Nitrogen input decreases microbial nitrogen use efficiency in surface soils of a temperate forest in northeast China

•N addition decreases microbial NUE by decreasing phosphorus availability and soil pH.•Microbial NUE is positively related to microbial biomass formation and negatively related to soil inorganic N cycling.•Microbial NUE controls the branchpoint between soil microbial N immobilization and inorganic N...

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Published inGeoderma Vol. 453; p. 117159
Main Authors Sun, Lifei, Qiao, Yanci, Wanek, Wolfgang, Moorhead, Daryl L., Cui, Yongxing, Peng, Yujiao, Song, Liquan, Hu, Baoqing, Zhang, Tuo, Li, Shuailin
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.01.2025
Elsevier
Subjects
Global change
Microbial growth
Nutrient limitation
soil C storage
Soil depth
soil N transformation
Microbial growth
soil N transformation
soil C storage
Nutrient limitation
Soil depth
Global change
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Abstract •N addition decreases microbial NUE by decreasing phosphorus availability and soil pH.•Microbial NUE is positively related to microbial biomass formation and negatively related to soil inorganic N cycling.•Microbial NUE controls the branchpoint between soil microbial N immobilization and inorganic N cycling. Microbial nitrogen use efficiency (NUE) reflects the allocation of microbially-acquired N between growth (anabolism) and the release of inorganic N to the environment (catabolism), and is central to understanding soil N cycling. However, the effects of N addition on microbial NUE are unclear. We determined microbial NUE in surface (0–10 cm) and subsurface (10–20 cm) soils in a temperate forest by the combined substrate-independent 18O-H2O tracer technique and 15N isotope pool dilution in a multi-level N addition experiment. We found that high N treatment (75 kg N ha−1 yr−1 as urea fertilizer) significantly decreased NUE in surface soil, but not in the subsurface soil. The decrease in NUE in surface soil was related to soil acidification, likely induced by N addition, and to reduced phosphorus availability, suggesting increased phosphorus limitation to microbial metabolism with N addition. Microbial NUE was inversely related to inorganic N flux (as NH4+) in both surface and subsurface soils and positively related to microbial biomass in surface soil. Our empirical evidence confirms that microbial NUE is a sensitive proxy and controlling branchpoint between soil microbial N immobilization and inorganic N cycling, which should be explicitly included in biogeochemical models to better predict soil N dynamics.
AbstractList Microbial nitrogen use efficiency (NUE) reflects the allocation of microbially-acquired N between growth (anabolism) and the release of inorganic N to the environment (catabolism), and is central to understanding soil N cycling. However, the effects of N addition on microbial NUE are unclear. We determined microbial NUE in surface (0–10 cm) and subsurface (10–20 cm) soils in a temperate forest by the combined substrate-independent 18O-H2O tracer technique and 15N isotope pool dilution in a multi-level N addition experiment. We found that high N treatment (75 kg N ha−1 yr−1 as urea fertilizer) significantly decreased NUE in surface soil, but not in the subsurface soil. The decrease in NUE in surface soil was related to soil acidification, likely induced by N addition, and to reduced phosphorus availability, suggesting increased phosphorus limitation to microbial metabolism with N addition. Microbial NUE was inversely related to inorganic N flux (as NH4+) in both surface and subsurface soils and positively related to microbial biomass in surface soil. Our empirical evidence confirms that microbial NUE is a sensitive proxy and controlling branchpoint between soil microbial N immobilization and inorganic N cycling, which should be explicitly included in biogeochemical models to better predict soil N dynamics.
