一株甲烷利用菌的分离及其在甲烷气体测定中的应用

从山西太原晋阳湖水样中分离得到一株能以甲烷为唯一碳源生长的菌株ME16.气相色谱分析表明ME16菌株能利用甲烷.ME16菌株的16S rDNA 序列与铜绿假单胞菌(Pseudomonasaeruginosa,ATCC 10145,AF094713)相似性为99%.该菌株最适培养条件为30℃、2%接种量、25%甲烷含量和培养基pH为6.0.用电化学法研究了ME16固定化细胞体系中不同含量甲烷对溶氧的响应时间以及溶氧变化与甲烷含量的关系.结果表明,加入固定化细胞后.溶氧变化在100s内达到平衡,溶氧消耗量与通入甲烷气体含量在0～16%呈线性关系,相关系数为0.9954.对样品气体8次测量,RSD为3.34%,表明该反应体系重现性良好,为该菌株进一步研究甲烷传感器奠定基础.     

甲烷利用菌培养条件的优化及其初步应用

利用统计学实验设计（RSM）对能够利用甲烷的假单胞菌菌株ME16主要培养条件进行了优化。以液体无机盐和甲烷气体作为培养基分别进行了温度、接种量、甲烷含量和培养pH对细菌生长影响的研究,并在此基础上,利用响应面法分析优化了ME16菌株的主要培养条件,得到最佳培养条件为：温度29.4℃,接种量1.8%,甲烷含量25%。采用优化培养条件进行培养,细菌生物量增大0.8倍,达到稳定期的培养时间缩短了50h。该菌株初步应用于甲烷气体的脱除,脱除率达65.7 %,表明该菌株能良好的脱除空气中甲烷。     

一株甲醇利用菌的分离及其在甲醇测定中的应用

【目的】筛选能够利用甲醇的微生物菌株,并将其应用于甲醇测定的初步研究中。【方法】采用富集培养及固体平板分离法分离菌株;通过生理生化特征及16S rDNA序列分析进行菌株鉴定;以固定化细胞和溶氧仪组合成测定系统,测定了不同含量甲醇的响应时间以及溶氧变化与甲醇含量的关系。【结果】从山西清徐农用沼气池中分离得到一株能以甲醇为唯一碳源和能源生长的菌株M211,通过生理生化特征及16SrDNA序列分析,该菌株被鉴定为嗜有机甲基杆菌(Methylobacterium organophilium)。传感系统在0.02%-1%(V/V)甲醇含量范围内测定,响应时间小于20 min,检出限为0.27 mg/L,溶氧消耗量同甲醇含量呈线性关系,拟合系数(R2)为0.9986。该测定体系不易受其它干扰物质影响,检测结果与实际样品浓度一致。【结论】该测定体系具有较强的选择性,及良好的重现性和稳定性,具有较好的应用前景。     

一个甲烷氧化菌株的分离、鉴定及其特性研究

实验室自行设计方案分离多株以甲烷为唯一碳源的菌株, 对其中的1株QJ16进行了研究, 根据该菌株形态特征与16S rDNA序列的同源性分析, 证实该菌株是一个与其最近的甲基单胞菌属各成员都不相同的菌株。对该菌株的培养条件和利用甲烷的特性进行研究结果表明, 氮源以氯化铵和硝酸钾共同作用最好, 碳源以甲烷最佳, 最佳生长温度为30℃, 最佳生长pH为6~7; 在批式实验时菌株利用甲烷的最适pH为6.5左右, 微量元素Cu2+的浓度为15 mmol/ L。     

含有甲烷氧化菌的混合菌群特性研究

为获得高效甲烷氧化微生物体系,从农业土壤中采样,以甲烷作为唯一碳源进行好氧选择性传代培养,得到生长性能稳定、生长优于Methylosinus trichosporium OB3b纯培养的具有甲烷单加氧酶(Methane Monooxygenase,MMO)活性甲烷氧化混合菌。利用MMO的共代谢特性,分别以苯酚和环氧丙烷作为目标对象,考察该混合菌对有机污染物的降解及用于生产有用化学物质的催化特性。结果表明,所得混合菌具有高效降解苯酚能力,对初始浓度为600mg/L的苯酚,经过11h培养,苯酚降解率可达99%。另外,以该混合菌为催化剂可以实现丙烯氧化生产环氧丙烷。通过降低磷酸盐浓度可以有效提高环氧丙烷的积累浓度,最大可至5mmol/L。此外,采用纯种分离方法结合PCR扩增、16SrRNA和MMO功能基因分析技术对混合菌群结构进行解析。结果表明,该混合菌群由Ⅱ型甲烷氧化菌及其它至少4种非甲烷氧化菌组成,它们分别属于Methylosinus trichosporium和Acinetobacter junii、Cupriavidusme tallidurans、Comamonas testosteroni和Stenotrophomonas maltophilia。采用PCR方法从混合菌及纯化菌株M.trichosporiums Y9总DNA中都能扩增得到mmoB、mmoX和pmoA基因片段,表明该甲烷氧化菌同时具有sMMO和pMMO两种形式的MMO。通过对从甲烷氧化混合菌中分离纯化得到的甲烷氧化菌进行PCR产物测序,结果发现其与Methylosinus trichosporium的同源性为99.9%。     

