Acidophilic denitrifiers dominate the N2O production in a 100-year-old tea orchard soil

Aerobic denitrification is the main process for high N₂O production in acid tea field soil. However, the biological mechanisms for the high emission are not fully understood. In this study, we examined N₂O emission and denitrifier communities in 100-year-old tea soils with four pH levels (3.71, 5.11...

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Published inEnvironmental science and pollution research international Vol. 22; no. 6; pp. 4173 - 4182
Main Authors Huang, Ying, Long, Xi-En, Chapman, Stephen J, Yao, Huaiying
Format Journal Article
LanguageEnglish
Published Berlin/Heidelberg Springer-Verlag 01.03.2015
Springer Berlin Heidelberg
Springer Nature B.V
Subjects
acid soils
Acidic soils
Acidification
Acids
Aquatic Pollution
Atmospheric Protection/Air Quality Control/Air Pollution
Bacteria - classification
Bacteria - genetics
Bacteria - metabolism
Base Sequence
Biofilms
Camellia sinensis - physiology
Climate change
Denitrification
denitrifying microorganisms
Earth and Environmental Science
Ecotoxicology
Ecotypes
Emissions
Environment
Environmental Chemistry
Environmental Health
Enzymatic activity
enzyme activity
Enzymes
Experiments
Freshwater environments
Hydrogen-Ion Concentration
Moisture content
nitrate nitrogen
Nitrates
Nitrogen
Nitrous oxide
Nitrous Oxide - chemistry
Nitrous Oxide - metabolism
orchard soils
Pesticide toxicity
Pesticides
Phylogeny
Polyethylene
Research Article
Soil - chemistry
Soil Microbiology
Soil pH
Soils
Tea
Toxicity
Waste Water Technology
Water Management
Water Pollution Control
China
Soil pH
Nitrate concentrations
O emission
T-RFLP
qPCR
Tea orchard soil
N
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Abstract Aerobic denitrification is the main process for high N₂O production in acid tea field soil. However, the biological mechanisms for the high emission are not fully understood. In this study, we examined N₂O emission and denitrifier communities in 100-year-old tea soils with four pH levels (3.71, 5.11, 6.19, and 7.41) and four nitrate concentration (0, 50, 200, and 1000 mg kg⁻¹of NO₃⁻-N) addition. Results showed the highest N₂O emission (10.1 mg kg⁻¹over 21 days) from the soil at pH 3.71 with 1000 mg kg⁻¹NO₃⁻addition. The N₂O reduction and denitrification enzyme activity in the acid soils (pH <7.0) were significantly higher than that of soils at pH 7.41. Moreover, TRF 78 of nirS and TRF 187 of nosZ dominated in soils of pH 3.71, suggesting an important role of acidophilic denitrifiers in N₂O production and reduction. CCA analysis also showed a negative correlation between the dominant denitrifier ecotypes (nirS TRF 78, nosZ TRF 187) and soil pH. The representative sequences were identical to those of cultivated denitrifiers from acidic soils via phylogenetic tree analysis. Our results showed that the acidophilic denitrifier adaptation to the acid environment results in high N₂O emission in this highly acidic tea soil.
AbstractList Aerobic denitrification is the main process for high N₂O production in acid tea field soil. However, the biological mechanisms for the high emission are not fully understood. In this study, we examined N₂O emission and denitrifier communities in 100-year-old tea soils with four pH levels (3.71, 5.11, 6.19, and 7.41) and four nitrate concentration (0, 50, 200, and 1000 mg kg⁻¹of NO₃⁻-N) addition. Results showed the highest N₂O emission (10.1 mg kg⁻¹over 21 days) from the soil at pH 3.71 with 1000 mg kg⁻¹NO₃⁻addition. The N₂O reduction and denitrification enzyme activity in the acid soils (pH <7.0) were significantly higher than that of soils at pH 7.41. Moreover, TRF 78 of nirS and TRF 187 of nosZ dominated in soils of pH 3.71, suggesting an important role of acidophilic denitrifiers in N₂O production and reduction. CCA analysis also showed a negative correlation between the dominant denitrifier ecotypes (nirS TRF 78, nosZ TRF 187) and soil pH. The representative sequences were identical to those of cultivated denitrifiers from acidic soils via phylogenetic tree analysis. Our results showed that the acidophilic denitrifier adaptation to the acid environment results in high N₂O emission in this highly acidic tea soil.
