PCR-SSCP技术用于脱臭微生物群落结构的研究

采用PCR-SSCP(单链构象多态性)技术对脱臭生物滤池中填料生物膜微生物群落结构进行了研究.生物滤池对臭气中的污染物随驯化时间逐渐增强,去除率从50%升高到89%.对2种填料树皮和秸秆上生物膜的分析结果表明,滤池内微生物多样性随运行时间先降后升,从1.6～1.9上升到2以上;而2种填料上微生物的相似性逐渐增加,表明随着驯化进程,生物填料上的微生物能够利用臭气污染物进行生长,并随运行时间逐渐趋于丰富和稳定;树皮比秸秆具有较高的生物多样性,平均值分别为2.2和2.0,说明树皮上容易附着多种微生物生长,电镜照片也显示2种填料生物膜的增长和生物多样性的提高.SSCP条带测序结果表明生物滤池生物膜优势微生物种属为芽孢杆菌属,占33.3%;条带中不可培养细菌占44.4%;填料生物膜上的细菌绝大多数是广泛存在于土壤、水体及生物体中的微生物,它们对环境适应能力强,在臭气的污染物去除中扮演重要角色.     

双氧水协同生化法强化处理印染废水

传统生化法对印染废水的处理有一定的局限性.本文研究了双氧水协同水解酸化-接触氧化系统,对印染废水进行强化处理.采用污泥挂膜、生化系统启动、双氧水协同启动的方法,将双氧水投加到水解酸化时的条件严格控制为:投加3m L·L~(-1)、投加量100.0 m L、流速0.67 m L·min-1、投加频率1次·d-1,可使整个系统成功启动与稳定运行.实验结果表明,双氧水协同水解酸化-接触氧化可对印染废水中的特征污染物进行有效强化处理.其中,COD平均去除率为89.8%,氨氮平均去除率为96.7%,PVA平均去除率为87.4%,废水平均脱色率为92.1%.采用16S rDNA宏基因组高通量测序技术,对比分析了接种种泥、水解酸化污泥和接触氧化污泥微生物的群落结构.结果表明,经过驯化,水解酸化和接触氧化微生物群落均发现了显著变化.其中,水解酸化污泥优势菌门主要为变形菌门Proteobacteria、拟杆菌门Bacteroidetes和疣微菌门Verrucomicrobia;接触氧化污泥优势菌门主要为浮霉菌门Planctomycetes、变形菌门Proteobacteria和酸杆菌门Acidobacteria.该实验从宏观和微观角度,均证实双氧水协同生化法强化处理印染废水具有技术可行性.     

生物膜复合系统脱氮除磷的特征及微生物群落结构分析

试验研究了序批式生物膜复合系统在不同有机负荷下氮磷等营养物质的去除特性.结果表明,复合系统在COD负荷为0.35kg.kg-1.d-1(以MLSS计)时能够很好解决脱氮除磷的泥龄矛盾,TP、TN、NH4+-N去除率分别能达到96%、89%和96%,高于对照组的SBR工艺.复合系统中,悬浮污泥对硝化起主要作用,悬浮态污泥和生物膜的硝化平均贡献比为1.66;附着态生物膜对反硝化和除磷起主要作用,生物膜和悬浮态污泥的反硝化贡献比为2.19,释磷贡献比为3.5,摄磷贡献比为3.76.利用PCR-DGGE技术发现,复合系统中存在丰富的脱氮功能菌和除磷功能菌,且悬浮态与附着态微生物的相似性仅为73%,区别较大,说明两者存在一定的分工协作,与反应器的处理特性相一致.     

Control of hydrogen sulfide emissions using autotrophic denitrification landfill biocovers: engineering applications

