三维电极电解硝基苯废水处理实验研究

以涂膜活性炭-活性炭为填充粒子,对三维电极电解硝基苯废水进行了研究。通过实验探讨了投盐量、槽电压、主电极间距、反应时间及初始浓度对电解硝基苯废水的影响。结果表明,三维电极在电极间距为9mm、槽电压为20V、硫酸钠投加量为1.5g/L、pH值为6、电解时间为90min的条件下,硝基苯去除率可达90%以上。在三维电极电解作用下,硝基苯转化为可生化和低毒的苯胺,苯胺在三维电极电解作用下还可以得到进一步的降解。     

TiO2光催化氧化的研究进展

概述了TiO2光催化氧化降解水中污染物的原理及TiO2光催化剂的制备，提出了增强其活性的途径。TiO2光催化氧化可应用于印染、农药、造纸等工业废水及饮用水处理中，研制高效的负栽型纳米TiO2光催化剂、解决太阳能利用问题、开发多功能光催化反应器是今后TiO2光催化氧化的发展趋势。     

世界末日的瘟神:生物武器

何为生物武器生物武器它可能像电影中那样是一阵烟雾,或像新闻中说的是一包粉末,也可能是一群老鼠或苍蝇。病原体通过空气,食物甚至皮肤等渠道侵入人、畜体内,迅速或缓慢地致死,也可大规模毁伤农作物。生物武器通常又称为细菌武器或病毒武器,由生物战剂和投放工具两部分组成。其中, 生物战剂是生物武器的核心,是用于杀伤人和动物,或破坏农作物的致病微生物及其所产生的毒素。根据现代战争要求,能够作为生物武器的病毒战剂通常要具有致病性、传染性和易使用性等几个特征。     

煤矿带式输送机事故分析及防护措施

带式输送机是煤矿生产中的一种主要运输设备,广泛应用在采区平巷、采区上下山、运输大巷及井口运输走廊等场所,是矿井煤炭运输系统的中枢,一旦发生故障,轻则耽误生产,重则造成人员伤亡。笔者以常见的煤矿带式输送机故障类型为例,分析其产生故障的根本原因,提出各种故障的预防措施;论述了煤矿带式输送机综合保护装置的基本功能和动作原理;通过带式输送机综合保护装置控制系统结构示意图,全面、客观地展示了煤矿用带式输送机容易发生各种故障的方位和自动保护装置测控元件的布局、电气控制原理,不仅可以适时监控带式输送机的工作状态,自动报警、显示、处理各种运行故障,还可以避免人为误操作带来的各种损失。     

城市可降解生活垃圾的生物综合处理模式初探

针对现有城市生活垃圾处理方式的不足,结合垃圾生物处理特点,设计了集混合菌群降解、生物过滤除臭、污水回用及植被绿化于一体的立体处理体系。结果表明,该系统在城市生活垃圾的“三化”处理中具有显著的潜势:既使生活垃圾在食物链外形成安全的闭路循环,防止有害物质向人居环境入渗;同时,处理设施的立体化、终产物的生物转化以及即刻的市场效应,有效地增强了系统的消纳能力,缓解了传统处理方式对城市空间的压力。该系统对我国中小城市生活垃圾的综合利用具有积极的参考价值。     

甲基汞对大鼠脑一氧化氮合酶,丙二醛和即刻早期基因的影响

为了寻找甲基汞神经毒性检测和评价效应指标以及探讨甲基汞神经毒性分子机制,对大鼠进行氯化甲基汞(MMC)急性暴露(对照组为0.9％生理盐水、暴露组浓度为0.05mg/kg),20min后对大鼠进行生理生化指标和即早基因的检测,大鼠大脑中枢神经系统的神经递质一氧化氮合酶活力采用一氧化氮合酶(NOS)测定试剂盒检测;自由基脂质过氧化产物丙二醛含量采用硫代巴比妥酸(TBA)比色法检测;即刻早期基因c-fos表达的变化采用免疫组化方法检测。结果表明,在暴露氯化甲基汞(MMC)20min后,大鼠大脑中枢神经系统的一氧化氮合酶活力、自由基脂质过氧化产物丙二醛含量以及即刻早期基因(IEG)c-fos蛋白阳性表达数量都有提高。但其中一氧化氮合酶活力及自由基脂质过氧化产物丙二醛含量同对照组相比没有显著性差异;而即刻早期基因c-fos的阳性表达同对照组相比有极显著性差异(P<0.01)。据此可以推测,即刻早期基因能作为甲基汞神经毒性检测和评价效应指标,一氧化氮合酶、丙二醛和即刻早期基因在甲基汞神经毒性过程中具有重要作用。     