甲烷氧化菌吸附膜反应器中环氧丙烷的连续生物转化

以流化床作为固定化体系 ,在硅藻土颗粒表面构建了混合培养的甲烷氧化细菌的吸附膜。研究发现延迟期后固定化细胞的甲烷单加氧酶活性明显增加。流化床中 90 %以上的甲烷氧化细菌以吸附形式存在。吸附膜浓度为 3.3～3.7 mgdryweightcell gDS。通过批式反应考察了丙烯 甲烷共氧化过程合成环氧丙烷的可能性。研究了甲烷对丙烯环氧化以及丙烯对甲烷氧化细菌生长的影响。通过最佳配比的混合反应气体 (methane :35 % ;propene :20% ;oxygen :45 % )连续循环通入流化床反应器中抽提产物环氧丙烷 ,克服了产物抑制。该生物反应器最初产生环氧丙烷的日产量为 110～ 150μmol d ,连续操作25d ,未观察到环氧丙烷生产能力的明显减小.     

一株甲烷利用菌的分离、鉴定和性能研究

目的：研究土壤中能利用甲烷的细菌类型及特性。方法：运用传统的富集、分离、纯化方法得到1株甲烷利用菌,结果：该菌株在显微镜下呈球形,在液体培养基中生长72h后OD值可达到0.8左右,其最适生长温度30℃,最佳pH值7左右。对该菌株进行了16SrDNA扩增,测序结果表明其与Pseudoxanthomonas菌属的序列相似性为93%,其生理生化特征和分子鉴定结果表明,该菌与假黄单胞菌为不同的属。甲烷消耗气相色谱分析结论显示,120h后培养瓶中的甲烷浓度降低60%左右,说明该菌株具有较好的利用甲烷的性能。     

甲烷利用细菌降解三氯乙烯的研究

GYJ3菌株细胞微细结构的电镜观察结果表明：它具有Ⅱ型甲烷利用细菌的特征,应归属于Ⅱ型菌。考察了Cu2+浓度、培养气相中甲烷浓度对菌株细胞中甲烷单加氧酶（EC1．14．13．25,简称MMO）活性的影响。结果表明,培养液中Cu2+浓度为1．5μmol／L,培养气相中甲烷：空气比为2∶1时,可溶性甲烷单加氧酶占细胞中MMO总量的95％。研究了GYJ3菌株细胞悬浮液降解三氯乙烯过程。实验结果表明,GYJ3菌株能够降解不同浓度的三氯乙烯,较高浓度的三氯乙烯对降解反应没有明最的抑制作用。加入甲酸盐作为电子给体能够提高三氯乙烯降解反应速率。实验中观察到GYJ3菌株降解三氯乙烯过程中反应速率随着反应的进行而下降,在三氯乙烯降解过程中三氯乙烯氧化产物是导致细胞失活的主要原因。实验室中测定了GYJ3菌株单位重量细胞降解三氯乙烯极限量,它可作为评价细菌降解三氯乙烯能力的重要指标。     

一株甲烷氧化菌的分离鉴定与特性

甲烷氧化菌是一类能以甲烷作为唯一碳源和能源进行同化和异化代谢的微生物。从若尔盖高原不同地点采集的样品中筛选得到一株名为XN1的甲烷氧化菌,根据此菌株的形态与16SrRNA序列同源性分析,证实该菌株属于Methylomonas属。对该菌株的培养条件进行研究的结果表明,以甲烷与甲醇共同作为碳源,硝酸钾和氯化铵共同为氮源时菌生长最好,最适生长温度为25℃,最适生长pH为6.5,培养基中CuSO4·5H2O和FeSO4·7H2O的浓度以0.03mg/L和0.4mg/L为宜。     

