关中典型城市及农村夏季PM2.5的化学组成对比

于2016年7~8月采集了陕西省西安市（城市）及蔺村（农村）夏季昼夜PM_2.5样品,分析其有机碳（OC）、元素碳（EC）和无机离子等化学组分的含量,探讨关中平原城市和农村地区PM_2.5的化学组成和来源的差异.结果表明,采样期间西安和蔺村的PM_2.5浓度分别为（49.7±22.8）和（62.6±14.2）μg/m³.西安PM_2.5中OC和EC的浓度[（6.5±2.5）μg/m³,（3.2±1.8）μg/m³]与蔺村[（6.8±1.8）μg/m³,（3.8±2.3）μg/m³]相当.西安OC/EC比值白天（2.6）高于夜晚（1.9）,蔺村反之（白天：1.6;夜晚：2.7）,主要是因为夜间城市地区重型卡车运输活动增强导致排放更多EC,而夜间农村地区人为活动较少导致EC排放显著降低.西安和蔺村无机离子总浓度分别为（20.2±14.6）和（30.1±10.5）μg/m³,占PM_2.5浓度的40.6%和47.6%.蔺村SO₄^2-的平均浓度高达19.0μg/m³,占PM_2.5浓度的30%以上,远高于西安（9.4μg/m³和18.9%）,主要与农村固体燃料（煤和生物质）使用有关.西安NO₃^-和Ca²⁺的浓度及其对PM_2.5的贡献、NO₃^-/SO₄^2-比值均明显大于蔺村,表明城市地区受机动车尾气和扬尘的影响更大.西安K⁺与Ca²⁺和Mg²⁺的相关性较强,而蔺村K⁺与EC的相关性显著强于西安,说明西安市区K⁺由粉尘源主导,而农村地区则主要来自生物质燃烧.     

基于稳定碳同位素技术的干旱区绿洲土壤有机碳向无机碳的转移

应用稳定碳同位素技术测定土壤无机碳稳定碳同位素组成(soil inorganic carbonδ13C,SICδ13C),并对干旱区绿洲土壤无机碳进行区分,结合土壤有机碳(soil organic carbon,SOC)与SIC含量关系进一步探讨SOC向SIC转移的碳量.结果表明,4种类型土壤SICδ13C值差异性极显著(P0.01),风沙土SICδ13C值最高且为正,均值为(0.32±0.04)‰,随土层深度增加而增加,说明风沙土原生性碳酸盐占绝对优势;灌漠土、棕漠土和盐碱土SIC的δ13C均值分别(-0.30±0.24)‰、(-1.96±0.66)‰和(-1.24±0.49)‰,随土层变化均呈先降低后逐渐增大的趋势,说明灌漠土原生性碳酸盐占优势,棕漠土和盐碱土发生性碳酸盐相对前者占优势.风沙土、灌漠土、棕漠土和盐碱土的发生性碳酸盐占SIC比例均值分别为1.33%、4.72%、15.01%、35.71%,均小于50%,说明干旱区绿洲土壤发生性碳酸盐比例总体水平较低.风沙土、灌漠土、棕漠土和盐碱土在土壤发生性碳酸盐形成或重结晶过程中固定土壤CO2的量分别为0.30、2.44、4.96、12.40 g·kg~(-1),其中固定来自大气CO2量平均为0.18、0.79、1.45、8.67 g·kg~(-1),来自SOC氧化分解转化为CO2的量分别为0.06、0.83、1.62、1.86g·kg~(-1),说明盐碱土、棕漠土SOC的贡献相对较高,灌漠土、风沙土较低;对土壤固定CO2量的来源比较发现,风沙土、盐碱土固定土壤CO2的量来自大气CO2量较高,SOC的贡献较低,而灌漠土、棕漠土固定来自SOC氧化分解CO2的量较高,大气贡献较低.研究区整体SOC向SIC的碳转移量介于0.03~2.38 g·kg~(-1)之间,平均每千克土壤固定1.09 g的CO2,说明干旱区绿洲土壤发生性碳酸盐所占比例较低,SOC的贡献较少.     

