共基质对10株细菌降解苯并芘的作用研究

从石油污染的污泥中分离驯化出10株细菌(SB01～SB10),利用生物摇床实验对其降解苯并芘(BaP)的效能进行试验,研究了有(或无)共基质(葡萄糖Glu,或菲PHE)对细菌降解BaP的影响,并采用ANOVA和Tukey多重比较进行分析。结果表明(,1)当以BaP为惟一碳源和能源且BaP初始浓度为50mg·L-1时(MS1),SB01的降解率最高,5d可降解31.0%;以Glu为共代谢基质时(MS2),SB09的降解率最高,可达36.9%;以PHE为共代谢基质时(MS3),SB01对BaP的降解率为46.0%。(2)Glu对SB01、SB02、SB03、SB07、SB10降解BaP有抑制作用,对SB01抑制作用最明显,使SB01的降解率降低了13.1%,Glu对SB05,SB08降解率无明显促进或抑制作用。(3)PHE对细菌降解BaP均表现出促进作用,对SB01的促进作用最明显,使其降解率提高15.0%。(4)Glu对SB09的促进作用大于PHE的促进作用,而对SB06,PHE的促进作用大于Glu。

固定化微生物对多环芳烃污染土壤的降解

利用微生物固定化技术,研究了微生物固定化菌剂对土壤中菲、蒽、芘、(艹屈)和苯并(a)芘的降解动态,并且采用Michaelis-Menton和Monod动力学模型对结果进行拟合。结果显示,4种处理(TB02、TB07、TBB03、TBB08)均有降解菲、蒽、芘、(艹屈)和苯并(a)芘的能力。其中,处理TB02的降解能力强、降解速率快、半衰期短且处理成本低,而处理TB07则需要较长时间作用于PAHs污染土壤,其降解能力才能充分发挥出来。当菲、蒽、芘、散发出(艹屈)和苯并(a)芘的初始浓度均为20mg·kg-1时,42d后,TB02对菲、蒽、芘、(艹屈)和苯并(a)芘的降解率分别为84.32%、85.24%、82.59%、43.75%和62.25%;133d后,TB07对5种污染物的降解率分别为95.00%、95.24%、90.93%、74.82%和72.20%。通过比较5种污染物半衰期,其可降解性由大到小依次为菲、蒽、芘、苯并(a)芘、(艹屈)。

均匀设计在固定化毛霉载体配方优化中的应用

将均匀设计方法应用于固定化毛霉(Mucorsp.)载体配方优化中。在单因素实验基础上,采用U(1557)均匀设计表对影响毛霉生长的主要营养因子进行优化,利用SPSS建立了固定化毛霉对土壤中芘、苯并(a)芘(BaP)和总多环芳烃(PAHs)降解率的回归方程。结果表明,全相关系数分别达到0.999,0.997和0.997。而后通过无约束规划求解获得了固定化载体最佳配方:玉米芯92.1%,豆饼4.8%,CaSO41.6%,白糖1.4%,MgSO40.2%,有效地提高了固定化毛霉对土壤中PAHs的降解率,为将固定化微生物技术应用于非流体介质中PAHs污染的原位修复提供了可行途径,而且该载体配方用料来源广泛,成本低廉,工艺简单,安全无毒。

Remediation of Persistent Organic Pollutants (POPs) in Two Different Soils

Persistent organic pollutants (POPs) are a set of chemicals that are toxic, persist in the environment for long periods of time, and biomagnify as they move up through the food chain. The most widely used method of POP destruction is incineration, which is expensive and could result in undesirable by-products. An alternative bioremediation technology, which is cheaper and environ-mentally friendly, was tested during this experiment. Two different soil types containing high and low organic matter (OM) were spiked with 100 mg/kg each of pyrene and Aroclor 1248 and planted with three different species of grasses. The objective of the study was to determine residue recovery levels (availability) and potential effectiveness of these plant species for the remediation of POPs. The results showed that recovery levels were highly dependent on the soil organic matter content—very low in all treatments with the high OM content soil compared to recoveries in the low OM soil. This indicates that availability, and, hence, biodegradability of the contaminants is dependent on the organic matter content of the soil. Moreover, the degree of availability was also significantly different for the two classes of chemicals. The polyaromatic hydrocarbon (PAH) recovery (availability) was extremely low in the high organic matter content soil compared to that of the polychlorinated biphenyls (PCBs). In both soil types, all of the plant species treatments showed significantly greater PCB biodegradation compared to the unplanted controls. Planting did not have any significant effect on the transformation of the PAHs in both soil types; however, planting with switchgrass was the best remedial option for both soil types contaminated with PCB.

