The influence of nitrate on the phosphorus flux to and from oxygen depleted lake sediments

Addition of nitrate to an oxygen depleted sediment leads to a stimulation of the mineralization process if a major part of the nitrate is dissimilatorily reduced. This may cause an increased release of phosphate from some sediments. Nitrate, however, maintains a high redox potential at the sediment surface and thus prevents a release of iron-bound phosphorus. These two counteracting effects of nitrate addition to sediment-water systems were demonstrated in laboratory experiments. A high supply of nitrate to a phosphorus-saturated sediment caused an increased release of phosphate and ammonium once the nitrate had been used up. However, from other sediments there was no or very little release of phosphate but an increased release of ammonium caused by high nitrate dissimilation, probably due to the very high capacity of these sediments to bind liberated phosphate or due to storage of phosphorus in an increased bacterial biomass. Phosphorus fractionation, before and after the experiments with the sediments, provided information on transfers to, from and within the sediments.     

厌氧氨氧化菌驱动脱氮途径的研究进展

厌氧氨氧化菌(anaerobic ammonia-oxidizing bacteria, AnAOB)的代谢多样性,使得该菌群能够在海洋、湿地和陆地等不同的自然生态系统中广泛分布,甚至在一些极热和极寒环境中也检测到了该菌群的存在。本文回顾并总结了厌氧氨氧化菌在不同生态系统中的发现、分布及脱氮贡献等方面的研究,分析了厌氧氨氧化菌分布的主要环境影响因素。该综述将帮助我们更好地理解全球氮循环中厌氧氨氧化菌的实际角色和功能,并基于厌氧氨氧化(anaerobicammoniaoxidation,anammox)过程,探究能与其进行协作的新型生物脱氮工艺,以期为这些工艺的研发和推广提供生态学基础和新的思考,从而实现脱氮工艺的技术变革。     

The influence of structural components of alkyl esters on their anaerobic biodegradation in marine sediment

Ester-based organic compounds are one type of synthetic base fluid added to drilling mud used during off-shore oil-drilling operations in the Gulf of Mexico. Concern over the environmental impact of synthetic base fluid (SBF) contaminated rock cuttings discharged into the Gulf of Mexico has prompted the promulgation of EPA regulations requiring that all SBF be tested for biodegradability in marine sediment prior to their use in the Gulf. In order to allow the design or selection of suitably biodegradable esters, the anaerobic biodegradability of a variety of ester compounds was tested using a marine sediment inoculum to reveal the effect of: (a) increasing the chain length of the acid moiety, (b) increasing the chain length of the alcohol moiety; (c) alternating the relative size of the alcohol and acid moieties, (d) branching in the alcohol moiety, and (e) the presence of an unsaturated bond in the acidic moiety. The chemical structure of esters was found to affect the completeness and rate of anaerobic biodegradation, and would affect their ability to be certified for use as an SBF in the Gulf of Mexico. Recommendations for ester usage include using esters that have a total carbon number of between 12 and 18 and avoiding the use of branched alcohols (or acids by inference). The presence of an unsaturated bond in the acid (or alcohol by inference) increased biodegradability of the ester.     

The effects of sediment desiccation on the potential for nitrification, denitrification, and methanogenesis in an Australian reservoir

Sediments from an Australian reservoir were selected for varying degrees of in situ desiccation (i.e. non-desiccated, partially desiccated and desiccated). Sediment samples were then chemically amended with appropriate electron donors and acceptors to ascertain the effect of sediment desiccation on the potential for nitrification, denitrification, methanogenesis, and the interaction of these processes. There was no detectable nitrification in these sediments yet up to 75% of added nitrate was converted to dinitrogen. Denitrification was predominantly limited by nitrate although there was evidence of carbon co-limitation. None of the nitrogen cycle processes were notably affected by sediment desiccation. There was no flush of mineral nitrogen from desiccated sediments upon rewetting. Methanogenesis did not begin in these sediments until nitrate concentrations fell below 2.25 * 10^-5 M. Methanogenesis was always carbon limited. Methanogens were affected by sediment desiccation but were capable of recovery over time upon rewetting of sediments.     

