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Modelling the contribution of biogenic volatile organic compounds to new particle formation in the Jülich plant atmosphere chamber

机译:模拟朱利希工厂大气室中生物挥发性有机化合物对新颗粒形成的贡献

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We used the Aerosol Dynamics gas- and particle-phase chemistry model forlaboratory CHAMber studies (ADCHAM) to simulate the contribution of BVOCplant emissions to the observed new particle formation during photooxidationexperiments performed in the Jülich Plant-AtmosphereChamber and to evaluate how well smog chamber experiments can mimic theatmospheric conditions during new particle formation events. ADCHAM couplesthe detailed gas-phase chemistry from Master Chemical Mechanism with a novelaerosol dynamics and particle phase chemistry module. Our model simulationsreveal that the observed particle growth may have either been controlled bythe formation rate of semi- and low-volatility organic compounds in thegas phase or by acid catalysed heterogeneous reactions betweensemi-volatility organic compounds in the particle surface layer (e.g.peroxyhemiacetal dimer formation). The contribution of extremelylow-volatility organic gas-phase compounds to the particle formation andgrowth was suppressed because of their rapid and irreversible wall losses,which decreased their contribution to the nano-CN formation and growthcompared to the atmospheric situation. The best agreement between themodelled and measured total particle number concentration (R2 > 0.95)was achieved if the nano-CN was formed by kinetic nucleation involving bothsulphuric acid and organic compounds formed from OH oxidation of BVOCs.
机译:我们将气溶胶动力学气相和颗粒化学模型用于实验室CHAMber研究(ADCHAM),以模拟在JülichPlant-AtmosphereChamber进行的光氧化实验中,BVOC植物排放物对观察到的新颗粒形成的贡献,并评估雾化室实验的效果在新的粒子形成过程中模拟大气条件。 ADCHAM将“主化学机理”中的详细气相化学与新型气溶胶动力学和颗粒相化学模块相结合。我们的模型仿真表明,观察到的颗粒生长可能是由气相中半挥发性和低挥发性有机化合物的形成速率控制的,也可能是由颗粒表面层中半挥发性有机化合物之间的酸催化异质反应(例如过氧半缩醛二聚体的形成)控制的。挥发性极低的有机气相化合物由于其快速且不可逆的壁损而对颗粒形成和生长的贡献得到抑制,与大气相比,它们对纳米CN的形成和生长的贡献减少了。如果纳米CN是通过涉及硫酸和形成的有机化合物的动力学成核而形成的,则可以达到模型总颗粒数浓度与实测总颗粒数浓度( R 2

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