纳米Fe3O4负载酸改性炭对水体中Pb2+、Cd2+的吸附

为探讨纳米Fe₃O₄负载联合硝酸改性椰壳炭对Pb²⁺、Cd²⁺单一及复合溶液的吸附特性，通过静态吸附实验，针对吸附剂的表面特性、投加量、溶液初始pH、吸附时间、重金属初始浓度等影响因素进行了探讨，应用等温吸附模型及吸附动力学模型对吸附特性进行了研究。结果表明，纳米Fe₃O₄负载酸改性炭比表面积较未改性椰壳炭增加了221.03 m²·g^-1，表面含氧官能团如O-H、C=O、C-O-C增加，芳香性增强，等电点提高至5.68。从经济效率角度考虑5 g·L^-1为合理吸附剂用量，pH为5.0时，吸附效果最好，吸附在4 h达到平衡。准二级动力学模型对吸附的拟合度更高，吸附主要是化学吸附，吸附由快速外扩散和颗粒内扩散共同作用，Pb²⁺、Cd²⁺的吸附分别更符合Langmuir和Freundlich等温吸附模型。纳米Fe₃O₄负载酸改性椰壳炭对Pb²⁺、Cd²⁺的最大吸附量（Q_m）分别达42.54 mg·g^-1和25.79 mg·g^-1，为未改性椰壳炭的1.87倍和2.23倍，复合溶液中Pb²⁺、Cd²⁺的Q_m分别为单一溶液的65.16%和54.21%，这揭示了离子共存条件下的吸附竞争现象。研究表明，纳米Fe₃O₄负载联合硝酸改性提高了椰壳炭对Pb²⁺、Cd²⁺的吸附能力，且Pb²⁺的吸附性能及吸附竞争性优于Cd²⁺。     

便携式XRF仪现场快速测定土壤中Pb的可行性研究

便携式XRF分析仪具有轻便、快速和可测对象较多与测量元素较广等特点而广泛应用于矿石、土壤等方面快速检测,但土壤的现场快速测定结果的准确性有待进一步研究与探讨。以安宁河谷平原土壤中Pb为研究对象,通过对便携式XRF仪现场快速检测结果与实验室分析结果的对比和影响因素的分析,建立基于安宁河谷平原表层土壤快速测定结果的线性函数为y=1.170 9x-17.326 0(R~2=0.992 9,x为现场检测结果),探讨其影响因素,为该区域表层土壤中Pb快速检测结果提供依据。     

铅和（或）镉对体外培养肾细胞的毒性损伤

在培养液中加入不同浓度的Cd（10、20、40μmol／L）、Pb（10、20、40μmol／L）和Pb-Cd联合（分别为5、10、20μmol／L），来探讨铅镉对肾细胞的作用及可能机制。在显微镜下观察细胞形态、测定细胞凋亡率和细胞周期及上清液脂质过氧化指标。结果表明：20μmol／L以上染毒组细胞皱缩、体积变小，表面有细胞碎片，甚至呈泡沫状或树枝状；铅、镉单独和联合染毒组GSH—Px、SOD活性随染毒剂量的增加，呈逐渐下降趋势（P〈0．05）．而MDA含量和凋亡率则呈升高趋势（P〈0．05），并存在剂量和时间效应。镉和铅也能使细胞周期停滞。Pb、Cd联合可加剧细胞损伤。     

土壤镉、锌、铅复合污染对芹菜的影响

采用盆栽试验,研究了红壤中Cd、Zn、Pb复合污染对芹菜生长及其重金属元素含量的影响.结果表明芹菜对Cd、Zn、Pb的吸收除了受到添加该元素的影响外,还受到共存元素的影响,且受共存元素影响的大小取决于元素间的浓度组合,即在某一点共存元素对重金属元素的拮抗或协同作用最强;正交试验方差分析结果表明,土壤添加元素对芹菜干质量及其重金属元素含量的影响均不显著;重金属元素从土壤向芹菜的迁移率大小顺序是Cd＞Zn＞Pb,Cd最易于被植物吸收;在酸性土壤中,芹菜对Cd、Zn的吸收量随土壤Cd、Zn添加量的增大而相应增加,但迁移率呈下降趋势;单一污染与复合污染对土壤重金属元素迁移率的影响无明显差异.     

Use of the BCR three-step sequential extraction procedure for the study of the partitioning of Cd, Pb and Zn in various soil samples

A slightly modified three-step sequential extraction procedure proposed by the Community Bureau of Reference (BCR) for analysis of sediments was successfully applied to soil samples. Contaminated soil samples from the lead and zinc mining area in the Mezica valley (Slovenia) and natural soils from a non-industrial area were analysed. The total concentrations of Cd, Pb and Zn and their concentrations in fractions after extraction were determined by flame or electrothermal atomic absorption spectrometry (FAAS, ETAAS). Total metal concentrations in natural soils ranged from 0.3 to 2.6 mg kg^-1 for Cd, from 20 to 45 mg kg^-1 for Pb and from 70 to 140 mg kg^-1 for Zn, while these concentrations ranged from 0.5 to 35 mg kg^-1 for Cd, from 200 to 10000 mg kg^-1 for Pb and from 140 to 1500 mg kg^-1 for Zn in soils from contaminated areas. The results of the partitioning study applying the slightly modified BCR three-step extraction procedure indicate that Cd, Pb and Zn in natural soils prevails mostly in sparingly soluble fractions. Cd in natural soils is bound mainly to Fe and Mn oxides and hydroxides, Pb to organic matter, sulphides and silicates, while Zn is predominantly bound to silicates. In contaminated soils, Cd, Pb and Zn are distributed between the easily and sparingly soluble fractions. Due to the high total Cd, Pb and Zn concentrations in contaminated soil close to the smelter, ! and their high proportions in the easily soluble fraction (80% of Cd, 50% of Pb and 70% of Zn), the soil around smelters represents an environmental hazard.     

