仿酶型磁性Fe~0-Fe_3O_4复合催化剂的制备及其催化性能

采用原位氧化沉淀法制备出仿酶型磁性Fe0-Fe_3O_4复合催化剂,并将其作为非均相类Fenton催化剂用于溶液中对硝基苯酚的降解;采用SEM和XRD等技术对催化剂进行了表征。表征结果显示,Fe_3O_4与Fe0结合牢固,有利于Fe0的分散。实验结果表明:Fe0-Fe_3O_4对对硝基苯酚的降解为拟一级反应;在Fe0与Fe_3O_4的质量比为0.75、Fe0-Fe_3O_4投加量为1.2 g/L、初始H_2O_2浓度为10 mmol/L、初始溶液p H为3、反应温度为30℃的条件下反应90min,反应速率常数为0.067 min-1,COD去除率为77.28%,Fe溶出量为2.12 mg/L;在对硝基苯酚的降解过程中,pH先增大后减小,Fe溶出量先降低后升高;Fe0-Fe_3O_4是一种稳定的催化剂,可再生使用。     

城市内河生物修复及其对底泥氮素转化影响的实验研究

对在城市内河底泥有机质与有机氮含量高的特殊环境下进行水体修复的可行性与修复方法进行了探讨.富含高有机氮的城市内河底泥是氮素的重要释放源,采用向水体曝气可以有效地促使总氮与NH3-N的降解,与未曝气相比,10 d后曝气条件下二者的去除率分别达到81%和92%;此时再以土著水生植物进行修复可以显著地提高水体修复的效果、稳定性与修复成功率,并使总氮、NH3-N维持在1 ms/L和0.5 ms/L以下.但应避免城市内河有效光辐射的减少对水体修复影响.     

生物膜富集系统的同步短程硝化反硝化研究

在自制生物膜反应器中接种精养鱼塘底泥进行富集培养,以期启动同步短程硝化反硝化过程。富集过程中记录反应器进、出水DO、NH4+-N、NO2--N和NO3--N变化。经过179 d运行后,反应器NH4+-N去除率达80%以上,出水NO2--N浓度非常低,低至检测极限以下,且没有NO3-积累。实时荧光定量PCR技术定量富集培养前后研究氨氧化细菌、反硝化细菌密度和厌氧氨氧化细菌数量,发现反应器中氨氧化细菌和反硝化细菌浓度分别增加了53.4倍和8.3倍,未检出厌氧氨氧化菌。综合上述结果判断生物膜反应器内启动了同步短程硝化反硝化过程。     

ABS树脂装置丁二烯聚合工段废水水质表征

为确定某ABS树脂装置丁二烯聚合工段废水水质,特别是特征有机物种类,采用吹扫捕集、静态顶空、固相萃取、固相微萃取和液液萃取等预处理方法与GC/MS(气相色谱/质谱)联用,定性检测出该工段废水中含有16种挥发、半挥发性有机物,主要包括烯烃、苯系物、有机腈、多环芳烃、醚、醇和胺. 废水ρ(SS)(SS为悬浮物)为540.31 mg/L;SS粒径主要分布在0.10~5.00 μm之间,可吸附水中4.83%~33.21%的对二甲苯、乙苯、苯乙烯和1,5-环辛二烯等有机物. 与生活污水不同,该工段废水三维荧光光谱图的荧光区域集中在λ_Ex/λ_Em(激发波长/发射波长)=205~285 nm/310~360 nm范围内,主要包括λ_Ex/λ_Em为285 nm/350 nm、260 nm/310 nm、225 nm/345 nm、210 nm/315 nm、230 nm/360 nm的5个荧光峰,由甲苯、靛蓝、苯乙烯、脱氢松香酸、芴、菲等苯系物和多环芳烃类有机物引起. 废水在200~250 nm之间有较强紫外吸收峰,主要由1,3-丁二烯、苯甲醛、苯乙酮、4-苯基-1-环己烯等共轭二烯、不饱和醛、酮和苯系物等有机物引起.      

恢复措施对排土场土壤酶活性和微生物量的影响

以海州露天矿排土场为研究对象,选取工程复垦、人工种植林地(榆树、刺槐和紫穗槐)和天然草地3种恢复措施作为修复地,以荒裸地作为对照,研究恢复措施对土壤酶活性和土壤微生物量的影响,探讨生态恢复措施对排土场土壤质量的改善情况.结果表明,在同一土层中,修复地土壤脲酶、蛋白酶、蔗糖酶、碱性磷酸酶的活性和土壤微生物量显著高于荒裸地(P0.05),人工林地和天然草地在提高上述4种土壤酶活性方面显著高于工程复垦地(P0.05),工程复垦能够显著提高土壤过氧化氢酶活性(P0.05),却不能显著提高土壤微生物量(P0.05).表层土壤中,微生物量C/N比值表现为人工林地和天然草地显著高于其他土壤(P0.05),深层土壤则为荒裸地最高.从垂直分布上看,土壤酶活性和土壤微生物量C、N随着土壤深度的增加而降低.相关分析表明,土壤酶活性和微生物量与土壤养分含量之间密切相关,说明土壤酶活性和微生物量可以作为评价排土场土壤质量的生物学指标.3种恢复措施对土壤质量的改善能力依次为人工林地天然草地工程复垦地,在林种的选择上为乔木灌木.     

