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1.
乙炔抑制法在硝化与反硝化过程中的应用   总被引:4,自引:0,他引:4  
硝化和反硝化作用在土壤氮素循环中扮演重要作用,由于硝化和反硝化作用一方面能够导致土壤中氮素的损失,另一方面能够产生温室气体-N2O,所以硝化和反硝化作用的研究备受关注.乙炔抑制法能同时测定硝化和反硝化作用,在硝化和反硝化作用中有着重要的应用.该文主要论述了乙炔抑制法的研究进展;以及对应用乙炔气体时存在的一些问题进行了综述.  相似文献   

2.
覆盖措施对雷竹林地土壤硝化和反硝化作用的影响   总被引:1,自引:0,他引:1       下载免费PDF全文
为探讨林地覆盖对雷竹林土壤硝化和反硝化作用的影响,以不覆盖雷竹林为对照,测定了林地覆盖期间(覆盖后30、60、90 d)雷竹林土壤基本理化性质,并用气压分离过程技术(Ba PS)测定了土壤硝化速率和反硝化速率。结果表明:覆盖措施和覆盖时间对雷竹林土壤硝化和反硝化作用均有显著影响,而且两者存在明显的交互作用;覆盖能促进雷竹林土壤反硝化作用,但长时间覆盖会抑制雷竹林土壤硝化作用;覆盖总体上会降低雷竹林土壤硝化速率、反硝化速率与土壤理化性质的相关性程度,并使土壤硝化和反硝化作用的主要环境影响因子趋于多样化和复杂化;覆盖雷竹林土壤硝化速率的主要环境影响因子是土壤含水量、p H值、铵态氮含量和总孔隙度,反硝化速率的主要环境影响因子是土壤p H值、含水量和总孔隙度。林地覆盖会显著影响雷竹林土壤的氮循环过程,可能会增加土壤氮素损失。  相似文献   

3.
土壤释放的 N_2O 的原位测定   总被引:4,自引:0,他引:4  
N_2O 是大气成分之一,它由微生物的硝化-反硝化作用、燃烧和大气闪电等过程产生,其中土壤微生物反硝化作用是最主要的来源。土壤微生物反硝化作用产生N_2O,不仅导致土壤中肥料氮素的损失,而且由于其“温室效应”和对臭氧层的破坏,受到国内外研究者  相似文献   

4.
土壤氮素转化的关键微生物过程及机制   总被引:47,自引:0,他引:47       下载免费PDF全文
微生物是驱动土壤元素生物地球化学循环的引擎.氮循环是土壤生态系统元素循环的核心之一,其四个主要过程,即生物固氮作用、氨化作用、硝化作用、反硝化作用,均由微生物所驱动.近10年来,随着免培养的分子生态学技术和高通量测序技术等的发展,在硝化微生物多样性及其作用机理、厌氧氨氧化过程和机理等研究方面取得了突破性进展.本文重点阐述了我国有关土壤硝化微生物方面的研究进展,在此基础上,简要介绍了反硝化微生物和厌氧氨氧化及硝酸盐异化还原成铵作用的研究进展,并对今后的研究工作提出了展望.今后土壤氮素转化微生物生态学的研究,应瞄准国际微生生态学发展的前沿,加强新技术新方法的应用,结合我国农业可持续发展、资源环境保护和全球变化研究的重大需求,重点开展以下几方面的工作:(1)开展大尺度上土壤硝化作用及氨氧化微生物分布的时空演变特征及驱动因子的研究;(2)加强氮素转化关键微生物过程与机理的研究,并与相关过程的通量(如氨挥发、N2O释放)和反应速率(如矿化速率、硝化速率)关联起来;(3)在特定生态系统中系统研究各个氮转化过程的耦合关系,构建相关氮素转化和氮素平衡模型,为定向调控土壤氮素转化过程,提高氮素利用效率并减少其负面效应提供科学依据.  相似文献   

