西安市降雪中DOM荧光特性和来源分析 |
摘要点击 2770 全文点击 1132 投稿时间:2019-07-08 修订日期:2019-09-29 |
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中文关键词 降雪 溶解性有机物 荧光特性 平行因子分析 后向轨迹模型 来源 |
英文关键词 snowfall dissolved organic matter fluorescence characteristics parallel factor analysis backward trajectory model source |
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中文摘要 |
利用三维荧光光谱、平行因子分析模型和后向轨迹模型等,分析西安市降雪中溶解性有机物(DOM)的荧光特性和来源,研究结果可为大气有机污染物的化学组成和来源分析提供数据基础.结果表明,降雪DOM的DOC含量为0.88~10.92 mg·L-1,主要含有类腐殖质、类富里酸、类色氨酸和类酪氨酸,它们荧光强度及其总和与DOC和UV254呈显著正相关(P<0.01).降雪过程中DOM的荧光指数(FI)、生物源指数(BIX)和腐殖化指数(HIX)值分别为1.50~1.75、0.87~1.25和1.11~1.97,且FI与BIX和HIX分别呈正相关和负相关(P<0.05).降雪期间气团传输轨迹包括:本地源、起始于新疆(途经甘肃、宁夏)的长距离传输、起始于内蒙古(途经宁夏)和山东(途经河南)的中距离传输,分别占总量的38.78%、24.04%、19.87%和17.31%.结果也表明,可利用代表类腐殖质、类富里酸、类色氨酸和类酪氨酸荧光峰的荧光强度与其总和表征降水中DOM的含量或相对含量,降雪中DOM兼具生物源和陆源,属于自生来源且有机质为新近产生或具有较强自源特征,本地源对降雪DOM的来源贡献最为显著. |
英文摘要 |
Fluorescence characteristics and sources of dissolved organic matter (DOM) in snowfall in Xi'an were studied by three-dimensional fluorescence spectroscopy, parallel factor analysis, and backward trajectory model, which provided a data basis for the analysis of the chemical composition and source of atmospheric organic pollutants. Results show that the DOC content of DOM was 0.88-10.92 mg·L-1. DOM mainly contained humus-like, fulvic acid-like, tryptophan-like, and tyrosine-like substances. The fluorescence intensity and the summed intensities of these substances exhibited significant positive correlations with the DOC and UV254 (P<0.01). The fluorescence index (FI), biological source index (BIX), and humic index (HIX) values of DOM during snowfall were 1.50-1.75, 0.87-1.25, and 1.11-1.97, respectively. FI was positively correlated with BIX and negatively correlated with HIX (P<0.05). During snowfall, the air mass transmission trajectories included the local transmission, long-distance transmission starting from Xinjiang (through Gansu and Ningxia), and medium-distance transmissions starting from Inner Mongolia (through Ningxia) and Shandong (via Henan), accounting for 38.78%, 24.04%, 19.87%, and 17.31% of the total, respectively. This indicates that the content or relative content of the DOM contained in the precipitation can be characterized by fluorescence intensities and their sums of the humic-like, fulvic acid-like, tryptophan-like, and tyrosine-like tyrosine. The DOM in snowfall had both biological and terrestrial characteristics, and belonged to a self-generated source with the newly produced organic matter or matter with stronger self-source characteristics. Local transmission had the most significant contribution to the source of snowfall DOM. |
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