不同密度下的鲤鱼扰动作用对沉积物-水界面硝化、反硝化和氨化速率的影响

为研究不同密度下的鲤鱼（Cyprinus carpio）扰动作用对沉积物-水界面硝化、反硝化及硝酸盐氨化速率的影响,实验设置了一个对照组（不放鲤鱼组,用C0表示）和5个不同鲤鱼放养密度组（2、4、6、8、10尾/水槽,分别用C2、C4、C6、C8、C10表示）,定期用无扰动底泥采集器采集沉积物样品,乙炔抑制法测定沉积物-水界面的硝化、反硝化及硝酸盐氨化速率,示踪颗粒法测定鲤鱼的物理扰动深度。主要实验结果如下：（1）在5种密度下,鲤鱼对底泥的物理扰动深度主要集中在15 cm。（2）空白组（C0）沉积物-水界面硝化速率显著高于鲤鱼放养组（P0.05）,而放养密度较大的C8和C10组,其沉积物-水界面的硝化速率显著高于低密度放养组（C2、C4和C6）（P0.05）。（3）实验期间,空白组（C0）沉积物-水界面几乎检测不出反硝化速率,而鲤鱼放养组则总体表现为放养密度越大,沉积物-水界面反硝化速率越高。（4）各组硝酸盐氨化速率波动范围不大,但放养密度较大的C8和C10组,其硝酸盐氨化速率相对其他组较高。实验结果表明：在实验条件下,鲤鱼对沉积物-水界面的硝化和反硝化作用均有明显的促进作用,放养密度越高促进作用越明显,在沉积物中有机碳含量充足的情况下,鲤鱼的扰动可以对富营养化池塘起到很好的去氮作用。     

限氧自养硝化-反硝化生物脱氮新技术

限氧自养硝化—反硝化是部分硝化与厌氧氨氧化相耦联的生物脱氮反应过程,通过严格控制溶解氧在0．1～0．3mg·L^-1,实现硝化反应控制在亚硝酸阶段,然后以硝化阶段剩余的NH4^+作为电子供体,在厌氧条件下实现反硝化,该反应过程是完全的自养硝化—反硝化过程,具有能耗低、脱氮效率高、反应系统占地面积小等优点,适用于处理COD／NH4^+—N低的废水,是一种非常有应用前景的生物脱氮技术,文中详细介绍了限氧自养硝化—反硝化生物脱氮反应过程的研究进展,讨论了其微生物学机理及应用前景。     

好氧反硝化菌

<正>养殖水体氮素污染问题是目前困扰我国水产养殖业可持续发展的一大难题。生物脱氮技术被认为是目前最具发展前景的水体脱氮技术,其效果的优劣与所采用菌株的特性密切相关。传统反硝化细菌仅能在厌氧及低氧条件下发挥脱氮作用,与养殖水体的高溶氧环境矛盾,而好氧反硝化细菌则可在高溶氧环境中发挥脱氮作用,显著提高生物脱氮技术在养殖水体中的应用效果,实现养殖水体的绿色、零污染脱氮。因而,对好氧反硝化细菌开展高效选育方法的研究,找到可适应养殖水体水环境的微生物菌株具有重要的理论价值和经济价值。     

海洋环境异养硝化-好氧反硝化菌的研究进展

异养硝化-好氧反硝化（heterotrophic nitrifying-aerobic denitrification,HN-AD）菌的发现打破了传统的脱氮理论,可以在有氧条件下同时进行硝化和反硝化,成为近年来的研究热点。HN-AD细菌在海洋氮循环中发挥着重要作用。本文对海洋环境中HN-AD菌的多样性和部分已知氮代谢途径及相关酶系进行了介绍,分析了盐度、碳氮比、溶解氧、pH等环境因素对HN-AD菌脱氮效果的影响,对其工艺和技术应用、前景和发展方向进行了综述和展望。     

