Contribution of suspended and sorbed groundwater bacteria to degradation of dissolved and sorbed aniline

The influence of sorption on the mineralisation of 50 pg aniline l(-1) was examined in an aquifer material under batch conditions. The study was designed to distinguish the rates and extent of biodegradation of the sorbed and the dissolved trace organic and the contribution of sorbed and suspended bacteria to the degradation. Four different mathematical models were developed with different assumptions about the partitioning of aniline degradation and bacterial activity between the solid and the aqueous phases. The models were developed by combining an expression for logistic growth of the degrading population with Michaelis-Menten kinetics for the transformation of aniline. It was tested by a series of laboratory experiments conducted with 14C-labelled aniline, aseptically treated aquifer sand and filter-sterilised groundwater in different proportions and bacteria isolated from pristine groundwater. Model evaluation of the experimental data suggested that the fate of aniline was mainly controlled by suspended bacteria degrading both the dissolved and sorbed fractions. The degradation was slow, with a first-order degradation rate equal to 10(-6) h(-1).     

2,4-二氯苯酚在土壤与河流底泥中降解动力学

以南京化学工业园内四柳河沿岸土壤与河流底泥为研究对象,通过土壤灭菌、温度与污染物初始浓度调控,研究了2,4-二氯苯酚在土壤与河流底泥中降解动力学及其影响因子。结果表明:微生物对2,4-二氯苯酚降解起主导作用,在45d内,非灭菌土壤和河流底泥的降解率分别是灭菌条件下的1.5～3倍、1.4～2.8倍,土壤和河流底泥中的2,4-二氯苯酚微生物降解量分别为0.128～0.599和0.113～0.718mg·kg-1,非灭菌处理半衰期时间短于灭菌处理;(10±1)℃～(30±1)℃范围内,随着温度的增高,2,4-二氯苯酚降解加快,在(30±1)℃土壤与河流底泥中残留量最小,分别为0.305和0.203mg·kg-1,半衰期也最短;土壤与河流底泥中的2,4-二氯苯酚均在其浓度为0.5mg·kg-1时降解最快,随着初始浓度的增加,2,4-二氯苯酚降解速度呈现递减趋势,半衰期增长。     

Degradation of 2,4-dichlorophenol and pentachlorophenol by two brown rot fungi

Wheat straw cultures of the brown rot fungi Gloeophyllum striatum and G. trabeum degraded 2,4-dichlorophenol and pentachorophenol. Up to 54% and 27% 14CO2, respectively, were liberated from uniformly 14C-labeled substrates within 6 weeks. Under identical conditions Trametes versicolor, a typical white rot species employed as reference, evolved up to 42% and 43% 14CO2 and expressed high activities of laccase, manganese peroxidase, and manganese-independent peroxidase. No such activity could be detected in straw or liquid cultures of Gloeophyllum. Moreover, G. striatum degraded both chlorophenols most efficiently under non-cometabolic conditions, i.e. on a defined mineral medium lacking sources of carbon, nitrogen and phosphate.     

Photosynthesis-dependent removal of 2,4-dichlorophenol by Chlorella fusca var. vacuolata

Of 7 green algae, Chlorella fusca var. vacuolata removed about 23% of 2,4-dichlorophenol (DCP) at 10–80 M after 4 d when grown photoautotrophically. Removal of DCP was growth-dependent and was suppressed dose-dependently by the photosynthesis inhibitor, 3-(3,4-dichlorophenyl)-1,1-dimethyl urea.     

Degradation of 2,4-dihydroxybenzoate by Pseudomonas sp. BN9

Abstract The aerobic degradation of 2,4-dihydroxybenzoate by Pseudomonas sp. BN9 was studied. Intact cells of Pseudomonas sp. BN9 grown with 2,4-dihydroxybenzoate oxidized 2,4-dihydroxybenzoate but not salicylate. Cell-free extracts of Pseudomonas sp. BN9 converted 2,4-dihydroxybenzoate after the addition of NAD(P)H. A partially purified protein fraction converted 2,4-dihydroxybenzoate with NADH to 1,2,4-trihydroxybenzene. 1,2,4-Trihydroxybenzene was converted by a 1,2-dioxygenase to maleylpyruvate, which was reduced by a NADH-dependent enzyme to 3-oxoadipate. 2,4-Dihydroxybenzoate 1-monooxygenase, 1,2,4-trihydroxybenzene 1,2-dioxygenase and maleylpyruvate reductase were induced in Pseudomonas sp. BN9 after growth with 2,4-dihydroxybenzoate.     

