稀土元素Pr辅助的类Fenton试剂氧化法处理染料废水

以靛蓝为目标污染物,采用稀土元素Pr辅助的类Fenton试剂氧化法处理模拟染料废水。制备了双金属氧化物催化剂Fe_2-xPr_xO₃,考察了催化剂中n（Pr）∶n（Fe）、催化剂加入量、初始靛蓝质量浓度、H₂O₂加入量、废水pH对废水脱色效果的影响。实验结果表明：Pr在很大程度上提高了类Fenton反应的效率,废水脱色率得到显著提高;在n（Pr）∶n（Fe）=1∶5、初始靛蓝质量浓度为30 mg/L、催化剂加入量为500 mg/L、H₂O₂加入量为40 mL/L、废水pH为3的最佳工艺条件下,反应50 min时废水脱色率达到92.78%。     

超细颗粒物凝聚中试试验均匀给料方案研究

给料的均匀性对PM2.5团聚试验至关重要,运用数值方法,采用LES模型计算湍流流场,采用DPM模型计算颗粒运动轨迹,分析PM2.5团聚中试试验台烟道内加设钝体后颗粒的均匀分布,得到了水平烟道各截面处颗粒浓度分布及数值的均方差曲线,发现在试验台圆方管处加设钝体,能有效改善烟道内煤灰颗粒的均匀分布。     

表面活性剂改性活性炭对阳离子染料的吸附

以阴离子表面活性剂十二烷基硫酸钠(SDS)为改性剂对粉末活性炭(AC)改性,研究了SDS在活性炭表面的吸附稳定性,用比表面积测定仪、Zeta电位测定仪对改性前后活性炭进行表征,并将其用于吸附模拟废水中的阳离子染料。结果表明,改性剂SDS浓度等于临界胶束浓度时,改性后活性炭(SDS-AC)对SDS吸附稳定,SDS在纯水和染料溶液中的解吸率分别为19.4%和1.6%。pH对活性炭吸附阳离子橙染料影响较小,SDS-AC和AC对染料的吸附平衡时间分别为4 h和12 h,SDS-AC和AC对阳离子橙染料的吸附动力学模型符合拟二级反应模型,吸附等温线更符合Langmuir吸附等温方程,SDS-AC对阳离子橙染料的最大吸附量较AC提高47.8%,SDS-AC对阳离子橙染料的吸附机制为物理吸附和化学吸附共同作用下的单分子层吸附,其中化学吸附是主要控速步骤。     

丝瓜瓤固定化脱色菌Enterobactor sp.S8 对活性黑5的脱色

利用植物载体丝瓜瓤对肠杆菌(Enterobactor sp.S8)进行固定,并对活性黑5进行脱色研究.探讨了固定化菌体的菌龄、菌量、pH、温度对染料脱色的影响.研究了该固定化菌体的重复利用和动力学实验.结果表明,最佳脱色条件为:菌龄3d、接菌量2％、温度30℃、pH 6.0.该固定化菌体对不同初始浓度活性黑5的脱色符合二级反应动力学方程.经9次重复利用后的该固定化菌体,其脱色率仍达76.8％.在优化实验条件下,根据降解3d前后的紫外-可见光谱图分析可知,活性黑5并非完全被降解为CO2和H2O,而是生成一些小分子有机中间体.     

剩余污泥催化剂的制备及其脱色性能

以焦化废水脱水污泥为载体、ZnCl2为活化剂和催化剂的活性组分,采用一步法制备污泥催化剂。实验结果表明,当ZnCl2浓度为4 mol/L、固液比1∶3、焙烧温度550℃、焙烧时间40 min时,制备的污泥催化剂对亚甲基蓝的脱色性能最佳。利用制备的催化剂对活性红X-3B、弱酸性艳红B、活性蓝X-BR溶液进行脱色处理,研究反应时间、染料浓度、溶液pH、催化剂投加量和H2O2用量对染料脱色性能的影响。最佳条件下,3种废水的脱色率分别达到90.7%、97.5%和94.4%。对脱色数据进行动力学模拟,结果表明,3种染料废水脱色反应分别符合二级动力学模型、一级动力学模型、二级动力学模型。     

感应热固定床CWPO处理染料废水的催化剂制备及其性能

感应热固定床(IHFB)作为新型热传递方式下非均相反应器,利用感应加热铁磁材料将热量传递至液相,形成固液界面高温微反应区,实现有机废水低能高效降解。实验以海绵铁为感应内核,淀粉为碳源,0.2 mol/L硝酸镍为浸渍溶液,按照一定固液比采用浸渍焙烧法制备了C包覆表层负载NiO的感应热催化剂(mNiO/C),对mNiO/C材料的形态结构进行了SEM、ES和XRD表征。结果表明,铁碳比(Fe/C)3∶1、浸渍固液比1∶1、500℃下焙烧2 h,重复包覆3次所得的mNiO/C材料结构最稳定、催化活性最大。并以直接紫D-BL模拟废水为进水,考察了流动状态下感应热固定床催化湿式过氧化氢氧化法(CWPO)降解染料废水的性能,在最优条件下,染料降解率高达80%以上。     

