沈阳市降雪中PFOS和PFOA污染现状调查

通过调查降雪中PFOS和PFOA的浓度,阐明了沈阳市大气中PFOS和PFOA的污染状况和污染规律.2006-02-06采集沈阳市区和郊区共计36个采样点的降雪样品,2006-02-25在其中5个采样点再次采集降雪样品.固相萃取融雪水中的PFOS和PFOA,利用LC-MS-SIM法测定样品中PFOS和PFOA浓度.全部样品中均检出PFOS和PFOA.2006-02-06降雪中PFOS和PFOA的浓度几何平均值分别为2.0 ng·L^-1（范围：0.4～46.2 ng·L^-1）和3.6 ng·L^-1（范围：1.6～22.4 ng·L^-1）,95%置信区间分别为1.5～2.8 ng·L^-1和3.1～4.2 ng·L^-1.PFOS和PFOA的最高浓度同时出现在郊区采样点朱尔屯,市中心区2种物质的浓度呈显著正相关.2006-02-25的5个采样点降雪中PFOS和PFOA的浓度几何平均值均为2.2 ng·L^-1.2次降雪中PFOS浓度差异不显著,2006-02-25降雪中PFOA浓度高于2006-02-06.结果表明,沈阳市区和郊区降雪中广泛存在PFOS和PFOA污染,局部区域可能存在共同的PFOS和PFOA污染来源;沈阳地区有较稳定的PFOS来源持续向大气中输送该类物质;PFOS和PFOA的环境行为可能不同.     

二级SBR系统处理染料废水长期运行的稳定性

考察了处理染料废水的二级SBR系统在连续运行120个周期过程中的稳定性.系统的运行先后经历了低染料浓度和高染料浓度2种情况.试验发现在长期运行过程中,二级SBR系统对进水水质及操作条件具有良好的适应性;能够有效去除废水中的污染物,对染料的平均去除率为81%～92.5%,对COD的平均去除率为89.4%～93.1%;出水水质比较稳定.在二级SBR系统中,厌氧污泥活性高,降解污染物能力强;好氧活性污泥形成团簇状结构,有利于稳定出水水质.     

滇池流域土壤活性腐殖质及其主要组分的紫外-可见与三维荧光光学特性

利用紫外-可见光谱和三维荧光光谱技术,结合土壤腐殖质及腐殖质组分(胡敏酸、富里酸)中的有机碳含量,研究了滇池流域土壤活性腐殖质及其组分胡敏酸和富里酸的光谱特征.结果表明,滇池流域土壤活性腐殖质中富里酸含量高于胡敏酸,流域范围内土壤活性腐殖质及其组分含量分布不均匀,活性腐殖质、胡敏酸和富里酸含量的变异系数分别达37.7%、36.4%、40.9%.土壤活性腐殖质及其组分胡敏酸和富里酸的碳含量均表现为菜地荒地草地湿地.光谱特征结果表明,滇池流域土壤活性腐殖质主要由自生源物质和经一定程度降解后的外源物质共同组成.此外,自生源性与光化学及生物活性具有正相关关系.因此,具有弱自生源性的滇池流域土壤活性腐殖质所具有的光化学和生物活性较弱.     

Adsorption mechanism of phenolic compounds from aqueous solution on hypercrosslinked polymeric adsorbent

The adsorption of two phenols, namely, phenol and salicylic acid(SA) onto a water-compatible hypercrosslinked polymeric resin (NJ-8) were studied in terms of pseudo-second-order and first order mechanisms for chemical sorption as well as an intraparticle diffusion mechanism process. Kinetic analysis showed that the intraparticle diffusion process was the essential rate-controlling step. The activation energies of sorption have also been evaluated with the pseudo-second-order and intraparticle diffusion constants, respectively. Adsorption equilibrium data were well fitted by the Langmuir, Freundlich and Redlich-Peterson isotherms. Adsorption was exothermic and basically of a type of transition between physical and chemical character. The sorption capacity was higher for SA due to its more hydrophobic. Phenol has a higher adsorption enthalpy since it could form stronger hydrogen bonding on NJ-8.     