Hydrogen sulfide (H₂S) emitted from construction and demolition waste landfills has received increasing attention. Besides its unpleasant odor, longterm exposure to a very low concentration of H₂S can cause a public health issue. In the case of construction and demolition (C&D) waste landfills, where gas collection systems are not normally required, the generated H₂S is typically not controlled and the number of treatment processes to control H₂S emissions in situ is limited. An attractive alternative may be to use chemically or biologically active landfill covers. A few studies using various types of cover materials to attenuate H₂S emissions demonstrated that H₂S emissions can be effectively reduced. In this study, therefore, the costs and benefits of H₂S-control cover systems including compost, soil amended with lime, fine concrete, and autotrophic denitrification were evaluated. Based on a case-study landfill area of 0.04 km², the estimated H₂S emissions of 80900 kg over the 15-year period and costs of active cover system components (ammonium nitrate fertilizer for autotrophic denitrification cover, lime, fine concrete, and compost), ammonium nitrate fertilizer is the most cost effective, followed by hydrated lime, fine concrete, and yard waste compost. Fine concrete and yard waste compost covers are expensive measures to control H₂S emissions because of the large amount of materials needed to create a cover. Controlling H₂S emissions using fine concrete and compost is less expensive at landfills that provide on-site concrete recovery and composting facilities; however, ammonium nitrate fertilizer or hydrated lime would still be more cost effective applications.     

The effects of climate warming on microbe-mediated mechanisms of sediment carbon emission

Due to significant differences in biotic and abiotic properties of soils compared to those of sediments, the predicted underlying microbe-mediated mechanisms of soil carbon emissions in response to warming may not be applicable for estimating similar emissions from inland water sediments. We addressed this issue by incubating different types of sediments, (including lake, small river, and pond sediments) collected from 36 sites across the Yangtze River basin, under short-term experimental warming to explore the effects of climate warming on sediment carbon emission and the underlying microbe-mediated mechanisms. Our results indicated that under climate warming CO₂ emissions were affected more than CH₄ emissions, and that pond sediments may yield a greater relative contribution of CO₂ to total carbon emissions than lake and river sediments. Warming-induced CO₂ and CH₄ increases involve different microbe-mediated mechanisms; Warming-induced sediment CO₂ emissions were predicted to be directly positively driven by microbial community network modularity, which was significantly negatively affected by the quality and quantity of organic carbon and warming-induced variations in dissolved oxygen, Conversely, warming-induced sediment CH₄ emissions were predicted to be directly positively driven by microbial community network complexity, which was significantly negatively affected by warming-induced variations in pH. Our findings suggest that biotic and abiotic drivers for sediment CO₂ and CH₄ emissions in response to climate warming should be considered separately when predicting sediment organic carbon decomposition dynamics resulting from climate change.     

氢氧化镁对水体内源磷释放的控制作用

本研究首先通过批量实验考察了氢氧化镁对水中磷酸盐的吸附性能,再通过底泥模拟释放实验考察了氢氧化镁覆盖和添加控制底泥中磷向上覆水体释放的效果及机制.结果表明,氢氧化镁对水中磷酸盐具有良好的吸附能力,其投加量的增加有利于水中磷酸盐被其所吸附去除,与Langmuir模型相比,其对水中磷酸盐的等温吸附行为更适合采用Freundlich和Dubinin-Radushkevitch （D-R）模型加以描述.氢氧化镁覆盖可以有效地控制底泥中磷向上覆水体的释放,使得上覆水中SRP浓度处于较低的水平,即使覆盖层的结构完整性受到扰动破坏而导致覆盖材料与表层底泥的混合,氢氧化镁仍然可以有效地控制底泥中磷向上覆水体的释放.氢氧化镁覆盖和添加均可以有效地降低最上层（0~10 mm）底泥间隙水中SRP的浓度,这对于其覆盖和添加有效控制底泥中磷向上覆水体的释放是至关重要的.人工合成的氢氧化镁对水中磷酸盐的吸附性能优于商业购买的氢氧化镁,前者控制水体内源磷向上覆水体释放的效果也优于后者.以上结果显示,氢氧化镁是一种有希望用于控制水体底泥内源磷释放的活性覆盖和改良材料.     