Pb,Zn对超富集植物(小鳞苔草)抗氧化酶活性的影响

通过人工气候箱盆栽实验,研究Pb,Zn及其复合胁迫对小鳞苔草(Carex gentilisFranch.)根和叶中SOD,POD及CAT活性的影响。结果表明:叶片SOD活性随Pb和Zn浓度增加均呈缓慢上升趋势,根部SOD则表现为有升有降的过程,Pb Zn复合处理可提高根部和叶片SOD活性,最高分别为201.8 U/gFW和233.1U/gFW。根部POD活性随Pb,Zn浓度增加均出现不同程度提高,但叶片POD活性呈有升有降的过程;根部和叶片POD在Pb Zn复合处理中活性增幅明显,最高分别为对照的7.47倍和1.49倍。根部和叶片中CAT在Pb,Zn及其复合处理中活性均受到不同程度的抑制。方差分析显示,Pb对根部3种酶活性影响显著;Zn对叶片POD活性影响显著;Pb Zn互作对植株体内POD和根部SOD影响极显著。经综合分析,小鳞苔草在Pb,Zn及其复合胁迫条件下,SOD和POD起主要作用,并具有耐Pb高浓度胁迫的抗氧化酶活性调控能力,可望在中国西部铅锌复合污染区植物修复中提供一种新资源。     

Historical change of soil Pb content and Pb isotope signatures of the cultural layers in urban Nanjing

Soils in urban areas are often artificially formed and preserved as cultural layers in which soil materials are mixed with artifacts. The vertical change of soil properties denotes the historical change of human activities, and therefore, urban soil can be considered as a record of history of urban development. We studied a deep profile of urban soil (600 cm) in Nanjing, China, by intensively sampling at every 5 cm. Soil samples were analyzed for lead content. Charcoal from several layers was found and was dated using ¹⁴C to recognize archaeological cultural layers that might be formed in different Chinese dynasties. Pb isotope ratios were determined by thermal ionization mass spectrometry (TIMS) technology. The study found that artificial deposition, i.e., the formation of cultural layer started about 1700 years ago and lasted until recently. All cultural layers above the original loess were heavily contaminated by Pb with total content varying from 100 mg kg^− 1 to more than 2000 mg kg^− 1. There were several historical periods in which Pb content peaked, indicating significant contamination by human activities, such as ancient ore smelting for various purposes and use of Pb-containing materials for handicraft manufacture. Various Pb isotope ratios of the cultural layers differed substantially from that of the original undisturbed loess in the deepest position. ²⁰⁶Pb/²⁰⁷Pb value decreased gradually from the bottom layer to top layer, although with occasional exceptions, indicating a long-lasting mixing of extraneous sources of Pb during the entire history since ca. 300 A.D. In comparison with the isotope ratios of lead ores of different sources and that of aerosols, it was illustrated that the source of Pb in cultural layers might come from lead ores of southern China in the earlier dynasties, while Pb from north China might have contributed to the Pb source in the more recent years, suggested by the lowering of ²⁰⁶Pb/²⁰⁷Pb ratio in the near-surface cultural layers. However, the impact of petrol burning on cultural layers was basically excluded, considering the relatively short history of petroleum use in this area.     

毛细管离子分析法测定茶叶中的锌、锰、铜、铅和镉

用毛细管离子分析(CIA)法测定了茶叶中的锌、锰、铜、铅和镉,在10mmol/L咪唑,10mmol/Lα-羟基乙酸,pH=4.0的电泳介质中,五种离子在10min内得到了分离,用间接紫外法检测,以外标法定量,五元素的线性关系良好,相关系数为0.9973~0.9997,平均回收率在96.4%~104.2%之间,相对平均偏差为2.1%~3.3%,检测限为0.02~0.2μg/ml。此方法快速简便、准确度高、测定成本低。     

离子液体[C4 mim][PF6]萃取-石墨炉原子吸收法检测食品中的痕量铅

离子液体因其具有不挥发,粘度大等特性,已被广泛代替有机溶剂用于液液萃取。建立了以二乙基二硫代氨基甲酸钠(DDTC)为螯合剂、离子液体1-丁基-3-甲基咪唑六氟磷酸盐([C4mim][PF6])为萃取剂、稀硝酸为反萃取溶剂的萃取体系,并对所建立的萃取体系的相关影响因素进行了优化,包括:体系pH、螯合剂DDTC的用量、反萃取溶剂的选择等。同时对该离子液体是否可循环利用以及该体系的抗干扰能力进行了评价。此外,将所建立的离子液体萃取-稀硝酸反萃取体系结合石墨炉原子吸收分光光度法应用于大米,茶,鱼,小麦,蛤以及油菜中的痕量铅的检测。