1,2,4—三氯苯在土壤中的降解

在好氧和厌氧两种条件下研究了１,２,４－三氯苯的降解。结果表明,１,２,４－三氯苯的好氧降解和厌氧降解均遵循一级反应动力学。在同样水分、温度及初始浓度条件下,１,２,４－三氯苯的好氧降解比厌氧降解比厌氧降解迅速,其半衰期分别为１．８９￣５．８６和５．０７￣１９．０８ｄ。土壤中１,２,４－三氯苯的初始浓度对于其降解也有显著影响,在０￣１００μｇ·ｇ＾－１的范围内,浓度增高时,其降解加快,说明污染物浓     

球形红细菌厌氧降解邻二氯苯及其机理研究

研究分析光合细菌球形红细菌在厌氧光照条件下降解邻二氯苯的条件和机理.结果表明,在厌氧光照条件下球形红细菌的最佳生长和对邻二氯苯的最佳降解条件为:pH 7.0,温度为30℃,接种量10%.在最佳条件下,邻二氯苯的去除率可达90%以上;其降解中间产物主要有氯苯、4-羟基苯甲酸;根据降解产物的分析,推断球形红细菌降解邻二氯苯的机理主要是按照先脱掉一个氯原子生成氯苯,然后氯苯进一步脱氯并通过4-羟基苯甲酸的代谢途径开环进行.     

球形红细菌厌氧降解邻二氯苯及其机理研究

研究分析光合细菌球形红细菌在厌氧光照条件下降解邻二氯苯的条件和机理。结果表明, 在厌氧光照条件下球形红细菌的最佳生长和对邻二氯苯的最佳降解条件为：pH 7.0, 温度为30℃, 接种量10％。在最佳条件下, 邻二氯苯的去除率可达90％以上; 其降解中间产物主要有氯苯、4-羟基苯甲酸; 根据降解产物的分析, 推断球形红细菌降解邻二氯苯的机理主要是按照先脱掉一个氯原子生成氯苯, 然后氯苯进一步脱氯并通过4-羟基苯甲酸的代谢途径开环进行。     

花色苷的酶降解

综述了降解花色苷的酶类及其降解机理的研究进展.降解花色苷的酶有花色苷酶、多酚氧化酶、过氧化物酶和果胶酶.花色苷酶和果胶酶均能水解花色苷糖苷键产生花色素和糖,花色素很不稳定,因吡喃烊环极易开环可自发转换成无色衍生物.花色苷不能直接作为PPO或POD的底物;PPO和POD氧化、降解花色苷须依赖具邻二酚结构的其他酚类的存在,...     

1，2，4－三氯苯在土壤中的降解

在好氧和厌氧两种条件下研究了１,２,４－三氯苯的降解,结果表明,１,２,４－三氯苯的好氧降解和厌氧降解均遵循一级反应动力学在同样水分、温度及初始浓度条件下,１,２,４－三氯苯的好氧降解比厌氧降解迅速,其半衰期分别为１．８９～５．８６和５．０７～１９．０８ｄ土壤中１,２,４－三氯苯的初始浓度对于其降解也有显著影响,在０～１００μｇ·ｇ－１的范围内,浓度增高时,其降解加快,说明污染物浓度对降解的影响;在１０～３０℃范围内,温度增高导致降解过程加快,归因于温度升高对微生物酶活性的激活作用．     

氯代苯胺类化合物微生物降解的研究进展*

对氯代苯胺类化合物(Chlovoanilines,CAS)好氧微生物降解的研究现状进行了系统的综述,内容包括具有降解氯代苯胺类化合物能力的微生物、氯代苯胺类化合物的代谢途径及相关代谢酶的分析、降解质粒和关键代谢酶的基因克隆和表达,并提出了氯代苯胺类化合物好氧微生物降解研究中存在的问题和尚需进一步研究的方面。     

多氯联苯微生物脱氯研究进展

多氯联苯(polychlorinated biphenyls,PCBs)是环境中典型的氯代持久性有机污染物.微生物脱氯是一种氯代有机物自然降解模式,对全球PCBs特别是高氯代同系物消减起到至关重要的作用.厌氧条件下高氯代PCBs能够发生脱氯反应,使其毒性大大降低,脱氯后形成的低氯代化合物可以进一步好氧降解,直至完全矿化.本文综述了PCBs生物脱氯的研究进展,介绍了微生物脱氯反应的机理和特征、参与微生物脱氯过程的专性脱氯菌等,探讨了该微生物过程的影响因素及厌氧脱氯与好氧降解耦合的意义,并对脱氯微生物群落的复杂代谢网络研究、专性脱氯新菌种筛选及其污染地实际修复应用等未来研究方向进行了展望.     