酸性冲击对微生物电解产氢阳极菌群影响及功能基因变化解析

微生物电解产氢工艺是借助能够直接与电极传递电子的功能菌在阳极降解有机质并将产生的电子在阴极与质子结合回收氢气能源的新技术.采用市政废水在固定外加电压相同条件下直接启动15个反应器,以葡萄糖为碳源驯化获得电极功能菌群,稳定运行1个月获得反应器稳定产氢和伴随产甲烷效能.初始稳定时采用pH为7的磷酸盐缓冲液可以获得稳定的产气量,平行反应器表现出不同的氢气和甲烷产量.最高产氢反应器的氢气转化率为32.2%,氢气产率为(3.9±0.6)mol·mol-1(以每mol葡萄糖产生的H2量(mol)计,下同);相同条件下最低产氢效率反应器的甲烷转化率则可达到48.4%.通过48 h阳极生物膜的酸性冲击试验对阳极菌群功能恢复效果进行分析,发现消除冲击10~15 d反应器的电子传递效率得到恢复,但功能菌群多样性增加,氢气与甲烷比例发生变化.最高产氢反应器氢气产率降低1.8 mol·mol-1,而甲烷增量为0.4 mol·mol-1(以每mol葡萄糖产生的CH4量(mol)计,下同).通过关键功能基因分析发现,初始产氢效能高的反应器功能菌群中电子传递功能菌优势较大;阳极功能菌群受到短暂酸性冲击后,基于细胞色素C基因的相关菌群能够较快恢复,其电子传递能力恢复更快;与碳源降解和产甲烷相关基因群落受酸性冲击后变化较为显著,甲烷增量与氢气减少量基本符合反应计量关系.     

生活垃圾堆肥接种技术

以复合微生物菌剂、马粪、成熟堆肥、果园土、污泥为接种剂,采用在线监测堆肥设备,通过温度传感器、出口气体O₂-H₂S监测仪,研究堆肥过程中温度、耗氧速率、有机物分解速率、H₂S气体浓度变化.试验结果表明,添加接种剂堆肥与对照组比,堆料能达到理想的温度,且高温停留时间长,堆肥反应速率加快及堆肥腐熟时间缩短,并能很好地控制出口H₂S气体浓度.特别是以复合微生物菌剂或马粪作为接种剂,能明显加速堆料的腐熟进程,其腐熟时间分别比对照组提前210h和180h.     

膜生物反应器处理甲苯性能及机制

采用膜生物反应器处理甲苯有机废气,研究了进气浓度、停留时间、循环液喷淋密度和pH值对甲苯去除率的影响.膜生物反应器能高效净化挥发性有机废气,甲苯去除率可达99%.适宜运行条件为:pH值为7.2、停留时间为6.4 s、循环液喷淋密度为2.5 m3.(m2.h)-1.采用GC-MS分析出口气样,研究结果表明乙醛酸(C2H2O3)和乙烯基甲酸(C3H4O2)为甲苯生物降解的中间产物.膜生物反应器处理甲苯机制为甲苯气体通过中空纤维膜传质到生物膜,被生物降解为乙醛酸和乙烯基甲酸,然后继续好氧降解为最终产物二氧化碳和水.     

Water at interfaces

Electrolyte cations and anions in aqueous solutions are hydrogen bond breaker. We found that most of anions are strong hydrogen bond breaker whereas cations are not. Further, the electro-reduction of Mg(H₂O)₆²⁺ to Mg(OH)₂ and the growth of the Mg(OH)₂ were observed on Au electrode surface at negative electrode potential. Water molecules in an electric double layer exhibit an ordered and a disordered structure at negative and pzc (point of zero charge) potentials, respectively. Therefore, electrode potential polarization (negative or pzc potential application) from an equilibrium potential operates an electrified interface to cause increased or decreased ordering, orientation and charge transfer of water molecules as well as dissociation of water on the electrode surface.     

Perturbations to tropospheric oxidants, 1985–2035: 2. Calculations of hydrogen peroxide in chemically coherent regions

Increasing global emissions of trace gases NO, CH₄, and CO, along with perturbations initiated by changes in stratospheric O₃ and H₂O, may cause tropospheric hydrogen peroxide (H₂O₂) levels to change. Specific scenarios of CH₄CONO emissions and global climate changes are used to predict HO₂ and H₂O₂ changes from 1985 to 2035 in a one-dimensional model that simulates different chemically coherent regions (e.g. urban, non-urban continental and marine mid-latitudes; marine and continental low latitudes).If CH₄ and CO emissions continue to increase throughout the troposphere at current rates (1% yr⁻), there will be large increases in H₂O₂, for example, more than 100% in the urban boundary layer from 1985 to 2035. Globally, H₂O₂ will increase 22% with HO₂ increasing 8% and O₃ increasing 13%. When CH₄, CO and NO emissions are specified on a regionally varying basis and are parameterized for high and low potential growth rates, globally averaged increases in surface concentrations are 12% for H₂O₂ and 18% for O₃. A global warming (with increased H₂O vapor) or stratospheric O₃ depletion superimposed on CH₄, CO and NO emissions changes will cut O₃ increases but add to peroxide, increasing levels as much as 150% above present day in some regions.Both globally uniform and region-specific scenarios predict a 10–15% loss in global OH from 1985 to 2035. Thus, conversion of OH to HO₂ and H₂O₂ in the atmosphere may signify a loss of gaseous oxidizing capacity in the atmosphere and an increase in aqueous-phase oxidizing capacity.     

