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安顺大气降水中低分子有机酸及其与贵州其它地区对比研究
其他题名Low Molecular Weight Carboxylc Acids in Precipitation,in the Rural Area of Anshun,West Guizhou Province:Comparison with Acid Precipitation in Other Areas of Guizhou,China
章炎麟
2008-12-26
学位授予单位中国科学院地球化学研究所
学位授予地点地球化学研究所
学位名称博士
关键词大气降水 低分子有机酸 亨利定律 酸度贡献 来源 沉降
摘要低分子有机酸是对流层大气的重要组成成分,广泛分布于大气中的气相、液相、气溶胶中。本文以贵州省安顺作为研究区域,在 2007 年 6 月~2008年 6月期间,收集大气降水样品118个,对降水中主要成份尤其是低分子有机酸及其对自由酸度的贡献进行了为期一年的研究。并通过与贵州其它3个地区的对比,重点讨论了大气降水中低分子有机酸时间和空间的变化规律、成因机制、对降水自由酸度的贡献以及来源等关键问题。得出的主要结论如下: (1) 安顺降水总体呈酸性,pH雨量加权平均值为 4.89,范围在3.57~7.09,酸雨频率为 57.0%。降水的电导率平均值为46.52μs•cm-1,变化范围为6.01~298.00 μs•cm-1,该值远远高于降水背景站点,表明该地区受到了明显的人为活动影响。 (2) 安顺大气降水中离子浓度的顺序依次为SO42->Ca2+>NH4+>NO3-> Mg2+>K+>Na+>Cl->H+>HCOOHt>CH3COOHt >(COOH)2(t)2-。大气降水中最重要的离子为SO42-、NO3-(阴离子)和Ca2+、NH4+ 和Mg2+(阳离子),平均浓度依次为140.9、46.1、124.2、45.4和36.2µmol/L。相关性分析和聚类分析表明,安顺SO2和NOx具有同源特征,且进入降水的途径相同。大气中的铵主要以硫酸铵与硝酸铵的形式存在于大气中,成为大气中重要的酸性气溶胶。另外,CaSO4、NaCl、MgCl2、(NH4)2SO4、NH4NO3、KNO3、H2SO4、HNO3是降水的主要化学组分。降水中Ca2+、NH4+、Mg2+和K+的中和因子分别为0.38、0.14、0.22、0.05,表明降水中最重要的中和物质是Ca2+,其次是Mg2+和NH4+。源分析表明,安顺大气降水中的K+和Ca2+主要来自以岩石和土壤为主的陆相输入,而SO42-和NO3-主要来自人为活动的贡献,其人为贡献量高达97.0%和94.3%。Mg2+主要来自陆源输入,仅有9.1%来自海水的贡献。Cl-属于海盐性离子,但在安顺降水中,仅有57.3%来自海相输入,小部分(1.3%)来自岩石和土壤风化的贡献,人类活动排放的Cl-也是该地区一个重要来源。 (3) 安顺大气降水中共检测出7种低分子有机酸,含量最高的有机酸组成依次是甲酸(HCOO-)、乙酸(CH3COO-)和草酸((COO)22-),雨量加权平均浓度分别为8.77、6.90和2.84µmol/L。降水中所测有机酸的平均总含量为19.00µmol/L,对阴离子总和的贡献为12.6%。对于 pH<5 的降水,甲酸、乙酸和草酸对自由酸度的平均贡献值(按最大贡献率法计算)分别为 19.2%、5.9和7.8%,总有机酸(三者之和)对自由酸度的平均贡献值为32.9%。这些事实表明,安顺大气降水中的有机酸是降水化学物质的重要组成部分,会对降水的物理和化学特征产生重要的影响。采样期间,安顺甲酸、乙酸和草酸的湿沉降通量分别为10.81、10.46和3.94 mmol/m2/year。根据气液平衡理论,估算出甲酸和乙酸的干沉降量,分别为4.78和1.63mmol/m2/year。 (4) 安顺降水有机酸浓度存在着明显的季节性变化,四季的有机酸浓度由高到低分别为:冬季>春季>夏季>秋季;非生长季节>生长季节。这种季节变化特征显然与植物生长的季节变化特征不一致。表明安顺大气中的有机酸浓度的影响因素非常复杂;植物生长、降雨量(降雨强度和持续时间)和人为活动等因素的季节变化都会影响大气有机酸的组成和分布特征。在连续降雨过程的监测中发现甲酸和乙酸的浓度是随降雨过程(时间)同步变化,这说明甲酸与乙酸很可能存在相同的来源或者相似的源强,它们在大气中的清除方式也可能相同。而草酸的浓度与日照强度和温度有关,与降雨发生的时间有很重要的关系,表明草酸多来源于光化学反应为主的间接来源。另外,还发现降雨初期降水酸性要强于降雨后期,这表明降雨对大气中污染物质有明显的清除和稀释作用。 (5) 相关性分析表明,甲酸和乙酸之间存在显著的相关关系,相关系数为0.80,这种强烈的正相关表明甲酸和乙酸具有相似的排放源或者排放源不同但有相似的排放强度;草酸与甲酸和乙酸也都具有显著相关关系,这可能是因为草酸与甲酸和乙酸具有相同的排放源或者是草酸的前体物如甲醛与甲酸、乙酸具有相似的排放源;甲酸与NH4+、NO3- 和NO2-的相关关系也很高,表明甲酸的主要来源是农业活动或者生物质燃烧和汽车尾气排放等。乙酸和草酸的情况与甲酸类似。论文建立了甲酸与乙酸分析浓度比值(F/A)T的判定方程曲线,结果表明安顺有机酸主要来源于直接来源,包括植物直接释放,生物质燃烧,汽车尾气排放等;间接来源如不饱和碳烃化合物(如烯烃和异戊二烯)和醛类物质(如甲醛)的光化学氧化不是该地区有机酸的主要来源。 (6) 对比贵州其它3个监测站点的降雨数据后,发现大气降水对降水酸度的贡献,偏远地区(尚重)要远大于工业城市。另外,安顺和尚重大气有机酸以直接来源为主。其中,尚重有机酸的主要来源是植物释放,而安顺有机酸的主要来源是生物质燃烧、汽车尾气等人类活动的释放。贵阳市有机酸的主要来源是间接来源,即有机酸前体物的光化学氧化。遵义有机酸的来源具有明显的季节周期性,在夏秋以直接释放为主,而春冬季节以间接释放为主。
其他摘要Low Molecular Weight(LMW) Carboxylc Acids is the important and ubiquitous chemical constituents in the atmosphere. A comprehensive study on the chemical compositions of wet precipitation was carried out from June 2007 to June 2008 in Anshun, west of Guizhou Province,China. During this periord,118 rainwater samples were collected and seven LMW carboxylic acids were determined;in addition, the major inorganic anions and cations were also analyzed to elucidate their occurrence, variation, possible sources and deposition. To gain an insight into the state of air pollution in southwest China and regional variations in rain acidity, we compared the chemistry of precipitation among major cities and remote area in Guizhou. The main conclusions are as follows: (1) The pH of rainwater in Anshun varied from 3.57 to 7.09 with an annual volume weighted average(VWA) 4.89 which is typical acidic value. About 53.0% of the rainwater had a pH of less than 5.6. The conductivity of rainwater varied from 6.01~298.00μS/cm with a mean 46.52μS/cm, which showed the serious air pollution in this region. (2) The concentrations in the precipitation of Anshun showed in this order: SO42->Ca2+>NH4+>NO3->Mg2+>K+>Na+>Cl->H+>HCOOHt>CH3COOHt>(COOH)22-. SO42-, Ca2+, Mg2+, NH4+ and NO3- were the dominate ions in rainwater. Their VWM concentrations were 140.9, 124.2, 36.2, 45.4 and 31.50μmol/l. It demonstrated SO42- and NO3- were