Burkholderia sp.FDS-1降解硝基苯酚类化合物的特性研究

从长期受农药污染的土壤中分离到1株高效杀螟硫磷降解菌株Burkholderia sp.FDS^-1,它能以3-甲基-4-硝基苯酚(MNP)为唯一碳源和氮源进行生长.该菌能在9h内将0.6mmol.L-1MNP完全转化成邻甲基对苯二酚(MHQ),并能继续降解MHQ.该菌降解MNP的最适温度和pH分别为30℃和7.0,菌株降解MNP的速率和起始接种量呈正相关.降解MNP的酶为诱导酶.     

Anaerobic phenanthrene biodegradation with four kinds of electron acceptors enriched from the same mixed inoculum and exploration of metabolic pathways

Anaerobic phenanthrene biodegradation enriched process was described in detail. The enriched bacterial communities were characterized under four redox conditions. The enriched archaeal communities were stated under high percentage conditions. Relatively intact pathways of anaerobic phenanthrene biodegradation were proposed. Polycyclic aromatic hydrocarbons (PAHs) are widespread and persistent contaminants worldwide, especially in environments devoid of molecular oxygen. For lack of molecular oxygen, researchers enhanced anaerobic zones PAHs biodegradation by adding sulfate, bicarbonate, nitrate, and iron. However, microbial community reports of them were limited, and information of metabolites was poor except two-ring PAH, naphthalene. Here, we reported on four phenanthrene-degrading enrichment cultures with sulfate, bicarbonate, nitrate, and iron as electron acceptors from the same initial inoculum. The high-to-low order of the anaerobic phenanthrene biodegradation rate was the nitrate-reducing conditions>sulfate-reducing conditions>methanogenic conditions>iron-reducing conditions. The dominant bacteria populations were Desulfobacteraceae, Anaerolinaceae, and Thermodesulfobiaceae under sulfate-reducing conditions; Moraxellaceae, Clostridiaceae, and Comamonadaceae under methanogenic conditions; Rhodobacteraceae, Planococcaceae, and Xanthomonadaceae under nitrate-reducing conditions; and Geobacteraceae, Carnobacteriaceae, and Anaerolinaceae under iron-reducing conditions, respectively. Principal component analysis (PCA) indicated that bacteria populations of longtime enriched cultures with four electron acceptors all obtained significant changes from original inoculum, and bacterial communities were similar under nitrate-reducing and iron-reducing conditions. Archaea accounted for a high percentage under iron-reducing and methanogenic conditions, and Methanosarcinaceae and Methanobacteriaceae, as well as Methanobacteriaceae, were the dominant archaea populations under iron-reducing and methanogenic conditions. The key steps of phenanthrene biodegradation under four reducing conditions were carboxylation, further ring system reduction, and ring cleavage.     

水势与用氮量对土壤中石油降解的影响

研究了石油降解过程中，土壤有效氮的动态变化，不同用氮水平在两种土壤上对石油降解速率的影响，以及石油降解的土壤水势条件。结果表明，石油对土壤的污染没有影响土壤水势；在土壤水势为－１００～－２０ｋＰａ范围内，水势的降低没有影响石油分解，而当土壤水势为－１０００ｋＰａ时，石油降解速率与对照相比下降了１０％～３５％。在壤土上，肥料氮添加在碳（石油中碳）氮（肥料中氮）比为９０时，石油降解最快；过多施用肥料氮会降低石油的分解速率。     

藻类对壬基酚微生物降解的影响

壬基酚(NP)为在水环境中广泛存在的一种典型环境内分泌干扰物质。为了探讨NP在自然水体中的归趋,研究了水体中藻类对微生物降解NP的影响。结果表明,本研究筛选的耗氧混合菌可以有效降解NP,在暗环境下半衰期为1.16d,光照不利于NP的微生物降解,半衰期增加到5.19d;藻类和藻胞外分泌物可以提高光照条件下NP的微生物降解,这是藻类和菌加和作用的结果;而破碎的藻对降解作用改善不大。藻类和微生物相互作用对于有机污染物降解的影响还鲜见报道,本研究为全面理解NP在水环境中的归驱提供了重要的数据。     