5.
好氧反硝化菌的研究进展   总被引:17,自引:2,他引:15  
综述了好氧反硝化菌的种类和特性、好氧反硝化菌的反硝化作用机制和影响因素.好氧反硝化菌主要包括假单胞菌属(Pseudomonas)、产碱杆菌属(Alcaligenes)、副球菌属(Para-coccus)和芽孢杆菌属(Bacillus)等,属好氧或兼性好氧异养微生物.好氧反硝化菌能在好氧条件下进行反硝化,其主要产物是N2O,并可将铵态氮直接转化成气态产物.催化好氧反硝化菌反硝化作用的硝酸盐还原酶是周质酶而不是膜结合酶.溶解氧和C/N往往是影响好氧反硝化菌反硝化作用的主要因素.介绍了间歇曝气法、选择性培养基法等好氧反硝化菌的主要分离筛选方法.概述了好氧反硝化菌在水产养殖、废水生物处理、降解有机污染物以及对土壤氮素损失的影响方面的研究进展.  相似文献   

6.
森林土壤氮素转换及其对氮沉降的响应   总被引:45,自引:5,他引:40  
近几十年人类活动向大气中排放的含氮化合物激增 ,并引起大气氮沉降也成比例增加。目前 ,氮沉降的增加使一些森林生态系统结构和功能发生改变 ,甚至衰退。近 2 0 a欧洲和北美有关氮沉降及其对森林生态系统的影响方面的研究较多 ,而我国少有涉及。森林土壤氮素转换是森林生态系统氮素循环的一个重要的组成部分 ,而矿化、硝化和反硝化作用是其核心过程 ,氮沉降作为驱动因子势必改变森林土壤氮素转换速度、方向和通量。根据国外近 2 0 a有关研究 ,首先介绍了森林土壤氮素转换过程和强度 ,论述森林土壤氮素在生态系统氮素循环中的作用 ,然后在此基础上 ,介绍了氮沉降对森林土壤氮素循环的研究途径 ,探讨了氮沉降对森林土壤氮素矿化、硝化和反硝化作用的影响及其机理  相似文献   

7.
采用有机肥替代部分化肥是实现化肥使用零增长和作物稳产增产的重要途径。基于近年来的研究进展,探讨了稻作系统有机肥替代部分化肥对水稻产量、氮素利用效率、土壤氮库组分和微生物固氮、氨化、硝化和反硝化等氮循环关键过程的影响。同时,就单施化肥与有机肥替代部分化肥的氮素循环特征进行了比较。有机肥替代部分化肥通过改变稻田土壤氮素循环多个环节(增强氨化过程、协调硝化和反硝化过程、降低氨挥发和减少氮素损失等),改善土壤氮素供给状态(提高小分子有机氮供给、协调无机氮组分与比例、提高土壤微生物量氮和总氮固持),进而促进水稻氮素吸收并协调植株氮素分配过程,最终实现水稻稳产增产。  相似文献   

8.
湖泊氮素氧化及脱氮过程研究进展   总被引:7,自引:0,他引:7  
范俊楠  赵建伟  朱端卫 《生态学报》2012,32(15):4924-4931
自然界中氮的生物地球化学循环主要由微生物驱动,由固氮作用、硝化作用、反硝化作用和氨化作用来完成。过去数十年间,随着异养硝化、厌氧氨氧化和古菌氨氧化作用的发现,人们对环境中氮素循环认识逐步深入,提出了多种脱氮途径新假说。对湖泊生态系统中氮素的输入、输出及其在水体、沉积物和水土界面的迁移转化过程进行了概括,对湖泊生态系统中反硝化和厌氧氨氧化脱氮机理及脱氮效率的最新研究进展进行了探讨,并对以后的氮素循环研究进行了展望。  相似文献   

