植物在CH4产生、氧化和排放中的作用

综合评述了植物对CH4产生、内源CH4氧化和CH4排放的影响．不同植物释放根系分泌物能力的不同是造成CH4产生量差异的主要原因。而植物不同生育期分泌分泌物能力的差异是造成季节性变化的关键．植物泌O2能力的高低和季节性变化通过影响内源CH4的氧化来改变CH4的排放数量．植物问通气组织数量和密度的差异及其随生育期的变化,通过影响对CH4的传输能力来改变CH4的排放量．因此,植物排放CH4的通量及其季节性变化规律是由植物根系分泌分泌物能力、分泌O2能力和传输CH4能力综合决定的．     

Biomass measurement of methane forming bacteria in environmental samples

Methane-forming bacteria contain unusual phytanylglycerol ether phospholipids which can be extracted from the bacteria in sediments and assayed quantitatively by high performance liquid chromatography (HPLC). In this procedure the lipids were extracted, the phospholipids recovered, hydrolyzed, purified by thin layer chromatography, derivatized and assayed by HPLC. Ether lipids were recovered quantitatively from Methanobacterium thermoautotrophicum and sediments at levels as low as 8 × 10^?14 moles. In freshwater and marine sediments the flux of methane to the atmosphere and the methane levels in the pore water reflects the recovery of the phytanyl glycerol ether lipid ‘signature’. The proportion of the ether phospholipid to the total recoverable phospholipid was highest in anaerobic digester sewage sludge and deeper subsurface freshwater sediment horizons.     

Thermophilic methane production and oxidation in compost

Methane cycling within compost heaps has not yet been investigated in detail. We show that thermophilic methane oxidation occurred after a lag phase of up to one day in 4-week old, 8-week old and mature (>10-week old) compost material. The potential rate of methane oxidation was between 2.6 and 4.1 micromol CH4(gdw)(-1)h(-1). Profiles of methane concentrations within heaps of different ages indicated that 46-98% of the methane produced was oxidised by methanotrophic bacteria. The population size of thermophilic methanotrophs was estimated at 10(9) cells (gdw)(-1), based on methane oxidation rates. A methanotroph (strain KTM-1) was isolated from the highest positive step of a serial dilution series. This strain belonged to the genus Methylocaldum, which contains thermotolerant and thermophilic methanotrophs. The closest relative organism on the basis of 16S rRNA gene sequence identity was M. szegediense (>99%), a species originally isolated from hot springs. The temperature optimum (45-55 degrees C) for methane oxidation within the compost material was identical to that of strain KTM-1, suggesting that this strain was well adapted to the conditions in the compost material. The temperatures measured in the upper layer (0-40 cm) of the compost heaps were also in this range, so we assume that these organisms are capable of effectively reducing the potential methane emissions from compost.     

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.     

Factors affecting rumen methanogens and methane mitigation strategies

The rumen is a highly diverse ecosystem comprising different microbial groups including methanogens that consume a considerable part of the ruminant’s nutrient energy in methane production. The consequences of methanogenesis in the rumen may result in the low productivity and possibly will have a negative impact on the sustainability of the ruminant’s production. Since enteric fermentation emission is one of the major sources of methane and is influenced by a number of environmental factors, diet being the most significant one, a number of in vitro and in vivo trials have been conducted with different feed supplements (halogenated methane analogues, bacteriocins, propionate enhancers, acetogens, fats etc.) for mitigating methane emissions directly or indirectly, yet extensive research is required before reaching a realistic solution. Keeping this in view, the present article aimed to cover comprehensively the different aspects of rumen methanogenesis such as the phylogeny of methanogens, their microbial ecology, factors affecting methane emission, mitigation strategies and need for further study.     

