaki in early summer. 2. Effects of light on nitrification in water. Arch. Hydrobiol., 105 : 1-9. – reference: CRUTZEN, P. J. (1981) : Atmospheric chemical processes of the oxides of nitrogen, including nitrous oxide, p.17-44. In C. C. DELWICHE (ed.), Denitrification, Nitrification, and Atmospheric Nitrous Oxide, 2. John Wiley & Sons. – reference: SHATTUCK, Jr., G. E. and M. ALEXANDER (1963) : A differential inhibitor of nitrifying microorganisms. Sail Sci. Soc. Proc., 27 : 600-601. – reference: YOSHIOKA, T., M. TAKAHASHI and Y. SAIJ0 (1985) Active nitrification in the hypolimnion of Lake Kizaki in early summer. 1. Nitrifying activity of rapidly sinking particles. Arch. Hydrobiol., 104 : 557-570. – reference: KAPLAN, W. A. and S. C. WOFSY (1985); The biogeochemistry of nitrous oxide : a review. p. 181-206. In Advances in Aquatic Microbiology, 3. Academic Press. – reference: YOH, M., H. TERAI and Y. SAIJ0 (1988b) : Nitrous oxide in freshwater lakes. Arch. Hydrobiol., 113 : 273-294. – reference: PIEROTTI, D. and R. A. RASMUSSEN (1980) : Nitrous oxide measurements in the eastern tropical Pacific Ocean. Tellus, 32 : 56-72. – reference: ROBERTSON, G. P. and J. M. TIEDJE (1987) : Nitrous oxide sources in aerobic soils : nitrification, denitrification and other biological processes. Soil Biol. Biochem., 19 : 187-193. – reference: HYNES, R. K. and R. KNOWLES (1984) : Production of nitrous oxide by Nit rosomonas europaea effects of acetylene, pH, and oxygen. Can. J. Microbiol., 30 : 1397-1404. – reference: BUTLER, J. H., J. W. ELKINS and T. M. THOMPSON (1989) : Tropospheric and dissolved N2O of the West Pacific and East Indian Oceans during the El Ninõ Southern Oscillation event of 1987. J. Geophys. Res., 94 : 14865-14877. – reference: ELKINS, J. W., S. C. WOFSY, M. B. M C ELROY, C. E. KOLB and W. A. KAPLAN (1978) : Aquatic sources and sinks for nitrous oxide. Nature, 275 : 602-606. – reference: BOLLAG, J. M. and G. TUNG (1972) : Nitrous oxide release by soil fungi. Soil Biol. Biochem., 4 : 271-276. |
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Snippet | The N2O production during nitrification was studied in Lake Kizaki by vertical observations and two incubation experiments. The apparent N2O production (ΔN2O),... Nitrous oxide production during nitrification in a freshwater lake was verified from the close correlations of apparent N sub(2)O production Delta N sub(2)O)... |
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Title | Experimental Examination on Nitrous Oxide Accumulation during Nitrification in a Freshwater Lake |
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