Junjie Zhou, Zhifei Chen, Chunxia Jian, Yang Luo, Furong Niu, Jairo A. Palta, Bingcheng Xu
{"title":"半干旱草地的自养呼吸比异养呼吸对氮磷供应更敏感","authors":"Junjie Zhou, Zhifei Chen, Chunxia Jian, Yang Luo, Furong Niu, Jairo A. Palta, Bingcheng Xu","doi":"10.1029/2024JG008230","DOIUrl":null,"url":null,"abstract":"<p>Quantification of autotrophic (Ra) and heterotrophic (Rh) components of soil respiration (Rs) could greatly improve our understanding of terrestrial carbon cycling. Here, we investigated the effect of nitrogen (N) and phosphorus (P) supply on soil respiration rates and its components, and seasonal cumulative soil CO<sub>2</sub> efflux in a semiarid grassland. A two-factor experiment of N (0, 50 and 100 kg N ha<sup>−1</sup> yr<sup>−1</sup>) and P (0, 18 and 36 kg P ha<sup>−1</sup> yr<sup>−1</sup>) supply was conducted on the Loess Plateau in 2018–2021. Our results indicated that the promoting effect of combination of N and P supply on soil respiration and its components was greater than that of N/P supply alone. N and/or P supply increased the cumulative soil CO<sub>2</sub> efflux in both non-growing and growing seasons, and the non-growing season CO<sub>2</sub> efflux accounted for ∼25% of the growing season CO<sub>2</sub> efflux. The increase of cumulative CO<sub>2</sub> efflux from Ra in response to N and/or P supply was significantly greater than that of Rh in 2018 and 2019, while it shifted to the opposite, that is, a greater increase in Rh than in Ra in 2020 and 2021. Our results suggest that 100 kg N ha<sup>−1</sup> yr<sup>−1</sup> supply alone is an optimum fertilization scheme to trade-off grassland productivity and soil CO<sub>2</sub> emissions. Our results highlighted that the promoting effects of N and P fertilization on different soil CO<sub>2</sub> efflux components could be reversed in a relatively short period (4 years), and this should be considered when nutrient addition is adapted to restore degraded grasslands.</p>","PeriodicalId":16003,"journal":{"name":"Journal of Geophysical Research: Biogeosciences","volume":null,"pages":null},"PeriodicalIF":3.7000,"publicationDate":"2024-07-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Autotrophic Respiration Is More Sensitive to Nitrogen and Phosphorus Supply Than Heterotrophic Respiration in Semiarid Grassland\",\"authors\":\"Junjie Zhou, Zhifei Chen, Chunxia Jian, Yang Luo, Furong Niu, Jairo A. Palta, Bingcheng Xu\",\"doi\":\"10.1029/2024JG008230\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Quantification of autotrophic (Ra) and heterotrophic (Rh) components of soil respiration (Rs) could greatly improve our understanding of terrestrial carbon cycling. Here, we investigated the effect of nitrogen (N) and phosphorus (P) supply on soil respiration rates and its components, and seasonal cumulative soil CO<sub>2</sub> efflux in a semiarid grassland. A two-factor experiment of N (0, 50 and 100 kg N ha<sup>−1</sup> yr<sup>−1</sup>) and P (0, 18 and 36 kg P ha<sup>−1</sup> yr<sup>−1</sup>) supply was conducted on the Loess Plateau in 2018–2021. Our results indicated that the promoting effect of combination of N and P supply on soil respiration and its components was greater than that of N/P supply alone. N and/or P supply increased the cumulative soil CO<sub>2</sub> efflux in both non-growing and growing seasons, and the non-growing season CO<sub>2</sub> efflux accounted for ∼25% of the growing season CO<sub>2</sub> efflux. The increase of cumulative CO<sub>2</sub> efflux from Ra in response to N and/or P supply was significantly greater than that of Rh in 2018 and 2019, while it shifted to the opposite, that is, a greater increase in Rh than in Ra in 2020 and 2021. Our results suggest that 100 kg N ha<sup>−1</sup> yr<sup>−1</sup> supply alone is an optimum fertilization scheme to trade-off grassland productivity and soil CO<sub>2</sub> emissions. 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Autotrophic Respiration Is More Sensitive to Nitrogen and Phosphorus Supply Than Heterotrophic Respiration in Semiarid Grassland
Quantification of autotrophic (Ra) and heterotrophic (Rh) components of soil respiration (Rs) could greatly improve our understanding of terrestrial carbon cycling. Here, we investigated the effect of nitrogen (N) and phosphorus (P) supply on soil respiration rates and its components, and seasonal cumulative soil CO2 efflux in a semiarid grassland. A two-factor experiment of N (0, 50 and 100 kg N ha−1 yr−1) and P (0, 18 and 36 kg P ha−1 yr−1) supply was conducted on the Loess Plateau in 2018–2021. Our results indicated that the promoting effect of combination of N and P supply on soil respiration and its components was greater than that of N/P supply alone. N and/or P supply increased the cumulative soil CO2 efflux in both non-growing and growing seasons, and the non-growing season CO2 efflux accounted for ∼25% of the growing season CO2 efflux. The increase of cumulative CO2 efflux from Ra in response to N and/or P supply was significantly greater than that of Rh in 2018 and 2019, while it shifted to the opposite, that is, a greater increase in Rh than in Ra in 2020 and 2021. Our results suggest that 100 kg N ha−1 yr−1 supply alone is an optimum fertilization scheme to trade-off grassland productivity and soil CO2 emissions. Our results highlighted that the promoting effects of N and P fertilization on different soil CO2 efflux components could be reversed in a relatively short period (4 years), and this should be considered when nutrient addition is adapted to restore degraded grasslands.
期刊介绍:
JGR-Biogeosciences focuses on biogeosciences of the Earth system in the past, present, and future and the extension of this research to planetary studies. The emerging field of biogeosciences spans the intellectual interface between biology and the geosciences and attempts to understand the functions of the Earth system across multiple spatial and temporal scales. Studies in biogeosciences may use multiple lines of evidence drawn from diverse fields to gain a holistic understanding of terrestrial, freshwater, and marine ecosystems and extreme environments. Specific topics within the scope of the section include process-based theoretical, experimental, and field studies of biogeochemistry, biogeophysics, atmosphere-, land-, and ocean-ecosystem interactions, biomineralization, life in extreme environments, astrobiology, microbial processes, geomicrobiology, and evolutionary geobiology