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Nitrifying populations and the destruction of NO2 sorbed by soil

Journal Article · · Am. Soc. Microbiol., Abstr. Annu. Meet.; (United States)
OSTI ID:6253793
Nitrifying microorganisms participate in the destruction of NO2 sorbed by soil by oxidizing the nitrite formed as a sorption product. The nitrite oxidation rate increases and shifts away from linearity as soil moisture increases to field capacity. At constant soil moisture levels, the rate of nitrite oxidation in samples preexposed to NO2 is greater than in samples not preexposed, suggesting adaptation and/or growth of a nitrifying population. However, inhibition of nitrite oxidation by 1mM but no 0.01mM chlorate suggests that, if autotrophs are involved, a resting rather than a growing population carries out the oxidation. Nitrobacter numbers in the soil rise only after at least half of the nitrite initially formed from NO2 is oxidized, but the population increase does not produce a corresponding increase in nitrite oxidation rate. Heating the soil to 42-45 C for 6 h reduces Nitrobacter numbers and retards but does not eliminate nitrite oxidation. No increase in Nitrobacter numbers is observed during nitrite oxidation in the heated soil. These results and estimates of nitrite turnover per autotrophic cell suggest that Nitrobacter is not a major contributor to nitrite oxidation in this soil, but heterotrophic nitrifiers may be involved in this mechanism for the destruction of NO2.
Research Organization:
Cornell Univ., Ithaca, NY
OSTI ID:
6253793
Journal Information:
Am. Soc. Microbiol., Abstr. Annu. Meet.; (United States), Journal Name: Am. Soc. Microbiol., Abstr. Annu. Meet.; (United States) Vol. 76; ISSN ASMAC
Country of Publication:
United States
Language:
English