准好氧填埋渗滤液水质变化特性研究

在大型模拟填埋试验装置(21 m×3.8 m×6.0 m)上,研究了准好氧填埋渗滤液水质的主要指标COD_Cr、BOD、NH₃⁺-N和pH的变化特性.结果表明,准好氧填埋结构下渗滤液COD_Cr、BOD浓度下降很快,没有出现在传统填埋场累积的现象,并且封场后39周分别降为173和30 mg·L^-1;NH₃⁺-N浓度下降更为显著,第39周降为1 mg·L^-1,下降率达到99.6%,为渗滤液后续处理解决了NH₃⁺-N浓度过高的难题;pH值在前2周略低于7,第3周后一直呈弱碱性.根据实验数据,拟合了准好氧填埋结构渗滤液污染物的衰减方程.     

五年填埋龄准好氧和厌氧填埋体及陈垃圾的理化特性

研究了5年填埋龄准好氧和厌氧填埋体的沉降量、温度和填埋气产生特性,并分析了填埋处理陈腐垃圾的理化性质.结果表明：5年填埋龄准好氧填埋体的表面沉降量和减容率均显著高于厌氧填埋体,同时渗滤液回灌比清水回灌更容易引起垃圾填埋体表面的不均匀沉降.厌氧填埋体的平均温度（25.6 ℃）略高于准好氧填埋体（24.8 ℃）,但差异不显著.准好氧填埋体不同时期的O₂浓度分别高于厌氧填埋体,而CH₄浓度则显著低于厌氧填埋体.5年填埋龄准好氧和厌氧填埋体陈垃圾中厨余物和纸类等易降解有机物含量显著降低,塑料、玻璃、砖瓦和竹木等含量则升高.其中,陈垃圾中有机质与营养元素含量均高于典型南方土壤;除厌氧填埋体陈垃圾中Cr含量超标外,其余重金属含量均未超出《土壤环境质量标准（GB 15618—1995）》的三级标准要求.     

长白落叶松冠层光合作用的空间异质性

以2014年黑龙江省帽儿山林场14年生人工长白落叶松为研究对象,对比分析了各项光合指标、环境因子及光合生理参数在冠层内的空间差异性,并探讨了净光合速率(P_n)与其他指标的关系.结果表明: 在树冠垂直方向,上层P_n、气孔导度(g_s)和蒸腾速率(T_r)显著高于中层和下层,胞间CO₂浓度(C_i)表现为下层>中层>上层;光合有效辐射(PAR)从上层外部到下层内部呈显著降低趋势,水汽压差(VPD)和叶片温度(T_l)表现为上层显著高于中层和下层,相对湿度(RH)则无显著差异;最大净光合速率(P_{n max})、暗呼吸速率(R_d)、光补偿点(LCP)和光饱和点(LSP)均表现为上层>中层>下层,下层比上层分别降低32.7%、55.8%、80.2%和51.6%,表观量子效率(AQY)表现为下层>中层>上层,下层分别是中层和上层的1.2和1.3倍.水平方向,光合指标和环境因子的差异性主要体现在树冠上层,P_n、g_s、T_r、PAR和VPD表现为树冠外部显著高于树冠内部,而C_i和RH差异不显著;P_{n max}、R_d、LCP和LSP表现为外部>内部,内部比外部分别降低0.4%、37.7%、42.0%和16.4%,而AQY在内部比外部高0.7%.C_i是限制P_n的主要生理因子,PAR是影响P_n的主要环境因子,尤其在弱光区域PAR对P_n的影响十分明显.因此,在模拟和预估树木冠层光合作用时,考虑空间异质性有一定的必要性.     

水稻土中CH4氧化的研究

在实验室条件下研究了水稻土中CH₄氧化的特性.结果表明,在早稻种植前采集的水稻土不能氧化大气中的CH₄,但当所供给的CH₄浓度>10μl·L^-1时,能迅速氧化CH₄,所供给的CH₄浓度越高,氧化CH₄的速度越大.经高浓度(>1000μl·L^-1)的CH₄预培养10d,可使本来不具有氧化大气CH₄能力的土壤氧化大气CH_4.大田CH₄排放通量高的水稻土,氧化CH₄的能力较大.     

