地下水中溶解性有机物的季节变化特征及成因

为阐明地下水中溶解性有机物(DOM)的分布特征与环境效应,联合三维荧光光谱、平行因子分析及主成分分析,研究了地下水中DOM的来源及随季节和空间变化特征,探究了地下水DOM组成对无机盐分布的影响.结果显示,地下水DOM主要来自微生物源,可鉴别出4种荧光组分,4种组分中,组分1和3为类蛋白组分,组分2和4属于类腐殖质组分.类蛋白组分来源差异较大,组成不稳定,其含量随季节变化明显,春冬季含量低而夏秋季含量高;类腐殖质组分来源相似,组成稳定,随季节变化小.两类荧光组分,尤其是类蛋白组分,是地下水氨氮的主要来源,可以影响地下水pH值.结果表明,三维荧光光谱结合平行因子和主成分分析,可以解析地下水中有机物的组成特征和季节变化规律.     

Fluorescence excitation-emission matrix combined with regional integration analysis to characterize the composition and transformation of humic and fulvic acids from landfill at different stabilization stages

Fluorescence excitation-emission matrix spectroscopy (EEMs) combined with fluorescence regional integration (FRI) analysis was used to investigate the composition and transformation of humic acid (HA) and fulvic acid (FA) from landfill. The EEMs of HAs at different landfill ages were characterized by two typical fluorescence chromophores with Ex/Em pairs at Ex = 420-470 nm/Em = 490-530 nm and Ex = 345-375 nm/Em = 450-465 nm. EEMs of FA were featured by other two distinctly different fluorophores with Ex/Em pairs at Ex = 315-335 nm/Em = 420-440 nm and Ex = 255-275 nm/Em = 425-455 nm. The results show that HA extracted from the refuse disposed in the year of 1989 was formed by connecting small-condensed aromatic structures with protein-like chains. Compared with HA extracted from the refuse disposed in the year of 1992, HA extracted from the refuse of 1996 had a higher fluorescence intensity and lower r_(B,A) (the ratio of the fluorescence intensities of peak B and peak A) value. It contained low molar mass components, low aromatic condensation degree, and more easily oxidized substituents. This indicates that the landfill time strongly affects the EEMs characteristics of HA, and that the humification degree of HA increases with the landfill time. A red shift to a longer wavelength region and an increase of fluorescence intensity were observed when the concentration of HA was increased, suggesting that concentration had a great influence on the fluorescence characteristics of HAs. pH (2-12) also had significant effects on the fluorescence intensity, although it exerted no effect on the peak position of fluorescence of HA and FA. The results of FRI show that increasing concentration lead to more interactions among various structure components and that small molecular weight units tend to aggregate or be masked into more complicated and larger structures. The pH influence on the fluorescence intensity of HA seems mainly through molecular configuration, while the fluorescence intensity change with pH may be due to various substituents of FA.     

膜-生物反应器中荧光物质对膜污染的影响

采用三维荧光(EEM)技术对膜-生物反应器(MBR)运行过程中进出水、膜面溶解性污染物、溶解性微生物(SMP)和胞外聚合物(EPS)进行分析,并对各运行条件下荧光强度与膜污染速率进行比较.结果表明:各工况膜污染顺序为工况1(0.55 kPa/d)<工况3(1.37 kPa/d)<工况2(1.71 kPa/d)<工况4(3.69 kPa/d),SMP中的类蛋白质和类富里酸,以及EPS中的类蛋白质和类腐殖酸,均与各工况膜污染速率呈一致的变化趋势,而膜面溶解性污染物中的类蛋白质荧光峰则与膜污染速率没有明显的关系,说明在膜表面积累的荧光物质可能与其他有机物共同作用影响了膜污染速率.      

苯酚三维荧光光谱特征参数影响因素的研究

用三维荧光光谱法研究了不同离子浓度,pH值对苯酚荧光光谱特征参数的影响,并探讨了腐殖酸对苯酚的荧光猝灭效应.结果表明,天然水中9种常见离子Na+、Mg2+、Ca2+、K+、NH4+、Cl-、HCO3-、SO42-、HPO42-对苯酚的荧光光谱形状和荧光强度基本无影响;NO3-的存在会使苯酚的荧光强度发生变化,荧光强度随着NO3-浓度增大而减小.苯酚在酸性和碱性条件下的存在形式不同,致使pH值对其荧光光谱特征参数影响较大:在酸性条件下,荧光强度基本保持不变;在碱性条件下,由于羟基的电离使荧光强度很弱.腐殖酸的存在使苯酚发生荧光猝灭,采用Stern-Volmer方程修正式对实验猝灭结果进行拟合,得到的拟合结果较好,相关系数为0.9995.     