Hydrogen as an electron donor for sulfate-reducing bacteria in slurries of salt marsh sediment

Experiments with a Warburg respirometer showed that a sediment slurry consumed hydrogen from a hydrogen atmosphere, and this consumption was not due to the activity of methanogenic bacteria. The hydrogren uptake was inhibited by the addition of 20 mM molybdate. Further experiments with sediment slurry held in conical flasks under an atmosphere of nitrogen showed that hydrogen accumulated in the headspace when bacterial sulfate reduction was inhibited either by the addition of 20 mM molybdate or by low (<5 mM) sulfate concentrations in the slurry. Methanogenesis was stimulated in the presence of a hydrogen atmosphere or by the addition of 20 mM molybdate. The results confirmed that hydrogren was an important electron donor for sulfate-reducing bacteria present in the sediment. The stimulation of methanogenesis by molybdate could be explained in part by a competition for hydrogen between sulfate-reducing bacteria and hydrogen-metabolizing methanogenic bacteria, but competition for another common substrate, possibly acetate, could also be significant.     

崇明东滩盐沼植被变化对滩涂湿地促淤消浪功能的影响

30年来在海平面上升、人类围垦、自然保护、外来物种入侵等自然与人为作用共同影响下,崇明东滩盐沼植被群落结构发生了巨大变化。基于长江口四期遥感影像解译结果,得到盐沼植被群落结构变化,结合对盐沼植被促淤消浪功能已有研究成果,量化崇明东滩盐沼植被促淤消浪功能潜力及其变化。研究表明:1980、1990、2000和2010年崇明东滩芦苇、互花米草、藨草群落面积比例分别为23∶0∶77、73∶0∶27、33∶9∶58、34∶34∶32,同期总植被覆盖面积分别为51、83、37、44 km2。30年来滩涂湿地促淤消浪能力均有下降,1990—2000年变化最大。其中,植被黏附悬浮颗粒物量分别为1976、4645、2192、4695 t;沉积量分别为960、1579、195、286万m3;常规波高情况下堤外没有足够植被保护的岸段长度分别为5、0、7、6 km;风暴潮情况下堤外没有足够植被保护的岸段长度分别为19、5、26、20 km。因此保护堤外盐沼植被对消浪促淤,特别是抵御风暴潮等恶劣气候灾害的影响具有重要意义。     

The influence of light and nutrient addition upon the sediment chemistry of iron in an arctic lake

The geochemical response of sediments to increased nutrient input to an Alaskan, arctic lake was examined using direct measurements of sediment-water chemical fluxes. An unexpected increase in Fe flux occurred when sediments were exposed to high incident radiation and nutrient concentrations. Correlation between light and acid-soluble Fe concentrations suggests that photoreduction of Fe(III) oxides may occur, but nutrient addition enhanced the effect indicating that primary productivity was also important. The processes controlling the flux of Fe from sediments in this lake were complex and included the redox potential (dissolved oxygen concentration) of the water, quality of organic matter present in the sediment, light, and nutrients supplied from the sediments and/or water column. These four factors together with the possibility of direct uptake of Fe by phytoplankton and the possible release of algal reductants may contribute to Fe cycling in this lake.     

Effect of 2,4‐dinitrotoluene on the anaerobic bacterial community in marine sediment

Aims: To study the impact of added 2,4‐dinitrotoluene (DNT) on the anaerobic bacterial community in marine sediment collected from an unexploded ordnance dumping site in Halifax Harbour. Methods and Results: Marine sediment was spiked with 2,4‐DNT and incubated under anaerobic conditions in the presence and absence of lactate. Indigenous bacteria in the sediment removed 2,4‐DNT with subsequent formation of its mono‐ and diamino‐derivatives under both conditions. PCR–DGGE and nucleotide sequencing were used to monitor the change in the bacterial population in sediment caused by the presence of 2,4‐DNT. The results showed that denaturing gradient gel electrophoresis banding patterns of sediment microcosms treated with 2,4‐DNT were different from controls that did not receive 2,4‐DNT. Bacteroidetes, Firmicutes and δ‐Proteobacteria were present in sediment incubated in the absence of 2,4‐DNT. However, several γ‐Proteobacteria became dominant in sediment in the presence of 2,4‐DNT, two of which were 99% similar to Shewanella canadensis and Shewanella sediminis. In the presence of both 2,4‐DNT and lactate, two additional δ‐Proteobacteria were enriched, one closely related (98% similarity) to Desulfofrigus fragile and the other affiliated (96% similarity) to Desulfovibrio sp. In contrast, none of the above four Proteobacteria were enriched in sediment incubated with lactate alone. Conclusions: Presence of 2,4‐DNT led to a significant change in bacterial population of marine sediment with the enrichment of several γ‐ and δ‐Proteobacteria. Significance and Impact of the Study: Our results provided the first evidence on the impact of the pollutant 2,4‐DNT on the indigenous bacterial community in marine sediment, and provided an insight into the composition of bacterial community that degrade 2,4‐DNT.     