巴氏甲烷八叠球菌BTC菌株的鉴定

本文报告了巴氏甲烷八叠妹菌BTC菌株的鉴定结果。该菌株在生活周期内均呈大小不等的团块聚集,8个不规则的球形细胞聚集在一起是团块构成的基本单位,未见单细胞阶段。在紫外线照射下,菌落荧光为蓝绿色,菌体荧光为蓝白色,活细胞或干制标本均可发出荧光。在以甲醇为生长基质时,其倍增时间为9．85h。可以利用甲醇,乙酸钠、三甲胺及H2／CO：为碳源;不能利用甲酸、乙醇、丙醇和丁醇等。最适生长pH为7．0。DNA的G+c mol％含量为41.5％。该菌株与巴氏甲烷八叠球菌近似或相同,而与马氏甲烷八叠球菌不同。其倍增时间较巴氏甲烷八叠球菌227菌株短,DNA中G+C mol％含量也与巳报道过的各菌株有 所差别,所以定名为巴氏甲烷八叠球曲BTC菌株(Methanosarcina barketi BTC)。     

Isolation of Methylococcus Strain Resistant to Abnormal Climate Change to Reduce Methane Emissions from the Iranian Salt Lake

Abstract

An increase in the atmospheric concentration of methane greenhouse gas results in an increase in global warming, surface water evaporation, and amount of the solutes in relevant areas besides, it also causes climate change. In these situations, methanotrophs that are resistant to climate change and deserted conditions could be applied. Methylococcus, as one of the most extensively studied methanotrophs is highly resistant to salinity, a strain of which was isolated in this study from Hoz-e Soltan Salt Lake in Iran as an example influenced by climate change. Isolated strain was identified. To determine the ability of the bacteria for decrease of methane gas, the culture medium was analyzed by gas chromatography. Results showed that isolated strain is able to grow in salt proportion of 3.3% and acidic pH of 3.5 in vitro, reducing more than 75% of total methane gas within 10?days. In addition to nitrogen fixation ability of the strain, positive results obtained regarding drought tolerance and heat shock in this study confirmed that Methylococcus strains may be able to withstand environmental conditions of foreseeable future. Thus, to prevent methane emission in regions such as Hoz-e Soltan Salt Lake in Iran, more compatible methanotroph strains need to be identified and used.     

Methane dosage to soil and its effect on plant growth

Two protocols for following soil methane enrichment were used, one with methane dosed as a carbon source ([C]-soil) and one with methane plus minerals ([C+M]-soil). Methane oxidation occurred much faster in soil receiving minerals in addition to methane than in the control soil receiving only methane. In both treatments, only a small fraction of methane (2% to 14%) was converted into microbial biomass C. Nevertheless, a strong increase in soil microbial biomass (up to 1.5 to 2.0-fold) was achieved in the [C+M]-soil in a 3-week period. Due to methane application, the NO₃ ^- content of the soil was significantly decreased, by 83% to 90% in the [C]-soil and by 56% to 83% in the [C+M]-soil. Soil enzymatic activities were slightly increased in the [C+M]-soil only. The soil-methane incubation did not alter the composition of the monitored microbial populations in the soil or in rhizosphere of plants. In the [C]-soil, methane incubation resulted in reduction of the shoot dry wt of maize by 8% to 12%. In the [C+M]-soil under non-limiting mineral-nutrient status, a significant increase in shoot dry wt was observed for maize (13%), a neutral effect was registered for spinach and a negative effect was observed for wheat.     

中国陆地自然植物有氧甲烷排放空间分布模拟及其气候效应

区域尺度陆地植物有氧条件下排放甲烷及其气候效应研究不仅对甲烷收支平衡研究具有重要意义,对于全球变化研究也具有重要推动作用。通过改进Keppler提出的公式,模拟了中国区域植物有氧甲烷排放的时空分布。利用IBIS模拟的NPP数据结合相关文献统计生物量与NPP的比值,计算得到中国区域自然植物叶片生物量,以及叶片甲烷排放。结果显示,2001年至2012年中国植物生物量与植物叶片甲烷排放量在Sres A2和Sres B1两种情景下差异不明显;但是气候变化模式差异的影响会随着时间的推移而扩大。在Sres A2情景下,中国地区年均植物生物量为10803.22Tg C,叶片生物量为1156.15Tg C。如果不考虑天气对光照的影响,植物叶片甲烷排放年均2.69Tg,约是全国年甲烷排放总量7.01%,是中国稻田甲烷排放总量的29.05%。在各植被类型中,草地叶片甲烷排放量最高,达到47.53%,其次是混交林。森林(针叶林、阔叶林、混交林)是主要的植物甲烷排放源,占中国区域植物甲烷排放总量的51.28%,其次是草地,占47.47%。中国区域植物叶片甲烷排放南高北低,东高西低的分布状态主要由地表植被覆盖类型决定,光照和温度也是重要影响因素。对Sres A2和Sres B1两种气候情景下中国植物甲烷排放预测分析,中国区域植物甲烷排放不断增加,在Sres A2情景下不同时期的平均增长率为9.73%,高于Sres B1情景的5.17%,且两种情景下的增长率都在降低。21世纪Sres A2和Sres B1变化情景下,年均植物排放的甲烷CO_2当量分别为83.18Tg和77.34Tg,约占中国年均CO_2排放总量的1.39%和1.29%。     

