Key Lab of Environmental Optics & Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei, 230031, China.
Key Lab of Environmental Optics & Technology, Anhui Institute of Optics and Fine Mechanics, Hefei Institutes of Physical Science, Chinese Academy of Sciences, Hefei, 230031, China; Department of Precision Machinery and Precision Instrumentation, University of Science and Technology of China, Hefei, 230026, China; Center for Excellence in Regional Atmospheric Environment, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, 361021, China; Key Laboratory of Precision Scientific Instrumentation of Anhui Higher Education Institutes, University of Science and Technology of China, Hefei, 230026, China.
J Environ Manage. 2022 Oct 1;319:115721. doi: 10.1016/j.jenvman.2022.115721. Epub 2022 Jul 18.
This study investigated the wintertime vertical distributions and source areas of aerosols, NO, and HCHO in a coastal city of Dongying from December 2020 to March 2021, using ground-based multi-axis differential optical absorption spectroscopy (MAX-DOAS) and a potential source contribution function (PSCF) model, respectively. Moreover, the chemical production sensitivity of O at different height layers was analyzed using HCHO/NO ratios. The results revealed that the wintertime averaged highest concentrations of aerosol (1.25 km), NO (14.81 ppb), and HCHO (2.32 ppb) were mainly distributed at the surface layer, 100-200 m layer, and 200-300 m layer, respectively. Regarding the diurnal cycles, high concentrations of aerosol (>1.4 km) and NO (>16.0 ppb) usually appeared in the early morning and late afternoon, while high concentrations of HCHO (>2.5 ppb) usually occurred during 12:00-15:00. The PSCF model revealed that the wintertime aerosol mainly originated from Shandong, northern Jiangsu, Korea, and the northwestern Mongolian Plateau. Below 200 m, NO was mainly from western Shandong, whereas above 600 m, it was mainly from northern Shandong and the Beijing-Tianjin-Hebei (BTH) region. The corresponding sources for HCHO were central and southern Shandong (below 200 m) and northern Shandong, northern Jiangsu, and southeastern BTH (above 600 m). In addition, the chemical production sensitivity of O below 100 m was observed only in the VOC-limited regime. The percentages of O production under the NO-limited, NO-VOC-limited, and VOC-limited regimes were 10.75% (31.18%), 4.30% (19.35%), and 84.95% (49.47%) at the 500-600 m (900-1000 m) layer. This study has guiding significance for the coordinated control of PM and O, and can assist in the implementation of regional joint prevention and control strategies for air pollutants.
本研究利用地基多轴差分吸收光谱(MAX-DOAS)和潜在源贡献函数(PSCF)模型,分别研究了 2020 年 12 月至 2021 年 3 月期间沿海城市东营冬季气溶胶、NO 和 HCHO 的垂直分布和来源区。此外,还通过 HCHO/NO 比值分析了不同高度层 O 的化学产生敏感性。结果表明,冬季气溶胶(1.25km)、NO(14.81ppb)和 HCHO(2.32ppb)的平均最高浓度主要分布在地表层、100-200m 层和 200-300m 层。关于日变化,高浓度的气溶胶(>1.4km)和 NO(>16.0ppb)通常出现在清晨和傍晚,而高浓度的 HCHO(>2.5ppb)通常出现在 12:00-15:00。PSCF 模型揭示了冬季气溶胶主要来源于山东、苏北、朝鲜和西北蒙古高原。在 200m 以下,NO 主要来自山东西部,而在 600m 以上,主要来自山东北部和京津冀地区。HCHO 的相应来源是山东中南部(200m 以下)和山东北部、苏北、东南京津冀地区(200m 以上)。此外,在 100m 以下,仅在 VOC 限制区观察到 O 的化学产生敏感性。NO 限制、NO-VOC 限制和 VOC 限制条件下 O 生成的百分比分别为 10.75%(31.18%)、4.30%(19.35%)和 84.95%(49.47%),在 500-600m(900-1000m)层。本研究对 PM 和 O 的协同控制具有指导意义,并有助于实施区域大气污染物联合防控策略。