Evaluation of Slow Release Substrates for Anaerobic Bioremediation

A variety of food-grade organic substrates were evaluated to identify materials that could be used to support long-term anaerobic bioremediation processes in the subsurface. In this work, the rate and extent of biogas production was used as an indicator of the potential for substrate fermentation to H₂ and acetate, the primary electron donors used in reductive dechlorination. The rate and extent of biogas (primarily CO₂+ CH₄) evolution varied widely between the different substrates. For many of the substrates, biogas generation declined to very low levels within 100 days of substrate addition. However, a few substrates including several vegetable oils and sucrose esters of fatty acid (SEFAs) did support biogas production for extended time periods. Column studies demonstrated that both soybean oil and a SEFA could support sulfate reduction, methanogenesis and reductive dechlorination of perchloroethene (PCE) to cis-dichloroethene (cis-DCE) for over 14 months. The slower degradation rate of the SEFAs could be used to control substrate degradation rate in the subsurface, increasing substrate lifetime and reducing the required reinjection frequency.     

Transformation of tetra- and trichloromethane to CO2 by anaerobic bacteria is a non-enzymic process

Abstract Degradation of tetrachloromethane was examined in the three strictly anaerobic bacteria, Acetobacterium woodii, Desulfobacterium autotrophicum and Methanobacterium thermoautotrophicum When incubated under anaerobic conditions in reduced buffer, suspensions of each organism degraded CCl₄ by both reductive and substitutive mechanisms. The products formed included less-highly chlorinated methanes and CO₂. Cell-free extracts of A. woodii degraded tetrachloromethane in a manner similar to that in whole cells but at a lower rate (63 vs. 110 μkat/kg of protein). When M. thermoautotrophicum or A. woodii was autoclaved, reductive dechlorination was partly abolished, whereas substitutive dechlorination was retained. Trichloromethane was oxidized to CO₂ by both native and autoclaved cells of A. woodii . Halomethanes are thus degraded anaerobically by reductive, substitutive and oxidative mechanisms.     

Monitoring Anaerobic Natural Attenuation of Petroleum Using a Novel In Situ Respiration Method in Low-Permeability Sediment

Assessing petroleum biodegradation rates is an important part of predicting natural attenuation in subsurface sediments. Monitoring carbon dioxide (CO₂) and methane (CH₄) produced in situ, and their radiocarbon ¹⁴C), stable carbon (¹³C) and deuterium (D). signature provide a novel method to assess anaerobic microbial processes. Our objectives were to: (1) estimate the rate of anaerobic petroleum hydrocarbon (PH) mineralization by monitoring the production of soil gas CH₄ and CO₂ in the vadose zone of low-permeability sediment, (2) evaluate the dominant microbial processes using δ¹³C and δD, and (3) determine the proportion of CH₄ and CO₂ attributable to anaerobic mineralization of PH using ¹⁴C analysis. Argon was sparged into the subsurface to dilute existing CO₂ and CH₄ concentrations. Vadose zone CO₂, CH₄, oxygen, total combustible hydrocarbons, and argon concentrations were measured for 75 days. CO₂ and CH₄ samples were collected on day 86 and analyzed for ¹⁴C, δ¹³C, and δD. Based on CH₄ soil gas production, the anaerobic biodegradation rate was estimated between 0.017 to 0.055 mg/kg soil-d. CH₄ ¹⁴C (2.6 pMC), δ¹³C (-45.64‰), and δD (-316‰) values indicated that fermentation of PH was the sale source of CH₄ in the vadose zone. CO₂ ¹⁴C (62 pMC) indicated that approximately 47% of the total CO₂ was from PH mineralization and 53% from plant root respiration. Although low-permeability sediment increases the difficulty of completely replacing in situ soil gas and assuring anaerobic conditions, this novel respiration method distinguished between anaerobic processes responsible for PH degradation.     