气体环境对厌氧益生菌乳双歧杆菌V9菌株生长影响的研究

<正>乳双歧杆菌(Bifidobacterium lactis)V9菌株分离自健康蒙古族儿童肠道,已被广泛应用于开发各类益生菌产品[1]。由于双歧杆菌为厌氧菌[2],因此培养和保存时的气体环境会影响其活菌数量和益生功效,也成为该菌实现产业化道路上必须关注的重要环节。本刊于2012年第7期刊登了其木格苏都、张和平等的文章"不同气体环境对益生菌Bifidobacterium lactis V9生长的影响"[3]。作者对该菌在不同气体环境中的生长代谢特性进行了系统研究,明确了在有微量二氧化碳和氧气存在的环境下更有利于其生长。该研究为提高乳双歧     

Microbial activity and community structure in a lake sediment used for psychrophilic anaerobic wastewater treatment

Aims: The aim of the study was to investigate the feasibility of a continuous reactor for psychrophilic anaerobic wastewater treatment by using the sludge from cold natural environment. Methods and Results: Six sludge samples (S1–S6) were collected from different cold natural locations to select sludge with high anaerobic microbial activity under low temperatures. After a 225‐day incubation, the maximum specific methane production rate of a waterfowl lake sediment (S1) at 15°C (70·5 mLCH₄ gVSS^?1 day^?1) was much higher than all other samples. S1 was thus chosen as the seed sludge for the reactor treating synthetic brewery wastewater at 15°C, by immobilizing the micro‐organisms on polyurethane foam carriers. The chemical oxygen demand (COD) removal efficiency reached over 80% after 240‐day operation at an organic loading rate of 5·3 kg m^?3 day^?1, and significant enrichment of biomass was observed. Clone libraries of the microbial communities in the inoculum had high diversities for both archaea and bacteria. Along with a decrease in microbial community diversities, the dominant bacteria (79·5%) at the end of the operation represented the phylum Firmicutes, while the dominant archaeon (41·5%) showed a similarity of 98% with the psychrotolerant methanogen Methanosarcina lacustris. Conclusions: The possibility of using anaerobic micro‐organisms from cold environments in anaerobic wastewater treatment under psychrophilic conditions is supported by these findings. Significance and Impact of the Study: This study enriches the theory on microbial community and the application on anaerobic treatment of sludge from cold natural environments.     

Chlorophenol dechlorination and subsequent degradation in denitrifying microcosms fed low concentrations of nitrate

The potential of using nitrate as a terminal electron acceptor to stimulate anaerobic degradation of mixtures of monochlorophenols (MCPs) or dichlorophenols (DCPs) was evaluated. Contaminated and non-contaminated soils were added to water saturated anaerobic microcosms supplemented with 1 mM or 5 mM nitrate. Denitrification and dechlorination activity were present in three diverse soil types and were maintained upon refeeding both nitrate and the appropriate chlorophenol. However, dechlorination activity could only be serially transferred in enrichments with an added electron donor such as acetate. Dehalogenation activity in enrichments from four of the primary microcosms showed at least five different dechlorination reactions, each mediated by different microbial communities. Three of these are distinct ortho-dechlorinating paths; two are meta-dechlorinating and one is the para-dechlorination of 3,4-DCP. Simultaneous dechlorination and denitrification was observed and both activities could be maintained in microcosms but only in the presence of low nitrate concentrations. Dechlorination and denitrification were mediated by two separate microbial communities; one that dechlorinates without use of nitrate and one that denitrifies while oxidizing the dechlorinated aromatic ring. There was no evidence that dechlorination is mediated by the denitrifying community, however the maintenance of a denitrification potential using low (< 1 mM) nitrate concentrations may be useful for completing the food chain by stimulating the mineralization of phenol and benzoate.     

