N_2/CO_2/H_2O抑制甲烷爆炸化学动力学机理分析

应用敏感性分析方法对N2,CO2和H2O抑制甲烷爆炸的化学动力学机理进行了理论分析,结果表明:在N2,CO2和H2O的抑制作用下,在甲烷氧化链式反应进程中起关键"桥梁"作用的自由基——CH3和HCO的生成受到强烈抑制,从而使得甲烷氧化链式反应进程受到影响和破坏;CO2和H2O除了具有N2所具有的抑燃、抑爆特性外,还会参与甲烷氧化链式反应,并对CH4氧化放热产生阻碍作用。     

PBXN-5传爆药安全可靠性试验方法研究

为满足引信传爆序列对高可靠性、高安全性火工药剂的需求,通过小隔板试验及升降法试验对PBXN-5传爆药的输出能力和冲击波感度作了分析和研究,小样本试验发现:当施主药柱装药相同,随施主与受主间隔板厚度增加,可靠起爆概率明显降低;但随受主药柱的装药尺寸的减小,传爆概率却增大。总之,受主药柱直径越小,隔板越薄,使用可靠性越高,结合安全使用性,计算得到合适的可靠度数据,为微型火工品装药提供参数依据。     

基于ASM 2d的数学模型在六箱一体化工艺分析中的应用

以六箱一体化工艺为例,建立了基于ASM 2d(activated sludge process 2d,活性污泥工艺2d)的数学模型,并研究其在脱氮除磷中的应用. 在HRT(水力停留时间)为16 h的工况下,利用灵敏度分析挑选了含有7个参数的待优化参数集,通过使用遗传算法优化校正函数的方式进行校正计算,获得了校正后的六箱一体化工艺模型,并在HRT为20和24 h下对该模型做了进一步验证. 结果表明,校正后的模型对出水水质的预测性较好,在HRT为16 h下,出水ρ(COD_Cr)、ρ(TN)、ρ(TP)和ρ(NH₄+-N)的模型计算值与实测值间的绝对差值较小,分别为1.96、0.83、0.06和0.24 mg/L. 在校正后模型的基础上,详细分析了HRT为20 h时各池中ρ(NH₄+-N)、ρ(NO₃--N)和ρ(PO₄3--P)在1个周期内的动态变化,指出了影响该工艺处理效果的主要原因(如碳源不足的问题),并与通过试验分析得到的结果基本一致.      

特异性拟杆菌引物在珠江三角洲的适应性研究

在珠江三角洲地区采集人、猪、牛、狗以及家禽等33个粪便样品,高效提取基因组DNA,选取14种特异性拟杆菌引物进行检验分析,并进一步采用已知污染源类型的水样对其进行验证.结果表明:采用粪便样品DNA专属提取试剂盒和水体样品DNA专属提取试剂盒提取的基因组模版纯度和提取率均符合后续实验要求.拟杆菌通用引物2#(Bac32F/Bac708R)检出率为85%(28/33),特别是对哺乳类动物和鸡的粪便具有更高的检出率.人的拟杆菌特异性引物3#(HF134F/ Bac708R)和4#(HF183F/Bac708R)、反刍动物的拟杆菌特异性引物8#(CF128F/Bac708R)以及猪的拟杆菌特异性引物10#(PF163F/Bac708R)在珠江三角洲地区同时具有较高的灵敏度和较强的特异性.水体样品验证实验与实际污染类型相符,说明拟杆菌通用引物2#、人的特异性引物3# 和4# 以及猪的特异性引物10# 在珠江三角洲地区具有很好的适用性.     

陈家大院泡湖泊湿地植物多样性研究

研究陈家大院泡湖泊湿地植物多样性规律对于改善大庆市萨尔图区的生态环境,了解物种群落丰富度具有重要意义.通过野外样地调查,分析了陈家大院泡湖泊湿地植物群落组成,并计算了植物群落多样性特征指数,包括Margalef指数,Simpson指数,Shannon-wiener指数和Pielou均匀度指数,结果表明,研究区湖泊湿地共有38种植物,分别隶属于18科34属,除榆树为木本植物外,有36种草本植物以及1种藓类植物.经数据处理后得出,每个样方平均含有3个物种,植株个体数目平均为115,Margalef指数平均值为0.567,Simpson指数平均值为0.814,Shannon-wiener指数平均值为0.313,Pielou均匀度指数平均值为0.267.由此看出,陈家大院泡湖泊湿地植物多样性水平较低,植物群落组成较为单一,生态环境脆弱.     