Growth of Dehalobacter and Dehalococcoides spp. during degradation of chlorinated ethanes

Mixed anaerobic microbial subcultures enriched from a multilayered aquifer at a former chlorinated solvent disposal facility in West Louisiana were examined to determine the organism(s) involved in the dechlorination of the toxic compounds 1,2-dichloroethane (1,2-DCA) and 1,1,2-trichloroethane (1,1,2-TCA) to ethene. Sequences phylogenetically related to Dehalobacter and Dehalococcoides, two genera of anaerobic bacteria that are known to respire with chlorinated ethenes, were detected through cloning of bacterial 16S rRNA genes. Denaturing gradient gel electrophoresis analysis of 16S rRNA gene fragments after starvation and subsequent reamendment of culture with 1,2-DCA showed that the Dehalobacter sp. grew during the dichloroelimination of 1,2-DCA to ethene, implicating this organism in degradation of 1,2-DCA in these cultures. Species-specific real-time quantitative PCR was further used to monitor proliferation of Dehalobacter and Dehalococcoides during the degradation of chlorinated ethanes and showed that in fact both microorganisms grew simultaneously during the degradation of 1,2-DCA. Conversely, Dehalobacter grew during the dichloroelimination of 1,1,2-TCA to vinyl chloride (VC) but not during the subsequent reductive dechlorination of VC to ethene, whereas Dehalococcoides grew only during the reductive dechlorination of VC but not during the dichloroelimination of 1,1,2-TCA. This demonstrated that in mixed cultures containing multiple dechlorinating microorganisms, these organisms can have either competitive or complementary dechlorination activities, depending on the chloro-organic substrate.     

Complete reductive dechlorination of tetrachloroethene to ethene by anaerobic microbial enrichment culture developed from sediment

A mixed, anaerobic microbial enrichment culture, AMEC-4P, was developed that uses lactate as the electron donor for the reductive dechlorination of tetrachloroethene (PCE) to ethene. AMEC-4P consistently and completely converted 2 mM PCE to cis-1,2-dichloroethene (cis-DCE) within 13 days, and the intermediate, cis-DCE, was then completely dechlorinated to ethene after 130 days. Dechlorination rates for PCE to cis-DCE, cis-DCE to VC, and VC to ethene were 243, 27, and 41 μmol/l/day, respectively. Geobacter lovleyi and a Dehalococcoides sp. were identified from their 16S rRNA sequences to be the dominant phylotypes in AMEC-4P.     

Bioremediation of Hexachlorocyclohexane Isomers,Chlorinated Benzenes,and Chlorinated Ethenes in Soil and Fractured Dolomite

Groundwater at an industrial site is contaminated with α hexachlorocyclohexane (HCH) and γ -HCH (i.e., lindane) (0.3 to 0.5 ppm). Other contaminants in the 1 to 15 ppm range include 1,2,4-trichlorobenezene (TCB), 1,2-dichlorobenzene (DCB), 1,3-DCB, 1,4-DCB, chlorobenzene (CB), benzene, trichloroethene (TCE), and cis-1,2-dichloroethene (cDCE). The aquifer consists of a shallow layer of soil over fractured dolomite, where most of the contaminant mass resides. The objective of this study was to compare (1) anaerobic reductive dechlorination of the polychlorinated contaminants, followed by aerobic biodegradation of the daughter products (mainly DCBs, CB, and benzene); and (2) aerobic biodegradation of α - and γ -HCH, TCB, DCBs, CB, and benzene, followed by anaerobic reduction of TCE and cDCE to ethene. Conventional wisdom suggests that sequential anaerobic and aerobic conditions are desirable for bioremediating sites contaminated by mixtures of polychlorinated organics. The results of this microcosm study suggest that a sequential aerobic and anaerobic approach may be more successful, although implementing this in the field presents some major challenges. In the dolomite microcosms incubated under aerobic conditions first (59 days), α - and γ -HCH were biodegraded close to the maximum contaminant level for lindane; all of the aromatic compounds were consumed; and there was partial removal of TCE and cDCE (presumptively via cometabolism). The subsequent switch to anaerobic conditions (day 101) yielded reductive dechlorination of the remaining TCE; a significant level of ethene was produced, although some cDCE and VC persisted. In contrast, sequential anaerobic (393 days) and aerobic treatment (498 days) for the dolomite microcosms was ineffective in completely removing the aromatic compounds, α -HCH, cDCE, and VC. For the soil microcosms, both treatment sequences were effective, most likely reflecting a greater abundance of the necessary microbes and electron donor in this part of the site.     

