义乌市分质供水系统水质变化分析

为探究义乌市分质供水系统中水质及有机物的变化特征,分季度调研了3个水厂沿程水质的变化,并采用光谱技术与高分辨率质谱分析了处理工艺对溶解性有机质的去除效果。水质调研结果表明,传统工艺(混凝沉淀-砂滤)对总磷和氨氮的去除率分别达到80%与50%以上,但对水体中的总氮与总溶解性有机碳的去除效果差。双膜法(超滤-反渗透)全面优于传统工艺,可以将营养盐和有机物的浓度降至极低的水平(去除率>90%)。三维荧光结合平行因子分析结果表明,混凝沉淀仅对地表水中陆源腐殖质组分有明显的去除,对类蛋白质组分的去除效果较差。高分辨率质谱的检测结果表明,混凝对木质素、单宁及稠环芳烃等物质有较好的去除效果。在混凝前增设曝气生物滤池并在混凝过程中添加粉末活性炭,能强化工艺对类蛋白质组分和腐殖质组分的去除效果。本研究结果可为水处理工艺优化提供理论依据。     

有机固体废物堆肥化处理的微生物学机理研究

由于符合持续发展的理念 ,利用微生物技术处理有机固体废物越来越受到人们的重视 ,其核心问题则是木质纤维素的生物降解。随着园林废物等高木质纤维素含量的城市生活垃圾的不断增加 ,以及对农业固体废物和食品工业废物再利用的需要 ,这一领域的研究取得了很大的进展。在研究中 ,针对好氧堆肥和厌氧发酵 2项主要的微生物处理技术 ,对其优势微生物菌群、不同降解底物和微生物降解动力学方面的最新研究进展进行了回顾和总结 ,并对环境微生物制剂的应用以及有机固体废物的微生物处理技术的发展做了合理的展望。     

含氮芳香化合物的厌氧生物降解研究回顾

回顾了硝基芳香化合物和偶氮化合物在厌氧条件下的生物脱毒、转化和矿化作用的研究成果。这些研究表明 ,由于硝基和偶氮基具有强烈的吸电子性 ,好氧条件下很难降解。但是 ,硝基和偶氮基芳香化合物在产甲烷菌群作用下较易还原脱毒 ,转化为相应的芳香胺类 ,其毒性要小几个数量级 ,因而有些毒性很高的芳香化合物废水可利用厌氧反应器处理 ,而且反应过程中发现一些芳香胺类化合物可被完全矿化 ,表明一些含氮芳香化合物可作为厌氧菌的碳源和能源 ,在厌氧条件下被完全生物降解。     

有机固体废弃物热解生产脱水内醚糖的研究

以有机固体废弃物 (废棉絮、废纸 )为原料 ,在管式炉热解反应器热解生产脱水内醚糖。研究了热解温度对热解产物相态分布的影响。同时 ,利用HPLC对脱水内醚糖的产量进行了测定。HPLC分析结果表明 :热解液水相中主要化学物质是乙酸 ,而非水相中主要化学物质是脱水内醚糖     

单环硝基芳香化合物好氧生物降解及其遗传学研究进展

硝基芳香化合物是环境中难降解的有机污染物之一 ,对环境的污染日益严重 ,利用生物技术对这类有机物进行降解是行之有效的新途径。针对几种单环硝基芳香化合物好氧降解的微生物、降解途径以及降解过程中的主要酶、降解性质粒、基因定位等分子遗传学的研究进展进行了综述     

Kosetice, Czech Republic--ten years of air pollution monitoring and four years of evaluating the origin of persistent organic pollutants

The regional observatory Kosetice is a central European background station. Unique continuous monitoring from 1988 on is held here. POP (persistent organic pollutant) concentration values of air samples from Kosetice taken between 1996 and 2005 were statistically processed. Values of Czech ambient air quality standards were not exceeded. Concentrations of polycyclic aromatic hydrocarbons reached two maxima, in 1996 and 2001-2002. Polychlorinated biphenyls concentrations reached the highest values in 1997 and 1998 and hexachlorocyclohexanes concentrations in 1998. DDTs, hexachlorobenzene and pentachlorobenzene were analysed as well. Long-range transport of pollutants between 2002 and 2005 was evaluated using the Potential Source Contribution Function hybrid receptor model. Indicated potential source areas of PCBs coincide with many well-known urban and industrialised areas, while the indicated potential source areas of HCHs and DDTs coincide with many agricultural and/or forested regions and the potential source areas of HCB comprise all land use types.     

