金属改性碳脱除PH3和H2S动力学及反应机理研究

为综合利用黄磷尾气中的CO,通过计算平均活化能和测定XPS、TG/DTA和氮吸附特性的方法,研究了Cu²⁺和某金属离子Mn⁺改性碳脱除PH₃和H₂S的动力学和反应机理问题。结果表明：H₂S在金属改性碳上反应时平均活化能为134.4 J/mol为-0.76级反应,PH₃在金属改性碳上反应时平均活化能为1 247.6 J/mol为-0.8级反应;减小改性碳粒径增加流量可以显著提高其脱除PH₃和H₂S的速率;XPS、TG/DTA和孔径分布分析证明,改性碳净化H₂S和PH₃是一个催化吸附过程,H₂S和PH₃首先与氧在改性碳表面进行催化氧化反应,然后生成S和P₂O₅沉积吸附在改性碳表面。     

CPAM调质浓缩污泥脱水的影响因素及其机理研究

污水处理厂剩余污泥的处置是当前业界的热点。研究了阳离子聚丙烯酰胺(CPAM)调质浓缩污泥脱水的一些影响因素,如药剂投加量、污泥pH值、环境温度、搅拌条件等。同时,还对污泥絮凝脱水机理进行了一定的探讨。研究表明：阳离子聚丙烯酰胺(CPAM)作为浓缩污泥脱水剂,在优化投加量下、污泥pH值在5.0～7.5、低速搅拌时,有较好的脱水效果。环境温度对污泥的脱水效果也有一定的影响,夏天处理优于冬天处理。     

Fenton氧化法降解丙烯酸废水的研究

利用废铁屑与H₂O₂形成的Fenton氧化反应来降解工业丙烯酸废水中的丙烯酸。在间歇反应器中,系统地考察了反应时间、H2O2浓度、液固比(废水质量∶固体质量)和反应温度对丙烯酸的降解率的影响,优选了工艺条件。在连续固定床反应器中进行了对比实验,以考察固液接触状态的影响及系统的稳定性。结果表明,废铁屑与H₂O₂构成的Fenton体系能有效地降解废水中的丙烯酸。在间歇工况下,适宜的条件为,液固比40∶1,温度20～25℃,H₂O₂浓度800 mg/L ,反应时间35 min,在此条件下,丙烯酸的降解率可达到95%以上。对比实验表明,固液接触状态对降解效果的影响不大,铁屑的性能稳定,在连续93 h的稳定性实验中,丙烯酸的降解率保持在90%左右。     

COD浓度和进水流量比对一体化工艺脱氮除碳的影响

保持进水总流量不变,以一定流量比同时从缺氧区和厌氧区进水,探讨了不同进水流量比(R=Q_厌/Q_缺)和进水COD浓度对中心岛式一体化OCO工艺脱氮除碳的影响。研究结果表明,进水COD浓度和进水流量比Rs对COD的去除效果影响不大,出水COD浓度一直稳定在50 mg/L以下,去除率在92%以上;进水COD浓度和进水流量比Rs共同决定着系统TN的去除效果,进水COD浓度为100 mg/L、200 mg/L时,TN去除率随着进水流量比Rs的减小呈增加的趋势;当进水COD浓度为 300 mg/L时,TN去除率随着进水流量比Rs的减小呈先升高后降低的趋势,在进水流量比Rs为3∶1时TN去除率最高,达到87%。     

载硫活性炭微观结构和表面形态研究

为了增强活性炭脱除燃煤电厂烟气中汞的能力,利用汞和硫可以生成稳定的HgS的性质,研究了通过热沉淀增加了活性炭中的硫含量的改性方法,并以SEM、BET、TGA等方法,研究了改性对活性炭表面形貌、硫在活性炭中的分布、活性炭比表面积等性能的影响。结果表明,热沉淀改性方法可以增加活性炭中的硫含量;硫粘附在活性炭的炭链上量较多,孔壁较少;改性工艺降低了活性炭的比表面积,且改性活性炭的比表面积随着温度的升高而增大;载硫后,活性炭中元素硫和炭的结合被增强。     

上海虹桥综合交通枢纽灾害链及其在灾害评估中的应用

灾害的发生发展呈现链式有序的传承效应(灾害链),为灾害的预防和控制带来了不小的困难.上海虹桥综合交通枢纽工程集多种换乘方式于一体,一旦发生灾害,势必造成连锁反应,造成巨大损失,必须对其进行防灾治灾研究.应用灾害链思想结合模糊综合评判法的思路,提出了灾害链定量分析方法并对虹桥枢纽灾害等级进行了评估.     