Reductive dechlorination of high concentrations of tetrachloroethene to ethene by an anaerobic enrichment culture in the absence of methanogenesis.

Tetrachloroethene, also known as perchloroethylene (PCE), is a common groundwater contaminant throughout the United States. The incomplete reductive dechlorination of PCE--resulting in accumulations of trichloroethene, dichloroethene isomers, and/or vinyl chloride--has been observed by many investigators in a wide variety of methanogenic environments. Previous mixed-culture studies have demonstrated that complete dechlorination to ethene is possible, although the final dechlorination step from vinyl chloride to ethene is rate limiting, with significant levels of vinyl chloride typically persisting. In this study, anaerobic methanol-PCE enrichment cultures which proved capable of dechlorinating high concentrations PCE to ethene were developed. Added concentrations of PCE as high as 550 microM (91-mg/liter nominal concentration; approximately 55-mg/liter actual aqueous concentration) were routinely dechlorinated to 80% ethene and 20% vinyl chloride within 2 days at 35 degrees C. The methanol level used was approximately twice that needed for complete dechlorination of PCE to ethene. The observed transformations occurred in the absence of methanogenesis, which was apparently inhibited by the high concentrations of PCE. When incubation was allowed to proceed for as long as 4 days, virtually complete conversion of PCE to ethene resulted, with less than 1% persisting as vinyl chloride. An electron balance demonstrated that methanol consumption was completely accounted for by dechlorination (31%) and acetate production (69%). The high volumetric rates of PCE dechlorination (up to 275 mumol/liter/day) and the relatively large fraction (ca. one-third) of the supplied electron donor used for dechlorination suggest that reductive dechlorination could be exploited for bioremediation of PCE-contaminated sites.     

Growth of Dehalobacter and Dehalococcoides spp. during Degradation of Chlorinated Ethanes

Mixed anaerobic microbial subcultures enriched from a multilayered aquifer at a former chlorinated solvent disposal facility in West Louisiana were examined to determine the organism(s) involved in the dechlorination of the toxic compounds 1,2-dichloroethane (1,2-DCA) and 1,1,2-trichloroethane (1,1,2-TCA) to ethene. Sequences phylogenetically related to Dehalobacter and Dehalococcoides, two genera of anaerobic bacteria that are known to respire with chlorinated ethenes, were detected through cloning of bacterial 16S rRNA genes. Denaturing gradient gel electrophoresis analysis of 16S rRNA gene fragments after starvation and subsequent reamendment of culture with 1,2-DCA showed that the Dehalobacter sp. grew during the dichloroelimination of 1,2-DCA to ethene, implicating this organism in degradation of 1,2-DCA in these cultures. Species-specific real-time quantitative PCR was further used to monitor proliferation of Dehalobacter and Dehalococcoides during the degradation of chlorinated ethanes and showed that in fact both microorganisms grew simultaneously during the degradation of 1,2-DCA. Conversely, Dehalobacter grew during the dichloroelimination of 1,1,2-TCA to vinyl chloride (VC) but not during the subsequent reductive dechlorination of VC to ethene, whereas Dehalococcoides grew only during the reductive dechlorination of VC but not during the dichloroelimination of 1,1,2-TCA. This demonstrated that in mixed cultures containing multiple dechlorinating microorganisms, these organisms can have either competitive or complementary dechlorination activities, depending on the chloro-organic substrate.     

Isolation of an aerobic vinyl chloride oxidizer from anaerobic groundwater

Vinyl chloride (VC) is a known human carcinogen and common groundwater contaminant. Reductive dechlorination of VC to non-toxic ethene under anaerobic conditions has been demonstrated at numerous hazardous waste sites. However, VC disappearance without stoichiometric production of ethene has also been observed at some sites and in microcosms. In this study we identify an organism responsible for this observation in presumably anaerobic microcosms and conclude that oxygen was not detectable based on a lack of color change from added resazurin. This organism, a Mycobacterium sp. closely related to known VC oxidizing strains, was present in high numbers in 16S rRNA gene clone libraries from a groundwater microcosm. Although the oxidation/reduction indicator resazurin remained in the clear reduced state in these studies, these results suggest inadvertent oxygen contamination occurred. This study helps to elucidate the dynamic behavior of chlorinated ethenes in contaminated groundwater, through the isolation of a strictly aerobic organism that may be responsible for at least some disappearance of VC without the concomitant production of ethene in groundwater considered anaerobic.     