烟气成分对负载V_2O_5-WO_3/TiO_2聚苯硫醚纤维脱除烟气中Hg~0的影响

通过固定床实验系统模拟烟气脱除Hg0的实验,研究了O2、HCl、NO、SO2、H2O和NH3对滤袋常用的聚苯硫醚(PPS)纤维负载V2O5-WO3/TiO2新型催化剂后脱除烟气中Hg0的影响,并分析其影响机理。结果表明,在温度为200℃、高纯N2气氛下,Hg0的脱除率很低,加入4%O2后,脱除率有所增加;0.05‰HCl条件下Hg0的脱除率仅为5%,而0.01‰HCl与4%O2并存的条件下,脱除率明显提高;NO对Hg0的催化氧化促进作用不是很显著;SO2对Hg0氧化具有毒害作用;H2O和NH3可抑制Hg0的脱除,O2的存在可抵消NH3的部分抑制作用。     

Modelling of iron cycling and its impact on the electron balance at a petroleum hydrocarbon contaminated site in Hnevice, Czech Republic

Over a period of several decades multiple leaks of large volumes from storage facilities located near Hnevice (Czech Republic) have caused the underlying Quaternary aquifer to be severely contaminated with nonaqueous phase liquid (NAPL) petroleum hydrocarbons. Beginning in the late 1980's the NAPL plume started to shrink as a consequence of NAPL dissolution exceeding replenishment and due to active remediation. The subsurface was classified geochemically into four different zones, (i) a contaminant-free zone never occupied by NAPL or dissolved contaminants, (ii) a re-oxidation zone formerly occupied by NAPL, (iii) a zone currently occupied by NAPL, and (iv) a lower fringe zone between the overlying NAPL and the deeper underlying contaminant-free zone. The study investigated the spatial and temporal variability of the redox zonation at the Hnevice site and quantified the influence of iron-cycling on the overall electron balance. As a first step inverse geochemical modelling was carried out to identify possible reaction models and mass transfer processes. In a subsequent step, two-dimensional (forward) multi-component reactive transport modelling was performed to evaluate and quantify the major processes that control the geochemical evolution at the site. The study explains the observed enrichment of the lower fringe zone with ferrihydrite as a result of the re-oxidation of ferrous iron. It suggests that once the NAPL zone started to shrink the dissolution of previously formed siderite and FeS by oxygen and nitrate consumed a significant part of the oxidation capacity for a considerable time period and therefore limited the penetration of electron acceptors into the NAPL contaminated zone.     

Modelling geochemical and microbial consumption of dissolved oxygen after backfilling a high level radiactive waste repository

Dissolved oxygen (DO) left in the voids of buffer and backfill materials of a deep geological high level radioactive waste (HLW) repository could cause canister corrosion. Available data from laboratory and in situ experiments indicate that microbes play a substantial role in controlling redox conditions near a HLW repository. This paper presents the application of a coupled hydro-bio-geochemical model to evaluate geochemical and microbial consumption of DO in bentonite porewater after backfilling of a HLW repository designed according to the Swedish reference concept. In addition to geochemical reactions, the model accounts for dissolved organic carbon (DOC) respiration and methane oxidation. Parameters for microbial processes were derived from calibration of the REX in situ experiment carried out at the Asp? underground laboratory. The role of geochemical and microbial processes in consuming DO is evaluated for several scenarios. Numerical results show that both geochemical and microbial processes are relevant for DO consumption. However, the time needed to consume the DO trapped in the bentonite buffer decreases dramatically from several hundreds of years when only geochemical processes are considered to a few weeks when both geochemical reactions and microbially-mediated DOC respiration and methane oxidation are taken into account simultaneously.     

Long-range transport of acidifying substances in East Asia—Part II: Source–receptor relationships

Region-to-grid source–receptor (S/R) relationships are established for sulfur and reactive nitrogen deposition in East Asia, using the Eulerian-type Community Multiscale Air Quality (CMAQ) model with emission and meteorology data for 2001. We proposed a source region attribution methodology by analyzing the non-linear responses of the CMAQ model to emission changes. Sensitivity simulations were conducted where emissions of SO₂, NO_x, and primary particles from a source region were reduced by 25%. The difference between the base and sensitivity simulations was multiplied by a factor of four, and then defined as the contribution from that source region. The transboundary influence exhibits strong seasonal variation and generally peaks during the dry seasons. Long-range transport from eastern China contributes a significant percentage (>20%) of anthropogenic reactive nitrogen as well as sulfur deposition in East Asia. At the same time, northwestern China receives approximately 35% of its sulfur load and 45% of its nitrogen load from foreign emissions. Sulfur emissions from Miyakejima and other volcanoes contribute approximately 50% of the sulfur load in Japan in 2001. Sulfur inflows from regions outside the study domain, which is attributed by using boundary conditions derived from the MOZART global atmospheric chemistry model, are pronounced (10–40%) over most parts of Asia. Compared with previous studies using simple Lagrangian models, our results indicate higher influence from long-range transport. The estimated S/R relationships are believed to be more realistic since they include global influence as well as internal interactions among different parts of China.