Biogenesis of methane in primate dental plaque

Dental plaque samples collected from monkeys (Macaca mulatta) were found to contain a large amount of dissolved methane gas (0.6 nmol CH4/mg wet wt plaque). Enrichment cultures inoculated with dental plaque obtained from Macaca fascicularis produced methane when the medium contained ethanol, methanol, lactate, acetate or a hydrogen + CO2 atmosphere. Methane formation in the enrichments was inhibited by oxidation of the culture medium, autoclaving or the addition of 2-bromoethane sulfonic acid (BES). The methane producing enrichments were observed to contain fluorescent cocci occurring singly and in short chains. It was concluded that methane formation in the monkey dental plaque was the result of the presence of methanogenic bacteria.     

Molecular dynamics study of methane in water: diffusion and structure

In this study, theoretical analysis on the geometries and electronic properties of various conjugated oligomers based on thiophene (Th) or bicyclic non-classical Th units is reported. The dihedral angle, bond length, bond-length alternation, bond critical point (BCP) properties, nucleus-independent chemical shift (NICS) and Wiberg bond index (WBIs) are analysed and correlated with conduction properties. The changes of bond length, BCP properties, NICS and WBIs all show that the conjugational degree is increased systematically with main chain extension. As a result, the highest occupied molecular orbital–lowest unoccupied molecular orbital energy separation (E _g) is decreased upon chain elongation. The E _g of oligomers based on bicyclic non-classical Th unit is much lower than that of Th-based oligomers due to the narrower E _g of bicyclic non-classical Ths compared to Th, which indicates that the narrow E _g of the bicyclic non-classical Ths can be carried over to their polymers by using them as building blocks for the polymers. The band structures and density of states analysis show that the four polymers all have small band gap ( < 0.9 eV), wide highest occupied bandwidth and relatively small effective mass of hole, which indicate that those proposed polymers may be potential conductors.     

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。     

An influence of methane concentration on the methanotrophic activity of a model landfill cover

Evaluation of kinetic parameters of methane oxidation under various conditions, on the basis of an analysis of the literature and the authors’ own laboratory research, is presented. Variation in methanotrophic activity in the profile of a simulated landfill cover was observed. The greatest activity was found at a depth of 60 cm. A low affinity (1/K_M) and high potential activity (V_max) were observed. V_max values ranged from 0.11 × 10⁻³ to 0.86 × 10⁻³ units. The values of K_M ranged from 0.6 to 2.9% of CH₄ (v/v).     

Growth of methanotrophs in methane and oxygen counter gradients

Abstract A gel-stabilized system with counter gradients of CH₄ and O₂ was used to grow methanotrophs from wetland, agricultural and forest soils and lake sediment. Columns of semi-solid nitrate- or ammonium-minerai salts medium were continuously flushed at opposite ends with CH₄ and O₂ to create opposing concentration gradients of the two gases. Methanotrophs grew from all samples except forest soil, and were visible as thin bands after 5 to 15 days of incubation. The position of growth was CH₄ and O₂ concentration-dependent and occurred at the point of maximum possible CH₄ oxidation, where both substrates were completely consumed. Evidence was obtained for denitrification and nitrification activities concomitant with CH₄ oxidation. This approach may be useful to isolate methanotrophs with different CH₄ and O₂ requirements and to study their interactions with other groups of bacteria in nature.     

Predicting enteric methane emission in lactating Holsteins based on reference methane data collected by the GreenFeed system