Reductive dechlorination of high concentrations of tetrachloroethene to ethene by an anaerobic enrichment culture in the absence of methanogenesis.

Tetrachloroethene, also known as perchloroethylene (PCE), is a common groundwater contaminant throughout the United States. The incomplete reductive dechlorination of PCE--resulting in accumulations of trichloroethene, dichloroethene isomers, and/or vinyl chloride--has been observed by many investigators in a wide variety of methanogenic environments. Previous mixed-culture studies have demonstrated that complete dechlorination to ethene is possible, although the final dechlorination step from vinyl chloride to ethene is rate limiting, with significant levels of vinyl chloride typically persisting. In this study, anaerobic methanol-PCE enrichment cultures which proved capable of dechlorinating high concentrations PCE to ethene were developed. Added concentrations of PCE as high as 550 microM (91-mg/liter nominal concentration; approximately 55-mg/liter actual aqueous concentration) were routinely dechlorinated to 80% ethene and 20% vinyl chloride within 2 days at 35 degrees C. The methanol level used was approximately twice that needed for complete dechlorination of PCE to ethene. The observed transformations occurred in the absence of methanogenesis, which was apparently inhibited by the high concentrations of PCE. When incubation was allowed to proceed for as long as 4 days, virtually complete conversion of PCE to ethene resulted, with less than 1% persisting as vinyl chloride. An electron balance demonstrated that methanol consumption was completely accounted for by dechlorination (31%) and acetate production (69%). The high volumetric rates of PCE dechlorination (up to 275 mumol/liter/day) and the relatively large fraction (ca. one-third) of the supplied electron donor used for dechlorination suggest that reductive dechlorination could be exploited for bioremediation of PCE-contaminated sites.     

Methanosarcina spp. drive vinyl chloride dechlorination via interspecies hydrogen transfer

Two highly enriched cultures containing Dehalococcoides spp. were used to study the effect of aceticlastic methanogens on reductive vinyl chloride (VC) dechlorination. In terms of aceticlastic methanogens, one culture was dominated by Methanosaeta, while the other culture was dominated by Methanosarcina, as determined by fluorescence in situ hybridization. Cultures amended with 2-bromoethanesulfonate (BES), an efficient inhibitor of methanogens, exhibited slow VC dechlorination when grown on acetate and VC. Methanogenic cultures dominated by Methanosaeta had no impact on dechlorination rates, compared to BES-amended controls. In contrast, methanogenic cultures dominated by Methanosarcina displayed up to sevenfold-higher rates of VC dechlorination than their BES-amended counterparts. Methanosarcina-dominated cultures converted a higher percentage of [2-(14)C]acetate to (14)CO(2) when concomitant VC dechlorination took place, compared to nondechlorinating controls. Respiratory indices increased from 0.12 in nondechlorinating cultures to 0.51 in actively dechlorinating cultures. During VC dechlorination, aqueous hydrogen (H(2)) concentrations dropped to 0.3 to 0.5 nM. However, upon complete VC consumption, H(2) levels increased by a factor of 10 to 100, indicating active hydrogen production from acetate oxidation. This process was thermodynamically favorable by means of the extremely low H(2) levels during dechlorination. VC degradation in nonmethanogenic cultures was not inhibited by BES but was limited by the availability of H(2) as electron donor, in cultures both with and without BES. These findings all indicate that Methanosarcina (but not Methanosaeta), while cleaving acetate to methane, simultaneously oxidizes acetate to CO(2) plus H(2), driving hydrogenotrophic dehalorespiration of VC to ethene by Dehalococcoides.     