磁微球负载硝基锌卟啉光催化剂的制备及催化性能研究

以氯化血红素为原料,制备了磁负载的硝基锌卟啉光催化剂.同时,利用热重分析仪(TG)、透射电子显微镜(TEM)、扫描电子显微镜(SEM)和振动磁强计(VSM)对催化剂进行了表征,发现制备的催化剂负载率为32.06%,催化剂为粒径均一的球形壳-核结构,具有良好的磁性.其次,研究了催化剂的催化降解性能.结果表明,磁负载硝基锌卟啉光催化剂在可见光下,对水中的双酚A(BPA)、对硝基苯酚(PNP)等均有90%以上的去除率;对于活性红染料废水的降解也取得了83.67%的降解率.自由基捕获实验证明,电子(e-)、羟基自由基(·OH)、空穴(h+)和氧自由基(O-·2)是降解反应中重要的活性物种.最后通过GC-MS等手段对降解机理进行了研究.     

Oxidative properties of ambient PM2.5 and elemental composition: Heterogeneous associations in 19 European cities

We assessed the extent to which constituents of PM_2.5 (transition metals, sodium, chloride) contribute to the ability to generate hydroxyl radicals (OH) in vitro in PM_2.5 sampled at 20 locations in 19 European centres participating in the European Community Respiratory Health Survey. PM_2.5 samples (n = 716) were collected on filters over one year and the oxidative activity of particle suspensions obtained from these filters was then assessed by measuring their ability to generate OH in the presence of hydrogen peroxide. Associations between OH formation and the studied PM constituents were heterogeneous. The total explained variance ranged from 85% in Norwich to only 6% in Albacete. Among the 20 centres, 15 showed positive correlations between one or more of the measured transition metals (copper, iron, manganese, lead, vanadium and titanium) and OH formation. In 9 of 20 centres OH formation was negatively associated with chloride, and in 3 centres with sodium. Across 19 European cities, elements which explained the largest variations in OH formation were chloride, iron and sodium.     

In vitro toxicity of fungicides with different modes of action to alfalfa anthracnose fungus,Colletotrichum destructivum

Abstract

Sensitivity of 24 isolates of Colletotrichum destructivum O’Gara, collected from alfalfa plants in Serbia, to eight selected fungicides, was investigated in this study. Molecular identification and pathogenicity test of isolates tested were also performed. Fungicide sensitivity was evaluated in vitro, using mycelial growth assay method. All isolates exhibited significant pathogenicity, causing necrosis at the alfalfa seedling root tips two days after inoculation. Using the primer pair GSF1-SR1 and by comparing the amplified fragments of the tested isolates with the marker (M), the presence of the amplicon of the expected size of about 900?bp was determined for all isolates. The isolates tested in this study showed different sensitivity towards fungicides in vitro. Mycelial growth was highly inhibited by QoI (quinone outside inhibitors) fungicide pyraclostrobin (mean EC₅₀=0.39?µg mL^?1) and by DMI (demethylation-inhibiting) fungicide tebuconazole (mean EC₅₀=0.61?µg mL^?1), followed by azoxystrobin (mean EC₅₀=2.83?µg mL^?1) and flutriafol (mean EC₅₀=2.11?µg mL^?1). Multi-site fungicide chlorothalonil and MBC (methyl benzimidazole carbamate) fungicide thiophanate-methyl evinced moderate inhibition with mean EC₅₀=35.31 and 62.83?µg mL^?1, respectively. Thirteen isolates were sensitive to SDHI (succinate dehydrogenase inhibitors) fungicide boscalid and fluxapyroxad, (mean EC₅₀=0.49 and 0.19?µg mL^?1, respectively), while the rest of isolates were highly resistant.     

Thioarsenate formation upon dissolution of orpiment and arsenopyrite

Thioarsenates were previously determined as dominant species in geothermal and mineral waters with excess sulfide. Here, we used batch leaching experiments to determine their formation upon weathering or industrial leaching of the arsenic-sulfide minerals orpiment (As₂S₃) and arsenopyrite (FeAsS) under different pH and oxygen conditions. Under acidic conditions, as expected based on their known kinetic instability at low pH, no thioarsenates formed in either of the two mineral systems. Under neutral to alkaline conditions, orpiment dissolution yielded mono-, di- and trithioarsenate which accounted for up to 43-55% of total arsenic. Thioarsenate formation upon arsenopyrite dissolution was low at neutral (4%) but significant at alkaline pH, especially under suboxic to sulfidic conditions (20-43%, mainly as monothioarsenate). In contrast to orpiment, we postulate that recombination of arsenite and sulfide in solution is of minor importance for monothioarsenate formation during alkaline arsenopyrite dissolution. We propose instead that hydroxyl physisorption lead to formation of As-OH-S surface complexes by transposition of hydroxyl anions to arsenic or iron sites. Concurrently formed ironhydroxides could provide re-sorption sites for the freshly released monothioarsenate. However, sorption experiments with goethite showed slower sorption kinetics of monothioarsenate compared to arsenite, but comparable with arsenate. The discovery that thioarsenates are released by natural weathering and industrial leaching processes and that, once they are released, have a higher mobility than the commonly-investigated species arsenite and arsenate requires future studies to consider them when assessing arsenic release in sulfidic natural or mining-impacted environments.