Methods for physical separation and characterization of soil organic matter fractions

Turnover of soil organic matter (SOM) is coupled to the cycling of nutrients in soil through the activity of soil microorganisms. Biological availability of organic substrate in soil is related to the chemical quality of the organic material and to its degree of physical protection. SOM fractions can provide information on the turnover of organic matter (OM), provided the fractions can be related to functional or structural components in soil. Ultrasonication is commonly used to disrupt the soil structure prior to physical fractionation according to particle size, but may cause redistribution of OM among size fractions. The presence of mineral particles in size fractions can complicate estimations of OM turnover time within the fractions. Densiometric separation allows one to physically separate OM found within a specific size class from the heavier-density mineral particles. Nutrient contents and mineralization potential were determined for discrete size/density OM fractions isolated from within the macroaggregate structure of cultivated grassland soils. Eighteen percent of the total soil C and 25% of the total soil N in no-till soil was associated with fine-silt size particles having a density of 2.07-2.21 g/cm3 isolated from inside macroaggregates (enriched labile fraction or ELF). The amount of C and N sequestered in the ELF fraction decreased as the intensity of tillage increased. The specific rate of mineralization (mug net mineral N/mug total N in the fraction) for macroaggregate-derived ELF was not different for the three tillage treatments but was greater than for intact macroaggregates. The methods described here have improved our ability to quantitatively estimate SOM fractions, which in turn has increased our understanding of SOM dynamics in cultivated grassland systems.

邻苯二酚2,3-双加氧酶基因克隆、定位和高效表达

采用特异性引物 ,以菲、芘降解菌株ZL5的代谢性质粒为模板 ,扩增出邻苯二酚 2 ,3-双加氧酶 (C2 3O)基因 .将该基因和表达载体pET - 30a(+)连接 ,转化E .coliJM10 9(DE3) ,获得了高效表达的转化子 .SDS -PAGE结果表明 ,转化子的C2 3O蛋白不仅在细胞内存在 ,而且能被分泌到胞外 ,薄层扫描显示 ,转化子细胞内和细胞外表达蛋白总量占细胞总蛋白的 4 2 % .酶活分析表明 ,分布在转化子细胞内、外的表达蛋白都具有较高的C2 3O比活力 .Southern杂交将菌株ZL5的C2 3O基因定位在内生质粒的不同酶切片段上 .图 5表 1参 12

中国西部沙漠化与沙尘风暴问题探讨

我国西部地表植被向恶性循环方向发展 ,土地沙漠化面积迅速增长 ,沙尘风暴日趋频繁。分析中国西部沙漠化和沙尘风暴存在的主要问题 ,进一步探讨沙漠化和沙尘风暴形成的原因和对国民经济发展所造成的危害 ,因地制宜提出了相应的治理对策

芘在土壤中的共代谢降解研究

高分子量多环芳烃 (PAHs)的降解通常以共代谢方式进行 .研究比较了高分子量多环芳烃代表种类芘作为唯一C源和能源的降解过程和有共代谢底物存在下芘的降解过程 ,结果表明 ,2 5d后前者中芘的降解率5 7% ,而后者中芘的降解率为 80 % .且有共代谢底物存在下 ,芘在降解过程中半衰期缩短 ;水杨酸 ,邻苯二甲酸 ,琥珀酸钠能作为共代谢底物提高芘的降解率 ,琥珀酸钠效果最好 .芘和低分子量多环芳烃之间也有共代谢关系 ,菲促进了芘的降解 ,但萘未出现同样的结果 .此外 ,这阐明了共代谢原理和适宜作高分子量多环芳烃共代谢底物的物质 .

