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Characteristics of the Interactions Pattern of Surface Ozonewith its Precursors in the Fraser Valley, British Columbia

机译:不列颠哥伦比亚省弗雷泽谷地表臭氧与其前驱物相互作用的模式特征

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Hourly raw ambient data on air criteria pollutants of the Greater Vancouver Regional District(GVRD), British Columbia were analyzed to investigate the relationships of ozone with itsprecursors (NO, NO2, NOx, and Total Volatile Organic Compounds (TVOC)) and theirinteractions. Four monitoring sites of different land habitats, namely coastal DowntownVancouver, Industrial-commercial-residential mix (Burnaby) with low elevated topography (upto 400 m), inland industrial-commercial-residential mix (Surrey) with relatively plain land, andMountain-based urban (Chilliwack) sites were selected for analysis.Trends of ozone and its precursors were computed. Despite relatively higher concentrations ofNOx and TVOC, the coastal site of Downtown Vancouver experienced relatively lower levels ofozone than the other urban sites as fresh NO emissions scavenges the ozone concentrations inrelatively more quantity and also for possible meteorological effects on the precursor movements.Ozone production and destruction rates varied in different land habitats with highest rates inChilliwack (approximately 1.97 ppb/hr and 2.0 ppb/hr respectively) and lowest in the downtownVancouver site (approximately 1.11 ppb/hr and 1.15 ppb/hr respectively). Distinct interactionpatterns between ozone and NO2/NO were observed in different land habitats. Regressionanalysis showed that the ratio NO2/NO, photochemical process indicator, significantly influencesozone levels at all sites but varies with different land habitats (R2: 0.25 to 0.65) and withdifferent seasons (R2: 0.04 to 0.67). Stronger relationships between NOx and TVOC at downtownVancouver, Burnaby, and Surrey indicate potential contributions of TVOC in the ozoneproduction processes of those sites.
机译:每小时分析不列颠哥伦比亚省大温哥华地区区域(GVRD)空气标准污染物的原始原始环境数据,以研究臭氧与其前体(NO,NO2,NOx和总挥发性有机化合物(TVOC))之间的关系及其相互作用。四个不同土地栖息地的监测点,分别是温哥华市中心的沿海地区,高架势低(最高400 m)的工商业-住宅混合区(伯纳比),土地相对平坦的内陆工商业-住宅混合区(萨里)和山地城市选择(Chilliwack)地点进行分析,并计算了臭氧及其前体的趋势。尽管NOx和TVOC的浓度相对较高,但温哥华市中心的沿海地区臭氧水平却低于其他市区,因为新鲜的NO排放清除了相对更多的臭氧浓度,并且还可能对前兆运动产生了气象影响。速率在不同的土地生境中各不相同,其中奇利瓦克(Chilliwack)的速率最高(分别约为1.97 ppb / hr和2.0 ppb / hr),而温哥华市中心的速率最低(分别约为1.11 ppb / hr和1.15 ppb / hr)。在不同的土地生境中观察到了臭氧与NO2 / NO之间的独特相互作用模式。回归分析表明,光化学过程指标NO2 / NO的比值显着影响所有地点的SO2水平,但随不同的土地生境(R2:0.25至0.65)和不同季节(R2:0.04至0.67)而变化。温哥华,本那比和萨里市中心的NOx与TVOC之间的联系更紧密,这表明TVOC在这些场所的臭氧生产过程中可能发挥了作用。

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