Aerobic denitrification is the main process for high N2O production in acid tea field soil. However, the biological mechanisms for the high emission are not fully understood. In this study, we examined N2O emission and denitrifier communities in 100-year-old tea soils with four pH levels (3.71, 5.11, 6.19, and 7.41) and four nitrate concentration (0, 50, 200, and 1000 mg kg(-1) of NO3 (-)-N) addition. Results showed the highest N2O emission (10.1 mg kg(-1) over 21 days) from the soil at pH 3.71 with 1000 mg kg(-1) NO3 (-) addition. The N2O reduction and denitrification enzyme activity in the acid soils (pH <7.0) were significantly higher than that of soils at pH 7.41. Moreover, TRF 78 of nirS and TRF 187 of nosZ dominated in soils of pH 3.71, suggesting an important role of acidophilic denitrifiers in N2O production and reduction. CCA analysis also showed a negative correlation between the dominant denitrifier ecotypes (nirS TRF 78, nosZ TRF 187) and soil pH. The representative sequences were identical to those of cultivated denitrifiers from acidic soils via phylogenetic tree analysis. Our results showed that the acidophilic denitrifier adaptation to the acid environment results in high N2O emission in this highly acidic tea soil.Aerobic denitrification is the main process for high N2O production in acid tea field soil. However, the biological mechanisms for the high emission are not fully understood. In this study, we examined N2O emission and denitrifier communities in 100-year-old tea soils with four pH levels (3.71, 5.11, 6.19, and 7.41) and four nitrate concentration (0, 50, 200, and 1000 mg kg(-1) of NO3 (-)-N) addition. Results showed the highest N2O emission (10.1 mg kg(-1) over 21 days) from the soil at pH 3.71 with 1000 mg kg(-1) NO3 (-) addition. The N2O reduction and denitrification enzyme activity in the acid soils (pH <7.0) were significantly higher than that of soils at pH 7.41. Moreover, TRF 78 of nirS and TRF 187 of nosZ dominated in soils of pH 3.71, suggesting an important role of acidophilic denitrifiers in N2O production and reduction. CCA analysis also showed a negative correlation between the dominant denitrifier ecotypes (nirS TRF 78, nosZ TRF 187) and soil pH. The representative sequences were identical to those of cultivated denitrifiers from acidic soils via phylogenetic tree analysis. Our results showed that the acidophilic denitrifier adaptation to the acid environment results in high N2O emission in this highly acidic tea soil.
Aerobic denitrification is the main process for high N₂O production in acid tea field soil. However, the biological mechanisms for the high emission are not fully understood. In this study, we examined N₂O emission and denitrifier communities in 100-year-old tea soils with four pH levels (3.71, 5.11, 6.19, and 7.41) and four nitrate concentration (0, 50, 200, and 1000 mg kg⁻¹of NO₃⁻-N) addition. Results showed the highest N₂O emission (10.1 mg kg⁻¹over 21 days) from the soil at pH 3.71 with 1000 mg kg⁻¹NO₃⁻addition. The N₂O reduction and denitrification enzyme activity in the acid soils (pH <7.0) were significantly higher than that of soils at pH 7.41. Moreover, TRF 78 of nirS and TRF 187 of nosZ dominated in soils of pH 3.71, suggesting an important role of acidophilic denitrifiers in N₂O production and reduction. CCA analysis also showed a negative correlation between the dominant denitrifier ecotypes (nirS TRF 78, nosZ TRF 187) and soil pH. The representative sequences were identical to those of cultivated denitrifiers from acidic soils via phylogenetic tree analysis. Our results showed that the acidophilic denitrifier adaptation to the acid environment results in high N₂O emission in this highly acidic tea soil.
Aerobic denitrification is the main process for high N 2 O production in acid tea field soil. However, the biological mechanisms for the high emission are not fully understood. In this study, we examined N 2 O emission and denitrifier communities in 100-year-old tea soils with four pH levels (3.71, 5.11, 6.19, and 7.41) and four nitrate concentration (0, 50, 200, and 1000 mg kg −1 of NO 3 − -N) addition. Results showed the highest N 2 O emission (10.1 mg kg −1 over 21 days) from the soil at pH 3.71 with 1000 mg kg −1 NO 3 − addition. The N 2 O reduction and denitrification enzyme activity in the acid soils (pH <7.0) were significantly higher than that of soils at pH 7.41. Moreover, TRF 78 of nirS and TRF 187 of nosZ dominated in soils of pH 3.71, suggesting an important role of acidophilic denitrifiers in N 2 O production and reduction. CCA analysis also showed a negative correlation between the dominant denitrifier ecotypes ( nirS TRF 78, nosZ TRF 187) and soil pH. The representative sequences were identical to those of cultivated denitrifiers from acidic soils via phylogenetic tree analysis. Our results showed that the acidophilic denitrifier adaptation to the acid environment results in high N 2 O emission in this highly acidic tea soil.
