Abstract

In the oxygen-depleted layer of Lake Fukami-ike during March to July in 1985, denitrifying activities were measured by the acetylene blockage method, and the denitrifying bacterial population was estimated by the MPN method. Up till 22 March, no detectable denitrifying activity was found. On 6 April at and below 5 m depth, lower but distinct denitrifying activities were found. Thereafter, denitrifying activity became higher with time. Maximum activity (0.64 μg·at N·l-1·day-1) was obtained at 4.5 m depth on 2 July. In accordance with the development of denitrifying activity, the average denitrifying bacterial population increased from 3.9 cells·ml-1 on 22 March to 87 cells·ml-1 on 2 July. From the analysis of the correlation between denitrification and in situ dissolved oxygen content, it was shown that denitrifying activity was initiated at 0.25 ml·l-1 D. O. and increased with the decrease of dissolved oxygen content. It was also shown that the ratio of N2O emission in the total denitrification [N2O/(N2+N2O)] was decreased with decrease of in situ dissolved oxygen content.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.