降解2,4-二氯酚微生物的分离及其2,4-二氯酚羟化酶基因的克隆和表达

从土壤中分离到一株降解2,4-二氯酚能力较强的细菌菌株GT241-1,经鉴定该菌株属于假单胞菌属。菌株GT241-1在最适条件下能在48h内将90mg/L的2,4-DCP降解91%,能利用2,4-二氯酚、2,4-二氯苯氧乙酸、苯甲酸和儿茶酚为唯一碳源生长。采用Southern杂交对2,4-二氯酚羟化酶基因（dcpA）定位后构建基因组文库,再用斑点杂交筛选目的转化子,克隆了该菌株的dcpA。序列测定得知含dcpA的亚克隆片段全长2389bp,其中dcpA基因编码区1797bp。核苷酸和氨基酸序列分析表明,dcpA与已在GenBank登记的相关基因有一定的差异。dcpA基因能够在大肠杆菌转化子中成功地表达有生物活性的酶。     

假单胞菌菌株CTN-3对百菌清污染土壤的生物修复

百菌清被美国环境保护署列为优先控制污染物,利用微生物的降解作用修复被污染的土壤、清除环境中的污染物等具有重要的现实意义.假单胞菌(Pseudomonas sp.)菌株CTN-3是一株从污染土壤中分离得到的百菌清降解菌,考察了其在实验室条件下对百菌清污染土壤的生物修复能力及其影响因素.结果表明:降解菌株在灭菌土壤中的降解效果略好于未灭菌土壤;在外源添加降解菌106 CFU·g-1、温度15 ～ 30℃和pH5.8～8.3条件下,该菌株能有效降解土壤中10 ～200 mg·kg-1的百菌清.菌株CTN-3在百菌清污染土壤的生物修复中具有良好的应用前景.     

铁还原菌降解石油烃的研究进展

铁还原菌是指能够利用细胞外Fe(III)作为末端电子受体,通过氧化有机物将Fe(III)还原为Fe(II)微生物的总称。铁还原作用广泛存在于土壤、河流、海洋、地表含水层以及高温高压的地下深部油藏。在厌氧或兼性厌氧条件下,Fe(III)还原耦合有机物的降解,对铁、碳元素的生物地球化学循环具有重要意义。本文介绍了铁还原菌的多样性和铁还原作用机理,综述了铁还原菌在石油烃降解方面的研究进展。此外,还总结了铁还原菌在生物修复中的潜在作用,并对未来的研究方向进行了展望。     

Degradation of 2,4-dichlorophenoxyacetic acid by mixed cultures of bacteria

Summary We explored the feasibility of using mixed cultures for herbicide degradation, with the ultimate aim of application for effluent treatment. The present study reports on mixed cultures which were developed to grow aerobically with 2,4-dichlorophenoxyacetic acid (2,4-D) as the sole carbon substrate. Degradation of 2,4-D was verified by HPLC and UV-spectroscopic analysis of the residual 2,4-D concentration in the test cultures. Cultures that were initially developed with 2,4-D also grew readily with glucose, but the degradation of 2,4-D was effectively prevented under mixed substrate conditions. Mamor intermediates or metabolites resulting from 2,4-D degradation were not detected with the HPLC methodology except 2,4-dichlorophenol which appeared to accumulate transiently in the growth medium.     

Oxidative consumption of nitric oxide by heterotrophic bacteria in soil

Abstract: Uptake rate constants for nitric oxide were measured in a neutral calcic cambisol (KBE) and an acidic luvisol (PBE). The NO uptake was higher under oxic than under anoxic incubation conditions by a factor of about three. Gassing the soils with air containing 10 ppmv NO resulted in the accumulation of nitrate which accounted for 57–94% of the NO consumed. Aerobic heterotrophic bacteria were isolated on glucose-yeast extract medium from soil dilutions corresponding to a most probable number of 10⁸–10⁹ bacteria per gram dry weight soil. One of the isolates (strain PS88, a Pseudomonas sp.) exhibited NO consumption activity that was much higher under oxic than anoxic incubation conditions. When sterile KBE amended with strain PS88 was gassed with air containing 10 ppmv NO, 88% of the consumed NO was recovered as nitrate and nitrite. A screening of various bacteria obtained from culture collections showed a widespread ability for consumption of low NO concentrations. Our results indicate that NO consumption in soil is not only possible by reductive denitrification, but also by oxidation due to aerobic heterotrophic bacteria such as strain PS88.     