•N addition decreases microbial NUE by decreasing phosphorus availability and soil pH.•Microbial NUE is positively related to microbial biomass formation and negatively related to soil inorganic N cycling.•Microbial NUE controls the branchpoint between soil microbial N immobilization and inorganic N cycling. Microbial nitrogen use efficiency (NUE) reflects the allocation of microbially-acquired N between growth (anabolism) and the release of inorganic N to the environment (catabolism), and is central to understanding soil N cycling. However, the effects of N addition on microbial NUE are unclear. We determined microbial NUE in surface (0–10 cm) and subsurface (10–20 cm) soils in a temperate forest by the combined substrate-independent 18O-H2O tracer technique and 15N isotope pool dilution in a multi-level N addition experiment. We found that high N treatment (75 kg N ha−1 yr−1 as urea fertilizer) significantly decreased NUE in surface soil, but not in the subsurface soil. The decrease in NUE in surface soil was related to soil acidification, likely induced by N addition, and to reduced phosphorus availability, suggesting increased phosphorus limitation to microbial metabolism with N addition. Microbial NUE was inversely related to inorganic N flux (as NH4+) in both surface and subsurface soils and positively related to microbial biomass in surface soil. Our empirical evidence confirms that microbial NUE is a sensitive proxy and controlling branchpoint between soil microbial N immobilization and inorganic N cycling, which should be explicitly included in biogeochemical models to better predict soil N dynamics.
ArticleNumber 117159
Author Zhang, Tuo
Song, Liquan
Wanek, Wolfgang
Sun, Lifei
Moorhead, Daryl L.
Peng, Yujiao
Li, Shuailin
Cui, Yongxing
Hu, Baoqing
Qiao, Yanci
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  surname: Sun
  fullname: Sun, Lifei
  organization: Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education, and Guangxi Key Laboratory of Earth Surface Processes and Intelligent Simulation of Nanning Normal University, Nanning 530001, China
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  givenname: Yanci
  surname: Qiao
  fullname: Qiao, Yanci
  organization: Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education, and Guangxi Key Laboratory of Earth Surface Processes and Intelligent Simulation of Nanning Normal University, Nanning 530001, China
– sequence: 3
  givenname: Wolfgang
  surname: Wanek
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  organization: Division of Terrestrial Ecosystem Research, Center of Microbiology and Environmental Systems Science, University of Vienna, Djerassiplatz 1, 1030 Vienna, Austria
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  givenname: Daryl L.
  surname: Moorhead
  fullname: Moorhead, Daryl L.
  organization: Department of Environmental Sciences, University of Toledo, 43606, Toledo, USA
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  givenname: Yongxing
  surname: Cui
  fullname: Cui, Yongxing
  organization: Institute of Biology, Freie Universität Berlin, Berlin, Germany
– sequence: 6
  givenname: Yujiao
  surname: Peng
  fullname: Peng, Yujiao
  organization: Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education, and Guangxi Key Laboratory of Earth Surface Processes and Intelligent Simulation of Nanning Normal University, Nanning 530001, China
– sequence: 7
  givenname: Liquan
  surname: Song
  fullname: Song, Liquan
  organization: Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education, and Guangxi Key Laboratory of Earth Surface Processes and Intelligent Simulation of Nanning Normal University, Nanning 530001, China
– sequence: 8
  givenname: Baoqing
  surname: Hu
  fullname: Hu, Baoqing
  organization: Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education, and Guangxi Key Laboratory of Earth Surface Processes and Intelligent Simulation of Nanning Normal University, Nanning 530001, China
– sequence: 9
  givenname: Tuo
  surname: Zhang
  fullname: Zhang, Tuo
  organization: Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education, and Guangxi Key Laboratory of Earth Surface Processes and Intelligent Simulation of Nanning Normal University, Nanning 530001, China
– sequence: 10
  givenname: Shuailin
  surname: Li
  fullname: Li, Shuailin
  email: lishuailin007@163.com
  organization: Institute of Applied Ecology, Chinese Academy of Sciences, 110016 Shenyang, China
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Keywords Microbial growth
soil N transformation
soil C storage
Nutrient limitation
Soil depth
Global change
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Snippet •N addition decreases microbial NUE by decreasing phosphorus availability and soil pH.•Microbial NUE is positively related to microbial biomass formation and...
Microbial nitrogen use efficiency (NUE) reflects the allocation of microbially-acquired N between growth (anabolism) and the release of inorganic N to the...
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StartPage 117159
SubjectTerms Global change
Microbial growth
Nutrient limitation
soil C storage
Soil depth
soil N transformation
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Title Nitrogen input decreases microbial nitrogen use efficiency in surface soils of a temperate forest in northeast China
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