Characterization of submicron particles during autumn in Beijing, China

In this study, we performed a highly time-resolved chemical characterization of nonrefractory submicron particles(NR-PM_1) in Beijing by using an Aerodyne high-resolution time-of-flight aerosol mass spectrometer(HR-ToF-AMS). The results showed the average NR-PM_1 mass concentration to be 56.4 ± 58.0 μg/m~3, with a peak at 307.4 μg/m~3. Due to the high frequency of biomass burning in autumn, submicron particles significantly increased in organic content, which accounted for 51% of NR-PM_1 on average. Secondary inorganic aerosols(sulfate + nitrate + ammonium) accounted for 46% of NR-PM_1, of which sulfate,nitrate, and ammonium contributed 15%, 20%, and 11%, respectively. To determine the intrinsic relationships between the organic and inorganic species, we used the positive matrix factorization(PMF) model to merge the high-resolution mass spectra of the organic species and NO+and NO_2~+ions. The PMF analysis separated the mixed organic and nitrate(NO+and NO_2~+) spectra into four organic factors, including hydrocarbon-like organic aerosol(HOA), oxygenated organic aerosol(OOA), cooking organic aerosol(COA), and biomass burning organic aerosol(BBOA), as well as one nitrate inorganic aerosol(NIA) factor. COA(33%) and OOA(30%) contributed the most to the total organic aerosol(OA) mass, followed by BBOA(20%) and HOA(17%). We successfully quantified the mass concentrations of the organic and inorganic nitrates by the NO+and NO2+ions signal in the organic and NIA factors. The organic nitrate mass varied from 0.01-6.8 μg/m~3, with an average of 1.0 ±1.1 μg/m~3, and organic nitrate components accounted for 10% of the total nitrate mass in this observation.     

基于物元分析法的古建筑火灾风险评价

古建筑火灾风险评估是突发事件应对中"关口前移"的体现,以物元分析法为基础提出了古建筑火灾风险评价的物元模型,并对某世界名镇内古建筑进行风险评估。首先,在火灾风险影响因素的事故树分析基础上,选取能够反映古建筑火灾风险特性的51个指标作为评价指标体系;其次,建立古建筑火灾风险评价的物元模型;最后,根据实地调研数据进行标准化赋值,实现对古建筑火灾风险的定量化评价,通过评价方法对比验证了模型有效性和先进性。结果表明,所评价建筑的总体关联度系数为-0.248,四项"优秀"级别指标关联度分别为-0.129、-0.183、-0.211、-0.216,两项"较差"级别指标关联度为0.025、-0.016,表明所评价建筑火灾风险等级的显性结果为"优秀"级别,但隐性结果为"良好+"级别,火灾风险等级潜在提升能力较强。     

青岛采暖期不同天气状况下大气颗粒态无机氮分布研究

于2007-10～2008-04采集了青岛近海采暖前及采暖期内大气气溶胶样品,并运用离子色谱法(IC)分析了颗粒物中的无机氮组分.结果表明,采暖期内青岛颗粒物和无机氮的浓度都有明显增加,采暖期颗粒物质量浓度为137.41μg/m3,比采暖前增加了82.2%;NO3--N和NH4+-N浓度分别由采暖前的2.48μg/m3和6.95μg/m3增加到采暖期的4.43μg/m3和10.28μg/m3.天气过程对于青岛颗粒物浓度和无机氮离子浓度均有较大影响.采暖期晴天颗粒物浓度均值为181.34μg/m3,较采暖前增加32.0%,主要源于二次气溶胶的NH4+-N和NO3--N浓度分别为5.56μg/m3和1.86μg/m3,低于采暖前.雾天因为低温高湿和污染物的循环积累,样品中颗粒物、NH4+-N和NO3--N平均浓度比采暖前浓度增加了1～2倍.大风降温天气下颗粒物浓度及无机氮组分浓度均有所降低.采暖期烟尘和飞灰的排放明显影响青岛大气颗粒物和无机氮的粒径分布,特别是细粒子部分.青岛近海颗粒物及NO3--N质量浓度呈现双峰分布,采暖前峰值出现在0.43～0.65μm与3.3～4.7μm的范围内,采暖期积聚模态峰值移至0.65～1.1μm范围内.NH4+-N粒径分布均呈现明显的单峰分布,峰值出现在积聚模态.     