菌株J1对铜绿微囊藻光合作用的影响及其溶藻活性成分的研究

利用浮游植物荧光仪研究了芽胞杆菌属菌株J1胞外溶藻活性物质对铜绿微囊藻叶绿素荧光活性的影响,并采用α-萘酚反应、考马斯亮蓝法和定磷法对无菌滤液中溶藻活性物质进行了初步判定,结合蛋白酶处理、透析、活性炭吸附与解吸的方法对其相关特性进行了研究. 结果表明:试验第9天,加入无菌滤液的处理组,反映铜绿微囊藻叶绿素荧光活性的参数显著下降,其最大电子相对传递速率,光能转化效率,PSⅡ潜在活性和PSⅡ实际光合效率分别是对照的0.22%,0.33%,4.37%和5.56%;J1的溶藻活性物质可能为糖类物质,但不是蛋白质和核酸类物质,其分子质量小于8 ku,可被活性炭吸附.      

大气二氧化硫浓度的光学测定方法

介绍了测定二氧化硫浓度的几种光学方法 ,指出了目前一些化学方法的局限性 ,特别对紫外荧光法的原理、二氧化硫的吸收光谱以及荧光光谱进行分析探讨 ,设计了实验分析系统 ,得出该方法具有操作简单、灵敏度高、可实时在线的智能化优点 ,将会成为今后研究的主导方向。     

大沽河-胶州湾段溶解有机物类腐殖质荧光特征变化

利用荧光激发-发射矩阵光谱(excitation-emission matrix spectroscopy,EEMS)技术研究了溶解有机物类腐殖质荧光特征从大沽河到胶州湾的变化及其与盐度、pH、叶绿素a、溶解有机碳、化学需氧量和碳水化合物的关系.结果表明,大沽河溶解有机物类腐殖质荧光强度较大,胶州湾溶解有机物类腐殖质荧光强度较小,大沽河是胶州湾类腐殖质荧光物质的重要来源.类腐殖质荧光强度与叶绿素a含量的相关性较差,说明浮游植物并不是大沽河类腐殖质荧光物质的主要来源.类腐殖质荧光强度与溶解有机碳、化学需氧量和碳水化合物的相关性较好,说明类腐殖质荧光物质是水体溶解有机物的重要组成部分,其分布情况一定程度地反映了水体中有机物的分布.     

河流与海洋溶解有机物荧光激发-发射矩阵光谱的测定

通过对河流与海洋现场样品、微藻培养液和牛血清蛋白溶液的实验,确定了HITACHI F-4500型荧光分光光度计的测定河流和海洋溶解有机物荧光激发-发射矩阵光谱的激发和发射通带分别为5 nm和10 nm,波长扫描速度为12 000 nm/min,标准偏差在0.6%~8%。     

Differences in U root-to-shoot translocation between plant species explained by U distribution in roots

Accumulation and distribution of uranium in roots and shoots of four plants species differing in their cation exchange capacity of roots (CECR) was investigated. After exposure in hydroponics for seven days to 100 μmol U L⁻¹, distribution of uranium in roots was investigated through chemical extraction of roots. Higher U concentrations were measured in roots of dicots which showed a higher CECR than monocot species. Chemical extractions indicated that uranium is mostly located in the apoplasm of roots of monocots but that it is predominantly located in the symplasm of roots of dicots. Translocation of U to shoot was not significantly affected by the CECR or distribution of U between symplasm and apoplasm. Distribution of uranium in roots was investigated through chemical extraction of roots for all species. Additionally, longitudinal and radial distribution of U in roots of maize and Indian mustard, respectively showing the lowest and the highest translocation, was studied following X-ray fluorescence (XRF) analysis of specific root sections. Chemical analysis and XRF analysis of roots of maize and Indian mustard clearly indicated a higher longitudinal and radial transport of uranium in roots of Indian mustard than in roots of maize, where uranium mostly accumulated in root tips. These results showed that even if CECR could partly explain U accumulation in roots, other mechanisms like radial and longitudinal transport are implied in the translocation of U to the shoot.     

Monitoring of the microbial community composition in saline aquifers during CO2 storage by fluorescence in situ hybridisation

This study reveals the first analyses of the composition and activity of the microbial community of a saline CO₂ storage aquifer. Microbial monitoring during CO₂ injection has been reported. By using fluorescence in situ hybridisation (FISH), we have shown that the microbial community was strongly influenced by the CO₂ injection. Before CO₂ arrival, up to 6 × 10⁶ cells ml⁻¹ were detected by DAPI staining at a depth of 647 m below the surface. The microbial community was dominated by the domain Bacteria that represented approximately 60% to 90% of the total cell number, with Proteobacteria and Firmicutes as the most abundant phyla comprising up to 47% and 45% of the entire population, respectively. Both the total cell counts as well as the counts of the specific physiological groups revealed quantitative and qualitative changes after CO₂ arrival. Our study revealed temporal outcompetition of sulphate-reducing bacteria by methanogenic archaea. In addition, an enhanced activity of the microbial population after five months CO₂ storage indicated that the bacterial community was able to adapt to the extreme conditions of the deep biosphere and to the extreme changes of these atypical conditions.