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首页> 外文期刊>Journal of earth system science >Investigating daytime and night-time differences with the seasonal trend and sources of inorganic fine aerosols in Indo-Gangetic plain
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Investigating daytime and night-time differences with the seasonal trend and sources of inorganic fine aerosols in Indo-Gangetic plain

机译:利用印度洋-恒河平原的季节趋势和无机细小气溶胶的来源调查白天和晚上的差异

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摘要

This study investigates the seasonal distribution of inorganic aerosols in Central New Delhi and identifies their potential source regions using concentration weighted trajectories (CWTs). Secondary inorganic aerosols (NO$_{3}^{-}$, SO$_{4}^{2-}$, NH$_{4}^{+}$) are the largest contributors to fine particulate matter in New Delhi, India. The concentrations of secondary inorganic aerosols showed very distinct seasonal patterns with higher concentrations in winter and post-monsoon seasons. Inorganic ions Ca$^{2+}$, Mg$^{2+}$ and K$^{+}$ were also examined to understand their temporal trends. The primary aerosols were found to have smaller diurnal differences than secondary aerosols. The higher coefficient of divergence for secondary aerosols indicated a significant difference in their chemistry and/or meteorology during daytime and night-time, respectively. The backward trajectory analysis revealed the advection of ionic species from distant sources responsible for their significant seasonality. The highest concentrations of K$^{+}$ during the post-monsoon season were mainly influenced by air masses arriving from Punjab and Haryana regions resulting from the prominent agricultural crop residue burning in these areas. CWT also identified the Thar Desert and Punjab as potential regions for enhanced levels of Ca$^{2+}$ and K$^{+}$, respectively. Also, the brick kilns located in western UP were observed as the major potential sources for NO$_{3}^{-}$ and SO$_{4}^{2-}$.
机译:这项研究调查了新德里中部无机气溶胶的季节分布,并使用浓度加权轨迹(CWT)确定了其潜在的源区。次生无机气溶胶(NO $ _ {3} ^ {-} $,SO $ _ {4} ^ {2-} $,NH $ _ {4} ^ {+} $)是造成细粒物质的最大贡献者印度新德里。次生无机气溶胶的浓度表现出非常明显的季节模式,在冬季和季风后季节浓度较高。还检查了无机离子Ca $ ^ {2 +} $,Mg $ ^ {2 +} $和K $ ^ {+} $,以了解其时间趋势。发现主要气溶胶的昼夜差异小于次要气溶胶。次生气溶胶的较高发散系数分别表明其白天和晚上的化学和/或气象学差异显着。向后的轨迹分析表明,来自遥远源头的离子物种的平流导致其明显的季节性。在季风后季节,K $ ^ {+} $的最高浓度主要受到旁遮普邦和哈里亚纳邦地区产生的空气质量的影响,这些地区的农业作物残渣燃烧突出。 CWT还确定塔尔沙漠和旁遮普邦分别是潜在的Ca $ ^ {2 +} $和K $ ^ {+} $含量升高的区域。而且,位于UP西部的砖窑被认为是NO $ _ {3} ^ {-} $和SO $ _ {4} ^ {2-} $的主要潜在来源。

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