Enrichment and characterization of a trichloroethene-dechlorinating consortium containing multiple "dehalococcoides" strains

A microbial consortium that reductively dechlorinates trichloroethene, cis-1,2-dichloroethene (cis-DCE), and vinyl chloride (VC) to ethene with methanogenesis was enriched from chloroethene-contaminated soil from Japan. Dechlorination activity was maintained for over 4 years. Using quantitative polymerase chain reaction (PCR) and denaturing gradient gel electrophoresis (DGGE) analysis targeting the "Dehalococcoides" 16S rRNA gene, four strains were detected. Their growth and dechlorination activities were classified into two types: one that grows by converting cis-DCE to ethene and the other that grows by converting cis-DCE to VC. Then, the vcrA and bvcA genes encoding cis-DCE/VC reductive dehalogenases were detected. Inhibitors of methanogenesis (2-bromoethanesulfonate) and sulfidogenesis (molybdate) led to accumulation of cis-DCE and of VC respectively. These results suggest that methanogens and sulfate-reducing bacteria can play a significant role in dechlorination by "Dehalococcoides."     

Biodegradation of cis-1,2-dichloroethylene and vinyl chloride in anaerobic cultures enriched from landfill leachate sediment under Fe(III)-reducing conditions

An anaerobic, Fe(III)-reducing enrichment culture, which originatedfrom a sediment sample collected at a landfill in Nanji-do, Seoul, Korea, was capable ofdegrading cis-1,2-dichloroethylene (cis-DCE) and vinylchloride (VC). Although it exhibited the ability under Fe(III)-reducing conditions, the chlorinated ethenes degradationwas not linked to the Fe(III) reduction. During cis-DCE degradation, no VC, ethene, or ethanewas detected through the experimental period. Also, this culture did not accumulate ethene andethane during the VC degradation. It was unlikely that cis-DCE was reductivelydechlorinated to VC and then the VC formed was dechlorinated fast enough. Because the kinetic datashowed that the rate of cis-DCE degradation was 3.5 times higher than that of VC. Whereasglucose supported the culture growth and the degradation, formate, acetate, butyrate, propionate,lactate, pyruvate, and yeast extract did not. The results appeared consistent with the involvement ofoxidative degradation mechanism rather than reductive dechlorination mechanism. The traits of the culturedescribed here are unusual in the anaerobic degradation of chlorinated ethenes and may be usefulfor searching an effective organism and mechanism regarding anaerobic cis-DCE and VC degradation.     

Correlation of Dehalococcoides 16S rRNA and Chloroethene-Reductive Dehalogenase Genes with Geochemical Conditions in Chloroethene-Contaminated Groundwater