9.
反硝化作用是水生态系统脱氮和控制水体富营养化的重要过程, 是氮循环的关键环节。该作用对去除陆地和水生生态系统中的硝酸盐、亚硝酸盐并将其以无反应氮气的形式重新输送到大气这一过程起着至关重要的作用。文章综述了土壤反硝化过程的关键微生物及其作用机制、土壤反硝化作用的主要影响因素及其作用规律以及反硝化作用的研究方法方面的研究进展, 并对今后的发展方向进行了展望。指出今后应进一步将分子生态学技术手段综合运用于土壤反硝化作用研究, 加强反硝化功能微生物种群结构的研究, 深入了解反硝化菌群结构及其种间的协同作用规律与机制, 进一步明确反硝化的微观作用机制与反应机理, 并结合景观生态因子建立氮循环生物地球化学模型, 剖析多尺度因素对反硝化作用的影响及其调控机制, 此外, 还应加强土壤反硝化研究新方法的开发与现有技术的改进, 逐步建立土壤反硝化强度测定的标准方法体系。  相似文献   

10.
溶解氧(dissolved oxygen,DO)在稻田氮素循环和水稻生长发育中发挥了重要作用,深入研究溶解氧对稻田氮素转化和水稻氮代谢的影响,对减少稻田氮素流失和提高水稻氮素利用具有重要意义。近年来,研究已阐明了溶解氧对土壤固氮作用、氨化作用、硝化作用和反硝化作用等生物化学过程以及土壤微生物多样性的影响;大量研究也表明,溶解氧在水稻氮素吸收与利用中起到了关键作用。本文系统介绍了溶解氧浓度对微生物群落结构和活性的影响及其与稻田不同形态氮素间转化的关系,综述了水稻根系生长特性、氮素吸收和同化及相关氨基酸代谢对溶解氧浓度响应机理的最新研究进展,并针对现阶段稻田氧营养研究提出了水稻生产中存在的问题及研究展望。  相似文献   

11.
The stoichiometric equations of ammonification, nitrification and denitrification have demonstrated that the nitrogen cycle in nature is rather complicated. The mechanisms of biological nitrogen transformations are very important for analysis, design, operation and optimal control of natural ecosystems or engineered systems for nitrogen removal, and accurate stoichiometric equations can help in the maintenance of these environments. In this study, the new stoichiometric equations of intermediate nitrification, and heterotrophic and autotrophic denitrification with sulfur as the electron donor have been developed and discussed. The parameter values of f(s) (the fraction of electron donor coupled to cell synthesis) in stoichiometric equations of nitrification and denitrification are calculated according to experimental results implied in previously reported stoichiometric equations. Some new stoichiometric relationships of nitrification and denitrification, such as the O(2) demand for nitrifications, chemical oxygen demand/N ratios and the yield coefficients for denitrifications have been established. The pathway steps of nitrification and denitrification have been discussed.  相似文献   

12.
 采用气压过程分离(Barometric process separation, BaPS)技术对川西亚高山针叶林不同恢复 阶段土壤的总硝化和反硝化作用速率进行了测定,结果表明:川西亚高山针叶林不同恢复阶段土壤的总硝化和反硝化速率差异不显著(p<0.05),不同恢复阶段土壤总硝化作用的 Q10值 差异不显著(p<0.05);总硝化作用速率与土壤含水量呈显著正相关(p<0.05),与土 壤pH值、 土壤有机质、全氮及C/N相关不显著;不同恢复阶段土壤反硝化速率均维持在一个较低的水 平,反硝化速率与土壤中的C/N显著正相关(p<0.05),与土壤含水量、pH值、有机质及全氮相关不显著。与反硝化作用相比,硝化作用对亚高山针叶林土壤氮损失的影响可能更大  相似文献   

13.
限氧自养硝化-反硝化生物脱氮新技术   总被引:10,自引:0,他引:10  
张丹  徐慧  李相力  张颖  陈冠雄 《应用生态学报》2003,14(12):2333-2336
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。  相似文献   