生物反应器填埋场系统渗滤液的脱氮性能

利用填埋场垂直分布的好氧-缺氧-厌氧的独特生态环境,并采用填埋垃圾上层间歇曝气充氧的方式,研究了生物反应器填埋场系统渗滤液的脱N性能.结果表明,填埋垃圾上层间歇曝气充氧,促进了填埋垃圾层硝化细菌和反硝化细菌的生长,且可使反硝化细菌的数量比普通的填埋垃圾层高4～13个数量级,硝化细菌的最大数量可达到10⁹个·g^-1;营建了填埋场内硝化、反硝化等脱N反应的生物环境,有利于回流渗滤液含N化合物的去除.试验结束时,其渗滤液NH₄⁺-N和TN浓度分别为186和289 mg·L^-1,仅为对照的18%和26％.此外,填埋垃圾上层间歇曝气充氧也有利于填埋垃圾的降解,提高垃圾的稳定化效果.     

添加氧化铁对水稻土中H2、CO2和CH4形成的影响

水稻土是甲烷产生的重要源地.厌氧条件下甲烷的形成与有机质厌氧降解产生的乙酸、H₂和CO₂有关.氧化铁作为电子受体可有效地竞争有机质向甲烷的转化,其抑制作用机理可能与乙酸、H₂和CO₂的有效消耗有关.通过向水稻土泥浆中添加无定形氧化铁和纤铁矿,分别测定了25℃厌氧恒温培养105d过程中的H₂、CO₂和CH₄的浓度变化.结果表明,添加无定形氧化铁及纤铁矿可导致H₂浓度显著降低;无定形氧化铁对H₂消耗的影响明显大于纤铁矿;添加不同氧化铁对CO₂浓度的影响与H₂浓度的变化有相同的趋势;添加氧化铁能显著抑制水稻土中甲烷形成,并导致有机碳的转移发生变化,使得CH₄-C显著降低,气相中CO₂-C量减少,而由土壤泥浆固定的CO₃^2--C量显著增加.     

脱甲河水系CH4关键产生途径及其稳定碳同位素特征

为明确脱甲河溶存CH₄关键产生途径,明晰水系碳同位素组成及其分布特征,为小流域CH₄排放估算和减排提供数据支撑.利用双层扩散模型法估算了CH₄浓度和传输通量,研究了周年内脱甲河4级河段(S₁～S₄)水体CH₄通量的时空分布及其主控环境因子;运用稳定同位素方法探究了溶存CH₄关键产生途径,分析了溶解CH₄、悬浮颗粒物和沉积物有机质δ¹³C分布特征.结果表明: 水体pH均值为(7.27±0.03),各河段四季差异均显著;溶解氧(DO)在0.43～13.99 mg·L^-1内变化,S₁河段DO浓度最高且夏、秋季差异显著,其他河段均为冬与春、夏、秋季差异显著;可溶性有机碳(DOC)变化范围是0.34～8.32 mg·L^-1,由S₁至S₄河段总体呈递增趋势;水体电导率(EC)和氧化还原电位(ORP)变化范围分别是17～436 μS·cm^-1和-52.30～674.10 mV,各河段差异明显;铵态氮(NH₄⁺-N)、硝态氮(NO₃^--N)浓度分别在0.30～1.35(平均0.90±0.10) mg·L^-1和0.82～2.45 (平均1.62±0.16) mg·L^-1内变化.溶存CH₄浓度和传输通量变化范围分别是0～5.28 (平均0.46±0.06) μmol·L^-1和-0.34～619.72 (平均53.88±7.15) μg C·m^-2·h^-1;均存在时空变化且变异规律相似,为春季>冬季>夏季>秋季,S₂>S₃>S₄>S₁.通量与水体铵态氮和DOC浓度均呈显著正相关.各级河段均以乙酸发酵产甲烷途径为主导,但不同河段差异明显,乙酸发酵途径产CH₄贡献率以S₁河段最高(87%),其次为S₄(81%),S₂、S₃分别达到78%和76%.溶存CH₄、悬浮颗粒物和沉积物有机质的δ¹³C均值分别为-41.64‰±1.91‰、-14.07‰±1.06‰和-26.20‰±1.02‰,溶存甲烷δ¹³C与沉积物有机质的δ¹³C呈显著正相关,与其传输通量呈极显著负相关.     

全球变化对森林土壤甲烷吸收的影响及其机制研究进展

大气CO₂浓度升高、降水格局改变、全球氮沉降增加和土地覆盖变化等全球变化不仅改变了森林土壤理化性质,而且影响了植物的生长和微生物活性,导致森林土壤碳、氮循环发生改变,进而影响土壤CH₄的吸收.本研究综述了森林土壤CH₄吸收的重要性,森林土壤CH₄吸收对大气CO₂浓度升高、降水格局改变、全球氮沉降增加和土地覆盖变化等全球变化的响应差异及驱动机制.大气CO₂浓度升高抑制土壤CH₄吸收;降水减少倾向于促进土壤CH₄吸收;外源氮输入抑制富氮森林土壤CH₄吸收,而对贫氮森林土壤CH₄吸收则表现为促进或不影响;森林转化为草地、农田或人工林会减少土壤CH₄的吸收量,而植树造林则会增加土壤CH₄的吸收量.今后的研究重点是探讨全球变化对森林土壤CH₄吸收产生长期影响和综合效应,并借助分子生物学方法进一步探究土壤CH₄吸收的微生物学机制.     