Methane emission is not included in the current breeding goals for dairy cattle mainly due to the expense and difficulty in obtaining sufficient data to generate accurate estimates of the relevant traits. While several models have been developed to predict methane emission from milk spectra using reference methane data obtained by the respiration chamber, SF6 and sniffer methods, the prediction of methane emission from milk mid-infrared (MIR) spectra using reference methane data collected by the GreenFeed system has not yet been explored. Methane emission was monitored for 151 cows using the GreenFeed system. Prediction models were developed for daily and average (for the trial period of 12 or 14 days) methane production (g/d), yield (g/kg DM intake (DMI)) and intensity (g/kg of fat- and protein-corrected milk) using partial least squares regression. The predictions were evaluated in 100 repeated validation cycles, where animals were randomly partitioned into training (80%) and testing (20%) populations for each cycle. The best performing model was observed for average methane intensity using MIR, parity and DMI with validation coefficient of determination (R²_val) and RMSE of prediction of 0.66 and 4.7 g/kg of fat- and protein-corrected milk, respectively. The accuracy of the best models for average methane production and average methane yield were poor (R²_val = 0.28 and 0.12, respectively). A lower accuracy of prediction was observed for methane intensity and production (R²_val = 0.42 and 0.17) when daily records were used while prediction for methane yield was comparable to that for average methane yield (R²_val = 0.16). Our results suggest the potential to predict methane intensity with moderate accuracy. In this case, prediction models for average methane values were generally better than for daily measures when using the GreenFeed system to obtain reference methane emission measurements.     

Recent advances toward the bioconversion of methane and methanol in synthetic methylotrophs

Abundant natural gas reserves, along with increased biogas production, have prompted recent interest in harnessing methane as an industrial feedstock for the production of liquid fuels and chemicals. Methane can either be used directly for fermentation or first oxidized to methanol via biological or chemical means. Methanol is advantageous due to its liquid state under normal conditions. Methylotrophy, defined as the ability of microorganisms to utilize reduced one-carbon compounds like methane and methanol as sole carbon and energy sources for growth, is widespread in bacterial communities. However, native methylotrophs lack the extensive and well-characterized synthetic biology toolbox of platform microorganisms like Escherichia coli, which results in slow and inefficient design-build-test cycles. If a heterologous production pathway can be engineered, the slow growth and uptake rates of native methylotrophs generally limit their industrial potential. Therefore, much focus has been placed on engineering synthetic methylotrophs, or non-methylotrophic platform microorganisms, like E. coli, that have been engineered with synthetic methanol utilization pathways. These platform hosts allow for rapid design-build-test cycles and are well-suited for industrial application at the current time. In this review, recent progress made toward synthetic methylotrophy (including methanotrophy) is discussed. Specifically, the importance of amino acid metabolism and alternative one-carbon assimilation pathways are detailed. A recent study that has achieved methane bioconversion to liquid chemicals in a synthetic E. coli methanotroph is also briefly discussed. We also discuss strategies for the way forward in order to realize the industrial potential of synthetic methanotrophs and methylotrophs.     

The anaerobic decomposition of benzoic acid during methane fermentation

Anaerobic rupture of the benzoic acid ring was investigated. Carbon 4 was converted primarily to carbon dioxide. Following ring rupture during methane fermentation, propanoic acid is an intermediate, and carbon 4 of benzoate becomes its carboxyl.Contribution No. 1285-j, Division of Biology, Kansas State University, Manhattan, KS 66506. This work was supported in part by funds from the Kansas Agricultural Experiment Station, Kansas State University, Manhattan, KS 66506. Paper II of this series is Fina and Fiskin (1960)     

Consuming un-captured methane from landfill using aged refuse bio-cover

A novel simulated bio-cover was developed to facilitate the biological methane oxidation process using aged refuse and aged sludge from landfill. It was found that 78.7% and 66.9% of CH₄ could be removed, with the aged refuse: aged sludge (w/w%) ratio of 7:3 and 6:4 in bio-cover system, respectively. The maximum CH₄ removal rate could reach 100%, when the aged refuse with the disposal time more than 14 years were applied in bio-cover. Some controlled factors for the methanotrophic activity, i.e. moisture, Eh and organic matter content, were also investigated. It was found that CH₄ oxidation rate increased greatly, when the moisture content and organic matter were increased from 6.0%, 4.8% to 8.0%, 9.5%, respectively. The optimum conditions for this bio-cover system was found to be as follows: aged refuse: aged sludge ratio of 7:3, the moisture content of 8-9%, Eh of 104-108 mV and organic matter of 9.5%.