Daytime and Phenological Characteristics of O3 and CO2 Fluxes of Winter Wheat Canopy Under Short-Term O3 Exposure

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• 作者：Lei Tong ; Hang Xiao ; Feizhong Qian ; Zhongwen Huang…
• 关键词：Chamber system ; Ozone ; Carbon dioxide ; Flux ; Phenology ; Triticum aestivum
• 刊名：Water, Air, and Soil Pollution
• 出版年：2016
• 出版时间：January 2016
• 年：2016
• 卷：227
• 期：1
• 全文大小：1,454 KB
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• 作者单位：Lei Tong (1) (2)
  Hang Xiao (1) (2)
  Feizhong Qian (3)
  Zhongwen Huang (1) (2)
  Jiayong Feng (3)
  Xiaoke Wang (4)
  
  1. Hazardous Air Pollutants Lab, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, 361021, China
  2. Ningbo Urban Environment Observation and Research Station-NUEORS, Chinese Academy of Sciences, Ningbo, 315830, China
  3. Environment Monitoring Center of Ningbo, Ningbo, 315012, China
  4. State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：Environment
  Environment
  Atmospheric Protection, Air Quality Control and Air Pollution
  Waste Water Technology, Water Pollution Control, Water Management and Aquatic Pollution
  Terrestrial Pollution
  Hydrogeology
  
• 出版者：Springer Netherlands
• ISSN：1573-2932

文摘

To analyze the daytime and phenological variations of canopy O₃ and CO₂ uptake of winter wheat, the canopy fluxes of wheat plants were measured using a chamber system with four different O₃ levels (0, 40, 80, and 120 nmol mol鈭?) being applied. During the daytime (7:30鈥?8:00 hours), canopy fluxes usually peaked around noon in early growing stages, while a generally decreasing trend from morning to afternoon was observed in the later stages. O₃ and CO₂ fluxes were positively and negatively correlated with O₃ concentration, respectively. Significant differences were observed in O₃ fluxes but CO₂ fluxes among O₃ treatments. Photosynthetically active radiation (PAR) and vapor pressure deficit (VPD) could affect canopy gas uptake in opposite ways. On the phenological timescale, both O₃ and CO₂ fluxes followed the variation of leaf area index (LAI) with the maximum occurring simultaneously at the booting stage. The daytime mean fluxes varied from 鈭?0.6 to 鈭?7.2 nmol m鈭? s鈭? for O₃ and from 鈭?.9 to 鈭?9.6 渭mol m鈭? s鈭? for CO₂. Quantitatively important O₃ deposition (鈭?.1鈭尖垝11.6 nmol m鈭? s鈭?) was also observed at night with the ratios being about 40鈭?0 % relative to the daytime O₃ fluxes for most measuring days, which indicates a significant contribution from non-stomatal components to canopy O₃ removal. This study confirms that environmental variables and plant phenology are important factors in regulating canopy O₃ and CO₂ uptake. O₃ exposure (鈮?20 nmol mol鈭?) could not significantly affect the CO₂ uptake of wheat canopy in a short time (ca. 10 min). Keywords Chamber system Ozone Carbon dioxide Flux Phenology Triticum aestivum