Quantitative analysis of genes that code for Dehalococcoides 16S rRNA and chloroethene-reductive dehalogenases TceA, VcrA, and BvcA was done on groundwater sampled from 150 monitoring wells spread over 11 chlorinated ethene polluted European locations. Redundancy analysis was used to relate molecular data to geochemical conditions. Dehalococcoides 16S rRNA- and vinyl chloride (VC)-reductase genes were present at all tested locations in concentrations up to 10⁶ gene copies per ml of groundwater. However, differences between and also within locations were observed. Variation in Dehalococcoides 16S rRNA gene copy numbers were most strongly correlated to dissolved organic carbon concentration in groundwater and to conditions appropriate for biodegradation of chlorinated ethenes (U.S. Environmental Protection Agency score). In contrast, vcrA gene copy numbers correlated most significantly to VC and chlorinated ethene concentrations. Interestingly, bvcA and especially tceA were more correlated with oxidizing conditions. In groundwater microcosms, dechlorination of 1 mM VC was correlated to an increase of vcrA and/or bvcA gene copies by 2 to 4 orders of magnitude. Interestingly, in 34% of the monitoring wells and in 40% of the active microcosms, the amount of individual VC-reductase gene copies exceeded that of Dehalococcoides 16S rRNA gene copies. It is concluded that the geographical distribution of the genes was not homogeneous, depending on the geochemical conditions, whereby tceA and bvcA correlated to more oxidized conditions than Dehalococcoides 16S rRNA and vcrA. Because the variation in VC-reductase gene numbers was not directly correlated to variation in Dehalococcoides spp., VC-reductase genes are better monitoring parameters for VC dechlorination capacity than Dehalococcoides spp.Chlorinated ethenes, such as tetrachloroethene (PCE) and trichloroethene (TCE), are persistent groundwater pollutants (15, 22). Because these compounds are toxic and mobile in groundwater systems, they form a serious risk for human health and the environment. PCE and TCE can be dechlorinated by microorganisms under anaerobic conditions by reductive dehalogenation to dichloroethene (DCE), vinyl chloride (VC), and ethene (20). Bioremediation strategies for chloroethene-contaminated sites are often based on (stimulation of) reductive dechlorination of the chlorinated ethenes to ethene (7, 12, 14). In practice, reductive dechlorination of PCE and TCE can be incomplete, resulting in accumulation of DCE or VC. Since VC is much more mobile, toxic, and carcinogenic than PCE and TCE (9), monitoring and stimulation of VC dechlorination are essential steps in bioremediation strategies.Only members of Dehalococcoides spp. are known to be able to reductively dechlorinate VC. Therefore, 16S rRNA genes of these species are often used as molecular target to indicate and monitor DCE and VC dechlorination capacity at contaminated sites. However, previous studies showed different dechlorination capacities for individual Dehalococcoides species, and only a few strains are known to metabolically dechlorinate VC (6, 8, 10, 17, 21). As a consequence, 16S rRNA gene-based detection can lead to overestimation of VC dechlorination capacity. In contrast, although metabolic reductive dechlorination of VC has mostly been linked to Dehalococcoides spp., it cannot be excluded that other microbial species that perform this dechlorination exist. Genes coding for DCE and VC reductases may be exchangeable between different microbial species via horizontal gene transfer. This is plausible since it has been shown that the metabolic genes for VC dechlorination, vcrA and bvcA, have a different evolutionary history than most other Dehalococcoides genes (16). Consequently, Dehalococcoides 16S rRNA gene-based detection can also lead to underestimation of VC dechlorination capacity.To more precisely determine VC dechlorination capacity, genes directly involved in reductive dechlorination of VC should be used as a molecular target, in addition to Dehalococcoides 16S rRNA genes. A quantitative method was described to detect genes coding for VC-reductases VcrA and BvcA identified in Dehalococcoides sp. strains VS and GT and in Dehalococcoides sp. strain BAV1, respectively (10, 17, 21). Different studies showed direct correlation of vcrA and bvcA gene copy numbers with reductive dechlorination of VC in batch cultures, soil columns, and contaminated sites (2, 11, 19).Quantification of genes that encode VC-reductases can be a useful method to monitor reductive dechlorination of VC in chloroethene-contaminated groundwater during enhanced natural attenuation activities (4, 19). However, little is known about the presence, dispersion, and importance of specific dehalogenase genes in chlorinated ethene polluted groundwater and their correlation to biogeochemical conditions and reductive dechlorination.The objective of the present study was therefore to identify the relative importance of TCE-reductase gene tceA and VC-reductase genes vcrA and bvcA in chloroethene-polluted groundwater and to identify geochemical parameters that contribute to variation in copy numbers of these genes. To this end, groundwater of 150 monitoring wells from 11 European polluted sites was analyzed. Furthermore, microcosms with groundwater from 6 locations were started to test whether VC dechlorination is directly correlated to an increase of vcrA or bvcA genes.     

添加氧化铁对水稻土中H2、CO2和CH4形成的影响

水稻土是甲烷产生的重要源地.厌氧条件下甲烷的形成与有机质厌氧降解产生的乙酸、H₂和CO₂有关.氧化铁作为电子受体可有效地竞争有机质向甲烷的转化,其抑制作用机理可能与乙酸、H₂和CO₂的有效消耗有关.通过向水稻土泥浆中添加无定形氧化铁和纤铁矿,分别测定了25℃厌氧恒温培养105d过程中的H₂、CO₂和CH₄的浓度变化.结果表明,添加无定形氧化铁及纤铁矿可导致H₂浓度显著降低;无定形氧化铁对H₂消耗的影响明显大于纤铁矿;添加不同氧化铁对CO₂浓度的影响与H₂浓度的变化有相同的趋势;添加氧化铁能显著抑制水稻土中甲烷形成,并导致有机碳的转移发生变化,使得CH₄-C显著降低,气相中CO₂-C量减少,而由土壤泥浆固定的CO₃^2--C量显著增加.     