important contributors of acidity. Ca2+ , NH4+ and Mg2+ buffered the precipitation acidity. Significant correlations were found soil-derived species among Ca2+ and Mg2+ and sea-salt species between Na+ and C1-. Other relative good correlations were observed between SO42- and NO3- due to their similar sources. Enrichment factor showed the sources of inorganic ions. Burning coal used by human activity is responsible for the sources of SO42-, while the soil and lime dust claimed the sources of Ca2+. NO3- mainly originated from the NOx emitted by factories. Mg2+ was mainly from terrestrial input with limited amount from marine. NH4+ had sever sources such as nitrogen fertilizer production and consumption. Cl- in precipitation of Anshun was primarily from sea-source,but anthropogenic sources including the emission of HCl and Cl2 clamed the other main origin. (3) Seven LMW carboxylic acids were determined in rainwater, they are formic, acetic, oxalic, pyruvic, propanic, methanesulfonic, and lactic acid. Formic,acetic and oxalic acids were found to be the three dominate carboxylic acids with the VWM concentrations of 8.77, 6.90, 2.84 μmol/l respectively. The total concentration of organic acids was 19.0 μmol/l, accounting for 12.6 % of the total anions. And carboxylic acids were estimated to account for 32.9 of the free acidity in rainwater(when pH<5). During the research period, the wet deposition flux of formic,acetic and oxalic acids were 10.81, 10.46, and 3.94 mmol/m2/yr repectively. Based on Henry’s Law, the dry deposition flux was 4.78 and 1.63mmol/m2/yr for formic and acetic acids. (4) The concentration of organic acids in seasons followed in the order: Winter>Spring>Summer>Autumn,showing remarkable seasonal variations. Furthermore, the acids often decreased with time in a precipitation event, indicating that organic acids are primarily scavenged from blow cloud. And the organic acids were found higher in the non-growing season than in the growing season. This seasonal variation indicated these LWM acids was not primarily from emission by vegetation’s growth. (5) With the high coefficient of 0.80, formic is significantly correlated with acetic acid, suggesting that two kinds of acids shared similar sources. From other statistical analysis,such as correlation analysis and principal component analysis in precipitation, it was suggeted that the LMW carboxylic acids in Anshun should be highly complicated; that is to say, both biogenic and anthropogenic sources might contribute to organic acids in atmosphere.Based on the Henry’s Law, we proposed the ratio of formic and acetic acids in the precipitation((F/A)aq) as the indicator of the sources, and thus found that the pollution were direct emissions from natural or anthropogenic sources . (6) Comparison with acid precipitation in other urban and rural cities in Guizhou was disscussed. There was a urban–rural-remote decreasing trend in the contributions of LMW carboxylc Acids acids to free acidity in rainwater within Guizhou. The rainwater in Guizhou showed remarkable spatial variations in concentration,deposition flux and possible sources of organic acids.Direct emission from vegetation accounted for main sources in Shangzhong Town, representative of remote area,while biomass burning and vehicular emissions in Anshun, representative of rural area. And organic acids in Guiyang might come primarily from products of the photochemical reactions of unsaturated hydrocarbon.A more complicate situation was found in Zunyi,that sourses of organic acids existed seasonal variation; the secondary sources were responsible for the organic acids in the Spring and Winter, while primary emissions claimed the sources in the Summer and Autumn.
页数90
语种中文
文献类型学位论文
条目标识符http://ir.gyig.ac.cn/handle/352002/3520
专题研究生_研究生_学位论文
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章炎麟. 安顺大气降水中低分子有机酸及其与贵州其它地区对比研究[D]. 地球化学研究所. 中国科学院地球化学研究所,2008.
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