秸秆还田配施生物炭对关中平原夏玉米产量和土壤N2O排放的影响

为探明秸秆还田配施生物炭对夏玉米产量和土壤氧化亚氮（N₂O）排放的影响,基于2019~2020年关中平原田间定位试验,利用静态暗箱-气相色谱法监测了土壤N₂O排放通量,综合分析夏玉米产量、土壤N₂O排放和土壤活性氮组分,明确了秸秆还田配施生物炭在培肥土壤、增产减排方面的效应.以秸秆不还田（S₀）为对照,设置秸秆还田（S）和秸秆还田配施生物炭（SB）共3个处理.结果表明,各处理N₂O排放峰值出现在秸秆还田后10 d,秸秆还田30 d后土壤N₂O排放通量处于较低水平,土壤N₂O排放通量与铵态氮（NH₄⁺-N）、无机氮、微生物量氮（MBN）和可溶性有机氮（DON）含量呈显著的正相关关系（P<0.05）.S较S₀显著增加夏玉米产量、N₂O累积排放量、单位产量N₂O累积排放量和土壤总氮（TN）含量,分别为7.4%~13%、65.8%~132.2%、54.6%~103%和27.8%~33%.虽然SB较S提高夏玉米产量（2.5%~3.3%）的趋势不显著（P>0.05）,但是SB较S显著降低N₂O累积排放量和单位产量N₂O累积排放量,分别为24.0%~27.3%和26.4%~29.2%.在土壤N₂O排放通量达到峰值时,SB较S显著降低土壤N₂O排放通量45.1%~69.6%,生物炭能够缓解秸秆还田所诱发的土壤N₂O排放,具有削峰的作用.SB较S显著增加土壤总氮9.1%~12.2%.综合作物产量、N₂O排放和土壤总氮,对夏玉米生产而言,秸秆还田配施生物炭不仅培肥地力,提高夏玉米产量,而且减少单位产量N₂O累积排放量,是可供推广的兼顾作物产量和环境友好的适宜管理措施.     

生物炭和有机肥对菜地土壤N2O排放及硝化、反硝化微生物功能基因丰度的影响

通过室内培养试验和实时荧光定量PCR技术,研究了田间施用生物炭和有机肥对菜地土壤氧化亚氮(N_2O)排放、氨单加氧酶(amo A)和亚硝酸盐还原酶(nir S、nir K)、氧化亚氮还原酶(nos Z)基因丰度的影响,并探讨功能基因丰度对N_2O排放的影响.试验设置5个处理:CK(对照)、N(尿素)、N+BC(尿素和生物炭)、N+M(尿素和有机肥)和N+BC+M(尿素、生物炭和有机肥).结果表明,与CK处理相比,各施肥处理均降低了土壤氨氧化细菌(AOB)和氨氧化古菌(AOA)丰度,增加了nir K、nir S和nos Z基因丰度,并提高了培养期间N_2O累积排放量.与N处理相比,N+BC处理的土壤p H值提高了11.1%,并增加了AOB、AOA、nir S、nir K和nos Z基因丰度,增幅分别为105.8%、57.3%、22.0%、176.2%和204.9%,同时显著降低了培养期间N_2O累积排放量,降幅为58.1%;N+M处理增加了nir K和nir S基因丰度,增幅分别为58.8%和7.1%,对N_2O排放的影响不显著;N+BC+M处理增加了AOB、nir K、nir S和nos Z基因丰度,增幅分别为30.7%、68.7%、6.5%和84.5%,降低了N_2O累积排放量,降幅为14.4%.生物炭通过增加amo A、nir S和nir K基因丰度间接增加N_2O排放,同时通过增加nos Z基因丰度促进N_2O还原,综合效应表现为降低了菜地土壤N_2O排放.因此,通过施用生物炭改善土壤性质,增加功能基因丰度,降低土壤N_2O排放,是一种较好的N_2O减排措施.施用有机肥可以增加反硝化作用功能基因丰度,但对N_2O减排效果不显著.     