14.
Nitrification and denitrification processes are crucial to plant nutrient availability, eutrophication and greenhouse gas production both locally and globally. Unravelling the major environmental predictors for nitrification and denitrification is thus pivotal in order to understand and model environmental nitrogen (N) cycling. Here, we sampled five plant community types characteristic of interior Alaska, including black spruce, bog birch, tussock grass and two fens. We assessed abundance of functional genes affiliated with nitrification (bacterial and archaeal amoA) and denitrification (nirK/S and nosZ) using qPCR, soil characteristics, potential nitrification and denitrification rates (PNR and PDR) and gross mineralization rates. The main chemical and biological predictors for PNR and PDR were assigned through path analysis. The potential N cycling rates varied dramatically between sites, from some of the highest (in fens) to some of the lowest (in black spruce) measured globally. Based on path analysis, functional gene abundances were the most important variables to predict potential rates. PNR was best explained by bacterial amoA gene abundance followed by ammonium content, whereas PDR was best explained directly by nosZ gene abundance and indirectly by nirK/S gene abundance and nitrate. Hence, functional gene abundance is a valuable index that integrates recent environmental history and recent process activity, and therefore is a good predictor of potential rates. The results of this study contribute to our understanding of the relative importance of different biological and chemical factors in driving the potential for nitrification and denitrification across terrestrial ecosystems.  相似文献   

15.
The biological nitrification-denitrification process is used extensively for removal of ammonia nitrogen from wastewaters. Saves in aeration, organic matter (for denitrification) and surplus sludge are achievable if nitrite accumulation is possible in the nitrification step. In this paper, operational parameters were studied for each process for maximum nitrite accumulation in the nitrification step and nitrite adaptation in the denitrification step. Nitrite accumulation during nitrification can be controlled by the dissolved oxygen (DO) concentration, presenting a maximum of 65% at around 0.7 mg DO/L. Denitrification can be adapted to nitrite and the process is stable if nitrite in the reactor is keep low. The performance of a continuous stirred tank reactor (CSTR) and an up flow sludge blanket reactor (USB) were compared. Once the operational parameters were established, a CSTR for nitrification and an USB reactor for denitrification were operated in series for 25 days. The process was stable and a steady state was maintained for 20 days, and 93.5% of overall nitrogen removal was achieved in the nitrification-denitrification via the nitrite process.  相似文献   

16.
森林土壤氮素的转化与循环   总被引:24,自引:3,他引:21  
森林土壤氮素转化与循环在森林生态系统功能中占有极其重要的意义。本文综述了森林土壤氮素转化与循环的研究历程和现状 ;介绍了凋落物的归还、施肥、大气沉降、自生固氮、氨化、硝化、反硝化、植物吸收、NH3 的挥发、NO3 -淋溶等土壤氮素输入、转化和输出的途径和过程 ;最后从研究目标、研究方法、研究对象和研究内容 4个方面归纳了森林土壤氮素转化与循环的发展趋势。  相似文献   

17.
We discuss the mechanisms leading to nutrient limitation in tropical marine systems, with particular emphasis on nitrogen cycling in Caribbean ecosystems. We then explore how accelerated nutrient cycling from human activities is affecting these systems.Both nitrogen and phosphorus exert substantial influence on biological productivity and structure of tropical marine ecosystems. Offshore planktonic communities are largely nitrogen limited while nearshore ecosystems are largely phosphorus limited. For phosphorus, the ability of sediment to adsorb and store phosphorus is probably greater for tropical carbonate sediments than for most nearshore sediments in temperate coastal systems. However, the ability of tropical carbonate sediments to take up phosphorus can become saturated as phosphorus loading from human sources increases. The nature of the sediment, the mixing rate between nutrient-laden runoff waters and nutrient-poor oceanic waters and the degree of interaction of these water masses with the sediment will probably control the dynamics of this transition.Nearshore tropical marine ecosystems function differently from their temperate counterparts where coupled nitrification/denitrification serves as an important mechanism for nitrogen depuration. In contrast, nearshore tropical ecosystems are more susceptible to nitrogen loading as depurative capacity of the microbial communities is limited by the fragility of the nitrification link. At the same time, accumulation of organic matter in nearshore carbonate sediments appears to impair their capacity for phosphorus immobilization. In the absence of depurative mechanisms for either phosphorus or nitrogen, limitation for both these nutrients is alleviated and continued nutrient loading fuels the proliferation of nuisance algae.  相似文献   

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