土壤和沉积物中多氯代有机化合物厌氧降解研究进展

多氯代有机化合物(PCOCs)是土壤和沉积物中的典型污染物,厌氧条件下PCOCs能够发生脱氯发应,从而使其毒性大大降低,脱氯后形成的低氯代化合物可以进一步好氧降解,直至完全矿化。从PCOCs的降解过程出发,重点综述了几种典型PCOCs的厌氧脱氯机理以及几种重要影响因素;阐明了脱氯反应是PCOCs厌氧降解的关键步骤,反应的发生必须有还原剂提供电子,微生物的参与尤为重要;同时展望了同位素示踪法在研究PCOCs降解机制上的应用,以及开发高效降解PCOCs微生物的必要性等。     

厌氧丁草胺降解菌BAD-20的分离鉴定及降解特性研究

【目的】分离并鉴定能够降解除草剂丁草胺的厌氧微生物菌株,研究其厌氧降解丁草胺的特性和代谢途径,为深入研究丁草胺厌氧降解机制提供依据。【方法】以丁草胺为碳源作为选择压力从水稻田土壤中富集驯化丁草胺降解菌,利用16S rRNA基因系统发育分析结合菌株培养特征对降解菌株进行初步鉴定,利用液相色谱-时间飞行质谱(LC-TOF-MS)检测菌株降解丁草胺的代谢产物。【结果】筛选到一株降解丁草胺的厌氧细菌,命名为BAD-20,初步鉴定为嗜蛋白质菌属(Proteiniphilum),菌株BAD-20降解丁草胺的最适条件为温度30–35℃、pH 7.5–8.0和0–0.5%NaCl,在有氧条件下该菌不能降解丁草胺。最适条件下,菌株BAD-20在10d降解90%的20mg/L丁草胺。菌株BAD-20还能降解甲草胺、乙草胺、丙草胺,降解效率从高到低依次为甲草胺乙草胺丙草胺丁草胺,对这些氯乙酰胺除草剂的降解动力学符合一级动力学方程。鉴定到2个丁草胺降解代谢产物,分别是N-(2,6-二乙基苯基)-N-(丁氧甲基)乙酰胺(DEPBMA)和N-(2,6-二乙基苯基)乙酰胺(DEPA),表明菌株BAD-20降解丁草胺的起始步骤为脱氯,随后脱去N-丁氧甲基。【结论】本研究富集分离到一株降解丁草胺的厌氧细菌嗜蛋白质菌属(Proteiniphilum) BAD-20,为深入研究丁草胺厌氧降解机制及研发含丁草胺废水厌氧生物处理技术提供依据。     

光合细菌对芳香族化合物厌氧降解的研究进展

许多被有毒性的芳香族化合物污染的环境实际上是缺氧的 ,因此芳香族化合物的厌氧降解逐渐引起人们的兴趣。芳香族化合物的厌氧还原降解机制从根本上不同于好氧条件下的氧化降解机制 ,而光合细菌一直以来是研究芳香族化合物厌氧降解的模式菌株。因此 ,从生理学、酶学及分子生物学角度出发概括了对光合细菌厌氧降解芳香族化合物的研究动态。     

Aerobic and Anaerobic Biodegradation of Aged Pentachlorophenol by Indigenous Microorganisms

Pentachlorophenol (PCP) use as a general biocide, particularly for treating wood, has led to widespread environmental contamination. Biodegradation has emerged as the main mechanism for PCP degradation in soil and groundwater and a key strategy for remediation. Examining the microbial biodegrading potential for PCP at a contaminated site is crucial in determining its fate. Hundreds of studies have been published on PCP microbial degradation, but few have described the biodegradation of PCP that has been in contact with soils for many years. The bioavailability of “aged” hydrophobic organics is a significant concern. PCP- and 2,3,4,6-tetrachlorophenol (2,3,4,6-TeCP)-contaminated soil samples from several depths at a former wood treatment site were placed under varying conditions in the laboratory to determine the anaerobic and aerobic potential for biodegradation of chlorophenols at the site. PCP biodegradation occurred in both anaerobic and aerobic soil samples. Rapid aerobic degradation occurred in samples spiked with 2- and 4-chlorophenol, but not with 3-chlorophenol. Reductive dechlorination of PCP in anaerobic samples resulted in the accumulation of 3-chlorophenol. In most anaerobic replicates, 3-chlorophenol was degraded with the appearance of detectable, but not quantifiable amounts of phenol. These results indicate excellent potential for remediation at the site using the indigenous microorganisms under both aerobic and anaerobic conditions. However, a fraction of the PCP was unavailable for degradation.     

