异养硝化机理的研究进展

硝化作用是自然界氮素循环的一个重要环节。除了传统上的自养硝化细菌以外,至今为止已发现许多异养微生物可以进行硝化作用。异养硝化已成为环境领域的热点问题。简要的介绍了自然界中的异养硝化微生物的分布以及针对其生物多样性而建立的探测和分离方法。着重从异养硝化的关键酶,相关基因,电子传递及代谢途径这几个方面综述了异养硝化机理的研究进展。最后总结了目前在研究异养硝化机理过程中存在的问题,并对其今后进一步的研究方向做出了展望。     

Fluxes of nitrous oxide from boreal peatlands as affected by peatland type,water table level and nitrification capacity

Peat soils with high nitrogen content are potential sources of nitrous oxide (N₂O). Fluxes of nitrous oxide were measuredin situ on nine virgin and ten drained peatlands of different hydrology and nutrient status. Numbers of nitrifying bacteria were estimated in different layers of the peat profiles with a most-probable-number technique. Nitrification potentials were determined in soil slurries of pH 4 and 6 from the profiles of six peat soils. Many virgin peatlands showed low N₂O uptake. Lowering of the water table generally increased the average fluxes of N₂O from the soils, although more in minerotrophic (nutrient rich) than in ombrotrophic (nutrient poor) sites. Ammonium oxidizing bacteria were found on only two sites but nitrite oxidizers were detected in almost all peat profiles. More nitrite oxidizers were found in drained than in virgin peat profiles. Nitrification was enhanced after lowering of the water table in minerotrophic peat but not in ombrotrophic peat. The N₂O fluxes correlated positively with the numbers of nitrite oxidizers, nitrification potential, N, P and Ca content and pH of the soil and negatively with the level of water table (expressed as negative values) and K content of the soil.     

Biodeterioration of mineral materials by microorganisms—biogenic sulfuric and nitric acid corrosion of concrete and natural stone

In general, microorganisms such as chemolithotrophic and chemo‐organotrophic bacteria, cyanohacteria, algae, fungi, and lichens living on and in stone material may be of importance in biodeterioration. These groups contribute substantially to the deterioration of mineral materials such as natural stone, concrete, ceramics, and glass. The attack on mineral materials may be either strongly or mildly aggressive or both. A strongly aggressive attack is caused by biogenic mineral or organic acids. A mildly aggressive attack results from hydrophilic slimes such as heteropolysaccharides and/or proteins (biofilm) and their ability to accumulate water and salts. Attack by exoenzymes seems to be unimportant.

In recent years it has become possible to test the resistance of mineral materials to microbial attack by means of a biotest. Three simulation apparatuses were constructed; each allowed the incubation of test materials under microbiologically optimized conditions. Biodeterioration involving biogenic sulfuric acid corrosion, which under natural conditions needs eight times as long, was detectable within a few months. The results differed from those of purely chemical and/or physical tests of materials. Physical/chemical test methods are not sufficient to determine the resistance of materials to biological attack, because they do not include the interactions between microorganisms and their substrate, the mineral material. In the case of biogenic sulfuric acid corrosion, simulation experiments demonstrated differences in resistance of various concrete types, which ranged from I to 20% weight loss of test blocks within I year. With chemical testing only negligible differences in weight loss were noted. This was also the case with biogenic nitric acid corrosion. Thus, biotests assist in the selection of appropriate materials from many different ones.     

亚热带米槠天然林土壤氨氧化微生物对模拟氮沉降的响应

我国亚热带地区是全球氮沉降的热点区域。氮沉降会影响氨氧化微生物的丰度和群落结构,进而改变土壤微生物驱动的养分循环。目前对新近发现的完全氨氧化菌认识不足,极大地制约了对森林土壤氨氧化微生物响应氮沉降的整体认识。本研究以福建省三明市辛口镇格氏栲自然保护区长期模拟氮沉降处理土壤为研究对象,利用实时定量PCR方法,研究氨氧化微生物(包括氨氧化细菌AOB、氨氧化古菌AOA和完全氨氧化菌comammox Nitrospira),尤其是完全氨氧化菌的amoA基因丰度。模拟氮沉降处理包括:不添加N(CK)、低氮(添加40 kg N·hm^-2·a^-1,LN)和高氮(添加80 kg N·hm^-2·a^-1,HN)。结果表明: 8年的氮添加降低了土壤pH值和有机碳含量,提高了土壤硝态氮含量。供试土壤的AOB丰度低于检测限,无法获得目的片段。高氮处理显著提高了AOA丰度,但对完全氨氧化菌clade A和clade B丰度无显著影响。两种氮添加处理均降低了完全氨氧化菌/AOA值,表明氮添加降低了完全氨氧化菌在亚热带森林土壤氨氧化微生物类群中的相对竞争力。针对完全氨氧化菌clade A和clade B的扩增都存在非特异性产物,表明针对森林土壤的高特异性和覆盖度设计引物的必要性。Clade A和clade B丰度与总氮和铵态氮含量呈显著正相关,clade B丰度还与有机碳含量呈显著正相关。总之,模拟氮沉降提高了AOA在亚热带米槠天然林土壤硝化过程中的相对重要性,这些发现可为该地区应对全球变化和氮沉降的风险评估提供理论依据。     

