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Radical chemistry at a rural site (Wangdu) in the North China Plain: observation and model calculations of OH, HO2 and RO2 radicals

机译:在华北地区的农村遗址(王都)的激进化学:OH,HO2和RO2自由基的观察和模型计算

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A comprehensive field campaign was carried out in summer 2014 in Wangdu, located in the North China Plain. A month of continuous OH, HO2 and RO2 measurements was achieved. Observations of radicals by the laser-induced fluorescence (LIF) technique revealed daily maximum concentrations between (5–15)??×?106?cm?3, (3–14)??×?108?cm?3 and (3–15)??×?108?cm?3 for OH, HO2 and RO2, respectively. Measured OH reactivities (inverse OH lifetime) were 10 to 20?s?1 during daytime. The chemical box model RACM 2, including the Leuven isoprene mechanism?(LIM), was used to interpret the observed radical concentrations. As in previous field campaigns in China, modeled and measured OH concentrations agree for NO mixing ratios higher than 1?ppbv, but systematic discrepancies are observed in the afternoon for NO mixing ratios of less than 300?pptv (the model–measurement ratio is between 1.4 and 2 in this case). If additional OH recycling equivalent to 100?pptv NO is assumed, the model is capable of reproducing the observed OH, HO2 and RO2 concentrations for conditions of high volatile organic compound (VOC) and low NOx concentrations. For HO2, good agreement is found between modeled and observed concentrations during day and night. In the case of RO2, the agreement between model calculations and measurements is good in the late afternoon when NO concentrations are below 0.3?ppbv. A significant model underprediction of RO2 by a factor of 3 to 5 is found in the morning at NO concentrations higher than 1?ppbv, which can be explained by a missing RO2 source of 2?ppbv?h?1. As a consequence, the model underpredicts the photochemical net ozone production by 20?ppbv per day, which is a significant portion of the daily integrated ozone production (110?ppbv) derived from the measured HO2 and RO2. The additional RO2 production from the photolysis of ClNO2 and missing reactivity can explain about 10?% and 20?% of the discrepancy, respectively. The underprediction of the photochemical ozone production at high NOx found in this study is consistent with the results from other field campaigns in urban environments, which underlines the need for better understanding of the peroxy radical chemistry for high NOx conditions.
机译:综合外地运动是在2014年夏季在王都进行的,位于华北平原。实现了一个月的连续OH,HO2和RO2测量。通过激光诱导的荧光(LiF)技术观察激光诱导的荧光(LiF)技术揭示了(5-15)×106°3之间的每日最大浓度(3-14)??×108?cm?3和(3 -15)??×108?cm 2,分别用于OH,HO2和RO2。在白天期间,测量的OH反应性(反应oh寿命)为10至20μl?1。化学盒模型RACM 2,包括Leuven Isoprene机制?(LIM),用于解释观察到的自由基浓度。与中国以前的野战活动一样,建模和测量的OH浓度不同意不高于1?PPBV的混合比,但在午后未观察到系统差异,没有少于300μm≤PPTV(模型 - 测量比在在这种情况下1.4和2)。如果假设额外的OH回收相当于100?PPTV NO,则该模型能够再现观察到的OH,HO2和RO2浓度,用于高挥发性有机化合物(VOC)和低NOx浓度的条件。对于HO2,在白天和夜晚的建模和观察到的浓度之间发现了良好的协议。在RO2的情况下,模型计算与测量之间的协议在下午晚些时候在没有浓度低于0.3℃时良好.PPBV。在早晨,在没有高于1〜PPBV的浓度下,在早晨发现Ro2的显着模型欠鉴定为3至5倍,这可以通过缺失的RO2源2〜PPBV源来解释。因此,该模型估计了光化学净臭氧产量为20?PPBV每天PPBV,这是来自测量的HO2和RO2的每日集成臭氧生产(110〜PPBV)的重要部分。从ClNO2的光解和缺失反应性的额外RO2产生分别可以分别解释约10?%和20?%差异。本研究发现的高NOx下光化学臭氧产生的潜在潜在的臭氧产量与城市环境中其他场地活动的结果一致,这强调了更好地了解高NOx条件的过氧自由基化学。
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