Characterizing nitric oxide emissions from two typical alpine ecosystems
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  • 英文篇名:Characterizing nitric oxide emissions from two typical alpine ecosystems
  • 作者:Fei ; Lin ; Chunyan ; Liu ; Xiaoxia ; Hu ; Yongfeng ; Fu ; Xunhua ; Zheng ; Rui ; Wang ; Wei ; Zhang ; Guangmin ; Cao
  • 英文作者:Fei Lin;Chunyan Liu;Xiaoxia Hu;Yongfeng Fu;Xunhua Zheng;Rui Wang;Wei Zhang;Guangmin Cao;State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences;College of Earth and Planetary Sciences, University of Chinese Academy of Sciences;Northwest Institute of Plateau Biology, Chinese Academy of Sciences;
  • 英文关键词:Alpine meadow;;Annual NO fluxes;;Non-growing season;;Freeze–thaw period;;Land use change;;Global warming
  • 中文刊名:HJKB
  • 英文刊名:环境科学学报(英文版)
  • 机构:State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences;College of Earth and Planetary Sciences, University of Chinese Academy of Sciences;Northwest Institute of Plateau Biology, Chinese Academy of Sciences;
  • 出版日期:2018-12-26
  • 出版单位:Journal of Environmental Sciences
  • 年:2019
  • 期:v.77
  • 基金:supported by the Ministry of Science and Technology of China(2016YFA0602303);; the National Natural Science Foundation of China(41375152,41603075,and 41775141)
  • 语种:英文;
  • 页:HJKB201903030
  • 页数:11
  • CN:03
  • ISSN:11-2629/X
  • 分类号:315-325
摘要
portion of alpine meadows has been and will continue to be cultivated due to the concurrent increasing demands for animal-and crop-oriented foods and global warming.However, it remains unclear how these long-term changes in land use will affect nitric oxide(NO) emission. At a field site with a calcareous soil on the Qinghai-Tibetan Plateau,the authors measured the year-round NO fluxes and related variables in a typically wintergrazed natural alpine meadow(NAM) and its adjacent forage oat field(FOF). The results showed that long-term plow tillage, fertilization and growing forage oats significantly yielded ca. 2.7 times more(p < 0.01) NO emissions from the FOF than the NAM(conservatively 208 vs. 56 g N/(ha·year) on average). The spring freeze–thaw period and non-growing season accounted for 17%-35% of the annual emissions, respectively. The Q10 of surface soil temperature(Ts) was 8.9 in the NAM(vs. 3.8 in the FOF), indicating increases of 24%–93% in NO emissions per 1–3 °C increase. However, the warming-induced increases could be smaller than those due to land use change and management practices. The Tsand concentrations of ammonium, nitrate and water-extractable organic carbon jointly explained 69% of the variance in daily NO fluxes from both fields during the annual period(p < 0.001). This result indicates that temporally and/or spatially distributed NO fluxes from landscapes with calcareous soils across native alpine meadows and/or fields cultivated with forage oats can be predicted by simultaneous observations of these four soil variables.
        portion of alpine meadows has been and will continue to be cultivated due to the concurrent increasing demands for animal-and crop-oriented foods and global warming.However, it remains unclear how these long-term changes in land use will affect nitric oxide(NO) emission. At a field site with a calcareous soil on the Qinghai-Tibetan Plateau,the authors measured the year-round NO fluxes and related variables in a typically wintergrazed natural alpine meadow(NAM) and its adjacent forage oat field(FOF). The results showed that long-term plow tillage, fertilization and growing forage oats significantly yielded ca. 2.7 times more(p < 0.01) NO emissions from the FOF than the NAM(conservatively 208 vs. 56 g N/(ha·year) on average). The spring freeze–thaw period and non-growing season accounted for 17%-35% of the annual emissions, respectively. The Q10 of surface soil temperature(Ts) was 8.9 in the NAM(vs. 3.8 in the FOF), indicating increases of 24%–93% in NO emissions per 1–3 °C increase. However, the warming-induced increases could be smaller than those due to land use change and management practices. The Tsand concentrations of ammonium, nitrate and water-extractable organic carbon jointly explained 69% of the variance in daily NO fluxes from both fields during the annual period(p < 0.001). This result indicates that temporally and/or spatially distributed NO fluxes from landscapes with calcareous soils across native alpine meadows and/or fields cultivated with forage oats can be predicted by simultaneous observations of these four soil variables.
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