城市垃圾填埋场的沉降研究

通过对位于上海老港填埋场的3000 m2试验场(垃圾填埋高度4 m,填入垃圾10800 t)历时880 d的沉降监测,根据垃圾在填埋场中的降解机理,建立了反映填埋场沉降规律的数学模型,证明了模型的可靠性。研究表明,填埋场的第二阶段沉降(由于垃圾的生物降解而产生的)与填埋时间的指数呈线性关系。根据沉降规律,上海老港填埋场完成大约79%的第二阶段沉降,才能处于高稳定化状态。     

生物降解途径的理论预测与QSBR研究

本文把有机污染生生物降解途径理论预测的结果与ＱＳＢＲ模型中化合物选择相结合，所遵循相同理论生物降解途径作为化合物分组的原则，以分子连接性接数和ＥＨＯＭＯ作为结构参数与电性参数，采用逐步回归的方法建立了新的ＱＳＢＲ模型，新模型的预测民实验结果能较好地吻合。     

二氯苯在土壤中的迁移行为和生物降解

主要从挥发、吸附与解吸、渗滤三个方面介绍了二氯苯在土壤中的迁移行为以及生物降解过程。探讨了二氯苯的物化性质、三种同分异构体的构型、土壤特性、外界环境条件等因素对二氯苯迁移行为的影响,以及迁移行为与生物降解的相互关系;同时介绍了可降解二氯苯的微生物种类、二氯苯好氧生物降解机理、共代谢现象,以及实验室研究方法。这些研究对于受二氯苯污染的土壤的修复具有理论指导意义。     

拓扑指数在定量结构生物降解性关系中的应用

本文采用二氧化碳生成量实验，对训练组有机物，利用逐步回归分析程序，从计算和十四种分子连接性指数中筛选出与生物降解性最为相关的分子结构描述参数，建立定量结构－生物降解性关系模型，其相关系数为０．９３１，利用该模型对预测组质的预测结果表明，此模型对芳香化合物的好氧生物降解性具有良好的预测能力，其正确预测率达８３．３％。     

A preliminary study of the phycological degradation of natural stone masonry

For many years it has been realised that the weathering of stone is not merely determined by physical and chemical factors but also by biological agents. When the stone in question is a historic building or monument, the damage done constitutes an irretrievable loss of our heritage and history. Laboratory studies have commenced in Paisley to study the effect of photoautotrophs on the major sedimentary rock forming minerals, with a view to expanding this work to study the overall effect of these micro-organisms on heritage masonry. Tests were carried out on Albite, Calcite, Dolomite, Orthoclase, Siderite and Quartz, using axenic cultures of the following: Chlorella vulgaris, Chlorococcum tetrasporum, Scenedesmus obliquus, Oocystis marsonii, Stichococcus bacillaris. The rock chips were immersed in either water or bolds basal media and exposed to a mix of the micro-organisms listed above and then tested weekly for their pH, fortnightly for the waters chemical composition using inductively coupled plasma-atomic emission spectrometry (ICP-AES) and visually utilising the universitys SEM facilities. Work so far has revealed biologically mediated etching of minerals, a well-defined pH profile over a period of 90 days, as well as a variety of elemental release patterns for the different minerals.     

土壤和地下水中多环芳烃生物降解研究进展

多环芳烃是一类普遍存在于环境中的难降解的危险性"三致"有机污染物。受污染的土壤和地下水中的多环芳烃,生物降解是其归宿的主要途径。研究表明,对于土壤中低分子量多环芳烃类化合物,微生物一般以唯一碳源方式代谢;而大多数细菌和真菌对四环或四环以上的多环芳烃的降解作用一般以共代谢方式开始。文章重点论述了多环芳烃的来源、降解多环芳烃的微生物、生物降解机理、影响生物降解的因素以及生物修复方法。认为今后的研究方向是高分子量多环芳烃的降解机理与降解途径,基因工程技术在多环芳烃生物降解方面的应用,以及生物表面活性剂产生的机理及其在实际处理中的应用等。