Effects of carbon substrate enrichment and DOC concentration on biodegradation of PAHs in soil

AIMS: Two common reasons to explain slow environmental biodegradation of polycyclic aromatic hydrocarbons (PAHs), namely lack of appropriate carbon sources for microbial growth and limited bioavailability of PAHs, were tested in a laboratory bioassay using a creosote-contaminated soil. METHODS AND RESULTS: The soil, containing a total of 8 mg g-1 of 16 PAHs, was sieved and incubated in bottles for 45 days. The first explanation was tested by enrichment with the analogue anthracene and the non-analogue myristic acid, and both failed to stimulate degradation of all PAHs except anthracene. The second explanation was tested by addition of different concentrations of dissolved organic carbon (DOC), with effects depending on the DOC concentration and the molecular size of the PAH. The degradation was enhanced from 10 to 35% for 12 PAHs when the soil was saturated. The degraded amounts of individual PAHs were proportional to their concentration in the soil. CONCLUSIONS: The slow in situ degradation of PAHs was enhanced by more than three times by adding water as a solvent. Addition of DOC facilitated the degradation of four- to six-ring PAHs. SIGNIFICANCE AND IMPACT OF STUDY: Bioremediation of PAH-contaminated sites may be facilitated by creating water-saturated conditions but retarded by addition of other carbon substrates, such as analogue compounds.     

Electrokinetic movement and biodegradation of 2,4-dichlorophenoxyacetic acid in silt soil

The coupling of electrokinetic movement of an organic contaminant, 2,4-dichlorophenoxyacetic acid (2,4-D), through soil and its biodegradation in situ has been demonstrated. In a first experiment, the direction and rate of movement of 2,4-D were determined using homogeneously contaminated soil (864 mg 2,4-D/kg dry weight soil) compacted into six individual compartments, 6 cm long, 3 cm wide, and 4 cm deep. Each compartment was bordered by a carbon felt anode and a stainless steel cathode. The application of a current density of 3.72 A/m(2) led to migration of 2,4-D towards the anode at a rate of approximately 4 cm/day. In a second experiment, electrokinetic movement and biodegradation were combined in situ. Sterilized silt soil contaminated with ring-labeled 14C-2,4-D (811 mg 2,4-D/kg dry weight soil) was compacted into a single soil compartment, 22 cm long, 7 cm wide, and 4 cm deep, in a 4.5 cm region adjacent to the cathode. The remainder of the compartment was filled with sterilized soil (to a total weight of 1,015 g). Burkholderia spp. RASC c2 (1.88 x 10(11) cells), a tetracycline-resistant bacterium with chromosomally encoded degradative genes for 2,4-D, was inoculated into the soil at a position 14-16 cm from the cathode. The reactor was placed within a sealed perspex box, with a constant air flow connected to sodium hydroxide traps. Under an applied current density of 0.89 A/m(2), the pollutant moved towards the bacteria. As it reached the inoculated region, its concentration decreased in the soil and 14CO2 was recovered in the traps. At the end of the experiment, 87.1% of radiolabel had been removed from the soil, 5.8% of which was recovered as 14CO2. A third, control, experiment showed a significant contrast in the absence of an electric current, where a slow rate of diffusion controlled the movement of both 2,4-D and bacteria in the soil and biodegradation occurred at the interface between the diffusing fronts.     

Repeated inoculation as a strategy for the remediation of low concentrations of phenanthrene in soil

Phenanthrene, a polycyclic aromatic hydrocarbon, becomes increasingly unavailable to microorganisms for degradation as it ages in soil. Consequently, many bioaugmentation efforts to remediate polycyclic aromatic hydrocarbons in soil have failed. We studied theeffect of repeatedly inoculating a soil with a phenanthrene-degrading Arthrobacter sp. on the mineralization kinetics of low concentrations of phenanthrene. After the first inoculation, the initial mineralization rate of 50 ng/g phenanthrene declined in a biphasicexponential pattern. By three hundred hours after inoculation, there was no difference in mineralization rates between the inoculated and uninoculated treatments even though a large fraction of the phenanthrene had not yet been mineralized. A second and third inoculation significantly increased the mineralization rate, suggesting that, though themineralization rate declined, phenanthrene remained bioavailable. Restirring the soil, without inoculation, did not produce similar increases in mineralization rates, suggesting absence of contact between cells and phenanthrene on a larger spatial scale (>mm) is not the cause of the mineralization decline. Bacteria inoculated into soil 280 hours beforethe phenanthrene was added could not maintain phenanthrene degradation activity. We suggest sorption lowered bioavailability of phenanthrene below an induction threshold concentration for metabolic activity of phenanthrene-degrading bacteria.     

