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The heterogeneous chemistry of mineral dust and sea salt and their components with trace atmospheric gases.

机译:矿物粉尘和海盐及其成分与微量大气气体的异质化学。

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Tropospheric aerosols can have a significant impact on the Earth's atmosphere, specifically through health effects, effects on the biogeochemical cycle and climate forcing. These aerosols react with trace atmospheric gases such as nitrogen oxides, sulfur oxides, and organics through heterogeneous chemistry which can alter their effect on the atmosphere. It is estimated that 1000--3000 Tg of mineral aerosols are emitted into the atmosphere annually. Calcite, CaCO3 and oxides such as MgO, Al2O 3 and SiO2 are all common components of aerosol particles in the troposphere. Sea salt is also a common aerosol found in the troposphere and has an estimated annual integrated flux on the order of 2800 Tg NaCl yr -1. Mineral dust and sea salt are both often represented as single entity aerosols. However, this is a poor representation of the rich mineralogy and varying chemical composition of mineral dust as well as the multi-component nature of sea salt.; In this dissertation research, several state of the art analytical techniques were used for the first time to study heterogeneous reactions. These techniques include scanning electron microscopy (SEM), computer-controlled SEM, environmental SEM and energy-dispersive X-ray (EDX) microanalysis. They were used to monitor and quantify phase transitions, morphology changes and compositional changes of individual particles of calcium carbonate, NaCl, sea salt and dust particles from 4 different dust source regions, as they are reacted with nitric acid and monitored as a function of time and relative humidity. Atomic force microscopy was also used to monitor the nanometer-scale changes in surface structures of freshly cleaved CaCO3(101¯4) and MgO(100) as they are allowed to age under ambient conditions as well as reacted with nitric acid. Finally, Fourier-transform infrared spectroscopy was used to investigate the adsorption of several gases (HNO3, CH3COOH, CH3OH and SO2) and chemical nature of adsorbed species on carbonate and oxide surfaces including CaCO3, alpha-Al2O3 and SiO2.
机译:对流层气溶胶可以对地球大气产生重大影响,特别是对健康的影响,对生物地球化学循环的影响和气候强迫。这些气溶胶通过异质化学物质与微量的大气气体(如氮氧化物,硫氧化物和有机物)发生反应,从而改变其对大气的影响。据估计,每年有1000--3000 Tg的矿物气溶胶排放到大气中。方解石,CaCO3和氧化物(例如MgO,Al2O 3和SiO2)都是对流层气溶胶颗粒的常见成分。海盐也是对流层中常见的气溶胶,估计年总通量约为2800 Tg NaCl yr -1。矿物粉尘和海盐通常都被表示为单实体气溶胶。但是,这不能很好地说明矿物粉尘的丰富矿物学特征和化学成分的变化以及海盐的多组分性质。在本文的研究中,首次使用了几种最先进的分析技术来研究异质反应。这些技术包括扫描电子显微镜(SEM),计算机控制的SEM,环境SEM和能量分散X射线(EDX)显微分析。它们用于监测和量化来自4个不同粉尘源区域的碳酸钙,NaCl,海盐和粉尘颗粒的单个颗粒的相变,形态变化和组成变化,因为它们与硝酸反应并作为时间的函数进行监测和相对湿度。原子力显微镜还用于监测刚裂解的CaCO3(101’4)和MgO(100)在环境条件下老化并与硝酸反应后表面结构的纳米级变化。最后,利用傅立叶变换红外光谱技术研究了碳酸盐和氧化物表面(包括CaCO3,α-Al2O3和SiO2)上几种气体(HNO3,CH3COOH,CH3OH和SO2)的吸附以及吸附物质的化学性质。

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