Hydrogen cycling in a three-tiered food web growing on the methanogenic conversion of 3-chlorobenzoate

Abstract A defined 3-chlorobenzoate-degrading methanogenic consortium was constructed by recombining key organisms isolated from a 3-chlorobenzoate-degrading methanogenic sludge enrichment. The organisms comprise a three-tiered food chain which includes: (1) reductive dechlorination of 3-chlorobenzoate; (2) oxidation of benzoate to acetate, H₂ and CO₂; (3) removal of H₂ plus CO₂ by conversion into methane. The defined consortium, consisting of a dechlorinating organism (DCB-1), a benzoate degrader (BZ-1) and a lithotrophic methanogen ( Methanospirillum strain PM-1) grew well in a basal salts medium supplemented with 3-chlorobenzoate (3.2 mM) as the sole energy source. The chlorine released from the aromatic ringe was recovered in stoichiometric amounts as the chloride ion. The reducing power required for reductive dechlorination was obtained from the hydrogen produced in the acetogenic oxidation of benzoate. One-third of the benzoate-derived hydrogen was recycled via the reductive dechlorination of 3-chlorobenzoate, indicating that the consortium operated as a food web rather than a food chain.     

Chloroethene biodegradation in sediments at 4 degrees C

Microbial reductive dechlorination of [1,2-14C]trichloroethene to [14C]cis-dichloroethene and [14C]vinyl chloride was observed at 4 degrees C in anoxic microcosms prepared with cold temperature-adapted aquifer and river sediments from Alaska. Microbial anaerobic oxidation of [1,2-14C]cis-dichloroethene and [1,2-14C]vinyl chloride to 14CO2 also was observed under these conditions.     

低浓度SO2对云杉幼苗中碳水化合物代谢的影响研究

研究了低浓度SO₂对云杉幼苗的光合作用速率及碳水化合物代谢的生理生化过程的影响,测定了CO₂摄取速率、幼苗蔗糖含量、蔗糖磷酸合成酶、蔗糖合成酶和转化酶活性及ATP/ADP值.结果表明,低浓度的SO₂(200μg·m^-3)能瞬时刺激幼苗对CO₂的吸收.与对照组相比,幼苗中的蔗糖含量及蔗糖磷酸酶活性明显下降,ATP/ADP处于低水平.因此,在受到SO₂污染形成可见伤害前,幼苗的生理生化过程可能已受到干扰.     

Methanosarcina spp. Drive Vinyl Chloride Dechlorination via Interspecies Hydrogen Transfer

Two highly enriched cultures containing Dehalococcoides spp. were used to study the effect of aceticlastic methanogens on reductive vinyl chloride (VC) dechlorination. In terms of aceticlastic methanogens, one culture was dominated by Methanosaeta, while the other culture was dominated by Methanosarcina, as determined by fluorescence in situ hybridization. Cultures amended with 2-bromoethanesulfonate (BES), an efficient inhibitor of methanogens, exhibited slow VC dechlorination when grown on acetate and VC. Methanogenic cultures dominated by Methanosaeta had no impact on dechlorination rates, compared to BES-amended controls. In contrast, methanogenic cultures dominated by Methanosarcina displayed up to sevenfold-higher rates of VC dechlorination than their BES-amended counterparts. Methanosarcina-dominated cultures converted a higher percentage of [2-¹⁴C]acetate to ¹⁴CO₂ when concomitant VC dechlorination took place, compared to nondechlorinating controls. Respiratory indices increased from 0.12 in nondechlorinating cultures to 0.51 in actively dechlorinating cultures. During VC dechlorination, aqueous hydrogen (H₂) concentrations dropped to 0.3 to 0.5 nM. However, upon complete VC consumption, H₂ levels increased by a factor of 10 to 100, indicating active hydrogen production from acetate oxidation. This process was thermodynamically favorable by means of the extremely low H₂ levels during dechlorination. VC degradation in nonmethanogenic cultures was not inhibited by BES but was limited by the availability of H₂ as electron donor, in cultures both with and without BES. These findings all indicate that Methanosarcina (but not Methanosaeta), while cleaving acetate to methane, simultaneously oxidizes acetate to CO₂ plus H₂, driving hydrogenotrophic dehalorespiration of VC to ethene by Dehalococcoides.