磁絮凝-吸附技术对黑臭水体中浊度、氨氮和总磷的去除效果及机理

采用磁絮凝-吸附技术开展了同步去除黑臭水体浊度、氨氮和总磷(TP)实验。在磁絮凝阶段,通过聚合硫酸铁(PFS)、磁粉(MPs)和聚丙烯酰胺(PAM)复配使用,利用电荷中和作用去除浊度和TP;同时,利用化学吸附沉淀去除TP;在此阶段中,当PFS、MPs、PAM的投加量分别为16.00、100.00、2.20 mg·L⁻¹且以PFS+MPs在快速阶段先投加,PAM在慢速阶段后投加的顺序投配时,絮凝效果达到最佳。在吸附阶段,吸附剂质化壳聚糖-沸石(PCZ)主要通过离子交换作用去除氨氮以及通过静电吸附作用去除TP;当PCZ的投加量为1.25 g·L⁻¹时吸附效果达到最佳。利用所研究的磁絮凝-吸附技术对实际黑臭水体进行处理,其出水浊度能达到城镇污水处理厂污染物排放一级标准(≤10.00 NTU),TP和氨氮也分别能满足地表水环境质量Ⅲ类标准(≤0.20 mg·L⁻¹)和Ⅴ类标准(≤2.00 mg·L⁻¹)要求。     

微纳米磁性粒子对膜生物反应器运行效能的影响

针对膜生物反应器(MBR)应用中膜污染这一难题,构建了3套MBR系统对比研究了微纳米磁性粒子对MBR运行效能的影响,包括污染物去除效果、污泥混合液特性、膜污染情况等;并基于高通量测序技术,深入分析了微生物群落演替规律与MBR运行效能的关系。结果表明：微纳米磁性粒子的引入均未在污染物去除方面产生负面影响,MBR出水COD浓度低于50 mg·L−1,出水NH$\ _{{4}}^{{ + }}$-N维持在5 mg·L−1以下,均可达到国家污水排放标准一级A标准(GB 18918-2002);微纳米磁性粒子的引入均有效减缓了膜污染,并且微米尺度材料延缓效果更显著。膜污染组分分析表明：不同粒径磁性材料引入均有效降低了SMP、LB-EPS各组分浓度;同时有效减少了反应器中大分子物质含量,增加了小分子物质含量,因而降低了膜污染速率。微生物群落分析表明,微纳米磁性粒子的引入可能抑制了应器中易引起膜污染的先锋物种Alphaproteobacteria的生长,有效延缓了膜污染,并且微米粒径材料抑制效果更显著。研究结果可为磁活性污泥法调控MBR膜污染的工程应用提供参考。     

同步辐射光谱技术在有机固废污染控制与资源化研究中的应用

有机固废中碳、磷、硫及重金属等元素赋存形态是决定其环境行为、反应活性及资源化再利用的关键因素.同步辐射光谱技术可以在分子水平、微纳米尺度原位表征有机固废中碳、磷、硫、重金属等元素赋存形态、结合位点、微观结构,为深入阐明有机固废环境行为、反应机制提供直接的证据.概述了X射线吸收光谱、微束X射线荧光光谱等同步辐射光谱技术在...     

南水北调中线清河溶解性有机物的光降解行为

溶解性有机物(dissolved organic matter, DOM)在水环境中普遍存在,其光降解行为与种类和来源密切相关。近年来,南水北调中线工程沿线中DOM含量过高问题逐渐引起了人们对饮用水水源水质的关注。利用三维荧光光谱与紫外可见吸收光谱表征了清河段DOM在水(Water DOM, W-DOM)、底泥(sediment-derived DOM, S-DOM)、藻胞内(intracellular DOM, I-DOM)和胞外(extracellular DOM, E-DOM)这4种典型来源中的光学性质和光降解行为。结果表明,W-DOM的主要来源是藻类代谢产生的E-DOM;S-DOM的主要形成原因是藻细胞破裂释放I-DOM。DOM的光漂白主要发生在紫外区,且UV-B波段的光漂白效率大于UV-A波段。W-DOM、S-DOM和E-DOM中有色DOM(chromophoric DOM, CDOM)的降解率基本相同,为40%~50%;I-DOM中CDOM降解率相对较低,约为25%。光照可以将W-DOM、S-DOM和E-DOM中复杂的大分子物质分解成结构简单的小分子物质。CDOM中类腐殖质的光降解率比类蛋白质更高,W-DOM、S-DOM和E-DOM中CDOM与类腐殖质的光降解速率在相同时间下基本保持一致;S-DOM和E-DOM中CDOM与类蛋白质的光降解速率在相同时间下基本保持一致。以上结果反映了太阳辐射对水环境中DOM的转化和去除机理,为河流水质保护提供了理论依据。     

磁性山竹壳炭的制备及对氯霉素吸附性能

以山竹壳为原料,K₂C₂O₄为活化剂,Fe(NO₃)₃为赋磁剂制备了磁性山竹壳炭。考察了制备条件对山竹壳炭理化性质的影响,并探究其对水体中氯霉素的吸附性能。结果表明,随着K₂C₂O₄用量的增加和炭化温度的升高,磁性山竹壳炭的比表面积和孔容增加,但Fe₃O₄逐渐被还原为单质Fe。当磁性山竹壳炭PGC-4-900投加量为0.3 g·L⁻¹,溶液质量浓度为125 mg·L⁻¹时,对氯霉素吸附容量最大可达316.3 mg∙g⁻¹。吸附过程为自发、吸热和无序度增加的过程。吸附动力学符合拟二级动力学模型,等温模型可用Langmuir方程描述。磁性山竹壳炭在吸附氯霉素方面具有宽泛的pH适应性,静电作用非磁性山竹壳炭对氯霉素吸附主要机理,孔隙填充和π—π作用在氯霉素吸附过程中起主导作用。     

