[1] PLATT U, PERNER D, PÄTZ H W. Simultaneous measurement of atmospheric CH2O, O3, and NO2 by differential optical absorption[J]. Journal of Geophysical Research Oceans, 1979, 84(C10): 6329-6335. doi: 10.1029/JC084iC10p06329
[2] PLANE J M C, NIEN C F. Differential optical absorption spectrometer for measuring atmospheric trace gases[J]. Review of Scientific Instruments, 1992, 63(3): 1867-1876. doi: 10.1063/1.1143296
[3] PLATT U, HAUSMANN M. Spectroscopic measurement of the free radicals NO3, BRO, IO, and OH in the troposphere[J]. Research on Chemical Intermediates, 1994, 20(3): 557-578.
[4] BARREFORS G E. Monitoring of benzene, toluene and p-xylene in urban air with differential optical absorption spectroscopy technique[J]. Science of the Total Environment, 1996, 189-190: 287-292. doi: 10.1016/0048-9697(96)05221-7
[5] VOLKAMER R, ETZKORN T, GEYER A, et al. Correction of the oxygen interference with UV spectroscopic (DOAS) measurements of monocyclic aromatic hydrocarbons in the atmosphere[J]. Atmospheric Environment, 1998, 32(21): 3731-3747. doi: 10.1016/S1352-2310(98)00095-8
[6] 邵理堂. 差分吸收光谱法在线测量烟气浓度的理论与系统研究[D]. 南京: 东南大学, 2008.
[7] 谢品华, 付强, 刘建国, 等. 差分吸收光谱方法反演大气环境单环芳香烃有机物[J]. 光谱学与光谱分析, 2006, 26(9): 1584-1588. doi: 10.3321/j.issn:1000-0593.2006.09.005
[8] WALLIN S, 黄兆开, 范海华. DOAS方法在连续排放污染源及过程气体在线监测中的实现[J]. 环境工程技术学报, 2011, 1(1): 38-45. doi: 10.3969/j.issn.1674-991X.2011.01.007
[9] 郑尼娜, 谢品华, 凌六一, 等. 紫外LED光纤耦合长程DOAS系统监测大气SO2和O3的研究[J]. 光学学报, 2013, 33(3): 44-52.
[10] 魏永杰, 耿晓娟, 陈博, 等. 光纤收发的空气差分吸收光谱测量方法研究[J]. 光谱学与光谱分析, 2013(10): 193-196.
[11] 孙延庆, 王飞, 邹捷书, 等. 基于光纤收发一体的紫外增强差分吸收光谱系统的研究[J]. 能源工程, 2015(4): 53-57.
[12] NAWAHDA A. Ozone monitoring using differential optical absorption spectroscopy (DOAS) and UV photometry instruments in Sohar, Oman[J]. Environmental Monitoring & Assessment, 2015, 187(8): 485-492.
[13] 生态环境部. 2018中国生态环境状况公报发布[J]. 中国能源, 2019, 41(6): 1.
[14] 苏爱华. 环境空气VOC在线监测系统在化工业园区环境监测中的应用研究[J]. 环境科学与管理, 2018, 43(11): 93-97. doi: 10.3969/j.issn.1673-1212.2018.11.021
[15] DRAXIER R R, HESS G D. An overview of the HYSPLIT_4 modelling system for trajectories, dispersion and deposition[J]. Australian Meteorological Magazine, 1998, 47(4): 295-308.
[16] NASSE J M, EGER P G, POHLER D, et al. Recent improvements of long-path DOAS measurements: Impact on accuracy and stability of short-term and automated long-term observations[J]. Atmospheric Measurement Techniques, 2019, 12(8): 4149-4169. doi: 10.5194/amt-12-4149-2019
[17] FINLAYSONPITTS B, PITTS J J, PITTS J, et al. Chemistry of the upper and lower atmosphere[J]. Chemistry of the Upper & Lower Atmosphere, 2000, 47(3): 17-18.
[18] 唐孝炎, 张远航, 邵敏. 大气环境化学[M]. 2版. 北京: 高等教育出版社, 2006.
[19] KLEFFMANN J, GAVRILOAIEI T, HOFZUMAHAUS A, et al. Daytime formation of nitrous acid: A major source of OH radicals in a forest[J]. Geophysical Research Letters, 2005, 32(5): 347-354.
[20] 楼晟荣. 大气环境中OH自由基反应活性的检测技术[D]. 上海: 上海交通大学, 2012.
[21] 黄健, 颜鹏, DRAXLER R R. 利用HYSPLIT_4模式分析珠海地面SO2浓度的变化规律[J]. 热带气象学报, 2004, 18(4): 407-414.
[22] 梁卓然, 江志红, 刘征宇, 等. 基于拉格朗日方法的气流轨迹模式在判定南海夏季风爆发时间中的应用分析[J]. 热带气象学报, 2011, 27(3): 357-364. doi: 10.3969/j.issn.1004-4965.2011.03.008