Aerobic denitrification is the main process for high N2O production in acid tea field soil. However, the biological mechanisms for the high emission are not fully understood. In this study, we examined N2O emission and denitrifier communities in 100-year-old tea soils with four pH levels (3.71, 5.11, 6.19, and 7.41) and four nitrate concentration (0, 50, 200, and 1000 mg kg(-1) of NO3 (-)-N) addition. Results showed the highest N2O emission (10.1 mg kg(-1) over 21 days) from the soil at pH 3.71 with 1000 mg kg(-1) NO3 (-) addition. The N2O reduction and denitrification enzyme activity in the acid soils (pH <7.0) were significantly higher than that of soils at pH 7.41. Moreover, TRF 78 of nirS and TRF 187 of nosZ dominated in soils of pH 3.71, suggesting an important role of acidophilic denitrifiers in N2O production and reduction. CCA analysis also showed a negative correlation between the dominant denitrifier ecotypes (nirS TRF 78, nosZ TRF 187) and soil pH. The representative sequences were identical to those of cultivated denitrifiers from acidic soils via phylogenetic tree analysis. Our results showed that the acidophilic denitrifier adaptation to the acid environment results in high N2O emission in this highly acidic tea soil.
Issue Title: Potential toxicity of pesticides in freshwater environments: passive sampling, exposure and impacts on biofilms Aerobic denitrification is the main process for high N2O production in acid tea field soil. However, the biological mechanisms for the high emission are not fully understood. In this study, we examined N2O emission and denitrifier communities in 100-year-old tea soils with four pH levels (3.71, 5.11, 6.19, and 7.41) and four nitrate concentration (0, 50, 200, and 1000 mg kg-1 of NO3 --N) addition. Results showed the highest N2O emission (10.1 mg kg-1 over 21 days) from the soil at pH 3.71 with 1000 mg kg-1 NO3 - addition. The N2O reduction and denitrification enzyme activity in the acid soils (pH <7.0) were significantly higher than that of soils at pH 7.41. Moreover, TRF 78 of nirS and TRF 187 of nosZ dominated in soils of pH 3.71, suggesting an important role of acidophilic denitrifiers in N2O production and reduction. CCA analysis also showed a negative correlation between the dominant denitrifier ecotypes (nirS TRF 78, nosZ TRF 187) and soil pH. The representative sequences were identical to those of cultivated denitrifiers from acidic soils via phylogenetic tree analysis. Our results showed that the acidophilic denitrifier adaptation to the acid environment results in high N2O emission in this highly acidic tea soil.
Author Chapman, Stephen J
Huang, Ying
Long, Xi-En
Yao, Huaiying
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BackLink https://www.ncbi.nlm.nih.gov/pubmed/25273518$$D View this record in MEDLINE/PubMed
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ISSN 0944-1344
1614-7499
IngestDate Fri Jul 11 07:41:53 EDT 2025
Tue Aug 05 10:24:30 EDT 2025
Fri Jul 25 23:25:19 EDT 2025
Mon Jul 21 06:01:19 EDT 2025
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Thu Apr 24 23:01:35 EDT 2025
Fri Feb 21 02:36:22 EST 2025
Thu Apr 03 09:45:59 EDT 2025
IsPeerReviewed true
IsScholarly true
Issue 6
Keywords Soil pH
Nitrate concentrations
O emission
T-RFLP
qPCR
Tea orchard soil
N
Language English
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Snippet Aerobic denitrification is the main process for high N₂O production in acid tea field soil. However, the biological mechanisms for the high emission are not...
Aerobic denitrification is the main process for high N 2 O production in acid tea field soil. However, the biological mechanisms for the high emission are not...
Aerobic denitrification is the main process for high N2O production in acid tea field soil. However, the biological mechanisms for the high emission are not...
Issue Title: Potential toxicity of pesticides in freshwater environments: passive sampling, exposure and impacts on biofilms Aerobic denitrification is the...
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SubjectTerms acid soils
Acidic soils
Acidification
Acids
Aquatic Pollution
Atmospheric Protection/Air Quality Control/Air Pollution
Bacteria - classification
Bacteria - genetics
Bacteria - metabolism
Base Sequence
Biofilms
Camellia sinensis - physiology
Climate change
Denitrification
denitrifying microorganisms
Earth and Environmental Science
Ecotoxicology
Ecotypes
Emissions
Environment
Environmental Chemistry
Environmental Health
Enzymatic activity
enzyme activity
Enzymes
Experiments
Freshwater environments
Hydrogen-Ion Concentration
Moisture content
nitrate nitrogen
Nitrates
Nitrogen
Nitrous oxide
Nitrous Oxide - chemistry
Nitrous Oxide - metabolism
orchard soils
Pesticide toxicity
Pesticides
Phylogeny
Polyethylene
Research Article
Soil - chemistry
Soil Microbiology
Soil pH
Soils
Tea
Toxicity
Waste Water Technology
Water Management
Water Pollution Control
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Title Acidophilic denitrifiers dominate the N2O production in a 100-year-old tea orchard soil
URI https://link.springer.com/article/10.1007/s11356-014-3653-6
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Volume 22
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