气相色谱技术及其在环境监测工作中的应用

气相色谱技术诞生于上世纪50年代中叶,它的出现给予了化学分离以及化学分析很大的技术支持,同时在环境监测等领域都有着广泛的应用。从类型上看气相色谱主要分为两类即气固色谱以及气液色谱,两者的本质区别在于固定相的不同,这也使得分离方法存在着一定的区别。本文对气相色谱技术进行了综合性阐述并对气相色谱技术在环境监测中的应用进行了讨论,供以参考。     

铝——水反应制氢发展浅析

本文就各种制氢方式中铝-水反应制氢发展进行了浅析,主要分析了铝-水制氢各方法的优劣、发展过程及发展前景,讨论了铝-水反应制氢的可行性。     

增湿除湿太阳能海水淡化系统的试验研究

基于增湿-除湿原理,设计了一种新型的太阳能海水淡化装置,该装置包含太阳能空气集热器、太阳能热管集热器、横管蒸发器、竖管冷凝器以及冷却水箱。介绍了各部件的尺寸结构和工作原理,研究了影响系统产水量的各因素。结果表明:热海水温度、进口空气流量以及冷凝海水流量对产水量影响较大,而一定范围内环境温度的变化对产水量影响较小。数据显示,系统的产水率和效率分别为5.79×10-4kg/kJ和43.5%。     

Photocatalytic activity of Fe-doped CaTiO3 under UV-visible light

The photocatalytic degradation of methylene blue（MB） over Fe-doped CaTiO3 under UV-visible light was investigated. The as-prepared samples were characterized using X-ray diffraction（XRD）, scanning electron microscope（SEM） equipped with an energy dispersive spectrometer（EDS） system, Fourier transform infrared spectra（FT-IR）, and UV-visible diffuse reflectance spectroscopy（DRS）. The results show that the doping with Fe significantly promoted the light absorption ability of CaTiO3 in the visible light region. The Fe-doped CaTiO3 exhibited higher photocatalytic activity than CaTiO3 for the degradation of MB.However, the photocatalytic activity of the Fe-doped CaTiO3 was greatly influenced by the calcination temperature during the preparation process. The Fe-doped CaTiO3 prepared at500°C exhibited the best photocatalytic activity, with degradation of almost 100% MB（10 ppm）under UV-visible light for 180 min.     

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.     

Formation pathways of brominated products from benzophenone-4 chlorination in the presence of bromide ions

The brominated products, formed in chlorination treatment of benzophenone-4 in the presence of bromide ions, were identified, and the formation pathways were proposed.Under disinfection conditions, benzophenone-4 would undertake electrophilic substitution generating mono- or di-halogenated products, which would be oxidized to esters and further hydrolyzed to phenol derivatives. The generated catechol intermediate would be transformed into furan-like heterocyclic product. The product species were p H-dependent,while benzophenone-4 elimination was chlorine dose-dependent. When the chlorination treatment was performed on ambient water spiked with benzophenone-4 and bromide ions, most of brominated byproducts could be detected, and the acute toxicity significantly increased as well.     

乙酰胺低共熔离子液体吸收SO_2的研究

制备了3种乙酰胺-无机盐类低共熔离子液体,测定了其物理性质并将其应用于SO2气体的吸收。结果表明,这些低共熔离子液体具有和传统离子液体相似的性质,例如熔点低、粘度低、密度高、电导率高以及较宽的液态范围。此类离子液体对SO2气体有较好的吸收能力,而且吸收量和温度的关系满足二次多项式方程。红外光谱结果表明吸收是可逆的,回收的离子液体可高效重复使用至少5次。乙酰胺-硫氰酸钠(3∶1)对SO2的质量分数吸收量为0.554 g/g(20℃,1 atm),具有吸收量高、成本低和易回收的优势,是一个很有前景的SO2吸收剂。     

基于主成分-聚类分析模型的生态环境脆弱性分析:以平潭综合实验区为例

目前对平潭综合实验区(平潭主岛)脆弱性评价方面的研究仅有地下水系统的脆弱性研究,对生态环境方面的脆弱性研究尚未见诸文献中。针对此情况,文章首先从自然因素、人为干扰因素和环境因素3个方面构建了生态环境脆弱性指标体系,然后运用主成分-聚类分析模型对平潭综合实验区的生态环境脆弱性进行分区。脆弱性分区结论为平潭综合实验区总体为中强度脆弱,其中极强脆弱区为白青乡,强度脆弱区为北厝镇和苏澳镇,中度脆弱区为中楼乡、澳前镇和敖东镇,轻度脆弱区为平原镇、潭城镇和流水镇,微脆弱区为芦洋乡。文章从增加防护林的面积和种类、调整优化土地利用结构、开展生态功能区划和生态环境保护规划的编制工作三方面提出了降低研究区域生态环境脆弱性的对策措施。     

贫营养条件下17β-雌二醇厌氧生物降解规律研究

17β-雌二醇作为环境甾体雌激素污染的主要污染物之一,广泛分布于自然环境中。采用批次实验,研究了在贫营养条件下17β-雌二醇厌氧生物降解规律。结果表明,在贫营养条件下,厌氧污泥对17β-雌二醇的去除率达到90%(35℃,76 d),且降解作用主要集中在快速降解阶段,降解规律符合一级降解动力学模型(R2=0.95);厌氧污泥对17β-雌二醇的去除主要是通过转化为雌性效力较低的雌酮,再由雌酮转化为其他的转化产物,如17α-雌二醇;Fe(Ⅲ)对17β-雌二醇的去除和转化没有显著的影响。接种污泥的内源代谢作用产生甲烷,Fe(Ⅲ)的存在可以提高甲烷的产率,但对甲烷的总量没有显著影响。     

星肋小环藻、铜绿微囊藻春化作用基因控制机理

实验证实了星肋小环藻、铜绿微囊藻的春化作用后,其暴发控制机理成为研究重点。该文通过分析单细胞生物基因操作原理、遗传物质转录复制控制、温度对蛋白质的作用和酶原激活过程等,研究微藻春化作用基因控制机理,提出基因控制模型:激活基因-操纵基因连锁的基因操纵模型,由基因操纵子、调节基因和激活基因组成。该模型阐释2种藻类春末夏初大规模暴发机理:春季,调节基因产生的调节蛋白原被调节蛋白激活酶激活产生的调节蛋白与操纵基因结合,启动结构基因转录合成DNA合成酶系,DNA复制完成,藻体裂殖(繁殖)群体增长;夏季,高温下温度敏感的调节蛋白激活酶变性,使调节蛋白原激活产生变构的调节蛋白,同时与操纵基因和激活基因结合,激活基因不能产生调节蛋白激活酶激活调节蛋白原产生激活蛋白,这时铜绿微囊藻进入生长被抑制状态,星肋小环藻进入高温休眠状态;进入秋季,因之前无低温出现使热变性的激活酶复性,激活产生正常的调节蛋白与操纵基因结合,启动结构基因复制繁殖所需DNA酶系,尽管秋季温光适宜,星肋小环藻不会生长活动,铜绿微囊藻可生长但生长速度低于春末夏初时的生长速度;进入冬季,低温使热变性的激活酶复性,等待来年春暖激活调节蛋白原,启动新一年的藻生长。