未来气候变化情景下中国自然湿地CH4排放的时空变化

应用TRIPLEX GHG模型,模拟未来气候变化背景下2006—2100年中国自然湿地生态系统CH₄排放的时空变化.结果表明： 保持中国现有自然湿地分布不变,在3种相对浓度路径(RCP2.6、RCP4.5和RCP8.5）情境下,21世纪末,中国自然湿地CH₄排放量与当前水平相比将分别增长32.0%、55.3%和90.8%.中国大陆南方自然湿地CH₄排放高于中部和北方,且自西向东呈现上升趋势.CH₄高通量排放区域主要集中在长江中下游湿地、东北湿地和珠江沿岸湿地.RCP4.5和RCP8.5情境下全国大部分自然湿地CH₄排放通量增加,而RCP2.6情境下21世纪中后期CH₄排放上升趋势得到控制并开始下降,到世纪末部分地区（尤其是青藏高原地区）CH₄排放通量与当前水平相比有所降低.     

鄂西南亚高山不同覆被类型泥炭藓沼泽湿地甲烷排放特征及其环境影响因子

沼泽湿地是大气甲烷(CH₄)的重要来源, 但有关亚热带亚高山沼泽湿地CH₄排放的研究却鲜有报道, 特别是对不同覆被类型泥炭藓沼泽湿地CH₄排放量的精确估算及其与环境因子的关系尚不清楚。该研究选择鄂西南亚高山泥炭藓沼泽湿地为研究区域, 于2018年11月-2019年10月间, 使用静态箱-气相色谱仪法原位测定3种覆被类型泥炭藓沼泽湿地CH₄通量, 同步记录大气和地下5 cm土壤的温度以及地下水位变化。结果表明: (1)光照下, 裸露地(B)、泥炭藓(Sphagnum paluster)(S)、金发藓(Polytrichum commune)(P) 3种覆被类型泥炭藓沼泽湿地CH₄-C通量全年变化范围分别为: 0.012-1.372、0.022-1.474、0.027-3.385 mg·m^-2·h^-1; 遮光处理下, B、S、P 3种覆被类型泥炭藓沼泽湿地CH₄-C通量的全年变化范围分别为: 0.012-1.372、0.009-1.839、0.017-2.484 mg·m^-2·h^-1, 均为CH₄排放源。同时, 光照条件下不同覆被泥炭藓沼泽湿地CH₄排放量略大于黑暗条件, 但差异不明显。(2)不同覆被类型泥炭藓沼泽湿地CH₄排放存在明显的季节变化规律, 即: 夏季>秋季>春季>冬季, 其中夏季CH₄排放量显著大于其他季节, 占全年的57%-84%。该研究发现泥炭藓沼泽湿地CH₄通量均与气温和地下5 cm土壤温度极显著相关, 且CH₄排放量随温度升高呈指数增加, 表明温度是影响泥炭藓沼泽湿地CH₄排放时间变化的主要环境因子。(3) 3种覆被类型泥炭藓沼泽湿地的年平均和年累计CH₄排放量均依次为: P > S > B, P显著大于B。该研究发现植被类型与泥炭藓沼泽湿地CH₄排放量存在显著相关性, 表明覆被类型是影响泥炭藓沼泽湿地CH₄排放量空间变异的主要因子。(4) 3种覆被类型泥炭藓沼泽湿地CH₄排放量均与地下水位变化不相关。该研究进一步丰富了泥炭藓沼泽湿地CH₄排放规律, 同时也为区域碳循环提供了详实的基础数据。     

Group-specific quantification of methanotrophs in landfill gas-purged laboratory biofilters by tyramide signal amplification-fluorescence in situ hybridization

The aim of this study was to quantitatively analyse methanotrophs in two laboratory landfill biofilters at different biofilter depths and at temperatures which mimicked the boreal climatic conditions. Both biofilters were dominated by type I methanotrophs. The biofilter depth profiles showed that type I methanotrophs occurred in the upper layer, where relatively high O(2) and low CH(4) concentrations were present, whereas type II methanotrophs were mostly distributed in the zone with high CH(4) and low O(2) concentrations. The number of type I methanotrophic cells declined when the temperature was raised from 15 degrees C to 23 degrees C, but increased when lowered to 5 degrees C. A slight decrease in type II methanotrophs was also observed when the temperature was raised from 15 degrees C to 23 degrees C, whereas cell numbers remained constant when lowered to 5 degrees C. The results indicated that low temperature conditions favored both type I and type II methanotrophs in the biofilters.     

