N,N-双(二硫代羧基)乙二胺对微量络合镍的深度脱除特性研究

以柠檬酸镍(CA-Ni)、酒石酸镍(TA-Ni)、焦磷酸镍(SP-Ni)3种低浓度模拟络合镍废水为研究对象,选用自制的重金属捕集剂N,N-双(二硫代羧基)乙二胺(EDTC),对废水中的Ni进行深度脱除.重点研究了EDTC投加量、初始p H、反应时间对Ni去除效果的影响及螯合沉淀物的沉淀性能和溶出特性,同时分析了EDTC去除络合Ni的机理.研究结果表明,处理初始浓度5 mg·L~(-1)的CA-Ni、TA-Ni、SP-Ni,p H为4~8,EDTC最佳投加量分别为60 mg·L~(-1)、55 mg·L~(-1)和70 mg·L~(-1),PAM(聚丙烯酰胺)为1 mg·L~(-1),反应时间2 min,Ni的出水浓度均低于0.05mg·L~(-1),去除率达99%以上.螯合沉淀物沉降性能好且在弱酸弱碱条件下能稳定存在.红外光谱图和元素分析结果表明:EDTC与Ni发生螯合反应,即EDTC直接脱除络合镍中的Ni2+,并与Ni2+生成更稳定的螯合产物EDTC-Ni,进而有效地去除废水中Ni.     

高岭石、针铁矿及其二元体对胡敏酸的吸附特性

研究了高岭石、针铁矿及其混合物(KGM)和复合物(KGC)的表面性质及吸附胡敏酸的特性.结果表明,4种物质的比表面积(SSA)表现为针铁矿KGCKGM高岭石,KGM的SSA接近两种纯物质的平均值,而KGC的SSA明显升高.高岭石、针铁矿、KGM和KGC的等电点(IEP)分别为3.2、7.9、6.1和6.7;初始p H=5.0时,其表面Zeta电位分别为-13.9、38.2、14.3和19.7 m V.4种样品对胡敏酸的动力学吸附过程适合用准二级动力学模型描述,表明化学吸附是主要作用机制.一、二位Langmuir模型可较好地拟合等温吸附数据(R~2为0.962~0.993),其中二位Langmuir模型对KGM和KGC吸附数据的拟合度R~2分别为0.989和0.993;Freundlich模型对等温吸附数据的拟合度较低,但两种二元体的拟合度高于两种纯物质.初始p H=5.0时,高岭石、针铁矿、KGM和KGC对胡敏酸的吸附容量(q_(max))分别为6.02、61.83、35.13和42.10 mg·g~(-1);两种二元体的q_(max)都高于两种纯物质q_(max)的平均值,其中KGC的q_(max)明显升高.热力学参数表明,4种样品对胡敏酸的吸附均属于吸热反应,其中高岭石的吸附为非自发过程,其余样品的吸附为自发过程.     

十六烷基三甲基季铵盐-乙硫醇铵盐复合改性膨润土吸附性能研究

用十六烷基三甲基季铵盐(HDTMA)和乙硫醇铵盐(AET)双阳离子同时复合改性内蒙钙基膨润土(NMB),制得新型吸附材料HDTMA-AET-NMB.利用X射线衍射(XRD)、热分析(TG-DTA)、红外光谱(FT-IR)及N2-BET等测定发现,复合改性膨润土的表面性质和层间结构已发生显著改变.对重金属离子Cd2+和对硝基苯酚(PNP)的吸附研究表明,HDTMA-AET-NMB能协同吸附混合水溶液中的目标污染物,对水中重金属离子的吸附机理是膨润土层间的AET与被吸附的Cd2+形成了稳定的配合物;对水中对硝基苯酚的吸附源于其在长碳链疏水介质中的分配.复合改性膨润土可望应用于重金属-有机物混合废水的处理.     

Preparation of rare-earth metal complex oxide catalysts for catalytic wet air oxidation

Catalytic wet air oxidation (CWAO) is one of the most promising technologies for pollution abatement. Developing catalysts with high activity and stability is crucial for the application of the CWAO process. The Mn/Ce complex oxide catalysts for CWAO of high concentration phenol-containing wastewater were prepared by coprecipitation. The catalyst preparation conditions were optimized by using an orthogonal layout method and single-factor experimental analysis. The Mn/Ce serial catalysts were characterized by Brunauer-Emmett-Teller (BET) analysis and the metal cation leaching was measured by inductively coupled plasma torch-atomic emission spectrometry (ICP-AES). The results show that the catalysts have high catalytic activities even at a low temperature (80°C) and low oxygen partial pressure (0.5 MPa) in a batch reactor. The metallic ion leaching is comparatively low (Mn<6.577 mg/L and Ce<0.6910 mg/L, respectively) in the CWAO process. The phenol, COD_Cr, and TOC removal efficiencies in the solution exceed 98.5% using the optimal catalyst (named CSP). The new catalyst would have a promising application in CWAO treatment of high concentration organic wastewater. Translated from Techniques and Equipment for Environmental Pollution Control, 2005, 6(2): 40–44 [译自: 环境污染治理技术与设备]     

基于复杂系统的民族地区非常规突发事件应急管理研究

民族地区非常规突发事件属罕见非常规突发事件,是典型的复杂系统。传统的应急管理模式不能适应这类具有非线性复杂系统特征的罕见非常规突发事件的应急管理需求。因此,应该将民族地区的各类民族因素和社会特征作为民族地区非常规突发事件应急管理研究的基础变量,并进行复杂性分析,进而构建民族地区非常规突发事件演化规律的可视化仿真模型,然后在PeMS(平行应急管理系统)的基础上实现对该类突发事件应急管理机制的评估、反馈与改进。     

