Evaluating the role of high N 2 O affinity complete denitrifiers and non-denitrifying N 2 O reducing bacteria in reducing N 2 O emissions in river

Freshwater rivers are hotspots of N O greenhouse gas emissions. Dissolved organic carbon (DOC) is the dominant electron donor for microbial N O reduction, which can reduce N O emission through enriching high N O affinity denitrifiers or enriching non-denitrifying N O-reducing bacteria (N ORB), but t...

Full description

Saved in:
Bibliographic Details
Published inJournal of hazardous materials Vol. 479; p. 135602
Main Authors Yeerken, Senbati, Deng, Min, Li, Lu, Thi Kinh, Co, Wang, Zezheng, Huang, Yongxia, Xiao, Yanlin, Song, Kang
Format Journal Article
LanguageEnglish
Published Netherlands 24.08.2024
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:Freshwater rivers are hotspots of N O greenhouse gas emissions. Dissolved organic carbon (DOC) is the dominant electron donor for microbial N O reduction, which can reduce N O emission through enriching high N O affinity denitrifiers or enriching non-denitrifying N O-reducing bacteria (N ORB), but the primary regulatory pathway remains unclear. Here, field study indicated that high DOC concentration in rivers enhanced denitrification rate but reduced N O flux by improving nosZ gene abundance. Then, four N O-fed membrane aeration biofilm reactors inoculated with river sediments from river channel, estuary, adjacent lake, and a mixture were continuously performed for 360 days, including low, high, and mixed DOC stages. During enrichment stages, the (nirS+nirK)/nosZ ratio showed no significant difference, but the community structure of denitrifiers and N ORB changed significantly (p < 0.05). In addition, N ORB strains isolated from different enrichment stages positioned in different branches of the phylogenetic tree. N ORB strains isolated during high DOC stage showed significant higher maximum N O-reducing capability (V : 0.6 ± 0.4 ×10 pmol h cell ) and N O affinity (a : 7.8 ± 7.7 ×1 L cell h ) than strains isolated during low (V : 0.1 ± 0.1 ×10 pmol h cell , a : 0.7 ± 0.4 ×1 L cell h ) and mixed DOC stages (V : 0.1 ± 0.1 ×10 pmol h cell , a : 0.9 ± 0.9 ×1 L cell h ) (p < 0.05). Hence, under high DOC concentration conditions, the primary factor in reducing N O emissions in rivers is the enrichment of complete denitrifiers with high N O affinity, rather than non-denitrifying N ORB.
ISSN:1873-3336