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Heterogeneous studies of atmospheric pollutants, nitric acid, nitrogen pentoxide, and hydroxide radicals, with sodium chloride, sodium nitrate, and synthetic sea salt using multiple analytical methods.

机译:使用多种分析方法,用氯化钠,硝酸钠和合成海盐对大气污染物,硝酸,五氧化二氮和氢氧化物自由基进行异构研究。

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Heterogeneous reactions involving sea salt aerosols and oxides of nitrogen are a potential source of photolyzable halogen compounds in the marine boundary layer. Specifically, the reactions of HNO3 and N2O 5 with NaCl, the major component in sea salt aerosols, results in production of gas phase HCl and ClNO2 leaving NaNO3 remaining within on particles. Experiments were conducted to elucidate a number of issues: (1) the reaction probability of each of the gases with NaCl; (2) the phase of NaNO3 aerosols and mixed aerosols of NaNO3 and NaCl under low relative humidity conditions; and (3) the extent to which the presence of nitrate affects the reactivity of chloride ions toward OH radicals. A number of analytical techniques were utilized including a Knudsen cell coupled to a quadrupole mass spectrometer, scanning electron microscopy with energy dispersive analysis of X-rays, and long path Fourier transform infrared spectroscopy.; Knudsen cell studies were conducted using less than one layer of salt particles and a new model was applied to account for the true available salt surface area. Reaction probabilities were determined to be (1.0 ± 0.8) × 10−3 and (2.9 ± 1.7) × 10 −3 for HNO3 and N2O5, respectively. Additionally, new models are proposed for each reaction involving water adsorbed on the salt surface. The data suggest that the reaction of HNO3 with effluoresced sea salt particles is less important than previously thought relative to reactions with N2O5 and ClONO2, which generate chlorine atom precursors, leaving nitrate remaining on the particles.; Hydration and dehydration studies of NaNO3 particles indicate that they exist as unusual metastable, amorphous solids at low relative humidities, and undergo continuous hygroscopic growth with increasing relative humidity. Mixed aerosol particles of NaCl and NaNO3 are shown to be comprised of a core of NaCl surrounded by a mixed layer of nitrate and chloride. Additionally, the presence of nitrate in these particles is found to actually enhance the depletion of chloride upon reaction with OH radicals, compared to reaction with NaCl particles alone.
机译:涉及海盐气溶胶和氮氧化物的多相反应是海洋边界层中可光解卤素化合物的潜在来源。具体来说,HNO 3 和N 2 O 5 与海盐气溶胶中主要成分NaCl的反应导致气相产生HCl和ClNO 2 留下的NaNO 3 留在颗粒上。进行实验以阐明许多问题:(1)每种气体与NaCl的反应概率; (2)在低相对湿度条件下,NaNO 3 气溶胶的相以及NaNO 3 和NaCl的混合气溶胶; (3)硝酸盐的存在影响氯离子对OH自由基的反应程度。利用了许多分析技术,包括耦合到四极质谱仪的Knudsen池,具有X射线能量色散分析的扫描电子显微镜和长距离傅里叶变换红外光谱。使用少于一层的盐颗粒进行了Knudsen细胞研究,并应用了一个新模型来说明真实的可用盐表面积。 HNO 3 和HNO <3的反应概率确定为(1.0±0.8)×10 -3 和(2.9±1.7)×10 -3 N 2 O 5 。另外,针对涉及吸附在盐表面上的水的每个反应,提出了新模型。数据表明,相对于与N 2 O 5 和N 2 O 5 的反应,HNO 3 与氟化海盐颗粒的反应没有以前想象的重要。 ClONO 2 ,生成氯原子前体,使硝酸盐残留在颗粒上。 NaNO 3 颗粒的水合和脱水研究表明,它们在低相对湿度下以不寻常的亚稳态无定形固体形式存在,并且随着相对湿度的增加而不断吸湿生长。 NaCl和NaNO 3 的混合气溶胶颗粒显示为由NaCl的核包裹,被硝酸盐和氯化物的混合层包围。另外,与仅与NaCl颗粒反应相比,发现这些颗粒中硝酸盐的存在实际上增强了与OH自由基反应时氯化物的消耗。

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