High resolution proton NMR spectroscopy of human amniotic fluid

Human amniotic fluid (HAF) is a dynamic system whose characteristics depend on continuous interchanges between fetal and maternal circulations. HAF reflects not only the environment of the fetus but may also provide information about fetal development or pathology. The concentration of HAF constituents varies with gestational age and pathological states. The number of the compounds currently implicated in fetal developmental pathology are relatively few. Currently used assay methods are not adequate to totally explain or predict the complex biochemistry of the fetus. The purpose of this work was to investigate HAF with NMR spectroscopy. In the present study HAF was obtained from 47 women undergoing routine amniocentesis. Cells were separated for karyological analysis and the supernatant was acid-extracted, lyophilized and re-suspended in D₂0 resulting in a concentration increase over native fluid. ¹H NMR spectra were obtained at 360 MHz and 60 MHz. Eighteen compounds including several amino acids, were identified using parallel reference and standard addition protocols. NMR spectroscopy detected compounds of known clinical importance including glucose, leucine, isoleucine, lactate and creatinine. In conclusion, we have demonstrated that a number of physiologically relevant compounds are readily observable in HAF using ¹H NMR spectroscopy. This technique can currently provide valuable information regarding HAF composition and has the potential of being used in vivo in the future.     

城市内河蓝藻复苏和生长规律研究

主要探讨城市化对城市内河蓝藻复苏和生长的影响。这些影响包括河流中营养物的升高、高等水生植物的灭绝、河水所受光照强度的变化以及由河水滞流带来的水体复氧效率降低对内河中蓝藻爆发条件的影响。通过实验我们发现金鱼藻与水网藻的存在可以在一定程度上抑制蓝藻的生长,金鱼藻的效果比水网藻更明显。适宜的光照是蓝藻大量生长的条件。对水体进行曝气复氧可以抑制蓝藻的生长。     

基于复杂网络理论的北京地铁网络脆弱性评估

以北京市现有地铁线网为研究对象,使用Space L方法构建拓扑网络,为更加符合实际情况,对换乘车站进行了拆分。分析中,综合考虑连通OD对和出行效率两个因素,以运输能力损失作为评估网络脆弱性指标。随后,计算分析了单节点攻击、随机攻击、静态攻击和动态攻击下造成的地铁网络运输能力损失的变化规律,得出动态攻击对地铁网络影响最大。在该攻击方式下,相对基于度的动态攻击,地铁网络对基于介数和基于ER的动态攻击,具有更高的脆弱性。同时攻击介数较大的节点对网络南北方向运输能力影响较大;攻击对出行效率影响较高的节点对网络东西方向运输能力影响较大。因此,在地铁运营过程中,应针对不同站点的节点属性和事故发生情况,采取相关防护措施。     

Observations of atmospheric pollutants at Lhasa during 2014–2015: Pollution status and the influence of meteorological factors

Atmospheric pollutants including SO₂, NO₂, CO, O₃ and inhalable particulate matter (PM_2.5 and PM₁₀) were monitored continuously from March 2014 to February 2015 to investigate characteristics of air pollution at Lhasa, Tibetan Plateau. Species exhibited similar seasonal variations except O₃, with the peaks in winter but low valleys in summer. The maximum O₃ concentration was observed in spring, followed by summer, autumn, and winter. The positive correlation between O₃ and PM₁₀ in spring indicated similar sources of them, and was assumed to be turbulent transport. Temperature was the dominant meteorological factor for most species in spring. High temperature accelerates O₃ photochemistry, and favors air disturbance which is conductive to dust resuspension in spring. Relative humidity (RH) and atmospheric pressure were the main meteorological factors in summer. RH showed negative correlations with species, while atmospheric pressure posed opposite situation. Wind speed (WS) was the dominant meteorological factor in autumn, the negative correlations between WS and species indicated diffusion by wind. Most species showed non-significant correlations with meteorological factors in winter, indicating the dependence of pollution on source emission rather than restriction by meteorology. Pollution weather character indicated that emissions were from biomass burning and dust suspension, and meteorological factors also played an important role. Air stream injection from the stratosphere was observed during O₃ pollution period. Air parcels from Southwest Asia were observed during air pollution period in winter. An enhancement in air pollutants such as O₃ would be expected in the future, more attention should be given to countermeasures for prevention of air pollution in the future.     

Characterization and acid-mobilization study for typical iron-bearing clay mineral

In this study, iron speciation in five standard clay samples was characterized. Iron mobilization from these clays was then measured in acidic media. For comparison, a commercially available Arizona test dust (ATD) was also observed. The results showed that the free-Fe contents of clays were commonly lower than that of dust aerosols. The components of clays were dominant by the structural Fe held in the aluminosilicate lattice. The iron solubility of the clays were in the order of KGa-2?>?SWy-2?>?CCa-2?>?IMt-2?>?NAu-2. Based upon the Mössbauer spectrum and transmission electron microscopy (TEM) analysis, the Fe(II) fraction and the Fe/Si ratio of clay particles changed after dissolution, suggesting the total Fe solubility depended on the Fe atom states existing within the aluminosilicate lattice. The Fe in KGa-2 and SWy-2 was most likely substituted for alkaline elements as the interlayer ions held by ionic bonds in the aluminosilicate, which are more liable to dissolution. However, the Fe in NAu-2 was more likely to be bound by strong covalent bonds in aluminosilicate mineral, which is less soluble. The much highly soluble Fe in ATD was not only linked to the dissolution of an appreciable fraction of Fe(II), but also could be attributed to the fact that the Fe bonds in the clay fraction of ATD were mainly present as ionic bonds. The TEM images showed that reacted clay particles displayed less aggregate particles, with nanoparticle aggregates and the Fe/S-rich tiny particles attached to the remains.