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稻田生态系统O3干沉积特性及其对气孔吸收的贡献
引用本文:赵辉,王思雨,张誉馨,刘贞,郑有飞.稻田生态系统O3干沉积特性及其对气孔吸收的贡献[J].中国环境科学,2021,41(7):3298-3305.
作者姓名:赵辉  王思雨  张誉馨  刘贞  郑有飞
作者单位:1. 复旦大学环境科学与工程系, 上海 200438;2. 南京信息工程大学江苏省大气环境监测与污染控制高技术研究重点实验室, 江苏 南京 210044;3. 香港科技大学理学院, 香港 999077;4. 秦皇岛市气象局, 河北 秦皇岛 066000
基金项目:中国博士后科学基金(2020M681157);江苏省大气环境监测与污染控制高技术研究重点实验室开放基金项目(KHK2003);河北省气象局青年基金(20ky32)
摘    要:选择江苏省南京市南京信息工程大学永丰农业气象试验站水稻种植区站点,实时观测气象因子、O3浓度、干沉积通量、沉积速率.基于课题组在本地修正过的水稻气孔导度模型量化O3干沉积通量在气孔与非气孔通道的分配特征.结果表明:整个水稻观测期间,O3干沉积速率与通量在夜间变化平缓,白天变化剧烈,均值分别为0.34cm/s与-0.0049μmol/(m2·s),峰值则分别出现在08:30与12:30.此外,水稻生长季期间平均日累积O3总通量、气孔通量与非气孔通量分别为0.40,0.14,0.26mmol/(m2·d),其累积值分别为27.8,9.8,18.0mmol/m2.平均O3气孔通量和非气孔通量所占总O3通量的比例分别为34.0%和66.0%,其中白天的比例分别为49.0%与51.0%.

关 键 词:微气象学法  O3通量  水稻  沉积速率  
收稿时间:2020-11-15

Ozone dry deposition characteristics and its contribution to stomatal absorption in a paddy ecosystem
ZHAO Hui,WANG Si-yu,ZHANG Yu-xin,LIU Zhen,ZHENG You-fei.Ozone dry deposition characteristics and its contribution to stomatal absorption in a paddy ecosystem[J].China Environmental Science,2021,41(7):3298-3305.
Authors:ZHAO Hui  WANG Si-yu  ZHANG Yu-xin  LIU Zhen  ZHENG You-fei
Institution:1. Department of Environmental Science and Engineering, Fudan University, Shanghai 200438, China;2. Jiangsu Provincial Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Nanjing University of Information Science & Technology, Nanjing 210044, China;3. School of Science, The Hong Kong University of Science and Technology, Hong Kong 999077, China;4. Qinhuangdao Meteorological Bureau, Qinhuangdao 066000, China
Abstract:This study selected the main rice planting area in Yongfeng Agro-meteorological Experimental Station of Nanjing University of Information Science and Technology, Nanjing City, Jiangsu Province to carry out continuous observations of meteorological factors, ozone concentration, dry deposition flux, and deposition rate. Based on the modified rice stomatal conductance model, the distribution characteristics of O3 dry deposition flux in stomata and non-stomata channels were quantified. During the observation period of rice, the rate and flux of O3 dry deposition displayed a relatively gentle change during the nighttime and a more intense change during the daytime, and their average values were 0.34cm/s and -0.0049 μmol/(m2·s), respectively, and their peaks appeared at 08:30 and 12:30, respectively, In addition, the daily accumulated O3 flux, stomatal flux and non-stomatal flux during the observation period of rice were 0.40, 0.14, and 0.26mmol/(m2·d), respectively, and their cumulative values were 27.8, 9.8, and 18.0mmol/m2, respectively. During the growing season of rice, the ratios of average stomatal O3 flux and non-stomatal O3 flux to total O3 flux were 34.0% and 66.0%, respectively, and the ratios during the daytime were 49.0% and 51.0%, respectively.
Keywords:micrometeorological method  ozone flux  rice  deposition rate  
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