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首页> 外文期刊>Atmospheric environment >Time-resolved inorganic chemical composition of fine aerosol and associated precursor gases over an urban environment in western India: Gas-aerosol equilibrium characteristics
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Time-resolved inorganic chemical composition of fine aerosol and associated precursor gases over an urban environment in western India: Gas-aerosol equilibrium characteristics

机译:印度西部城市环境中精细气溶胶及其伴生前体气体的时间分辨无机化学成分:气溶胶平衡特征

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Inorganic ionic constituents (Na+, NH4+, K+, Mg2+, Ca2+, Cl-, NO3- and SO42-) of PM2.5 and associated trace gases (NH3, HNO3 and HCl) were measured simultaneously by Ambient Ion Monitor - Ion Chromatograph (AIM-IC) system with a time resolution of one hour at an urban location in semi-arid region of western India during summer and winter. The average NH3, HNO3 and HCl concentrations were 11.6 +/- 5.0, 2.9 +/- 0.8 and 0.15 mu g m(-3), respectively, during winter. During summer, NH3 and HNO3 concentrations were of similar magnitude, whereas HCl concentration was less than similar to 0.03 mu g m(-3). NH3 concentration exhibited a distinct diurnal variation during both seasons. However, HNO3 did not show a specific diurnal trend during the observation period in both seasons. The data obtained were used to study gas-aerosol equilibrium characteristics using a thermodynamic equilibrium model, ISORROPIA The results suggest that NH3 exists in equilibrium between measured fine-mode particle and gas phase with a systematic bias of similar to 14%, whereas HCl and HNO3 deviate significantly from the modelled data. These observations have implications on thermodynamic equilibrium assumptions used for estimating various aerosol parameters such as liquid water content, pH, etc., thus causing significant bias in chemical transport model results over the study region. (C) 2015 Elsevier Ltd. All rights reserved.
机译:通过环境离子监测仪-离子色谱仪(AIM)同时测量PM2.5的无机离子成分(Na +,NH4 +,K +,Mg2 +,Ca2 +,Cl-,NO3-和SO42-)和相关的痕量气体(NH3,HNO3和HCl) -IC)系统,夏季和冬季在印度西部半干旱地区的城市位置,其时间分辨率为一小时。在冬季,平均NH3,HNO3和HCl浓度分别为11.6 +/- 5.0、2.9 +/- 0.8和0.15μg m(-3)。在夏季,NH3和HNO3的浓度相似,而HCl的浓度小于0.03μgm(-3)。在两个季节中,NH3浓度表现出明显的昼夜变化。但是,HNO3在两个季节的观察期内均未显示出特定的昼夜趋势。使用热力学平衡模型ISORROPIA,将获得的数据用于研究气溶胶平衡特性。结果表明,在被测细模式颗粒与气相之间存在平衡的NH3,系统偏差约为14%,而HCl和HNO3与建模数据有很大差异。这些观察结果对用于估算各种气溶胶参数(例如液态水含量,pH等)的热力学平衡假设有影响,从而在研究区域内的化学传输模型结果中造成明显偏差。 (C)2015 Elsevier Ltd.保留所有权利。

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