白腐真菌生物技术降解氯酚污染物

生物降解是降解氯酚污染物的一条重要的转化途径,白腐真菌是一种高效的生物降解菌种,应用白腐真菌生物技术降解具有毒性和抗降解性的氯酚具有重要意义。本文阐述了白腐菌降解氯酚类污染物的途径,阐述了白腐真菌技术,主要包括酶技术、固定化技术、真菌强化技术、堆肥化和生物反应器等在氯酚污染环境治理中的应用,并概述了近几年白腐菌降解氯酚的研究热点和白腐真菌生物技术的应用趋势。     

Regiospecificity of chlorophenol reductive dechlorination by vitamin b(12s)

Vitamin B(12), reduced by titanium (III) citrate to vitamin B(12s), catalyzes the reductive dechlorination of chlorophenols. Reductive dechlorination of pentachlorophenol and of all tetrachlorophenol and trichlorophenol isomers was observed. Reaction of various chlorophenols with vitamin B(12) favored reductive dechlorination at positions adjacent to another chlorinated carbon, but chlorines ortho to the hydroxyl group of a phenol were particularly resistant to reductive dechlorination, even if they were also ortho to a chlorine. This resulted in a reductive dechlorination pattern favoring removal of para and meta chlorines, which differs substantially from the pattern exhibited by anaerobic microbial consortia.     

Pentachlorophenol Dechlorination in Fluidized-Bed Reactors under Methanogenic Conditions

The reductive dechlorination of chlorophenols was studied in three fluidized-bed reactors (FBRs) with respect to enrichment, pathways, complete dechlorination, and overall performance. The methanogenic consortia, developed by previous researchers in our laboratory, have been further enriched by reducing the ratio of substrate to pentachlorophenol (PCP) and increasing the PCP loading. The performance of the consortia was improved, and complete dechlorination at high PCP loading rates was observed, reaching a PCP loading of 1227 µmol/L d with 99% chlorophenol removal. The dechlorination rates in the reactors for chlorophenol (CP) congeners were obtained and were used to evaluate the performance of the three consortia and to quantitatively estimate the fates of these chlorophenols in the reactors. The consortium with the best performance was further investigated in bottle tests by treatment with heat and metabolic inhibitors to examine chlorophenol degradation and to characterize the CP degraders. The degradation of all monochlorophenols was completely inhibited after heat treatment, but the degradation of all other tested chlorophenols was hardly affected by heat treatment, indicating that spore-forming bacteria likely were involved in dechlorination. Addition of sulfate negatively affected CP degradation, but addition of molybdate reduced the effect of sulfate. Tests with 2-bromoethanesulfonic acid and vancomycin indicated that bacteria were responsible for chlorophenol degradation in the consortium.     

Transformations of chloroguaiacols, chloroveratroles, and chlorocatechols by stable consortia of anaerobic bacteria.

