有机质对土壤气相抽提去除四氯化碳效率的影响

某重要岩溶地下水源地因附近农药厂排放含四氯化碳污水而受到严重污染,实验采用土柱通风试验模拟土壤气相抽提(SVE),研究环境温度为20℃,通风速率为40mL/min,土壤含水率10%,而土壤有机质含量分别为3.02%和0.13%条件下的两种供试土壤中四氯化碳污染物的去除过程.结果表明,土柱通风能有效去除土壤中的四氯化碳污...     

Effects of metal and acidic sites on the reaction by-products of butyl acetate oxidation over palladium-based catalysts

Catalytic oxidation is widely used in pollution control technology to remove volatile organic compounds. In this study, Pd/ZSM-5 catalysts with different Pd contents and acidic sites were prepared via the impregnation method. All the catalysts were characterized by means of N2 adsorption- desorption, X-ray fluorescence （XRF）, HE temperature programmed reduction （H2-TPR）, and NH3 temperature programmed desorption （NH3-TPD）. Their catalytic performance was investigated in the oxidation of butyl acetate experiments. The by-products of the reaction were collected in thermal desorption tubes and identified by gas chromatography/mass spectrometry. It was found that the increase of Pd content slightly changed the catalytic activity of butyl acetate oxidation according to the yield of CO2 achieved at 90%, but decreased the cracking by-products, whereas the enhancement of strong acidity over Pd-based catalysts enriched the by-product species. The butyl acetate oxidation process involves a series of reaction steps including protolysis, dehydrogenation, dehydration, cracking, and isomerization. Generally, butyl acetate was cracked to acetic acid and 2- methylpropene and the latter was an intermediate of the other by-products, and the oxidation routes of typical by-products were proposed. Trace amounts of 3-methylpentane, hexane, 2-methylpentane, pentane, and 2-methylbutane originated from iso4merization and protolysis reactions.     

Seasonal and diurnal variations of atmospheric peroxyacetyl nitrate, peroxypropionyl nitrate, and carbon tetrachloride in Beijing

Atmospheric peroxyacetyl nitrate(PAN), peroxypropionyl nitrate(PPN), and carbon tetrachloride(CCl4) were measured from September 2010 to August 2011 in Beijing. PAN exhibited low values from mid-autumn to early spring(October to March) with monthly average concentrations ranging from 0.28 to 0.73 ppbV, and increased from early spring to summer(March to August), ranging from 1.37–3.79 ppbV. The monthly variation of PPN was similar to PAN, with low values(below detection limit to 0.18 ppbV) from mid-autumn to early spring, and a monthly maximum in September(1.14 ppbV). The monthly variation of CCl4was tightly related to the variation of temperature, exhibiting a minimum in winter(69.3 pptV) and a maximum of 180.6 pptV in summer. Due to weak solar intensity and short duration, PAN and O3showed no distinct diurnal patterns from morning to night during winter, whereas for other seasons, they both exhibited maximal values in the late afternoon(ca. 15:00 to 16:00 local time) and minimal values during early morning and midnight. Good linear correlations between PAN and PPN were found in autumn(R = 0.91), spring(R = 0.94), and summer(R = 0.81), with slopes of 0.130, 0.222, and 0.133, respectively, suggesting that anthropogenic hydrocarbons dominated the photochemical formation of PANs in Beijing. Positive correlation between PAN and O3 in summer with the low slopes( O3 / PAN) ranging from 9.92 to 18.0 indicated serious air pollution in Beijing, and strong negative correlation in winter reflected strong O3consumption by NO titration and less thermal decompositin of PAN.     