稻田温室气体排放与土壤微生物菌群的多元回归分析

为揭示多种田间管理措施综合影响下双季稻田温室气体平均排放通量与土壤微生物菌群的多元回归关系,利用静态箱—气相色谱法和稀释培养计数法进行了温室气体排放通量和土壤产气微生物菌群数量的连续观测。两年研究结果显示,稻田甲烷排放通量与土壤微生物总活性和产甲烷菌数量关系密切,甲烷排放通量与二者的关系可分别由指数和二次多项式模型拟合。一元回归分析表明,仅产甲烷菌数量就能单独解释96.9%的稻田甲烷排放通量变异（R2=0.969,P<0.001）,但考虑两种因素以后的二元回归拟合优度高于一元回归（R2=0.975,P<0.001）。氧化亚氮排放通量与土壤硝化细菌和反硝化细菌数量也密切相关（P <0.05）,氧化亚氮排放通量与二者的二元非线性混合回归模型可以解释至少70.4%的稻田氧化亚氮排放通量（R2≥0.704, P <0.001）,其拟合优度也高于一元回归。稻田温室气体排放通量受多种影响因素控制,土壤产气微生物活性和数量是多种因素影响的直接响应,因此二者与温室气体排放存在显著相关,基于田间试验的多元非线性回归分析客观的揭示了温室气体排放通量与环境因子的相关关系。     

大气CO2浓度增高对麦田土壤硝化和反硝化细菌的影响

硝化和反硝化细菌是土壤中与氮转化有关的微生物菌群 ,大气CO2 浓度升高可能对它们的数量产生影响。位于中国无锡的稻 麦轮作农田生态系统FACE平台 2 0 0 1年 6月开始运行。本试验在 2 0 0 3年小麦生长季研究了土壤 (0～ 5cm和 5～ 10cm土层 )中硝化和反硝化细菌在大气CO2 浓度升高条件下的变化。试验采用最大可能法 (MPN)计这两种微生物菌群的数量。结果表明 ,0～ 5cm土层硝化菌数拔节期和成熟期FACE低于对照 ,而孕穗期FACE高于对照 ,5～ 10cm土层硝化菌数越冬期与成熟期FACE低于对照 ,大气CO2 浓度升高使得麦田土壤硝化细菌数目减少。 0～ 5cm土层各个生长期反硝化菌数FACE与对照均没有明显差异 ,5～ 10cm土层反硝化菌数拔节期FACE低于对照 ,大气CO2 浓度升高对麦田土壤反硝化菌的影响不大。     

饮用水系统硝化微生物分布规律、环境影响因素及调控应用的研究进展

硝化微生物广泛存在于饮用水系统中。水处理过程中,硝化微生物对含氮污染物的去除有突出贡献;而输配水过程中,硝化微生物会加剧消毒剂氯胺的降解,造成一系列饮用水微生物安全问题。本文介绍了常用硝化微生物检测方法,综述了硝化微生物在滤池、市政主管网、二次供水系统中的分布特征和规律,分析了环境因子及工程条件对硝化微生物的影响机制,探讨了硝化微生物强化应用及管控的实际工程措施,展望了未来饮用水系统中硝化微生物的研究重点与应用前景。     

The variability of nitrifying activity in field soils

The effect of pH on the activity of nitrifying organisms was examined in pasture soils ranging in pH from 4.9 to 7.3, using a short-term nitrification assay (SNA). The optimum pH for nitrifier activity (pH_opt) was generally close to the soil pH, suggesting that the indigenous nitrifier populations adjusted to the prevailing soil pH. A consequence was that the SNA at the soil pH (SNA_pH) bore a near 1:1 relationship with the SNA at the pH_opt (SNA_opt) over a wide range of SNA values. The effect of soil moisture tension on the SNA was less pronounced than that of pH, but an optimum occurred around pF 3.4.