Dimethyl sulfide emission behavior from landfill site with air and water control

Municipal solid waste landfills are responsible for odors affecting the environment and human health. Dimethyl sulfide (DMS) is one of the major odorous compounds known for its low odor threshold and wide distribution. This study examined the generation, migration and emission of DMS in four artificial landfill-simulating reactors: Reactor 1 and Reactor 2, running under anaerobic and semi-aerobic conditions, respectively, without leachate recirculation; and Reactor 3 and Reactor 4, running under anaerobic and semi-aerobic conditions, respectively, with leachate recirculation. From the odor control perspective, aeration can efficiently inhibit maximum DMS headspace concentration by 31.7–93.7%, especially with the functioning of leachate recirculation. However, leachate recirculation in anaerobic conditions may double the DMS emission concentration but may also shorten the period over which DMS is effective because of the upward migration of liquid DMS in the recirculated leachate. The DMS generation was active in the acidification and methane fermentation phase of the simulated landfill and was possibly affected by the volatile fatty acid concentration, chemical oxygen demand, total organic carbon concentration and pH of the leachate, as well as total organic carbon in the refuse. Most significantly, DMS emission can be effectually dealt with by aeration along with leachate recirculation.     

垃圾填埋场氧化亚氮排放控制研究进展

填埋是国内外城市生活垃圾处理的一种主要方式.垃圾填埋场是温室气体氧化亚氮(N2O)和甲烷(CH4)的重要排放源.作为一种高效痕量的温室气体,N2O具有极高的潜在增温效应,其每分子潜在的增温作用是二氧化碳(CO2)的296倍.而且N2O能在大气中长期稳定存在,对臭氧层具有较强的破坏作用.本文针对垃圾填埋场N2O排放的控制研究,概述了垃圾填埋处理过程中主要排放源的N2O排放及其影响因素,提出了现阶段适应我国垃圾填埋场N2O排放控制的一系列措施,并展望了垃圾填埋场温室气体N2O排放控制理论和技术的研究方向.     

Responses of oxidation rate and microbial communities to methane in simulated landfill cover soil microcosms

CH4 oxidation capacities and microbial community structures developed in response to the presence of CH4 were investigated in two types of landfill cover soil microcosms, waste soil (fine material in stabilized waste) and clay soil. CH4 emission fluxes were lower in the waste soil cover over the course of the experiment. After exposure to CH4 flow for 120 days, the waste soil developed CH4 oxidation capacity from 0.53 to 11.25-13.48micromol CH4gd.w.(-1)h(-1), which was ten times higher than the clay soil. The topsoils of the two soil covers were observed dried and inhibited CH4 oxidation. The maximum CH4 oxidation rate occurred at the depth of 10-20cm in the waste soil cover (the middle layer), whereas it took place mainly at the depth of 20-30cm in the clay soil cover (the bottom layer). The amounts of the phospholipid fatty acid (PLFA) biomarks 16:1omega8c and 18:1omega8c for type I and II methanotrophs, respectively, showed that type I methanotrophic bacteria predominated in the clay soil, while the type II methanotrophic bacteria were abundant in the waste soil, and the highest population in the middle layer. The results also indicated that a greater active methanotrophic community was developed in the waste soil relative to the clay soil.     

The biogeochemical controls of N2O production and emission in landfill cover soils: the role of methanotrophs in the nitrogen cycle