基于复杂网络的城市燃气输配系统失效因素分析

将复杂网络相关理论方法引入城市燃气输配系统失效因素的分析中。选取引起城市燃气输配系统失效的主要影响因素为节点,以它们之间的相互关系为边,建立网络并进行相关分析。发现节点的度分布近似具有幂律的特性,幂指数为1.76;通过节点度的分析,确定出管道附属设备、用户设施失效、第三方影响破坏等因素为引起输配系统失效的主要原因,与引起燃气事故的统计分析资料基本相符合。这为确定城市燃气输配系统关键失效因素提供了一种新的思路。     

金刚烷胺制药胺化废水与溴化废水的中和-络合萃取处理

考察了两种废水中和反应过程对污染物的去除效果,然后采用P204/正辛醇复配萃取剂对废水进行络合萃取处理.结果表明,采用溴化废水中和滴定胺化废水可以大幅消减废水中污染物,避免后续萃取过程中的乳化现象;在pH值为8.0,油/水相比为1:1的条件下,P204:正辛醇=3:2的复配萃取剂对废水中TOC和金刚烷胺的单级萃取效率分别为49.6%和99.5%;多级萃取对TOC去除率没有明显提高;以2.0mol/L的HCl溶液为反萃取剂,在水/油相比为1:1条件下,可以将47.5%的金刚烷胺从负载有机相中反萃分离,回收得到的金刚烷胺盐酸溶液可以回用,再生后的萃取剂可以多次重复使用.     

区域空气质量模拟中查表法的应用研究

在自行开发完善的区域空气质量模式系统RegSRRMS中应用查表法,模拟中国典型城市群对流层大气主要污染物的浓度变化,评估该方法在大气复合污染事件预测和控制中的有效性.首先,利用具有国际先进水平的空气质量模式WRF-CHEM中的化学模块建立了包含完善气相化学、气溶胶过程的箱模式WRFBOX.其次,利用WRFBOX进行化学反应敏感性分析,基于影响污染物的重要因子分别建立了臭氧(O3)及其前体物、无机盐气溶胶和二次有机气溶胶(SOA)查算表数据库,并检验其有效性.最后,将此查算表数据库引入RegSRRMS,建立简化的查表算法.利用直接耦合机制法和查表法对2000年3月珠三角地区污染个例中主要大气污染物浓度进行模拟.通过比较2种方法的模拟结果,显示查表法计算效率提高了57%,能够反映大气光化学反应的非线性特征、气溶胶及其前体物的平衡关系,具有高分辨率、高时效性,能够方便快捷地给出源和受体之间的响应关系,结果可靠.在区域空气质量模式中应用查表法有利于大气污染事件的快速预测以及大气污染控制的快速决策.     

复合金属氧化物Cu-Co-Al低温催化水解HCN

采用共沉淀法制备了Cu-Al、Co-Al和Cu-Co-Al复合金属氧化物催化剂,考察了3种催化剂对HCN的催化水解性能,并通过XRD、BET、XPS和H2-TPR等对催化剂的结构和性能进行表征.结果表明, Cu-Co-Al催化剂展示最高的催化活性. 反应温度200℃,反应180min后, Cu-Co-Al、Cu-Al和Co-Al催化剂对HCN的转化率分别为95%,90%,10%;NH3生成量分别为122,118,18mg/m3.低结晶度、高分散性、高比表面积的催化剂有利于低温HCN水解.适量的表面分子氧含量、较高的Cu2+和Co3+含量、较低的还原温度是Cu-Co-Al催化剂具有较高的HCN低温水解活性的主要原因.     

Bioindication of volatile elements emission by the Puyehue-Cordón Caulle (North Patagonia) volcanic event in 2011

The emission of volatile pollutants from the volcanic eruption of the Puyehue-Cordón Caulle complex (North Patagonia Andean Range) that started in June 4th, 2011, was investigated by bioindication means with the epyphytic fruticose lichen Usnea sp. The elemental composition of pooled samples made up with 10 lichen thalli were analysed by Instrumental Neutron Activation Analysis. Eleven sampling sites were selected within the impacted region at different distance from the volcanic source. Five sites were selected as they were already sampled in a previous study prior to the eruption. Two other new sampling sites were selected from outside the impacted zone to provide non-impacted baseline sites.The elements associated with the lichen incorporation of particulate matter (PM) of geological origin were identified by linear correlation with a geochemical tracer (Sm concentrations). The elements associated with PM uptake were Ce, Eu, Fe, Hf, La, Lu, Na, Nd, Sb, Sc, Se, Ta, Tb, Th, U, and Yb. Arsenic and Cs concentrations showed contributions exceeding the PM fraction in sites near the volcanic centre, also higher than the baseline concentrations, which could be associated with permanent emissions from the geothermal system of the Puyehue-Cordón Caulle complex. The lichen concentrations of Ba, Ca, Co, Hg, K, Rb, Sr, and Zn were not associated with the PM, not showing higher concentrations in the sites nearby the volcanic source or respect to the baseline values either. Therefore, there is no indication of the emission of volatile forms of these elements in the lichen records. The lichen records only identified Br volatile emissions associated with the Puyehue-Cordón Caulle complex eruption in 2011.