华南地区高山酸沉降化学研究

1987—1989年春季,在华南地区衡山、狮子山、苗儿山和白云山观测到华南高山降水酸化,各测点降水pH<5.6的频率大于68％,平均pH值在3.56—4.85之间,分析了高山降水的化学特征,及其与高山的地理环境等因素的关系.结果表明,高山雨水与高空云水有相似性,狮子山和白云山的云雾水主要属地形云,受局地源的影响更为严重,化学性质更接近于地面雨水.     

镉铅在粘土上的吸附及受腐殖酸的影响

试验研究了镉和铅2种重金属在蒙脱土和高岭土上的吸附,以及外加腐殖酸的3种组分（富里酸、棕色胡敏酸和灰色胡敏酸）的影响。镉铅在粘土上的吸附随着介质pH的升高而增加。在pH4-8范围内的任意pH点,镉在高岭土上的吸附量因富里酸而降低,因2种胡敏酸而升高;当pH值高于6时,吸附量急剧增加。外加富里酸使得铅在粘土上的吸附在pH＞6时意外出现随着介质pH而降低的趋势。     

煤矸石酸雨淋滤特征的研究

本文对重庆中梁山煤矸石在自然酸度和模拟酸雨下静态态及动态淋溶特征进行了研究。结果表明,淋出液成弱碱性,其中的铅、锌、铬、镍、铜和铁等元素的浓度均超过了水综合排放标准和地面水环境质量标准规定的阈值;在模拟酸雨中上述离子的溶出能力强于在于蒸溜水中;温度升高时各元素及总离子的淋出量增大。     

草酸浸取废SCR催化剂制备光催化剂

采用草酸浸取废SCR催化剂,得到钛钨粉,制备Bi₂WO₆/钛钨粉复合光催化剂,考察了其对罗丹明B的光催化降解性能。制备光催化剂的优化工艺条件为：采用聚乙烯吡咯烷酮为表面活性剂,n（Bi₂WO₆）∶n（钛钨粉）=2∶1,前驱液pH为5,水热反应时间为18 h。在此条件下制备的光催化剂在可见光下降解罗丹明B,反应 60 min,罗丹明B降解率达94.30%。表征结果显示：钛钨粉小颗粒散落在Bi₂WO₆片表面,为光催化反应提供了更多的活性位点;Bi₂WO₆和钛钨粉两者结合可提高光生电子和空穴的分离效率,进而提高催化剂的光催化活性。Bi₂WO₆/钛钨粉光催化剂对罗丹明 B 的降解符合一级反应动力学规律。     

对氨基苯胂酸的生命周期评价

本文介绍了最常用的有机胂制剂——对氨基苯胂酸的主要用途和污染特征,从生命周期的角度识别并定量评价了其生产、使用和残留过程的环境影响,评价结果表明对氨基苯胂酸在土壤中最终残留的环境骰响占其整个生命周期的99％以上,指出了常规环境影响评价在评价其环境污染上的局限性,据此提出逐步减少或禁止有机胂制剂的生产和使用、并在一些特殊的建设项目环境影响评价中推广生命周期评价的建议。     

Effects of Acid Rain on Competitive Releases of Cd, Cu, and Zn from Two Natural Soils and Two Contaminated Soils in Hunan, China

Leaching experiments of rebuilt soil columns with two simulated acid rain solutions (pH 4.6–3.8) were conducted for two natural soils and two artificial contaminated soils from Hunan, south-central China, to study effects of acid rain on competitive releases of soil Cd, Cu, and Zn. Distilled water was used in comparison. The results showed that the total releases were Zn>Cu>Cd for the natural soils and Cd>Zn≫Cu for the contaminated soils, which reflected sensitivity of these metals to acid rain. Leached with different acid rain, about 26–76% of external Cd and 11–68% external Zn were released, but more than 99% of external Cu was adsorbed by the soils, and therefore Cu had a different sorption and desorption pattern from Cd and Zn. Metal releases were obviously correlated with releases of TOC in the leachates, which could be described as an exponential equation. Compared with the natural soils, acid rain not only led to changes in total metal contents, but also in metal fraction distributions in the contaminated soils. More acidified soils had a lower sorption capacity to metals, mostly related to soil properties such as pH, organic matter, soil particles, adsorbed SO₄ ²⁻, exchangeable Al³⁺ and H⁺, and contents of Fe₂O₃ and Al₂O₃.