DOC removal paradigms in highly humic aquatic ecosystems

Background, aim, and scope  Dissolved humic substances (HS) usually comprise 50–80% of the dissolved organic carbon (DOC) in aquatic ecosystems. From a trophic and biogeochemical perspective, HS has been considered to be highly refractory and is supposed to accumulate in the water. The upsurge of the microbial loop paradigm and the studies on HS photo-degradation into labile DOC gave rise to the belief that microbial processing of DOC should sustain aquatic food webs in humic waters. However, this has not been extensively supported by the literature, since most HS and their photo-products are often oxidized by microbes through respiration in most nutrient-poor humic waters. Here, we review basic concepts, classical studies, and recent data on bacterial and photo-degradation of DOC, comparing the rates of these processes in highly humic ecosystems and other aquatic ecosystems. Materials and methods  We based our review on classical and recent findings from the fields of biogeochemistry and microbial ecology, highlighting some odd results from highly humic Brazilian tropical lagoons, which can reach up to 160 mg C L⁻¹. Results and discussion  Highly humic tropical lagoons showed proportionally lower bacterial production rates and higher bacterial respiration rates (i.e., lower bacterial growth efficiency) than other lakes. Zooplankton showed similar δ¹³C to microalgae but not to humic DOC in these highly humic lagoons. Thus, the data reviewed here do not support the microbial loop as an efficient matter transfer pathway in highly humic ecosystems, where it is supposed to play its major role. In addition, we found that some tropical humic ecosystems presented the highest potential DOC photo-chemical mineralization (PM) rates reported in the literature, exceeding up to threefold the rates reported for temperate humic ecosystems. We propose that these atypically high PM rates are the result of a joint effect of the seasonal dynamics of allochthonous humic DOC input to these ecosystems and the high sunlight incidence throughout the year. The sunlight action on DOC is positive to microbial consumption in these highly humic lagoons, but little support is given to the enhancement of bacterial growth efficiency, since the labile photo-chemical products are mostly respired by microbes in the nutrient-poor humic waters. Conclusions  HS may be an important source of energy for aquatic bacteria in humic waters, but it is probably not as important as a substrate to bacterial growth and to aquatic food webs, since HS consumption is mostly channeled through microbial respiration. This especially seems to be the case of humic-rich, nutrient-poor ecosystems, where the microbial loop was supposed to play its major role. Highly humic ecosystems also present the highest PM rates reported in the literature. Finally, light and bacteria can cooperate in order to enhance total carbon degradation in highly humic aquatic ecosystems but with limited effects on aquatic food webs. Recommendations and perspectives  More detailed studies using C- and N-stable isotope techniques and modeling approaches are needed to better understand the actual importance of HS to carbon cycling in highly humic waters.     

游离态氨基酸对羊角月牙藻的生物有效性

采用实验室模拟培养试验,以6种个体氨基酸——丝氨酸、天冬氨酸、谷氨酸、甘氨酸、丙氨酸和精氨酸为唯一氮源,采用一次性培养的方法,在无菌条件下,研究羊角月牙藻对不同种类个体氨基酸和不同浓度混合氨基酸的利用潜能。结果表明:藻细胞在生长过程中会释放氨基酸增加水体中氨基酸浓度,同时,藻类可迅速并直接利用多种游离态氨基酸快速生长。氨基酸浓度在培养周期的前2天减少90%以上,藻细胞数在第6~8天达到最大,说明藻细胞的生长滞后于游离氨基酸浓度的下降;在个体氨基酸试验中,藻细胞对氨基酸的利用程度为精氨酸>丙氨酸>谷氨酸>天门冬氨酸>丝氨酸>甘氨酸;在混合氨基酸试验中,藻细胞的比增殖速率明显高于个体氨基酸试验组,且随混合氨基酸浓度的增加,最大藻细胞生物量增加;羊角月牙藻在利用个体氨基酸的同时也会释放其他种类的氨基酸,其中,天冬氨酸和甘氨酸的释放浓度最大。羊角月牙藻在无机氮缺乏情况下,能迅速利用氨基酸。     

氧化锰共生矿烟气脱硫的机理及影响因素

利用南非的氧化锰共生矿进行烟气脱硫,研究了共生锰矿烟气脱硫性能及其机理,并考察了锰矿粒径、反应温度、液固比、进气流量、进口SO2浓度等因素对脱硫率的影响。结果表明,氧化锰共生矿中主要的锰化合物是MnO2、Mn2O3和MnCO3,烟气脱硫过程主要存在4种方式：MnO2与SO2发生氧化还原反应生成硫酸锰;液相中Mn2+催化氧化SO2产生硫酸;MnCO3与硫酸反应生成硫酸锰;Mn2O3与硫酸反应后生成的MnO2可以继续与SO2进行脱硫反应,但是Mn2O3与SO2直接反应的活性较差。氧化锰共生矿烟气脱硫的最佳工艺参数为：锰矿粒径200目、反应温度80 ℃、液固比10:1以及进气流量600 mL?min-1     

木屑-硫磺填充床反硝化生物滤池强化硝酸盐去除

针对污水处理厂二级出水深度脱氮的需求,设计了以木屑与硫磺颗粒为填料（质量比1:1）的反硝化生物滤池,对碳氮比失衡的污水处理厂二级出水进行深度脱氮处理。结果表明,木屑释放碳源速率在10 d之后趋于稳定,COD中（40.6±10.0）%是反硝化菌可直接利用的VFA。反硝化生物滤池运行的最佳HRT为10 h,在此条件下,进水硝酸盐（以N计）浓度为30 mg·L-1时,出水硝酸盐浓度最低为11.5 mg·L-1,亚硝酸盐（以N计）浓度最低为1.4 mg·L-1,反硝化生物滤池内未发生硝酸盐异化还原（DNRA）作用,出水无氨氮积累。出水SO42-浓度最高为73.8 mg·L-1。反硝化生物滤池运行稳定后,出水中COD未超过30 mg·L-1,木屑释放的碳源与异养反硝化过程消耗的碳源持平,经反硝化生物滤池深度处理的出水中无过量残留有机物。出水pH稳定在6.9~7.4范围内,反硝化生物滤池无需外加碱类物质。