Cultivation of syntrophic anaerobic bacteria in membrane-separated culture devices

A dialysis culture device was used for growth of syntrophic fatty acid-oxidizing and ethanol-oxidizing anaerobic bacteria. A pure culture of the fatty acid oxidizer Clostridium bryantii was grown inside dialysis tubing which was surrounded by a pure culture of Desulfovibrio vulgaris. The same apparatus was used for the syntrophic cultivation of Pelobacter acetylenicus and Acetobacterium woodii with ethanol as substrate. In both cases, substrate degradation and product formation were about half as fast as with the homogeneously mixed control cultures. In the compartment of the hydrogen producer, the concentration of free hydrogen during syntrophic ethanol degradation was about 10 times as high as in that of the hydrogen utilizer, whereas the homogeneously mixed culture exhibited an intermediate hydrogen partial pressure.     

The denitrification potential and density of denitrifying bacteria in the bottom sediments of Matupi Harbor (Papua New Guinea)

The denitrification potential and density of denitrifying bacteria were determined in suboxidized sediments of Matupi Harbor (Papua New Guinea). The sediments were characterized by low denitrification potentials, not exceeding 0.8 nM/(g h). The maximum density of denitrifying bacteria was recorded in the upper sediment horizons and was 10⁴ cells/g of wet ground.     

The influence of catchment characteristics on suspended sediment properties

In order to investigate the influence of catchment characteristics on suspended sediment properties, suspended sediment samples were collected from the outlets of 60 small catchments located throughout Southwest England over a 14-month period. The catchments were selected to provide a representative range of topographic, land use, soil and geological characteristics. The suspended sediment samples were collected using time-integrating trap samplers, emptied at monthly intervals. Laboratory analysis focused on a selection of suspended sediment properties, including particle size composition, cation exchange capacity, and organic carbon, nitrogen, metal, radionuclide and phosphorus content. The results presented show that despite the substantial variability of catchment characteristics associated with the 60 sampling sites, the suspended sediment properties generally fell within a relatively limited range. However, statistical analysis identified significant spatial variability of suspended sediment within Southwest England, which in turn can be linked to catchment characteristics.     

The kinetics of the degradation of chloroform and benzene in anaerobic sediment from the River Rhine

In anaerobic methanogenic sediment microcosms¹⁴C labelled chloroform was degraded mainly to carbon dioxide. At a concentration of 4 g.l^–1 the mineralization followed first order kinetics with a half life of 12 days at 10°C and 2.6 days at 20°C. At a concentration of 400 g.l^–1 the mineralization rate increased with time and followed logarithmic kinetics with a _max of 0.02.d^–1 at 10°C. The logarithmic kinetics can be explained by growth of the bacteria on the higher concentration of chloroform with a generation time of 35 days. Shaking and oxygenation did not inhibit the mineralization of chloroform, probably because of bacterial consumption of the dissolved oxygen. ¹⁴C labelled benzene was mineralized only for a small percentage to¹⁴C labelled carbon dioxide while other, not acid extractable, degradation products were formed. Under anaerobic conditions after one day when 5% of the benzene was degraded to carbon dioxide, the mineralization ceased, while the disappearance of benzene proceeded. With air in the headspace of the incubation bottles 25% of the benzene was mineralized to carbon dioxide. The anaerobic degradation of benzene at a concentration of 100 .l^–1 showed similar kinetics as the degradation at 1 g.l^–1. Hence no adaptation of the microflora in the sediment occurred during the 63 days of the experiment at 100 g.l^–1.     

Mass spectrometry as en ecological tool for in situ measurement of dissolved gases in sediment systems

Abstract The use of membrane-inlet quadrupole mass spectrometry, as a method for quantitative monitoring of dissolved gases in natural or semi-natural environments, is described. Its advantages over other methods lie in the fact that it provides an accurate, sensitive means for non-invasive, continuous analysis of several dissolved gases simultaneously. The potential of mass spectrometry as an ecological tool is illustrated by representative results from measurements made on undisturbed and experimentally amended estuarine and fresh-water sediments.
Dissolved gas profiles from the surface to a depth of 10 cm in the estuarine sediment showed that the dissolved oxygen decreased gradually until at 10 cm it was undetectable (< 0.25 μM); dinitrogen reached a maximum at 6 cm, where oxygen was 20 μM. In a fresh-water sediment, methane reached 1.5 mM at 10 cm depth. NO_x was also detected; quantitation of carbon dioxide necessitates a correction for the contribution of NO_x. Manipulation of conditions (gas phase, nitrogen and carbon sources) permitted ecological modelling.