一株硝化反硝化菌的筛选鉴定及反硝化特性研究

{{@ convertAbstractHtml(article.abstractinfoCn, \"cn\")}}       

好氧反硝化生物脱氮技术的研究进展

好氧反硝化生物脱氮技术自提出以来,凭借能实现同步硝化反硝化、节省基建投资及运行费用等诸多优点,受到国内外环境领域学者的广泛关注.本文首先总结了近年来好氧反硝化菌种的筛选分离情况,以及环境因子对好氧反硝化菌脱氮效能的影响,包括溶解氧(dissolved oxygen,DO)、碳氮比(C/N)、温度等.然后深入探讨了好氧反...     

同步硝化反硝化机理的研究进展*

结合近年来国内外脱氮的最新研究成果,从宏观环境理论、微环境理论和微生物学理论方面对同步硝化反硝化的产生机理进行了综述,并提出了今后在好氧颗粒污泥实现同步硝化反硝化、脱氮除磷一体化等方面的研究发展方向。     

异养硝化-好氧反硝化的研究进展

近年来,异养硝化-好氧反硝化菌的发现打破了传统硝化反硝化理论,其在去除氮素和有机污染物的同时,能够实现同时硝化反硝化(SND),因此受到广泛关注。文章介绍了异养硝化-好氧反硝化菌的影响因素和一些已筛选菌的最佳脱氮效果,及其与传统硝化反硝化菌作用酶系的不同,列出了一些已筛选菌的氮代谢途径,并对中间产物NO2--N积累和复合菌方面的研究进展进行了综述,最后提出了异养硝化-好氧反硝化在生物强化应用中的研究现状和面临的挑战。     

反硝化基因工程菌株YP4S的构建及对污水除氮特性研究

从养殖场污泥中筛选出菌株YP4,经16S rDNA分子发育树的同源序列比对,确定为克雷伯什菌属(Klebsiella sp.)。由NCBI数据库查编码亚硝酸还原酶(Nir)的基因nirS序列,设计引物,以铜绿假单胞菌PAOI基因组DNA为模板,应用PCR技术扩增目的片段nirS,经过双酶切、克隆和转化,得到重组质粒pYP4S,然后转化野生菌株YP4,构建反硝化基因工程菌YP4S。菌株生长曲线测定表明,工程菌株YP4S与YP4的生长特性基本一致。工程菌株YP4S对模拟污水COD、TN、NH_4^+-N和NO_3^--N具有较高的去除率,YP4S与YP4相比,对NO_2^--N积累的减少量为(32.44±3.96)%,明显减少了NO_2^--N的积累。通过正交试验获得工程菌株YP4S在C/N=10、T=30℃、r=200 r/min和pH=7.0的最佳组合条件下,对模拟污水TN去除率较高。应用工程菌株YP4S处理猪场沉淀池的实际污水,COD、TN、TP、NH_4^+-N和NO_3^--N去除率分别为(95.87±0.82)%、(76.38±3.84)%、(97.13±0.54)%和(75.35±2.57)%,NO_2^--N积累量为(3.31±1.24) mg/L,表明工程菌株YP4S具有较好反硝化作用,对含氮量高的实际污水修复具有潜在的应用前景。     

细菌好氧反硝化研究进展

阐述了好氧反硝化细菌的种类及有关性质 ,并从电子理论、氧的浓度、反硝化酶系等方面对细菌好氧反硝化的作用机制进行了探讨 ,对细菌好氧反硝化的研究概况、进展及其研究意义和目前存在的问题作了较为详细的介绍。     

