2008年北京采暖开始前后大气颗粒物化学成分及来源研究

为了系统反映北京采暖开始前后大气颗粒物的特征,于2008年10月底到12月初在北京北三环内城区使用分级式撞击采样仪进行了大气颗粒物采样,并用质子激发X射线荧光分析(PIXE)方法对其中16种化学元素浓度进行了分析.结果表明,采暖开始后16种元素总浓度较采暖期前增长3%,As、Cu在采暖期间的浓度增幅在30%以上,采暖开始后细粒子中Pb浓度增长为27%.富集因子分析结果表明,Cu、As、Pb等元素细粒子的富集因子比1999年同期有明显减小,说明北京近年来实行的环保措施较为有效.     

高密市高氟地下水成因研究

高密市曾经是全国氟中毒较为严重的地区之一,浅层高氟地下水是病区居民致病的主要原因。在系统环境地球化学调查的基础上,研究了当地高氟地下水的成因,认为岩石、土壤是当地高氟浅层地下水的主要来源。探讨了地下水中氟富集的因素与过程,提出了地氟病的防治措施。     

Chemical characteristics of precipitation at Nanping Mangdang Mountain in eastern China during spring

To study the characteristics of precipitation in eastern China, an automatic sampler was used to collect rainwater samples from 19 precipitation events at Mangdang Mountain, Nanping City, Fujiang Province, in the spring of 2009. We used ion chromatography to analyze the ionic components and concentrations, and inductively coupled plasma mass spectrometry (ICP-MS) to analyze element compositions and contents. The results demonstrated remarkable acidic characteristics: in more than 80% of precipitation events the pH was less than 5.6, with an average of 4.81. Mass concentration results showed SO4 2?? was the main anionic component (36.2% of the total anion mass), while NH4 + was the main cationic component (47.7% of the total cation mass) and main ion for acidity neutralization in the rainwater. Organic acid content accounted for 30.9% of total anion mass. The main trace metals were Ca, K, and Na. The SO4 2??/NO3?? ratio was 1.4, indicating that precipitation in this region was influenced by complex air pollution – the product of individual coal-burning combined with vehicle exhaust pollution. Correlation analysis of the chemical composition of the precipitation indicated that acidity in this region was determined by a combination of all acidic and neutralization ions rather than any single ion component. The results also showed that Na+ and Cl?? contributions were mainly by seawater; Mg2+ by seawater and crustal materials; the NH4 +, K+, Ca2+, NO3?? and SO4 2?? by anthropogenic sources; the trace metals were from the Earth’s crust; and organic acids were potentially from combustion of biomass.     

广东柘林湾至大埕湾海域表层沉积物重金属分布与环境地球化学特征

对广东柘林湾至大埕湾海域35个站点的表层沉积物样品进行了重金属和粒度分析,重金属Hg、As、Cu、Pb、Cd、Zn和Cr的平均含量(mg/kg)分别为:0.053、9.7、19.2、40.0、0.11、89.0和31.4。重金属(Cd除外)平面分布多呈西高东低、由柘林湾向大埕湾递减的变化趋势。本区粒度主要以细粒的粉砂(T)和粘土质粉砂(YT)为主,只有在湾口旗头山岬角附近以及黄冈河口附近粒度较粗,为砂质(S)过度至砂质粉砂(ST),显示出滨、浅海沉积环境。通过一些环境地球化学参数计算显示,重金属富集系数在0.73~1.37之间,其中Hg、Cu、Pb、Zn属弱富集,As、Cr和Cd与当地背景值相当。单因子潜在生态风险评价Hg属于中度污染,其余重金属为低度污染。多因子总生态风险评价广大区域属于低风险,中风险仅呈零星小斑块状分布,证明本区域沉积物环境总体良好。重金属之间(Cd除外)相关性为极显著~显著,显示出相似的来源。重金属与粒度相关性为显著~弱显著,重金属大致符合粒度控制规律。     

草本植物对土壤重金属的富集研究

介绍中国土壤重金属污染的概况及对土壤、植物、人类的影响;对植物修复机理及技术做了简要的阐述.结合近些年来国内学者的研究,筛选出了对Cd有富集作用的草本植物如叶用红菾菜、东南景天、球果薛菜等;对Pb有富集作用的草本植物如香根草、土荆芥等;对Zn有富集作用的草本植物如圆锥南芥、小鳞苔草等;对Cu有富集作用的草本植物如鸭跖草、海洲香薷等;对As有富集作用的草本植物如蜈蚣草、大叶井口边草.     

