附加电场对中空纤维膜污染的减缓作用

通过对新型附加电场的中空纤维膜组件的实验室研究,探讨了电场对缓解微滤膜污染的作用.在恒定流量下过滤含有20mg/L腐殖酸的原水,无电压时,跨膜压力从0.0200MPa上升到0.0300MPa耗时2h,而施加60V电压时该时间段延长至10h.研究表明,原水中的腐殖酸在电场中发生电泳迁移,减少了向膜表面的移动,其对膜的污染被减缓;同时腐殖酸在电场中发生凝聚现象,沉积在膜表面形成疏松的滤饼层,是跨膜压力增加缓慢的另一原因.     

Tb(Ⅲ)对辣根叶片膜脂脂肪酸构成的影响

以辣根为材料,研究叶面喷洒Tb(Ⅲ)对辣根叶片膜脂脂肪酸构成的影响,结果表明,5 mg·l-1和60 mg·l-1 Tb(Ⅲ)均能增加膜脂饱和脂肪酸的百分含量,而降低不饱和脂肪酸含量,尤其是亚麻酸,但5mg·l-1 Tb)(Ⅲ)未能改变不饱和度指数,60 mg·l-1 Tb(Ⅲ)使不饱和度指数显著降低,同时,Tb(Ⅲ)使辣根叶片HRP活性降低,膜脂发生过氧化,表现为MDA含量增加,因此,Tb(Ⅲ)处理下膜脂脂肪酸的变化与Tb(Ⅲ)诱导的自由基升高有关,且在所有脂肪酸中,亚麻酸在稀土对膜脂脂肪酸影响中贡献最大.     

有机磷阻燃剂生产废水预处理工艺研究

采用液膜萃取—酸析沉降—络合萃取组合工艺对有机磷阻燃剂生产废水进行预处理.最佳工艺条件为:液膜萃取时,液膜油相(表面活性剂与煤油的混合液)与内水相(H2SO4溶液)的体积比2∶1、乳化液膜与废水的体积比1∶8、废水pH 13.0,硫酸体积分数10％、煤油中表面活性剂质量浓度30 g/L、液膜萃取时间 15 min;酸析沉降时,废水pH l.0,酸析沉降时间30 min;络合萃取时,络合萃取剂(烷基叔胺N235与煤油的混合液)中烷基叔胺N235体积分数30％,络合萃取剂与废水的体积比1∶4,废水pH l.0,络合萃取时间30 min.在此最佳处理条件下,废水COD总去除率可达93％,吡啶去除率达99.9％以上,总磷去除率可达97％,BOD5/COD提高至0.32,有利于后续生化处理.     

废SCR催化剂中钒和钨的有机酸浸出

在对废SCR催化剂组成进行分析的基础上,采用草酸和酒石酸两种有机酸浸取废SCR催化剂中的V和W。实验结果表明：草酸对V、W的浸出率均大于酒石酸;在草酸浓度为1.00 mol/L、浸取温度为80 ℃、液固比为10 mL/g、浸取时间为180 min时,V和W的浸出率分别为63.50%和13.12%;在酒石酸浓度为0.5 mol/L、浸取温度为100 ℃、液固比为10 mL/g、浸取时间为180 min时,V和W的浸出率分别为44.00%和9.00%。酸性浸出未改变SCR催化剂中TiO₂的晶型,剩余残渣中依然保留着TiO₂骨架,可继续作为催化剂载体使用。     

模拟酸雨对土壤修复中重金属淋溶特征及土壤持水能力的影响

以磷酸二氢钾（PDP）钝化后的重金属污染土壤为研究对象,通过室内土柱淋溶和土壤吸水实验,考察pH为3.1、4.6和5.1的模拟酸雨对污染土壤修复过程中重金属淋溶特征及土壤持水能力的影响。实验结果表明：PDP处理显著增加了淋出液的pH、电导率、TOC和正磷酸盐态磷（ZP）含量,在淋溶初期显著降低了淋出液的Cu、Cd和Pb含量,但在淋溶后期增大了Pb含量;土壤持水量与电导率、pH、TOC和ZP含量呈现极显著负相关性;土壤修复过程中,有机质的淋失、盐分含量及pH的增大可引起土壤持水能力的减弱。     

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。     

35kV并联电抗器工频电磁场分布特性研究

针对500kV变电站内产生较高工频磁场强度的电气设备——35kV并联电抗器,研究不同类型、不同排列方式下35kV并联电抗器周围工频电磁场分布规律。结果表明,35kV并联电抗器的电磁场强度随着离开电抗器中心距离的增加而降低,三角形排列的电抗器磁场强度大于水平排列的。     

发烟硫酸贮罐清洗安全技术

根据事故隐患分析 ,采取安全措施 ,成功地用中和法清洗发烟硫酸贮罐 ,并提出了贮罐的改进措施。     

荧光灯厂醋酸丁酯废气治理

有机废气的化学吸收是使废物重新进入物质循环 ,避免二次污染并产生经济效益的环境工程方法。针对某市荧光灯厂工艺过程 ,分析研究了废气治理的各种方法 ,提出了用氨水吸收醋酸丁酯废气 ,转化生成乙酰胺和丁醇的吸收净化方案 ,并对生成物质进行回收利用     

Analysis of the relationship between ambient levels of O3, NO2 and NO as a function of NOx in the UK

Monitoring data from the UK Automatic Urban and Rural Network are used to investigate the relationships between ambient levels of ozone (O₃), nitric oxide (NO) and nitrogen dioxide (NO₂) as a function of NO_x, for levels ranging from those typical of UK rural sites to those observed at polluted urban kerbside sites. Particular emphasis is placed on establishing how the level of ‘oxidant’, OX (taken to be the sum of O₃ and NO₂) varies with the level of NO_x, and therefore to gain some insight into the atmospheric sources of OX, particularly at polluted urban locations. The analyses indicate that the level of OX at a given location is made up of NO_x-independent and NO_x-dependent contributions. The former is effectively a regional contribution which equates to the regional background O₃ level, whereas the latter is effectively a local contribution which correlates with the level of primary pollution. The local oxidant source has probable contributions from (i) direct NO₂ emissions, (ii) the thermal reaction of NO with O₂ at high NO_x, and (iii) common-source emission of species which promote NO to NO₂ conversion. The final category may include nitrous acid (HONO), which appears to be emitted directly in vehicle exhaust, and is potentially photolysed to generate HO_x radicals on a short timescale throughout the year at southern UK latitudes. The analyses also show that the local oxidant source has significant site-to-site variations, and possible reasons for these variations are discussed. Relationships between OX and NO_x, based on annual mean data, and fitted functions describing the relative contributions to OX made by NO₂ and O₃, are used to define expressions which describe the likely variation of annual mean NO₂ as a function of NO_x at 14 urban and suburban sites, and which can take account of possible changes in the regional background of O₃.