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淄博市2016-2019年近地面大气臭氧时空分布特征
引用本文:吴丽萍,李梦辉,张向炎,王信梧,耿春梅,赵雪艳,杨文,殷宝辉.淄博市2016-2019年近地面大气臭氧时空分布特征[J].环境科学研究,2021,34(5):1044-1052.
作者姓名:吴丽萍  李梦辉  张向炎  王信梧  耿春梅  赵雪艳  杨文  殷宝辉
作者单位:天津城建大学环境与市政工程学院,天津 300384;天津城建大学环境与市政工程学院,天津 300384;中国环境科学研究院,环境基准与风险评估国家重点实验室,北京 100012;淄博市生态环境监测中心,山东 淄博 255000;中国环境科学研究院,环境基准与风险评估国家重点实验室,北京 100012
基金项目:中国环境科学研究院中央级公益性科研院所基本科研业务专项2018-YSKY-041
摘    要:为认识淄博市近年来大气臭氧(O3)时空分布特征,基于山东省淄博市19个环境空气质量监测点2016-2019年近地面O3的连续观测数据,运用Pearson相关性分析法、反距离权重法等方法开展研究.结果表明:①淄博市2016-2019年ρ(O3-8 h)(O3-8 h为O3日最大8 h浓度)第90百分位数范围为184~203 μg/m3,是GB 3095-2012《环境空气质量标准》二级标准限值(160 μg/m3)的1.15~1.27倍.②ρ(O3-8 h)季节性变化呈夏季(155 μg/m3)>春季(129 μg/m3)>秋季(104 μg/m3)>冬季(60 μg/m3)的特征;ρ(O3-8 h)月变化呈双峰型,峰值分别出现在6月(186 μg/m3)和9月(147 μg/m3);ρ(O3-8 h)日变化呈单峰型,峰值(117 μg/m3)出现在14:00左右.③ρ(O3-8 h)空间分布呈南北低、中间高的特点,并具有区域均匀性发展趋势.④CO、NO、NO2和NOx等前体物浓度均与ρ(O3-8 h)呈负相关,但在夏季相关性较差;冬季夜晚局地污染物对Ox的贡献大于白天.⑤ρ(O3-8 h)与温度和风速均呈显著正相关,与相对湿度呈显著负相关,当风向为西南风时ρ(O3-8 h)较高.研究显示,淄博市O3表现为典型的光化学生成特征,2016-2019年O3污染总体呈加重趋势. 

关 键 词:臭氧(O3)  淄博市  时空分布  前体物  气象因素
收稿时间:2020-05-01

Spatial-Temporal Characteristics of Ground Ozone in Zibo City from 2016 to 2019
Institution:1.School of Environmental and Municipal Engineering, Tianjin Chengjian University, Tianjin 300384, China2.State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China3.Zibo Eco-Environmental Monitoring Center, Zibo 255000, China
Abstract:Based on continuous observation data of near-surface ozone from 19 ambient air quality monitoring stations in Zibo City, Shandong Province from 2016 to 2019, the spatial-temporal characteristics of atmospheric O3 were studied using Pearson correlation analysis and inverse distance weighting method. The results showed that: (1) From 2016 to 2019, the 90th percentile of ρ(O3-8 h) (maximum 8 h concentration on O3 day) in Zibo City was 184-203 μg/m3, which is 1.15-1.27 times of the limit value of level Ⅱ (160 μg/m3) in National Ambient Air Quality Standards (GB 3095-2012). (2) The seasonal average of ρ(O3-8 h) was characterized by summer (155 μg/m3) > spring (129 μg/m3) > autumn (104 μg/m3) > winter (60 μg/m3). The monthly variation of ρ(O3-8 h) showed 'double peak' pattern, peaking in June (186 μg/m3) and September (147 μg/m3), respectively. The diurnal variations of O3 showed a 'single peak' pattern, with the peak value of 117 μg/m3 at around 14:00. (3) The spatial distribution of ρ(O3-8 h) showed 'low in south-north area and high in middle area' pattern, with a uniform trend in the regional. (4) The variation of precursors such as CO, NO, NO2 and NOx were negatively correlated with ρ(O3-8 h), but this correlation was weak in summer. Local pollutants at night in winter contributed more to Ox than in daytime. (5) ρ(O3-8 h)was significantly positively correlated with temperature and wind speed, and negatively correlated with humidity. High ρ(O3-8 h) was observed under southwesterly dominated wind. The results showed typical photochemical characteristics of O3 in Zibo, and O3 pollution gradually increased from 2016 to 2019. 
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