广东某垃圾焚烧炉周边空气颗粒物中金属浓度特征及源解析研究

以广东某垃圾焚烧炉为研究对象,应用富集因子法、主成分分析法对其周边环境空气中金属(Fe、Al、Mg、Cu、Zn、Mn、Ba、Pb、Cr、Ni、Bi和Cd)含量及来源进行分析.结果如下:研究区域环境空气中各金属含量(各点均值)(ng·m-3)为:Fe(1092—3487)Al(939—3126)Mg(716—1339)Cu(63.4—995)Zn(227—427)Mn(162—291.1)Ba(61.4—372)Pb(21.9—41.8)Cr(12.3—25.7)Ni(5.70—15.5)Bi(0.70—1.22)Cd(0.42—0.82).相关分析和主成分分析发现,研究区域Fe与Ni、Cr、Mn、Ba主要来自于焚烧炉释放,Zn、Cd、Pb、Bi和Cu则来自于研究区域周边的交通污染源,而Al和Mg则主要来自于地壳或土壤背景值.     

Resolving the influence of nitrogen abundances on sediment organic matter in macrophyte-dominated lakes, using fluorescence spectroscopy

A controlled experiment was designed to resolve the influence of nitrogen abundance on sediment organic matters in macrophyte-dominated lakes using fluorescence analysis. Macrophyte biomass showed coincident growth trends with time, but different variation rates with nitrogen treatment. All plant growth indexes with nitrogen addition (N, NH₄Cl 100, 200, 400 mg/kg, respectively) were lower than those of the control group. Four humiclike components, two autochthonous tryptophan-like components, and one autochthonous tyrosine-like component were identified using the parallel factor analysis model. The results suggested that the relative component changes of fluorescence in the colonized sediments were in direct relation to the change of root biomass with time. In the experiment, the root formation parameters of the plants studied were significantly affected by adding N in sediments, whichmay be related to the reason that the root growthwas affected byNaddition. Adding a low concentration of N to sediments can play a part in supplying nutrients to the plants. However, the intensive uptake of NH₄⁺ may result in an increase in the intracellular concentration of ammonia, which is highly toxic to the plant cells. Hence, our experiment results manifested that organic matter cycling in the macrophyte-dominated sediment was influenced by nitrogen enrichment through influencing vegetation and relevant microbial activity.     

厌氧条件下 2,2',4,4'-四溴联苯醚的微生物降解

多溴联苯醚是环境中的新兴污染物,其中2,2’,4,4’-四溴联苯醚(BDE-47)在环境(尤其是水环境)中普遍存在且生物毒性很高.以BDE-47为对象,研究了6组含脱卤球菌的培养液对BDE-47的降解,目的是了解厌氧条件下BDE-47的微生物降解及其动力学.采用100 mL血清瓶作为厌氧反应器,对厌氧微生物进行培养.对每组菌作两种处理,一是仅加入BDE-47作为能源(设计终浓度为200μg.L-1),另一是同时加入BDE-47和三氯乙烯(TCE)作为能源(设计终浓度分别为200μg.L-1和13mg.L-1).经过3个月的实验,两组含脱卤球菌的培养液(6M6B和T2)均能明显降解BDE-47,生成BDE-17、BDE-4及少量的DE,TCE的存在一定程度上减弱了6M6B和T2菌对BDE-47的降解.采用PCR-DGGE法对不同培养菌液的群落结构进行比较,发现醋酸杆菌属与BDE-47的降解关联较大.在3种不同初始浓度(50、250和500μg.L-1)条件下,BDE-47的降解速率分别为0.003 3、0.001 4和0.001 0 d-1.本研究表明,厌氧条件下BDE-47在细菌的作用下可发生还原降解,生成BDE-17和BDE-4.醋酸杆菌属可能在BDE-47的降解中起较大作用.高浓度的BDE-47在一定程度上会抑制降解菌的活性.     

兰州市城区河道表层沉积物重金属污染及磁学参数相关关系研究

以兰州市城区8条河流的表层沉积物为研究载体,通过Hakanson潜在生态风险指数法、地质累积指数法及富集因子评价法等3种污染评价指标以及环境磁学方法对As、Co、Cr、Cu、Ni、Pb、V、Zn共8种重金属元素污染特征进行分析.结果显示,①元素As、Co、Ni、V在8条河流中均表现为轻微生态危害;元素Cr、Pb、Zn在...     

喀斯特高镉地质背景区水稻镉的富集、转运特征与机理

西南喀斯特地区土壤镉(Cd)具有"高地质背景、低污染风险"特征,但超过《土壤环境质量农用地土壤污染风险管控标准》风险管制值的区域是否仍具有低风险性,是迫切需要回答的问题.本文在罗甸县喀斯特峰丛谷地选择一个高Cd 土壤水稻种植区,开展土壤-水稻系统Cd含量特征和土壤Cd赋存形态等方面的研究,评价水稻各部位Cd的富集、转运...