首页> 外文期刊>Atmospheric chemistry and physics >Measurements of HNOsub3/sub and Nsub2/subOsub5/sub using ion drift-chemical ionization mass spectrometry during the MILAGRO/MCMA-2006 campaign
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Measurements of HNOsub3/sub and Nsub2/subOsub5/sub using ion drift-chemical ionization mass spectrometry during the MILAGRO/MCMA-2006 campaign

机译:在MILAGRO / MCMA-2006活动中使用离子漂移化学电离质谱法测量HNO 3 和N 2 O 5

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An ion drift-chemical ionization mass spectrometer (ID-CIMS) was deployed inMexico City between 7 and 31 March to measure gas-phase nitric acid(HNO3) and dinitrogen pentoxide (N2O5 during the Mexico CityMetropolitan Area (MCMA)-2006 field campaign. The observation site waslocated at the Instituto Mexicano del Petróleo in the northern part ofMexico City urban area with major emissions of pollutants from residential,vehicular and industrial sources. Diurnally, HNO3 was less than 200parts per trillion (ppt) during the night and early morning. Theconcentration of HNO3 increased steadily from around 09:00 a.m. centralstandard time (CST), reached a peak value of 0.5 to 3 parts per billion (ppb)in the early afternoon, and then declined sharply to less than half of thepeak value near 05:00 p.m. CST. An inter-comparison between the ID-CIMS andan ion chromatograph/mass spectrometer (ICMS) showed a good agreement betweenthe two HNO3 measurements (R2=0.75). The HNO3 mixing ratiowas found to anti-correlate with submicron-sized aerosol nitrate, suggestingthat the gas-particle partitioning process was a major factor in determiningthe gaseous HNO3 concentration. Losses by irreversible reactions withmineral dust and via dry deposition also could be important at this site.Most of the times during the MCMA 2006 field campaign, N2O5 wasfound to be below the detection limit (about 30 ppt for a 10 s integrationtime) of the ID-CIMS, because of high NO mixing ratio at the surface(>100 ppb) during the night. An exception occurred on 26 March 2006, whenabout 40 ppt N2O5 was observed during the late afternoon andearly evening hours under cloudy conditions before the build-up of NO at thesurface site. The results revealed that during the MCMA-2006 field campaignHNO3 was primarily produced from the reaction of OH with NO2 andregulated by gas/particle transfer and dry deposition. The production ofHNO3 from N2O5 hydrolysis during the nighttime was smallbecause of high NO and low O3 concentrations near the surface.
机译:3月7日至31日,在墨西哥城部署了离子漂移化学电离质谱仪(ID-CIMS),用于测量气相硝酸(HNO 3 )和五氧化二氮(N 2 < / sub> O 5 在墨西哥城都市区(MCMA)-2006野战期间,观测地点位于墨西哥城市区北部的墨西哥石油研究所(Instituto Mexicano delPetróleo)中,居民主要排放污染物每天晚上和清晨,HNO 3 的浓度均低于200 ppb(ppt),HNO 3 的浓度从09左右开始稳定增长:美国中部标准时间(CST)凌晨00点,在下午早些时候达到0.5到十亿分之三的峰值(ppb),然后在CST下午05:00急剧下降到不到峰值的一半。 ID-CIMS和离子色谱/质谱仪(ICMS)表明,这两种HNO 3 测量( R 2 = 0.75)。发现HNO 3 的混合比与亚微米尺寸的硝酸盐气溶胶有反相关关系,这表明气体-颗粒分配过程是决定气态HNO 3 浓度的主要因素。与矿物粉尘的不可逆反应以及通过干燥沉积造成的损失在该地点也可能很重要。在MCMA 2006野战期间,大多数时候发现N 2 O 5 低于ID-CIMS的检出限(约10 s积分时间约30 ppt),这是因为夜间表面的NO混合比例较高(> 100 ppb)。 2006年3月26日发生了一个异常,当时在多云条件下的下午晚些时候和傍晚在地面形成NO之前观察到约40 ppt N 2 O 5 现场。结果表明,在MCMA-2006野战期间,HNO 3 主要是由OH与NO 2 的反应产生,并受气体/颗粒转移和干式沉积的调节。夜间由N 2 O 5 水解产生HNO 3 的原因是NO含量高而O 3 含量低表面附近的浓度。

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