城镇社区地震应急能力评价指标体系的构建

城镇社区是构成城镇的基本单元,是政府实施社会管理的基本单元和主要依托,也是城镇防灾减灾的基本单元.城镇社区地震应急能力评价是地震应急管理的重要内容,建立社区地震应急能力评价指标体系对提高社区地震应急能力、建设地震安全社区和促进城镇地震应急管理工作具有重要意义.     

High methane emissions from a littoral zone on the Qinghai-Tibetan Plateau

The littoral zones of lakes have been regarded as hotspots of methane (CH₄) fluxes through several studies. In the present study, we measured CH₄ fluxes in six kinds of littoral zones of Huahu Lake on the Qinghai-Tibetan Plateau in the peak growing season of 2006 and 2007. We found that CH₄ efflux (ranging from −0.1 to 90 mg CH₄ m⁻² h⁻¹) from the littoral zones of this lake was relatively high among those of boreal and temperate lakes. Our results also showed that emergent plant zones (Hippuris vulgaris and Glyceria maxima stands) recorded the highest CH₄ flux rate. The CH₄ flux in the floating mat zone of Carex muliensis was significantly lower than those of the emergent plant zones. CH₄ fluxes in the floating-leaved zone of Polygonum amphibium and bare lakeshore showed no significant difference and ranked last but one, only higher than that of the littoral meadow (Kobresia tibetica). Plant biomass and standing water depths were important factors to explain such spatial variations in CH₄ fluxes. No significant temporal variations in CH₄ fluxes were found due to the insignificant variations of physical factors in the peak growing season. These results may help in our understanding of the importance of the littoral zone of lakes, especially the emergent plant zone, as a hotspot of CH₄ emission.     

Measurement of aerosol number size distributions in the Yangtze River delta in China: Formation and growth of particles under polluted conditions

Particle size distribution is important for understanding the sources and effects of atmospheric aerosols. In this paper we present particle number size distributions (10 nm–10 μm) measured at a suburban site in the fast developing Yangtze River Delta (YRD) region (near Shanghai) in summer 2005. The average number concentrations of ultrafine (10–100 nm) particles were 2–3 times higher than those reported in the urban areas of North America and Europe. The number fraction of the ultrafine particles to total particle count was also 20–30% higher. The sharp increases in ultrafine particle number concentrations were frequently observed in late morning, and the particle bursts on 5 of the 12 nucleation event days can be attributed to the homogeneous nucleation leading to new particle formation. The new particle formation events were characterized with a larger number of nucleation-mode particles, larger particle surface area, and larger condensational sink than usually reported in the literature. These suggest an intense production of sulfuric acid from photo-oxidation of sulfur dioxide in the YRD. Overall, the growth rate of newly formed particles was moderate (6.4 ± 1.6 nm h^?1), which was comparable to that reported in the literature.     

Measurement of black carbon aerosols near two Chinese megacities and the implications for improving emission inventories

Knowledge of the distribution and sources of black carbon (BC) is essential to understanding its impact on radiative forcing and the establishment of a control strategy. In this study, we analyze atmospheric BC and its relationships with fine particles (PM_2.5) and trace gases (CO, NO_y and SO₂) measured in the summer of 2005 in two areas frequently influenced by plumes from Beijing and Shanghai, the two largest cities in China. The results revealed different BC source characteristics for the two megacities. The average concentration of BC was 2.37 (±1.79) and 5.47 (±4.00) μg m^?3, accounting for 3.1% and 7.8% of the PM_2.5 mass, in Beijing and Shanghai, respectively. The good correlation between BC, CO and NO_y (R² = 0.54–0.77) and the poor correlation between BC and SO₂ suggest that diesel vehicles and marine vessels are the dominant sources of BC in the two urban areas during summer. The BC/CO mass ratio in the air mass from Shanghai was found to be much higher than that in the air mass from Beijing (0.0101 versus 0.0037 ΔgBC/ΔgCO), which is attributable to a larger contribution from diesel burning (diesel-powered vehicles and marine vessels) in Shanghai. Based on the measured ratios of BC/CO and annual emissions of CO, we estimate that the annual emissions of BC in Beijing and Shanghai are 9.51 Gg and 18.72 Gg, respectively. The improved emission rates of BC will help reduce the uncertainty in the assessment of the impact of megacities on regional climate.