农牧交错带不同人工植被下荒漠化土壤肥力的变化

研究了陕北农牧交错带荒漠化土地上种植人工植被后,在不同的植被恢复类型和生长状态下土壤物理、化学和生物学性状的特征。结果表明,随着人工植被的建立与生长,土壤肥力总体趋于好转,土壤理化性质得到显著改善,土壤质地变细,微生物数量增加,土壤酶活性增强;同时,使流动沙地向半固定、固定沙丘方向转化。但随着植被盖度和植被种类的不同,不同样地土壤肥力差异很大;多年生乔木林改良土壤肥力的潜力最高,耕作粗放的农地土壤肥力有所下降。

根际沉积及其在植物-土壤碳循环中的作用

植物根际沉积是一种重要的植物与土壤交换的界面过程,在土壤碳周转方面具有重要的作用;根际碳的沉积也是联系植物、土壤及微生物的桥梁.本文就近年来关于根际沉积中碳平衡、碳循环等相关研究,阐述了根际碳沉积的机制,探讨了相关试验中存在的问题,以及不同植物品种、种类和生育期根际沉积的差异和根际沉积物与土壤呼吸的关系,指出了根际沉积在植物-土壤体系中碳循环的重要作用.在此基础上,提出了未来的研究领域及方向.

石油污染土壤生物修复过程中微生物生态研究

The analysis on microbiological ecology for four types of oil contaminates soils showed that the bacteria utilizing the oil as carbon sources increase,wheras the fugi become less .Zooloea and Bacillu are the dominant bacteria ; Mocor and Cunninghamella ,and Fursarium are the dominant fungi streptomyces take the superiority among the actinomyces.The anaiysis on esterase activity showed that the microbes above mentioned have abilies of degrading esters. The biodeg radationrates are 55.45%,56.74%,38.37% and 45.19%respectively,after 53 days,the biodegradation rate can be increased by 12.6% when the dominant microbes are added.

土壤的芘污染与土壤酶活性

选择芘作为多环芳烃(PAHs)代表污染物、敏感土壤酶作为污染物的生态毒理指标,探讨芘暴露下土壤酶活性的变化。结果表明:芘的添加浓度>50μg·kg-1时,对土壤脲酶、土壤脱氢酶活性有先抑制、后激活的作用,对土壤磷酸酶活性有激活作用;芘的添加浓度为50～1200μg·kg-1时,对土壤过氧化氢酶活性没有影响。土壤脲酶、脱氢酶、磷酸酶活性有可能作为芘污染土壤的生态毒理指标。

土壤中多环芳烃的微生物降解及土壤细菌种群多样性

利用室内模拟方法,研究中、低浓度多环芳烃(PAHs)污染土壤的微生物修复效果,阐明土壤微生物(接种和土著)与PAHs降解的关系.结果表明:投加PAHs高效降解菌可以促进土壤中PAHs的降解,2周内效果显著;典型PAHs降解的难易程度依据为:菲<蒽<芘<苯并(a)芘和屈艹;细菌种群丰度和多样性均与PAHs降解呈负相关关系,同一处理细菌种群结构随时间变化不大.对于中、低浓度PAHs原位污染土壤,增强土著菌的活性是提高土壤PAHs降解率的有效途径之一.

污染土壤中苯并(a)芘的微生物降解途径研究进展

苯并(a)芘(BaP)是一种具有强致癌、致畸和致突变的多环芳烃(PAHs)。为了修复BaP污染的土壤,探索其降解途径是很重要的。为此,综述了国内外有关污染土壤中苯并(a)芘的微生物降解情况,对不同真菌、细菌降解苯并(a)芘的能力、代谢途径、共代谢底物以及环境影响因素进行了介绍和比较,提出了苯并(a)芘中间代谢产物的累积及其环境毒性方面的研究是修复苯并(a)芘污染土壤的重要方向。

污染土壤中多环芳烃的共代谢降解过程

The biodegradation of most PAHs with high molecular weight is carried out by means of cometabolism. The development of the theory about cometabolic degradation is reviewed in this paper, and the achievements on the cometabolic degradations of PAHs are also summarized. It is demonstrated that glucose, biphenyl, organic acids and mineral oil could be used as cometabolic substrate to enhance the degradation rate of PAHs, and there are complex interactions in the microbiological degradation process among different PAHs. Some low molecular PAHs could serve as cometabolic substrate, which could also be used to enhance the transformation rate of high molecular weight recalcitrant PAHs. To achieve the cometabolic degradation of the PAHs in the soils, the following problems must be solved: the screening out of efficient degradative strains, the selection of the appropriate cometabolic substrate, the addition of surfactant if necessary and the optimization of operational parameters with the contaminated soils. These problems are the important parts of the project for the cometabolic degradation of PAHs in the soils.