放牧家畜排泄物N转化研究进展

放牧家畜排泄物氮转化是草原生态系统氮循环的关键。自 2 0世纪 70年代以来 ,以提高氮利用效率和减少温室气体排放为目的的家畜排泄物氮转化的研究越来越受到人们的重视。放牧家畜排泄物氮的转化研究主要包括 3个方面 :氮的矿化、硝化与反硝化 ,氮的氨化。家畜粪氮矿化速度慢 ,持续时间长 ;尿氮矿化速度快 ,持续时间短。氮矿化与家畜排泄物 C∶ N比、木质素/氮素比、木质素含量和纤维素含量呈负相关关系 ,而与全氮含量和水溶性氮含量呈正相关 ;土壤动物和微生物可以显著促进氮的矿化过程 ;高温和相对干燥、砂质土壤较壤土和粘土有利于氮的矿化。 4～ 4 0℃氮硝化作用与温度呈正相关 ;硝化作用的底物和产物浓度、土壤溶液渗透压和氯化物浓度的增加对硝化作用有强烈的抑制效应 ;p H6 .0～ 8.0条件下硝化作用强度随着土壤p H值的升高而增加 ,而 p H值高于 8.0或低于 6 .0时硝化作用受到抑制 ;硝化作用与土壤氧气含量呈正相关关系 ,而与土壤含水量呈负相关 ;温暖湿润较干燥炎热的气候条件有利于硝化过程的进行。反硝化作用与土壤氧气浓度呈负相关关系 ,而与土壤含水量和可利用有机碳含量呈正相关 ;0～ 6 5℃反硝化作用强度随温度升高而增大 ,10～ 35℃条件下温度成为影响反硝化作用的关键因素 ;反硝化作用在     

Biological nitrogen fixation: rates,patterns and ecological controls in terrestrial ecosystems

New techniques have identified a wide range of organisms with the capacity to carry out biological nitrogen fixation (BNF)—greatly expanding our appreciation of the diversity and ubiquity of N fixers—but our understanding of the rates and controls of BNF at ecosystem and global scales has not advanced at the same pace. Nevertheless, determining rates and controls of BNF is crucial to placing anthropogenic changes to the N cycle in context, and to understanding, predicting and managing many aspects of global environmental change. Here, we estimate terrestrial BNF for a pre-industrial world by combining information on N fluxes with ¹⁵N relative abundance data for terrestrial ecosystems. Our estimate is that pre-industrial N fixation was 58 (range of 40–100) Tg N fixed yr⁻¹; adding conservative assumptions for geological N reduces our best estimate to 44 Tg N yr⁻¹. This approach yields substantially lower estimates than most recent calculations; it suggests that the magnitude of human alternation of the N cycle is substantially larger than has been assumed.     

模拟增温对青藏高原东部高寒灌丛土壤氮转化的影响

本文研究了青藏高原东部窄叶鲜卑花高寒灌丛生长季前期、生长季后期和非生长季3个生育期的土壤氮转化速率对模拟增温的响应,分析全球气候变暖对高寒灌丛土壤氮循环过程的影响.结果 表明:模拟增温使高寒灌丛土壤温度显著升高1.2℃,土壤水分显著降低2.5％.高寒灌丛生长季土壤净氮矿化(氨化和硝化)速率显著高于非生长季,但土壤净氮固...     

一株海水异养硝化-好氧反硝化菌系统发育及脱氮特性

【目的】确定一株分离自海水的异养硝化-好氧反硝化菌的系统发育地位并探索其脱氮特性和机理,以期为解释异养硝化-好氧反硝化机理以及改进海水养殖及废水的生物脱氮工艺提供理论依据。【方法】通过形态观察、生理生化实验和16S rRNA基因序列分析,鉴定该菌株;通过测定菌株在不同无机氮源降解测试液中的生长和脱氮效率,分析其异养硝化和好氧反硝化性能。【结果】经鉴定该菌株属于盐单胞菌属(Halomonas);最适生长条件为盐度3%、pH 8.5、温度28℃、碳氮比10:1,在盐度为15%的培养液中仍能生长;可以同时去除氨氮、亚硝酸氮和硝酸氮,24 h时对NH4+-N、NO2--N、和NO3--N的去除率可分别达到98.29%、99.07%、96.48%,3种形态无机氮同时存在时,会优先利用NH4+-N,且总无机氮去除率较单一存在时更高,说明该菌株可实现同步硝化反硝化。【结论】该分离自海水的异养硝化-好氧反硝化菌属于盐单胞菌属(Halomonas),在高盐环境中仍能生长,同时具有高效的异养硝化和好氧反硝化能力,能够独立完成脱氮的全部过程。     