基于模糊综合评判模型的污水管道缺陷定量化评价方法

利用模糊综合评判模型,从污水管道的密封性、稳定性和功能性三方面分别考虑不同缺陷类型的影响,利用层次分析法确定权重,建立定量化的污水管道缺陷状况评价方法模型.对南方某市一段污水管道进行评判,得到污水管道缺陷综合评价指数H=1.09,其中密封性指数Ht=0.44,稳定性指数Hs=0.78,功能性指数Hf=1.79,判定结果...     

生物质炭与有机物料混施对土壤温室气体排放和微生物活性的影响

土壤是温室气体的重要排放源,在土壤中施入生物质炭和有机物料对土壤微生物在土壤碳氮转化和微量气体代谢方面有着重要作用,不过迄今在生物质炭和有机物料混施对土壤温室气体排放和微生物活性的影响方面的研究尚少.本研究采用室内培养试验,利用土壤添加生物质炭和生物质炭与不同有机物料混施,探究生物质炭和有机物料混施对土壤温室气体排放及微生物活性的影响.共设5个处理:新鲜土壤(S)、新鲜土壤+2%生物质炭(SB)、新鲜土壤+2%生物质炭+1%大豆饼(SBS)、新鲜土壤+2%生物质炭+1%小麦秸秆(SBW)、新鲜土壤+2%生物质炭+1%鸡粪(SBC).研究表明:只添加生物质炭对温室气体的排放影响不明显;生物质炭与有机物料混施使土壤的CO2、N2O排放明显增加,而对CH4的排放影响不明显;从温室气体增温潜势(GWP)变化可以看出有机物料施用对温室效应具有明显的增强作用;生物质炭与有机物料混施在一定程度上增加微生物生物量碳和代谢熵(q CO2),各处理的代谢熵是对照处理S的0.18~4.37倍;不同有机物料对FDA水解酶、过氧化氢酶、脲酶和碱性磷酸酶活性都表现为激活作用.     

低温下磁性载体MBBR系统微生物群落特征和功能预测分析

为阐明低温下磁性载体对移动床生物膜反应器(MBBR)处理能力的影响,探究了反应器内生物膜的微生物多样性、群落结构、功能特征和氮代谢通路.结果表明,与商用载体反应器(对照组)相比,磁性载体反应器具有更高的污染物去除率,其对NH⁺₄-N和TN的平均去除率分别提高了16.2%和12.1%.Illumina高通量测序结果显示,磁性载体生物膜的微生物多样性和丰富度更高.由于不同微生物的磁化率不同,导致两种载体生物膜微生物群落结构存在显著差异.磁性载体生物膜中硝化菌属(如：Nitrosomonas、Nitrospira)和反硝化菌属(如：Sphaerotilus、Zoogloea)的相对丰度显著增多.PICRUSt2功能预测分析显示,磁性载体生物膜的整体基因功能表达水平更高,在信号传导机制和细胞内运输、分泌和囊泡运输等方面优势更明显.此外,大多数与氮代谢相关基因在磁性载体生物膜中丰度更高,如涉及硝化过程的基因amo、hao和反硝化过程基因nap、nor等,使得生物膜的低温脱氮潜力增强.以上结果从微观生物学角度更好地解释了反应器处理能力的差异,为磁性载体强...     

Response of anaerobes to methyl fluoride, 2-bromoethanesulfonate and hydrogen during acetate degradation

To use the selective inhibition method for quantitative analysis of acetate metabolism in methanogenic systems,the responses of microbial communities and metabolic activities,which were involved in anaerobic degradation of acetate,to the addition of methyl fluoride(CH3F),2-bromoethanesulfonate(BES)and hydrogen were investigated in a thermophilic batch experiment.Both the methanogenic inhibitors,i.e.,CH3F and BES,showed their effectiveness on inhibiting CH4 production,whereas acetate metabolism other than acetoclastic methanogenesis was stimulated by BES,as reflected by the fluctuated acetate concentration.Syntrophic acetate oxidation was thermodynamically blocked by hydrogen(H2),while H2-utilizing reactions as hydrogenotrophic methanogenesis and homoacetogenesis were correspondingly promoted.Results of PCR-DGGE fingerprinting showed that,CH3F did not influence the microbial populations significantly.However,the BES and hydrogen notably altered the bacterial community structures and increased the diversity.BES gradually changed the methanogenic community structure by affecting the existence of different populations to different levels,whilst H2 greatly changed the abundance of different methanogenic populations,and induced growth of new species.     