Behavior of Cu and Zn under combined pollution of 2,4-dichlorophenol in the planted soil

Behavior of heavy metals under combined pollution of 2,4-dichlorophenol (2,4-DCP) was investigated using metal contaminated soil which was sampled from the heavily industrialized areas, Fuyang county, Zhejiang Province, P.R. China and pretreated with 100 μg g^?1 2,4-DCP for 1 month. Metal complexes were the predominant species for Cu and Zn in the soil solution. The treatment of 2,4-DCP had limited effect on the dissolution of Cu and Zn in the soil without plant root growth. But the metal species might be changed due to the addition of organic pollutant. Planting with rye grass for 1 month, greatly increased both water soluble Cu and Zn. The increase of water soluble Cu and Zn in the presence of 2,4-DCP was much more than that in the absence of 2,4-DCP, which suggested more attention should be paid to the behavior of heavy metals under combined pollution of organic pollutants in the planted soil. The results also indicated that in comparison to Cu, soil planted with ryegrass was more effective in activating Zn from soils, which was consistent with its relative weak chemisorptions on clays, oxides and humus of soils.     

Degradation of polycyclic aromatic hydrocarbons in soil by a two-step sequential treatment

The objectives of this work were to isolate the microorganisms responsible for a previously observed degradation of polycyclic aromatic hydrocarbons (PAH) in soil and to test a method for cleaning a PAH-contaminated soil. An efficient PAH degrader was isolated from an agricultural soil and designated as Mycobacterium LP1. In liquid culture, it degraded phenanthrene (58%), pyrene (24%), anthracene (21%) and benzo(a)pyrene (10%) present in mixture (initial concentration 50 μg ml⁻¹ each) and phenanthrene (92%) and pyrene (94%) as sole carbon sources after 14 days of incubation at 30°C. In soil, Mycobacterium LP1 mineralised ¹⁴C-phenanthrene (45%) and ¹⁴C-pyrene (65%) after 10 days. The good ability of this Mycobacterium was combined with the benzo(a)pyrene oxidation effect obtained by 1% w/w rapeseed oil in a sequential treatment of a PAH-spiked soil (total PAH concentration 200 mg kg⁻¹). The first step was incubation with the bacterium for 12 days and the second step was the addition of the rapeseed oil after this time and a further incubation of 22 days. Phenanthrene (99%), pyrene (95%) and anthracene (99%) were mainly degraded in the first 12 days and a total of 85% of benzo(a)pyrene was transformed during the whole process. The feasibility of the method is discussed.     

Degradation of fluoranthene in a soil matrix by indigenous and introduced bacteria

Microbial growth and degradation of fluoranthene in amended soil microcosms by the indigenous microbial population and a PAH degrading mixed culture inoculum were characterised. Percentages of fluoranthene disappearance ranged from 14.4 % in sterilised uninoculated soil microcosms to 52.1 % in unsterilized inoculated microcosms. Inoculated soils had initial microbial counts approximately one order of magnitude higher than the indigenous soil count and exhibited enhanced fluoranthene degradation. Over a nine week incubation period, total viable counts in inoculated non-sterile soil declined to the levels observed for the original indigenous population.     

Effect of aeration on ethylene production by soil bacteria and soil samples cultivated in a closed system

Summary Ethylene production was studied in shaken cultures ofPseudomonas putida andPseudomonas fluorescens isolated from soil and in unsterile garden soil samples moistened to 60% of the water holding capacity. The highest ethylene accumulation in bacterial cultures was reached under conditions of delayed aeration,i.e. when the culture was closed and the aeration started after the oxygen content decreased to 4%. The ethylene production rose immediately after the beginning of aeration. Under these conditions ethylene production was inP. fluorescens 2–3 times and in glucosecultivatedP. putida 6 times higher than in the fully aerated cultures. Methionine stimulated ethylene production byP. fluorescens, whereas glucose proved to be more suitable forP. putida. This strain was incapable of growth on methionine as the sole carbon source. Samples of nonsterile garden soil produced the highest amounts of ethylene under anaerobic conditions. Artificial inoculation of soil samples byP. putida resulted in an increase of ethylene formation in samples with delayed aeration. Addition of glucose or glucose with methionine stimulated ethylene production in all soil samples.