Evaluating the e ects of granular and membrane filtrations on chlorine demand in drinking water

In this study, chlorine decay experiments were conducted for the raw water from Nakdong River that is treated by Chilseo Water Treatment Plant (CWTP) situated in Haman, Korea as well as the e uents from sand and granular activated carbon (GAC) filters of CWTP and fitted using a chlorine decay model. The model estimated the fast and slow reacting nitrogenous as well as organic/inorganic compounds that were present in the water. It was found that the chlorine demand due to fast and slow reacting (FRA and SRA) organic/inorganic substances was not reduced significantly by sand as well as GAC filters. However, the treated e uents from those filters contained FRA and SRA that are less reactive and had small reaction rate constants. For the e uents from microfiltration, ultrafiltration, and nanofiltration the chlorine demand because FRA and SRA were further reduced but the reaction rate constants were larger compared to those of sand and GAC filter e uents. This has implications in the formation of disinfection by products (DBPs). If DBPs are assumed to form due to the interactions between chlorine and SRA, then it is possible that the DBP formation potential in the e uents from membrane filtrations could be higher than that in the e uents from granular media filters.     

基于分形方法确定合肥大兴地区土壤中Cd元素的异常下限

在土壤元素异常下限值的确定对环境地球化学评价具有重要意义,传统异常下限值计算方法仅适用于元素含量数据呈正态分布的情况,而事实上土壤元素含量的空间分布极其复杂,很可能具有多重分形分布特征,元素背景和异常有各自独立的幂指数关系。本文探讨利用分形方法确定典型工业区土壤中Cd元素的异常下限值。基于分形的含量一面积方法确定了合肥大兴地区（典型工业区）土壤中污染元素Cd的异常下限值为0．445mg／kg,并根据该异常下限值圈定了异常范围。同时与传统方法（平均值加两倍标准离差）确定的土壤中Cd元素异常下限值及异常范围进行了对比分析,结果显示,分形方法圈定的异常区域是有效的、合理的,控制了区内主要的导致土壤Cd元素污染的企业。     

长江口及邻近海域水体主元素和锶同位素地球化学

根据2005年6月对长江口及其邻近海域水体的现场调查,分析探讨了长江口水体主元素、Sr及Sr同位素的组成变化。长江河水的Sr含量和87Sr/86Sr同位素比值分别为1.75μmol/L和0.7105,反映出长江流域以碳酸盐岩风化为主的化学风化特征;河口区主元素与盐度的显著正相关关系显示出它们在河水与海水混合过程中的保守特性;87Sr/86Sr与1/Sr的非线性关系则暗示了长江口水体的Sr不是河水与海水的简单混合,可能伴有其他端元水体的混入。     

基于改进TOPSIS法的规划环评情景方案建立方法及应用

目前,情景分析法在规划环评中进行应用时,情景方案的建立方法仍存在较大不确定性。针对这一问题,结合广西石化产业规划环评,为在广西区6个重点城市分布44个石化项目建立多套可行方案,以供后续方案筛选。通过层次分析法计算出影响因素特性的权重,将改进后的多属性决策TOPSIS方法引入规划环评,并与情景分析法相结合。探讨了基于TOPSIS法对构建情景方案的影响因素进行筛选,并最终确定核心因子的新方法。结论为：利用筛选出的三种核心因子——规划相容性、资源环境因子和产业链结构——构建出了18套情景方案,作为规划环评的初始可行方案,并在三维坐标系中分别将这些方案表示出来,从而实现了将方案定量化、形象化,为规划环评中后续方案筛选提供了定量化科学依据。     

基于条件高斯模拟的城市灰尘Pb元素的空间分布特征

城市灰尘是分散于城市不同区域的表面固体颗粒物。城市灰尘对城市环境造成的污染越来越多地受到人们的关注,尤其是城市灰尘重金属对城市生存环境造成的危害。本文利用R软件中的Gstat包,对金华市城市地表灰尘中的Pb元素含量进行500次条件高斯模拟,并从中随机抽出3次模拟对其模拟结果进行分析,从模拟结果可以看出研究区Pb元素总体上显示出相似的空间变化趋势,但在细部空间变化上是有差别的。条件高斯模拟法对未知点的模拟值具有不确定性,克服了普通克里格法的平滑效应,能够更好地反映研究区的随机性和结构性。