Bedoukian   RussellIPM   RussellIPM   Piezoelectric Micro-Sprayer


Home
Animal Taxa
Plant Taxa
Semiochemicals
Floral Compounds
Semiochemical Detail
Semiochemicals & Taxa
Synthesis
Control
Invasive spp.
References

Abstract

Guide

Alphascents
Pherobio
InsectScience
E-Econex
Counterpart-Semiochemicals
Print
Email to a Friend
Kindly Donate for The Pherobase

« Previous AbstractAllelopathically inhibitory effects of eucalyptus extracts on the growth of Microcystis aeruginosa    Next AbstractNutrient variation induced by rodent disturbance in Haloxylon ammodendron as a target transfer strategy »

J Environ Sci (China)


Title:"Evolution of boundary layer ozone in Shijiazhuang, a suburban site on the North China Plain"
Author(s):Zhao W; Tang G; Yu H; Yang Y; Wang Y; Wang L; An J; Gao W; Hu B; Cheng M; An X; Li X; Wang Y;
Address:"Nanjing University of Information Science and Technology, Nanjing 210044, China; State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China. State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; Key Laboratory of Atmospheric Chemistry, China Meteorological Administration, Beijing 100081, China; Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China. Electronic address: tgq@dq.cern.ac.cn. Nanjing University of Information Science and Technology, Nanjing 210044, China; Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan 430074, China. Electronic address: yuhuan_1981@163.com. Weather Modification Office of Hebei Province, Shijiazhuang 050021, China. State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China. Key Laboratory of Meteorological Disaster, Ministry of Education (KLME), Joint International Research Laboratory of Climate and Environment Change (ILCEC), Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science and Technology, Nanjing 210044, China. Key Laboratory of Atmospheric Chemistry, China Meteorological Administration, Beijing 100081, China. State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China; University of Chinese Academy of Sciences, Beijing 100049, China"
Journal Title:J Environ Sci (China)
Year:2019
Volume:20190227
Issue:
Page Number:152 - 160
DOI: 10.1016/j.jes.2019.02.016
ISSN/ISBN:1001-0742 (Print) 1001-0742 (Linking)
Abstract:"The structure of the boundary layer affects the evolution of ozone (O(3)), and research into this structure will provide important insights for understanding photochemical pollution. In this study, we conducted a one-month observation (from June 15 to July 14, 2016) of the boundary layer meteorological factors as well as O(3) and its precursors in Luancheng County, Shijiazhuang (37 degrees 53'N, 114 degrees 38'E). Our research showed that photochemical pollution in Shijiazhuang is serious, and the mean hourly maximum and mean 8-hr maximum O(3) concentrations are 97.9?ª++/-?ª+26.1 and 84.4?ª++/-?ª+22.4?ª+ppbV, respectively. Meteorological factors play a significant role in the formation of O(3). High temperatures and southeasterly winds lead to elevated O(3) values, and at moderate relative humidity (40%-50%) and medium boundary layer heights (1200-1500?ª+m), O(3) production sensitivity occurred in the transitional region between volatile organic compounds (VOC) and nitrogen oxides (NO(x)) limitations, and the O(3) concentration was the highest. The vertical profiles of O(3) were also measured by a tethered balloon. The results showed that a large amount of O(3) was stored in the residual layer, and the concentration was positively correlated with the O(3) concentration measured the previous day. During the daytime of the following day, the contribution of O(3) stored in the residual layer to the boundary layer reached 27%?ª++/-?ª+7% on average"
Keywords:Air Pollutants/*analysis China *Environmental Monitoring Nitrogen Oxides/analysis Ozone/*analysis *Stratospheric Ozone Volatile Organic Compounds/analysis Boundary layer Ozone Residual layer Sensitivity Vertical evolution;
Notes:"MedlineZhao, Wei Tang, Guiqian Yu, Huan Yang, Yang Wang, Yinghong Wang, Lili An, Junlin Gao, Wenkang Hu, Bo Cheng, Mengtian An, Xingqin Li, Xin Wang, Yuesi eng Netherlands 2019/06/22 J Environ Sci (China). 2019 Sep; 83:152-160. doi: 10.1016/j.jes.2019.02.016. Epub 2019 Feb 27"

 
Back to top
 
Citation: El-Sayed AM 2024. The Pherobase: Database of Pheromones and Semiochemicals. <http://www.pherobase.com>.
© 2003-2024 The Pherobase - Extensive Database of Pheromones and Semiochemicals. Ashraf M. El-Sayed.
Page created on 19-12-2024