Biogeochemistry of methane and methanogenic archaea in permafrost

This study summarizes the findings of our research on the genesis of methane, its content and distribution in permafrost horizons of different age and origin. Supported by reliable data from a broad geographical sweep, these findings confirm the presence of methane in permanently frozen fine-grained sediments. In contrast to the omnipresence of carbon dioxide in permafrost, methane-containing horizons (up to 40.0 mL kg(-1)) alternate with strata free of methane. Discrete methane-containing horizons representing over tens of thousands of years are indicative of the absence of methane diffusion through the frozen layers. Along with the isotopic composition of CH(4) carbon (delta(13)C -64 per thousand to -99 per thousand), this confirms its biological origin and points to in situ formation of this biogenic gas. Using (14)C-labeled substrates, the possibility of methane formation within permafrost was experimentally shown, as confirmed by delta(13)C values. Extremely low values (near -99 per thousand) indicate that the process of CH(4) formation is accompanied by the substantial fractionation of carbon isotopes. For the first time, cultures of methane-forming archaea, Methanosarcina mazei strain JL01 VKM B-2370, Methanobacterium sp. strain M2 VKM B-2371 and Methanobacterium sp. strain MK4 VKM B-2440 from permafrost, were isolated and described.     

Mass spectrometric measurements of methane and oxygen utilization by methanotrophic bacteria

Abstract A mass spectrometer with membrane inlet was used to measure methane and oxygen utilization rates at various methane concentrations in Methylosinus trichosporium and a locally isolated strain of a methane-oxidizing coccus (OU-4-1). The apparent K _m for methane was found to be 2 μM for M. trichosporium and 0.8 μM for strain OU-4-1. These K _m-values are 10–30 times lower than most previously reported values. The ratio of oxygen to methane utilization rates was 1.7 for M. trichosporium and 1.5 for strain OU-4-1 corresponding to a growth yield of 0.38 and 0.63 g dry weight/g methane, respectively.     

Optimization of solubilization and purification procedures for the hydroxylase component of membrane-bound methane monooxygenase from Methylococcus capsulatus strain M

The hydroxylase component of membrane-bound (particulate) methane monooxygenase (pMMO) from Methylococcus capsulatus strain M was isolated and purified to homogeneity. The pMMO molecule comprises three subunits of molecular masses 47, 26, and 23 kD and contains three copper atoms and one iron atom. In solution the protein exists as a stable oligomer of 660 kD with possible subunit composition (alpha beta gamma)6. Mass spectroscopy shows high homology of the purified protein with methane monooxygenase from Methylococcus capsulatus strain Bath. Pilot screening of crystallization conditions has been carried out.     

甲基磺酸乙酯诱变选育竹红菌甲素高产菌株

以从短穗竹(Brachystachyum densiflorum)茎秆中分离获得的竹黄菌(Shiraia sp.S8)菌株为出发菌株,以0.5%~2.5%甲基磺酸乙酯(EMS)处理竹黄菌悬浮孢子10~30 min,结合平板初筛和高效液相色谱(HPLC)分析进行复筛。经诱变筛选得到高产菌株10-5,发现其竹红菌甲素产量达到26.8 mg/L,与原始出发菌株相比提高了46.4%,且遗传稳定性良好,具有较高的医药及工业应用价值。     

Characterization of a strain of Methanospirillum hungatti.

The results of morphological, base ratio, nutritional, temperature, and pH studies on a strain of Methanospirillum hungatii, isolated from an anaerobic pear waste digester, are described. The isolate, designated as strain GP 1, was compared with some of the characteristics of type-strain M. hungatii JF 1. Strain GP 1 is Gram-negative, weakly motile, and a strict anaerobe with a guanine plus cytosine (G +C) content of 46.5 mol%. The preferred substrates for methane production are hydrogen, carbon dioxide, and formate. Acetate is used under certain conditions but its specific contribution to cell carbon and (or) methane formation was not established. The optimum temperature for both growth and methane production is 35 degrees C, but growth and methane production occur over the range 25-45 degrees C. Methane production is optimal at pH 7.0.