Metabolically stable consortia of anaerobic bacteria obtained by enrichment of sediment samples with 3,4,5-trimethoxybenzoate (TMBA), 3,4,5-trihydroxybenzoate (gallate [GA]), or 5-chlorovanillin (CV) were used to study the anaerobic transformation of a series of chloroveratroles, chloroguaiacols, and chlorocatechols used as cosubstrates. Experiments were carried out with growing cultures, and the following pathways were demonstrated for metabolism of the growth substrates: (i) TMBA produced GA, which was further degraded without the formation of aromatic intermediates; (ii) GA formed pyrogallol, which was stable to further transformation; and (iii) CV was degraded by a series of steps involving de-O-methylation, oxidation of the aldehyde group, and decarboxylation to 3-chlorocatechol before ring cleavage. Mono-de-O-methylation of the cosubstrates occurred rapidly in the order 4,5,6-trichloroguaiacol greater than 3,4,5-trichloroguaiacol approximately 3,4,5-trichloroveratrole approximately tetrachloroveratrole greater than tetrachloroguaiacol and was concomitant with degradation of the growth substrates. For the polymethoxy compounds--chloroveratroles, 1,2,3-trichloro-4,5,6-trimethoxybenzene, and 4,5,6-trichlorosyringol--de-O-methylation took place sequentially. The resulting chlorocatechols were stable to further transformation until the cultures had exhausted the growth substrates; selective dechlorination then occurred with the formation of 3,5-dichlorocatechol from 3,4,5-trichlorocatechol and of 3,4,6-trichlorocatechol from tetrachlorocatechol. 2,4,5-, 2,4,6-, and 3,4,5-trichoroanisole and 2,3,4,5-tetrachloroanisole were de-O-methylated, but the resulting chlorophenols were resistant to dechlorination. These results extend those of a previous study with spiked sediment samples and their endogenous microflora and illustrate some of the transformations of chloroguaiacols and chlorocatechols which may be expected to occur in anaerobic sediments.     

Transformations of chloroguaiacols, chloroveratroles, and chlorocatechols by stable consortia of anaerobic bacteria

Metabolically stable consortia of anaerobic bacteria obtained by enrichment of sediment samples with 3,4,5-trimethoxybenzoate (TMBA), 3,4,5-trihydroxybenzoate (gallate [GA]), or 5-chlorovanillin (CV) were used to study the anaerobic transformation of a series of chloroveratroles, chloroguaiacols, and chlorocatechols used as cosubstrates. Experiments were carried out with growing cultures, and the following pathways were demonstrated for metabolism of the growth substrates: (i) TMBA produced GA, which was further degraded without the formation of aromatic intermediates; (ii) GA formed pyrogallol, which was stable to further transformation; and (iii) CV was degraded by a series of steps involving de-O-methylation, oxidation of the aldehyde group, and decarboxylation to 3-chlorocatechol before ring cleavage. Mono-de-O-methylation of the cosubstrates occurred rapidly in the order 4,5,6-trichloroguaiacol greater than 3,4,5-trichloroguaiacol approximately 3,4,5-trichloroveratrole approximately tetrachloroveratrole greater than tetrachloroguaiacol and was concomitant with degradation of the growth substrates. For the polymethoxy compounds--chloroveratroles, 1,2,3-trichloro-4,5,6-trimethoxybenzene, and 4,5,6-trichlorosyringol--de-O-methylation took place sequentially. The resulting chlorocatechols were stable to further transformation until the cultures had exhausted the growth substrates; selective dechlorination then occurred with the formation of 3,5-dichlorocatechol from 3,4,5-trichlorocatechol and of 3,4,6-trichlorocatechol from tetrachlorocatechol. 2,4,5-, 2,4,6-, and 3,4,5-trichoroanisole and 2,3,4,5-tetrachloroanisole were de-O-methylated, but the resulting chlorophenols were resistant to dechlorination. These results extend those of a previous study with spiked sediment samples and their endogenous microflora and illustrate some of the transformations of chloroguaiacols and chlorocatechols which may be expected to occur in anaerobic sediments.     

Bioavailability of chlorocatechols in naturally contaminated sediment samples and of chloroguaiacols covalently bound to c(2)-guaiacyl residues

Bacteria in anaerobic enrichment cultures that dechlorinated a range of chlorocatechols were used to examine the stability of endogenous chlorocatechols in a contaminated sediment sample and in interstitial water prepared from it. During incubation of the sediment sample for 450 days with or without added cells, there was a decrease in the concentration of solvent-extractable chlorocatechols but not in that of the total chlorocatechols, including sediment-associated components. In the presence of azide, the decrease in the concentrations of the former was eliminated or substantially decreased. Control experiments in which 3,4,5-trichlorocatechol was added to the sediment suspensions after 130 days showed that its dechlorination was accomplished not only by the added cells but also by the endemic microbial flora. It was concluded that the endogenous chlorocatechols in the sediment were not accessible to microorganisms with dechlorinating activity. On the other hand, microorganisms were apparently responsible for decreasing the solvent extractability of the chlorocatechols, and this effect decreased with increasing length of exposure time. Similar experiments carried out for 70 days with the sediment interstitial water showed that the chlorocatechols that were known to be associated with organic matter were also inaccessible to microbial dechlorination. Experiments with model compounds in which 4,5,6-trichloroguaiacol and tetrachloroguaiacol were covalently linked to C(2)-guaiacyl residues showed that these compounds were resistant to O demethylation or dechlorination during incubation with a culture having these activities. The only effect of microbial action was the quantitative reduction in 12 days of the C'1 keto group to an alcohol which was stable against further transformation for up to 65 days. The results of these experiments are consistent with the existence of chlorocatechols and chloroguaiacols in contaminated sediments and illustrate the cardinal significance of bioavailability in determining their recalcitrance to dechlorination and O demethylation, respectively. It is suggested that bioavailability is an important factor in determining the persistence of xenobiotics in natural ecosystems and that its omission represents a serious limitation in the interpretation of many laboratory experiments directed towards determining the persistence of xenobiotics in aquatic ecosystems.     

