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Ammonia emissions, concentrations and implications for particulate matter formation in Houston, TX

机译:德克萨斯州休斯顿的氨气排放,浓度和对颗粒物形成的影响

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摘要

Seasonal average observational data, photochemical modeling analyses, and detailed observational data for a summer air pollution episode were used to assess the spatial and temporal distribution of ammonia-rich and ammonia poor conditions in southeast Texas. Seasonal average observational data and photochemical modeling analyses both suggest ammonia rich conditions throughout southeast Texas, but not enough ammonia present to create elevated concentrations of ammonium nitrate, except during morning hours. Analyses of ambient data available for the summer air pollution episode (which was also the modeled episode) indicate that ammonia-poor conditions may be more pervasive in southeast Texas during periods of intense photochemistry. Overall, the results of all three methods are consistent in suggesting that average ammonia availability in southeast Texas is comparable to the ammonia required to neutralize sulfate. Temporal and spatial variability in sulfate formation creates morning excesses of ammonia (leading to some morning nitrate formation) and ammonia poor conditions in SO_2 plumes and during periods of high photochemical activity.
机译:使用季节性平均观测数据,光化学模型分析和夏季空气污染事件的详细观测数据,来评估德克萨斯州东南部富氨和贫氨条件的时空分布。季节性平均观测数据和光化学模型分析均表明,得克萨斯州东南部地区氨水含量丰富,但除早间外,氨水含量不足以产生较高浓度的硝酸铵。对夏季空气污染事件(也是模拟事件)可用的环境数据的分析表明,在强烈的光化学作用期间,得克萨斯州东南部的氨缺乏条件可能更普遍。总体而言,这三种方法的结果一致,表明德克萨斯州东南部的平均氨利用率与中和硫酸盐所需的氨相当。硫酸盐形成的时间和空间变化会在早晨产生过量的氨(导致早晨形成硝酸盐),并在SO_2羽流和高光化学活性期间形成氨缺乏的条件。

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