Application of tracer ratio and inverse dispersion methods with boat-based plume measurements to estimate ammonia emissions from seabird colonies

Ammonia emissions from two contrasting seabird colonies in Scotland were measured, based on the determination of atmospheric concentrations downwind of the colonies. Atmospheric concentrations of ammonia (NH₃) across the downwind plume were compared with the inverse application of a Gaussian dispersion model (ID) to calculate the modelled NH₃ emission that would generate the measured cross-wind-integrated plume concentration. In parallel, a tracer gas (sulphur hexafluoride, SF₆) was released from the colonies with air samples taken to allow determination of SF₆ concentrations. On the basis of the known emission rate of SF₆, the magnitude of ammonia emissions was estimated by the cross-wind-integrated tracer ratio (TR) of NH₃/SF₆ concentrations. Coupled with data on annual bird attendance, the measurements indicate annual emissions from the Isle of May and the Bass Rock of 18 and 132 tonnes NH₃-N year^–1, respectively. The measured NH₃ emissions were compared with estimates of seabird nitrogen excretion to estimate the proportion of excreted N that is volatilised as NH₃ (F_Nr). The emission estimates of the two methods compared favourably, giving 4 and 6 kg NH₃-N h^–1 (F_Nr = 15%) for the Isle of May for the ID and TR methods, respectively, and 21 and 25 kg NH₃-N h^–1 (F_Nr = 50%) for the Bass Rock for the ID and TR methods, respectively. The results provide the first measurement-based estimates to allow regional up scaling of ammonia emissions from seabirds.     

The GaNE programme in a global perspective

This paper provides the background to this special issue, outlining the extent to which the global atmospheric nitrogen cycle has been modified by human activity and outlining the range of effects. The global total emissions of reduced and oxidized nitrogen, amount to 124 Tg N, and exceed those from natural sources (34 Tg N) by almost a factor of four showing the extent to which anthropogenic activity has taken over the global N cycle. Of the 124 Tg N, 70 Tg N is emitted in the oxidized form, largely as NO and 70% of which results directly from anthropogenic activity. The remaining 54 Tg N is emitted as NH₃, (66% anthropogenic). The enhanced nitrogen emissions are associated with a range of local, regional and global issues including, acidification, eutrophication, climate change, human health and tropospheric O₃. The paper also places the Global Nitrogen Enrichment (GaNE) research programme in the UK in a wider perspective.     

Modelling nitrogen fluxes at the landscape scale

The distribution and impacts of different nitrogen pollutants are inextricably linked. To understand the problem fully, the interactions between the different pollutants need to be taken into account. This is particularly important when it comes to abatement techniques, since measures to reduce emissions of one nitrogen pollutant can often lead to an increase in another. This project represents a step towards greater understanding of these issues by linking together new and existing nitrogen flux models into a larger framework. The modelling framework has been constructed and some of the nitrogen flows between fields, farms and the atmosphere have been modelled for a UK study area for typical farm management scenarios.     

Rapid amino acid cycling in arctic and antarctic soils

Amino acids constitute one of the largest inputs of organic nitrogen (N) to most polar soils and have been hypothesized to be important in regulating vegetational succession and productivity in Arctic ecosystems. Our understanding of amino acid cycling in these soils, however, is poor. The aim of this study was to investigate the size and rate of turnover of the amino acid pool in a range of Arctic and Antarctic soils. Our results indicate that in polar soils with either high or low ornithogenic inputs the amino acid pool is small in comparison to the inorganic N pool (NO^–₃ and NH⁺₄). The free amino acid pool constituted only a small proportion of the total dissolved organic nitrogen (DON) pool in these soils. Here we show that these low concentrations may be due to rapid use by the soil microbial community in both Arctic and Antarctic soils. The turnover of the amino acid pool in soil was extremely rapid, with a half-life ranging from 2 to 24 h, indicating that this N pool can be turned over many hundred times each summer when polar soils are frequently unfrozen. The implications of amino acids in N cycling and plant and microbial nutrition are discussed.