城市空气质量研究的光化学箱模型

Shengxin Jin, Kenneth Demerjian
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引用次数: 27

摘要

本研究建立的光化学盒模型(PBM)基于质量守恒原理。它有一个典型城市大小的水平域和一个由混合层高度定义的垂直维度。任何污染物的浓度是由水平平流、垂直夹带、源排放和化学反应决定的。Blackadar的一维高分辨率边界层模型(预印本,第三期)。大气湍流,扩散和空气质量,罗利,美国。满足。Soc。,第443-447页,1976;《环境科学与工程进展》,第一卷,第1期(由Pfafflin J.和Ziegler E.编辑),第50-85页。Gordon and Breach, New York, 1979)已被纳入PBM,并进一步发展为在混合层高度模拟中考虑城市热岛的影响。预测的混合层高度与观测结果吻合良好。区域酸沉积模型II (RADM2)中使用的气相化学动力学机制和早期版本的PBM已被用于计算化学反应对污染物浓度变化的贡献。对两种化学机理进行了详细的分析和比较。使用这两种化学机制模拟的污染物浓度与CO、NO、NO2和O3的现有观测值非常吻合。Madronich (J. geophys. Madronich)提出的辐射传输模型。Res.92, 9740-9752, 1987)已被纳入PBM,用于计算光化通量和光分解速率常数。高度平均和辐射校正的光解速率常数用于光化学反应。对CO、NO、NO2和O3进行的预算分析增强了我们对水平平流、垂直夹带、源排放和化学反应对其浓度总体变化率的相对贡献的理解。模型预测对城市条件下RADM2化学机制中大量的过氧自由基-过氧自由基反应不敏感。
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A photochemical box model for urban air quality study

The photochemical box model (PBM) developed in the present study is based on the principle of mass conservation. It has a horizontal domain of the size of a typical city and a vertical dimension defined by the mixed-layer height. The concentration of any pollutant is determined by horizontal advection, vertical entrainment, source emissions and chemical reactions. A one-dimensional high resolution boundary layer model by Blackadar (Preprints, Third Symp. on Atmospheric Turbulence, Diffusion, and Air Quality, Raleigh, Am. Met. Soc., pp. 443–447, 1976; Advances in Environmental Sciences and Engineering, Vol. 1, No. 1 (edited by Pfafflin J. and Ziegler E.), pp. 50–85. Gordon and Breach, New York, 1979) has been incorporated in the PBM and further developed to consider the effect of urban heat islands in the simulation of mixed layer height. The predicted mixed-layer heights compare very well with observations. The gas phase chemical kinetic mechanism used in the Regional Acid Deposition Model II (RADM2) and that of an earlier version of PBM have been used to calculate the contributions of chemical reactions to the changes of pollutant concentrations. Detailed analysis and comparisons of the two chemical mechanisms have been made. The simulated pollutant concentrations using both chemical mechanisms are in very good agreement with available observations for CO, NO, NO2 and O3. A radiative transfer model developed by Madronich (J. geophys. Res.92, 9740–9752, 1987) has been incorporated in the PBM for the calculation of actinic flux and photolytic rate constants. Height-averaged and radiation-corrected photolytic rate constants are used for the photochemical reactions. Budget analyses conducted for CO, NO, NO2 and O3 have enhanced our understanding of the relative contributions of horizontal advection, vertical entrainment, source emissions and chemical reactions to the overall rate of change of their concentrations. Model predictions are not sensitive to the large number of peroxy radical-peroxy radical reactions in the RADM2 chemical mechanism under urban conditions.

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