Origin of major ions in monthly rainfall events at the Bamenda Highlands, North West Cameroon

Rainwater characteristics can reveal emissions from various anthropogenic and natural sources into the atmosphere. The physico-chemical characteristics of 44 monthly rainfall events （collected between January and December 2012） from 4 weather stations （Bamenda, Ndop plain, Ndawara and Kumbo） in the Bamenda Highlands （BH） were investigated. The purpose was to determine the sources of chemical species, their seasonal inputs and suitability of the rainwater for drinking. The mean pH of 5 indicated the slightly acidic nature of the rainwater. Average total dissolved solids （TDS） were low （6.7 mg/L）, characteristic of unpolluted atmospheric moisture/air. Major ion concentrations （mg/L） were low and in the order K＋ 〉 Ca2＋ 〉 Mg2~ 〉 Na＋ for cations and NO3 〉〉 HCO3 〉 SO] 〉 CI- 〉 PO3- 〉 F- for anions. The average rainwater in the area was mixed Ca-Mg-SO4-CI water type. The CI-/Na＋ ratio （1.04） was comparable to that of seawater （1.16）, an indication that N a＋ and CI originated mainly from marine （Atlantic Ocean） aerosols. High enrichments of Ca2＋, Mg2＋ and SO2- to Na＋ ratios relative to seawater ratios （constituting 44% of the total ions） demonstrated their terrigenous origin, mainly from Saharan and Sahelian arid dusts. The K＋/Na＋ ratio （2.24）, which was similar to tropical vegetation ash （2.38）, and NO3 was essentially from biomass burning. Light （〈 100 mm） pre-monsoon and post-monsoon convective rains were enriched in major ions than the heavy （〉 100 mm） monsoon rains, indicating a high contribution of major ions during the low convective showers. Despite the acidic nature, the TDS and major ion concentrations classified the rainwater as potable based on the WHO guidelines.     

Fe2+和Fe3+对厌氧氨氧化污泥活性的影响

通过接种厌氧氨氧化污泥研究了Fe离子浓度及价态变化对厌氧氨氧化污泥活性的影响.短期浓度影响结果表明,当进水铁离子浓度由0升高到5 mg·L-1时,厌氧氨氧化污泥活性因受刺激而逐渐增强;当进水铁离子浓度大于5 mg·L-1时,因厌氧氨氧化反应产碱,铁离子形成氢氧化物沉淀,生物活性未受到影响.不同价态铁离子浓度变化对厌氧氨氧化污泥活性的影响无明显区别.长期价态影响结果表明,经过71个周期培养,含Fe2+进水的厌氧氨氧化反应器R1脱氮效能(以氮计)由0.28 kg·(m3·d)-1升高到0.65 kg·(m3·d)-1,是含Fe3+进水反应器R2的1.28倍.因此Fe2+更适合厌氧氨氧化菌生长的需求.实验结果进一步表明,Fe3+易导致厌氧氨氧化反应器R2内氨氮过量转化,亚硝氮与氨氮转化比(1.17)明显低于含Fe2+进水的反应器R1内亚硝氮与氨氮转化比(1.24).     

双组分VOCs的催化氧化及动力学分析

考察了微波加热与管式炉加热下挥发性有机化合物(VOCs)甲苯与氯苯的催化氧化性能,并对双组分VOCs的反应动力学进行了分析.结果表明,VOCs的竞争吸附使得双组分中甲苯和氯苯的转化率比单组分降低3%~12%;微波的"热点效应"与"非热效应"使得VOCs转化效率明显优于管式炉加热,尤其是氯苯的转化率提高了31%~38%;微波加热降低了氧化反应温度和处理能耗.动力学分析表明,微波加热下甲苯和氯苯的反应活化能比管式炉加热下减少了2146 J·mol-1和1450J·mol-1,微波加热下氯苯的化学反应速率常数是管式炉加热的35倍,甲苯的反应速率常数提高了6倍.     

流化床O2/CO2气氛燃煤痕量元素的排放特性及控制

通过平顶山烟煤在小型流化床中的燃烧实验,采用X-射线荧光光谱仪(XRF)对低压撞击器(LPI)收集到的细颗粒物元素组成进行定量测定,研究了O2/CO2气氛下硅藻土对煤粉燃烧痕量元素的排放控制.结果表明,Zn、Mn和Ni的含量随粒径呈双峰分布,峰值分别在0.1μm和2μm附近,Hg和Co的含量在0.1μm附近有一峰值;Hg和Zn在亚微米颗粒上有一定程度的富集,Mn、Ni和Co在亚微米和超微米颗粒上的含量基本相当;当颗粒物粒径一定时,随着硅藻土含量的增加,5种元素的富集因子呈减小的趋势;随着添加剂粒径的减小,颗粒物中Hg、Mn、Zn、Ni和Co的含量呈减少的趋势;当颗粒物粒径一定时,5种元素含量顺序为MnZnNiCoHg.     