电磁浮动床除尘装置的设计与实验研究

针对所设计的电磁浮动床除尘装置,为了掌握该装置的运行规律以及除尘效果,以铁磁颗粒为床料,通过实验分析了铁磁颗粒质量对床层高度的影响,以及风量和磁场强度等因素对床层高度和压强降的影响,并对风量和磁场强度与除尘效率的关系进行了研究,确定最佳运行条件：进口含尘气体浓度为20 g·m-3,磁场强度为300 Gs,风量为110 m3·h-1,除尘效率高达99.34%,为电磁浮动床用于高温除尘工艺奠定了基础。     

NiFe2O4/ZnAl-LDH吸附去除水中Cr(VI)

采用共沉淀法合成磁性复合材料NiFe2O4/ZnAl-LDH,通过静态吸附试验考察复合材料去除水中Cr（VI）的性能,系统地研究了溶液初始pH值、吸附剂投加量、吸附时间和温度等因素对Cr（VI）去除效果的影响。结果表明,当溶液初始pH值为2、初始Cr（VI）浓度为50 mg·L-1、吸附剂投加量为4 g·L-1时,吸附过程在240 min内达到平衡,此时Cr（VI）的去除率为89.5%。动力学和吸附等温式的研究表明：NiFe2O4/ZnAl-LDH吸附Cr（VI）的过程符合准二级动力学和Langmuir等温吸附模型。热力学参数表明该吸附过程为自发、放热的反应过程,低温有利于吸附剂对Cr（VI）的吸附。吸附剂经4次再生后对Cr（VI）仍有83.1%的去除率,且其在外加磁场的作用下能快速与水溶液分离,因此NiFe2O4/ZnAl-LDH可作为去除水中Cr（VI）的良好吸附剂。     

磁性生物膜载体的规模化制备、表征和应用

利用机械力化学表面改性原理设计了卧式双旋搅拌混合反应设备,通过磁铁矿粉和适量浓硫酸的球磨混合反应制备得到磁性生物膜载体,其XRD、IR、SEM和BET表征分析结果表明,磁性生物膜载体表层生成了多羟基硫酸铁为主的活性组分.进而在膜生物反应器实验装置中投加磁性生物膜载体进行了中试实验,结果表明,磁性生物膜载体能与活性污泥中的微生物聚合形成稳定的菌胶团,活性污泥SV30从实验初期89%降到了稳定期的39%,此外,磁性生物膜载体还具有稳定膜生物反应池出水COD,强化脱氮除磷的能力.     

Assessing safety culture in the Spanish nuclear industry through the use of working groups

This paper presents the design and the implementation of a methodology for measuring and improving safety culture at a nuclear power plant (NPP). The study has involved the completion of a pilot project aimed at seeing how to make use of the RADAR logic (Results, Approach, Deployment, Assessment and Review) of the EFQM model as a tool for the self assessment of safety culture in a nuclear power plant. The work was aimed at finding evidence of the safety culture that was in place at the plant and at identifying both the strengths of that culture and any areas in which it could be improved. The score obtained from an analysis of those strengths and areas for improvement has made it possible to prioritise the actions to be taken. The identification of perceptions and evidence, the agreement on the strong points and areas for improvement and the quantification of the safety culture have been performed by groups comprising volunteers who work at the NPP. The advantages of this methodology are assessed in the paper.     

Characterisation of Organic Matter and Carbon Cycling in Rehabilitated Lignite-rich Mine Soils

Open-cast lignite mining in the Lusatian mining district resulted in rehabilitated mine soils containing up to four organic matter types: (1) recent plant litter, (2) lignite deposited by mining activity, (3) carbonaceous ash particles deposited during amelioration of the lignite-containing parent substrate and (4) airborne carbonaceous particles deposited during contamination. The influence of lignite-derived carbon types on the organic matter development and their role in the soil carbon cycle was unknown. This paper presents the findings obtained during a six year project concerning the impact of lignite on soil organic matter composition and the biogeochemical functioning of the ecosystem. The organic matter development after rehabilitation was followed in a chronosequence of rehabilitated mine soils afforested in 1966, 1981 and 1987. A differentiation of the organic matter types and an evaluation of their role within the ecosystem was achieved by the use of ¹⁴C activity measurements, ¹³C CPMAS NMR spectroscopy and wet chemical analysis of plant litter compounds. The results showed that the amount and degree of decomposition of the recent organic matter derived from plant material of the 30 year old mine soil was similar to natural uncontaminated forest soil which suggests complete rehabilitation of the ecosystem. The decomposition and humification processes were not influenced by the presence of lignite. On the other hand it was shown that lignite, which was thought to be recalcitrant because of its chemical structure, was part of the carbon cycle in these soils. This demonstrates the need to elucidate further the stabilisation mechanisms of organic matter in soils.