Effect of liming on sulfate transformation and sulfur gas emissions in degraded vegetable soil treated by reductive soil disinfestation

Reductive soil disinfestation (RSD), namely amending organic materials and mulching or flooding to create strong reductive status, has been widely applied to improve degraded soils. However, there is little information available about sulfate (SO₄^2 −) transformation and sulfur (S) gas emissions during RSD treatment to degraded vegetable soils, in which S is generally accumulated. To investigate the effects of liming on SO₄^2 − transformation and S gas emissions, two SO₄^2 −-accumulated vegetable soils (denoted as S1 and S2) were treated by RSD, and RSD plus lime, denoted as RSD₀ and RSD₁, respectively. The results showed that RSD₀ treatment reduced soil SO₄^2 − by 51% and 61% in S1 and S2, respectively. The disappeared SO₄^2 − was mainly transformed into the undissolved form. During RSD treatment, hydrogen sulfide (H₂S), carbonyl sulfide (COS), and dimethyl sulfide (DMS) were detected, but the total S gas emission accounted for < 0.006% of total S in both soils. Compared to RSD₀, lime addition stimulated the conversion of SO₄^2 − into undissolved form, reduced soil SO₄^2 − by 81% in S1 and 84% in S2 and reduced total S gas emissions by 32% in S1 and 57% in S2, respectively. In addition to H₂S, COS and DMS, the emissions of carbon disulfide, methyl mercaptan, and dimethyl disulfide were also detected in RSD₁ treatment. The results indicated that RSD was an effective method to remove SO₄^2 −, liming stimulates the conversion of dissolved SO₄^2 − into undissolved form, probably due to the precipitation with calcium.     

PCR-DGGE研究处理垃圾渗滤液序批式生物膜反应器(SBBR)中的细菌多样性

为了研究序批式生物膜反应器中的细菌多样性及其脱氮的微生物学机理,为工艺改进提供依据,从同步高效去除垃圾渗滤液中高氨氮和高COD的SBBR生物膜和渗滤液原水中采集微生物样品并提取微生物总DNA,使用细菌通用引物对（GC341F/907R）从总DNA中成功扩增出目标16S rDNA片段,然后对扩增的16S rDNA进行DGGE,对凝胶染色并进行条带统计分析和切胶测序,使用序列数据进行同源性分析并建立了系统发育树.结果表明,该驯化后的SBBR生物膜和渗滤液原水中都有比较丰富的细菌多样性,驯化的生物膜细菌主要来自渗滤液原水,而且生物膜细菌在反应器正常运行时不会出现明显的群落结构变化;在该SBBR中有多种硝化细菌与反硝化细菌、好氧反硝化细菌和厌氧氨氧化细菌共存,说明该反应器中可能同时存在全程硝化反硝化、同步硝化反硝化和厌氧氨氧化3种脱氮方式.研究结果为SBBR脱氮微生物机理研究提供了一些有价值的参考依据.     

基于高通量测序的流化床生物滤器细菌群落结构分析

为了解流化床生物滤器内部细菌群落组成及其净水机制,通过高通量测序方法,研究了不同时期滤器中表层和底层滤料的细菌群落结构,分析了滤器不同床层的营养盐变化情况及水处理性能.结果表明,滤器的硝化作用主要发生于床层下部,表层对其的贡献率不显著.稳定工况下,流化床生物滤器对NH_4~+-N、TN、BOD_5和SS的去除率达到(68.3±2.24)%、(49.54±3.56)%、(60.35±4.98)%和(45.21±2.11)%,对氨氮的去除负荷达到(343.28±75.5)g·(m~3·d)~(-1),其硝化性能优于常规生物滤器.试验共筛选31个门,490个细菌属,其生物多样性显著高于常规生物滤器.自清洗装置的启停对滤器中不同区域载体表面细菌的多样性没有影响,对各样品的优势菌群略有影响.在滤器稳定运行时,表层区域的优势细菌基本维持不变,主要包括厌氧绳菌科、黄杆菌科、红杆菌科、硝化螺菌属、暖绳菌科.而底层区域的优势细菌随着时间的推移有所变化,主要包括硝化螺菌属、微丝菌属、Muricauda、Defluviimonas、红杆菌科.