流动搅动法研究针铁矿对亚砷酸盐的吸附特征

采用流动搅动法,在溶液p H、浓度和温度影响条件下,研究针铁矿对亚砷酸盐吸附的特征.结果表明,在不同条件下,亚砷酸盐的吸附过程分为快反应和慢反应这2个阶段.随溶液p H的升高,砷的吸附量逐渐降低,表观吸附速率常数(k')逐渐增大,半反应时间(t1/2)也就越小,砷的吸附反应达到平衡时间就越短,且砷的扩散速率常数b值也逐渐降低.溶液p H 3.0和p H7.0时,砷最大吸附量分别为246.9 mg·kg~(-1)和99.8 mg·kg~(-1).随着砷浓度的升高,针铁矿对砷的吸附量增加,表观吸附速率常数(k')逐渐增大;砷浓度为0.10 mg·L~(-1)和1.00 mg·L~(-1)时,砷的最大吸附量分别为96.5 mg·kg~(-1)和249.1 mg·kg~(-1).Freundlich方程中吸附常数Kf值随着时间的延长逐渐降低,其吸附能力是逐渐减弱的.Langmuir方程分配因子RL在0~1之间,表现为针铁矿上砷的吸附为优惠吸附.随着温度的升高,针铁矿对砷的吸附量增加,表观吸附速率常数k'值也逐渐升高.温度为298K和313 K时,砷最大吸附量分别为241.1 mg·kg~(-1)和315.6 mg·kg~(-1).用抛物线扩散方程b值来计算扩散过程的伪热力学常数,砷吸附反应的活化能(E*a)为14.60 k J·mol~(-1).砷扩散活化焓变(ΔHθ)随着温度的升高有所降低,ΔHθ均为正值,扩散过程为吸热反应,升高温度有利于砷的吸附;活化自由能变(ΔGθ)随着温度的上升而升高,升高温度有利于加快扩散过程;ΔSθ值均为负,说明吸附反应使体系有序度增加.     

水热法制备玉米叶基生物炭对亚甲基蓝的吸附性能研究

以农业废弃物玉米叶和玉米秆为原材料,采用水热法制备生物炭,通过批试验方法考察了接触时间、污染物初始浓度、生物炭投加量、反应体系温度及溶液p H值等因素对2种生物炭吸附亚甲基蓝的影响,并对吸附规律进行了探讨.吸附动力学拟合结果发现,准二级动力学能更好地拟合吸附过程(R~2=0.9986~0.9999);颗粒内扩散方程拟合结果表明,2种生物炭对亚甲基蓝的吸附由液膜扩散和颗粒内扩散2个过程控制.玉米叶基生物炭对亚甲基蓝的吸附可以通过Freundlich方程来进行拟合(R~2=0.9898),说明吸附在生物炭表面是多分子层吸附过程;而玉米杆基生物炭对亚甲基蓝的吸附更符合Langmuir方程(R~2=0.9825),说明吸附在生物炭表面是单分子层吸附过程.与玉米杆基生物炭相比,玉米叶基生物炭具有更好的吸附性能,拟合理论最大吸附量为玉米杆基生物炭的1.25倍.     

贵阳市一居民区大气颗粒态汞的污染状况

2004年4、7、8、11、12月采用微型捕集管-冷原子荧光光谱法对贵阳市一个居民区大气中的痕量颗粒态总汞(TPM)进行了测定。结果表明:TPM日均浓度范围是0.149~4.853 ng.m-3,平均值是1.091 ng.m-3,显著高于背景参考值1~86 pg.m-3;TPM浓度采暖期大于非采暖期,夜间通常大于白昼;TPM与大气气态总汞(TGM)可能具有同源性;燃煤、垃圾焚烧以及周边工厂排放的含尘烟气可能是居民区大气颗粒态汞的主要人为来源。