滨海湿地生态系统微生物驱动的氮循环研究进展

滨海湿地生态系统介于陆地生态系统和海洋生态系统之间,其类型多种多样,环境差异极大,微生物种类丰富。近年来,随着人为氮源的大量输入,造成滨海湿地生态系统富营养化污染问题日趋严重。本文主要总结了滨海湿地生态系统微生物驱动的固氮、硝化、反硝化、厌氧氨氧化、NO_3~-还原成铵等主要氮循环过程,并综述了通过功能基因(如nifH、amoA、hzo、nirS、nirK、nrfA)检测微生物群落多样性及其环境影响因素的相关研究,旨在更好理解微生物驱动氮循环过程以去除氮,以期为减轻富营养化和危害性藻类爆发提供科学依据。     

Nitrogen cycling in lake sediments bioturbated by Chironomus plumosus larvae, under different degrees of oxygenation

Sediment cores containing different densities of Chironomus plumosus, ranging from 0 to 12 000 ind. m^–2, were incubated in the laboratory, with 100 and 39% O₂ saturation in the overlying water. Rates of O₂ uptake, and fluxes of the various inorganic N species were measured after addition of ¹⁵NO _inf3 ^su– to the overlying water. The animals enhanced O₂ and NO _inf3 ^su– uptake, due to irrigation. Denitrification of NO _inf3 ^su– coming from the overlying water (Dw) and dissimilatory NO _inf3 ^su– reduction to NH _inf4 ^sup+ (DNRA) represented 20–30 and 4–10% of the NO _inf3 ^su– uptake, respectively. Only 20–40% of the measured NH _inf4 ^sup+ effluxes corresponded to DNRA, the rest was probably due to animal excretion. Nitrite production, mostly from dissimilatory NO _inf3 ^sup– reduction, was detected at both 39 and 100% oxygen saturation. Higher rates of NO _inf2 ^su– production at the lower oxygen concentrations, were probably due to a thinner oxic layer, compared to fully oxygenated waters. The presence of Chironomus plumosus increased nitrification rates, relative to non-inhabited microcosms. However, nitrification rates were low compared to Dw, probably due to low numbers of nitrifiers in the sediment. At 39% oxygen saturation, rates of nitrification and denitrification of NO _inf3 ^su– generated within the sediment were not measurable.     

Diurnal variation of rates of denitrification and nitrogen fixation of periphyton associated with Oryza glumaepatula Steud in an Amazonian Lake

The rates of denitrification and biological nitrogen fixation of the periphyton communities associated with the culms and adventitious root of Oryza glumaepatula in Lake Batata, State of Pará, Brazilian Amazonia, were investigated over the course of 24 h. N₂O was not detected during the period, demonstrating that denitrification was not occurring. The low concentration of nitrate in the water column was indicated as the main factor limiting the denitrification process. The rates of biological nitrogen fixation (BNF) in culms were lowest at night and early morning, while the highest values were measured at 1200 h. BNF rates in periphyton associated with adventitious roots were lowest during the morning, while highest values were measured at 1600 h. The difference in the daily patterns of BNF rates in the periphyton of culms and roots of O. glumaepatula in the euphotic zone was attributed to defferences in the availability of organic carbon which supports this process. In the periphyton of the culms, the BNF process was carried out by heterocystous cyanobacteria, which was photoautotrophs. In the periphyton of the adventitious roots, BNF was carried out by periphytic bacteria, and is heterotrophically mediated. This revised version was published online in July 2006 with corrections to the Cover Date.