Bioreclamation of chlorophenol-contaminated soil by composting

Summary Microbiological decontamination of technical chlorophenol-containing soil by composting was studied. In two 50 m³ windrows the concentration of chlorophenols went down from 212 mg kg^-1 to 30 mg kg^-1 in 4 summer months and after the second summer of composting it was only 15 mg kg^-1. All chlorophenol congeners present in the technical chlorophenol were degraded, but the main dimeric impurities, polychlorinated phenoxyphenols were recalcitrant. The contaminated soil was found to contain chlorophenol-degrading microbes, 5x10⁶ cfu g^-1 of dry windrow soil. Laboratory experiments with samples from the windrow compost showed that chlorophenols were truly degraded and that chlorophenol loss by evaporation was less than 1.5% under the circumstances studied. Laboratory experiments also showed that degradation of chlorophenols (120 mg kg^-1) was accelerated when sterilized contaminated soil was inoculated with Rhodococcus chlorophenolicus (mineralizer of several chlorophenols) or naturally occurring microbes of the field composts. Biomethylation of chlorophenols in the composts was insignificant compared to biodegradation.     

Bioavailability of Chlorocatechols in Naturally Contaminated Sediment Samples and of Chloroguaiacols Covalently Bound to C2-Guaiacyl Residues

Bacteria in anaerobic enrichment cultures that dechlorinated a range of chlorocatechols were used to examine the stability of endogenous chlorocatechols in a contaminated sediment sample and in interstitial water prepared from it. During incubation of the sediment sample for 450 days with or without added cells, there was a decrease in the concentration of solvent-extractable chlorocatechols but not in that of the total chlorocatechols, including sediment-associated components. In the presence of azide, the decrease in the concentrations of the former was eliminated or substantially decreased. Control experiments in which 3,4,5-trichlorocatechol was added to the sediment suspensions after 130 days showed that its dechlorination was accomplished not only by the added cells but also by the endemic microbial flora. It was concluded that the endogenous chlorocatechols in the sediment were not accessible to microorganisms with dechlorinating activity. On the other hand, microorganisms were apparently responsible for decreasing the solvent extractability of the chlorocatechols, and this effect decreased with increasing length of exposure time. Similar experiments carried out for 70 days with the sediment interstitial water showed that the chlorocatechols that were known to be associated with organic matter were also inaccessible to microbial dechlorination. Experiments with model compounds in which 4,5,6-trichloroguaiacol and tetrachloroguaiacol were covalently linked to C₂-guaiacyl residues showed that these compounds were resistant to O demethylation or dechlorination during incubation with a culture having these activities. The only effect of microbial action was the quantitative reduction in 12 days of the C′1 keto group to an alcohol which was stable against further transformation for up to 65 days. The results of these experiments are consistent with the existence of chlorocatechols and chloroguaiacols in contaminated sediments and illustrate the cardinal significance of bioavailability in determining their recalcitrance to dechlorination and O demethylation, respectively. It is suggested that bioavailability is an important factor in determining the persistence of xenobiotics in natural ecosystems and that its omission represents a serious limitation in the interpretation of many laboratory experiments directed towards determining the persistence of xenobiotics in aquatic ecosystems.     

瘤胃微生物对纤维素降解机理

城市有机垃圾中木质纤维素难以被降解的根本原因 ,在于其木质素的物理屏障作用及纤维素本身的结晶结构 ,瘤胃微生物能够高效降解木质纤维素 ,是因为瘤胃菌群中存在各种可以分别降解木素和结晶纤维素微生物 ,它们分泌的各种酶类是降解的关键所在。