Emissions of N2O from cover soils of both abandoned (> 30 years) and active landfills greatly exceed the maximum fluxes previously reported for tropical soils, suggesting high microbial activities for N2O production. Low soil matrix potentials (<-0.7 MPa) indicate that nitrification was the most likely mechanism of N2O formation during most of the time of sampling. Soil moisture had a strong influence on N2O emissions. The production of N2O was stimulated by as much as 20 times during laboratory incubations, when moisture was increased from -2.0 MPa to -0.6 MPa. Additional evidence from incubation experiments and delta13C analyses of fatty acids (18:1) diagnostic of methanotrophs suggests that N2O is formed in these soils by nitrification via methanotrophic bacteria. In a NH3(g)-amended landfill soil, the rate of N2O production was significantly increased when incubated with 100 ppmv methane compared with 1.8 ppmv (atmospheric) methane. Preincubation of a landfill soil with 1% CH4 for 2 weeks resulted in higher rates of N2O production when subsequently amended with NH3(g) relative to a control soil preincubated without CH4. At one location, at the soil depth (9-16 cm) of maximum methane consumption and N2O production, we observe elevated concentrations of organic carbon and nitrogen and distinct minima in delta15N (+1.0%) and delta13C (-33.8%) values for organic nitrogen and organic carbon respectively. A delta13C value of -39.3% was measured for 18:1 carbon fatty acids in this soil, diagnostic of type II methanotrophs. The low delta15N value for organic nitrogen is consistent with N2 fixation by type II methanotrophs. These observations all point to a methanotrophic origin for the organic matter at this depth. The results of this study corroborate previous reports of methanotrophic nitrification and N2O formation in aqueous and soil environments and suggest a predominance of type II rather than type I or type X methanotrophs in this landfill soil.     

Colour removal from landfill leachate by coagulation and flocculation processes

A study was conducted to investigate the efficiency of coagulation and flocculation processes for removing colour from a semi-aerobic landfill leachate from one of the landfill sites in Malaysia. Four types of coagulant namely aluminium (III) sulphate (alum), ferric (III) chloride, ferrous (II) sulphate and ferric (III) sulphate were studied using standard jar test apparatus. Results indicated that ferric chloride was superior to the other coagulants and removed 94% of colour at an optimum dose of 800 mg/l at pH 4. The effect of coagulant dosages on colour removal showed similar trend as for COD, turbidity and suspended solids. This suggested that colour in landfill leachate was mainly contributed by organic matters with some insoluble forms that exhibited turbidity and suspended solids readings. The results from this study suggested that ferric chloride could be a viable coagulant in managing colour problems associated with landfill leachate.     

Effects of sulfur-metabolizing bacterial community diversity on H<Subscript>2</Subscript>S emission behavior in landfills with different operation modes

Hydrogen sulfide (H₂S) is one of the major contributors to offensive odors from landfills, and its concentration differs under different operation modes. This study examined the distribution of H₂S emission from different landfill depths under different operation modes (anaerobic, semi-aerobic, semi-aerobic transformation, and the three operation modes with additional leachate recirculation). The microbial community (especially the sulfur-metabolizing bacterial community) was investigated using high-throughput sequencing technology. The results showed that the semi-aerobic mode could substantially lower the risks of H₂S pollution in landfills, which might be because of the difference in biological processes related to sulfur metabolism driven by functional microbes. A myriad of factors are responsible for mutually shaping the sulfur-metabolizing bacterial community composition in landfills that might subsequently affect the behavior of H₂S emission in landfills. The differences in abundance of the genera Acinetobacter and Paracoccus (phylum Proteobacteria) caused by environmental factors might explain the differences in H₂S emission. H₂S odor control could be realized if the related functional microbe diversity can be influenced by adjustments to landfill operation.     

Layered structure of bacterial and archaeal communities and their in situ activities in anaerobic granules

The microbial community structure and spatial distribution of microorganisms and their in situ activities in anaerobic granules were investigated by 16S rRNA gene-based molecular techniques and microsensors for CH(4), H(2), pH, and the oxidation-reduction potential (ORP). The 16S rRNA gene-cloning analysis revealed that the clones related to the phyla Alphaproteobacteria (detection frequency, 51%), Firmicutes (20%), Chloroflexi (9%), and Betaproteobacteria (8%) dominated the bacterial clone library, and the predominant clones in the archaeal clone library were affiliated with Methanosaeta (73%). In situ hybridization with oligonucleotide probes at the phylum level revealed that these microorganisms were numerically abundant in the granule. A layered structure of microorganisms was found in the granule, where Chloroflexi and Betaproteobacteria were present in the outer shell of the granule, Firmicutes were found in the middle layer, and aceticlastic Archaea were restricted to the inner layer. Microsensor measurements for CH(4), H(2), pH, and ORP revealed that acid and H(2) production occurred in the upper part of the granule, below which H(2) consumption and CH(4) production were detected. Direct comparison of the in situ activity distribution with the spatial distribution of the microorganisms implied that Chloroflexi contributed to the degradation of complex organic compounds in the outermost layer, H(2) was produced mainly by Firmicutes in the middle layer, and Methanosaeta produced CH(4) in the inner layer. We determined the effective diffusion coefficient for H(2) in the anaerobic granules to be 2.66 x 10(-5) cm(2) s(-1), which was 57% in water.