一株高效脱硫菌的分离鉴定和脱硫特性研究

从污水净化厂二沉池回流污泥中分离到一株硫杆菌菌株dj-5,该菌株是一种兼性厌氧菌,通过生理生化特性鉴定,并结合16S rDNA序列分析及鉴定,该菌株可以确定为脱氮硫杆菌（Thiobacillus denitrificans）。该菌株的生长曲线表明菌体生长迅速,延滞期约为8 h,然后细菌进入对数生长期,这一阶段持续时间大约20～24 h,稳定期较短,细菌很快进入衰亡期。通过脱硫工艺实验考察了pH值、温度和搅拌速度对脱硫率和菌体生长的影响,结果表明,在进气量180 L/h、pH=6～8、温度为25～35℃和搅拌速度为270 r/min时,该菌株能正常生长,对进气浓度高达2 500 mg/m³的硫化氢脱除率在91%以上。     

PCR-酶切技术在石油烃降解菌筛选鉴定中的应用

将以原油驯化所得的纯培养微生物菌株作为模板,采用PCR(聚合酶链式反应)法,用扩增细菌16S rDNA的一对通用引物(8 f,1492 r)对模板扩增,并用限制性内切酶R saI和M spI对PCR产物进行ARDRA多态性分析。聚类去除重复菌株后60株菌株可分为11种不同分类操作单元(OTU),同时得出每个分类操作单元的数量。实验结果表明,此方法可快速去除重复菌株并反映出菌株间的系统进化关系;同时实验数据可构建成库,使后续分离菌株的筛选工作只需比对数据即可完成。     

Metabolic fate of the 14C-labeled herbicide clodinafop-propargyl in a sediment–water system

The metabolic fate of ¹⁴C-phenyl-labeled herbicide clodinafop-propargyl (¹⁴C-CfP) was studied for 28 days in lab assays using a sediment–water system derived from a German location. Mineralization was 5.21% of applied ¹⁴C after 28 days exhibiting a distinct lag phase until day 14 of incubation. Portions of radioactivity remaining in water phases decreased at moderate rate to 18.48% after 28 days; 62.46% were still detected in water after 14 days. Soxhlet extraction of the sediment using acetonitrile released 35.56% of applied ¹⁴C with day 28, while 33.99% remained as non-extractable residues. A remarkable increase of bound ¹⁴C was observed between 14 and 28 days correlating with the distinct increase of mineralization. No correlation was found throughout incubation with microbial activity of the sediment as determined by dimethyl sulfoxide reduction. Dissolved oxygen and pH value of water phases remained almost constant for 28 days. Analyses of Soxhlet extracts of the sediment and ethyl acetate extracts of water phases by radio-TLC and radio-HPLC revealed that CfP was rapidly cleaved to free acid clodinafop (Cf), which was further (bio-) transformed. DT₅₀ values (based on radio-HPLC) were below 1 day (CfP) and slightly above 28 days (Cf). Further metabolites were not detected. Fractionation of humic and non-humic components of the sediment demonstrated that CfP's non-extractable residues were predominantly associated with fulvic acids up to 14 days of incubation (3.36%), whereas after 28 days, the majority of radioactivity was found in the humin/mineral fraction (13.30% of applied ¹⁴C). Due to high-performance size-exclusion chromatography of the fulvic acids fraction derived from assays incubated for 28 days, this portion of ¹⁴C was firmly, possibly covalently bound to fulvic acids and did not consist of CfP or Cf. Using an isolation strategy comprising preincubation of sediment with CfP and mineralization of ¹⁴C-CfP as criterion, a microorganism was isolated from the sediment examined. It grew on ¹⁴C-CfP as sole carbon source with evolution of ¹⁴CO₂. The bacterium was characterized by growth on commonly used carbon sources and 16S rDNA sequence analysis. Its sequence exhibited high similarity with that of Nocardioides aromaticivorans strain H-1 (98.85%; DSM 15131, JCM 11674).     

甲硫醇脱臭菌的分离、分子鉴定及应用

以低浓度甲硫醇臭气的生物降解为研究对象, 从不同的菌源中筛选得到一株能高效降解甲硫醇的菌株.运用16S rDNA的分子鉴定技术,确定筛选菌Jll的16S rDNA序列同芸苔根际菌(Rape rhizosphere)的相似性最大(97%),为同属.筛选菌Jll生长迅速,挂膜时间短.将其接种于生物滴滤反应器中,在甲硫醇进气流量为0.3 m3/h,质量浓度为40　mg/m3,运行仅4 d后,其去除率可逐渐升到100%.当进气流量分别为0.3,0.6和1.2 m3/h时,该反应器对甲硫醇的最大去除能力分别为36.2,41.8和16.4 　mg/(m3·h).反应器进气负荷提高到(96±3)　mg/(m3·h),运行一段时间后,恢复适宜的进气负荷,生物滴滤反应器对甲硫醇的去除率很快回升.这表明菌Jll不但降解能力高,而且抗逆性强.      

同时产甲烷反硝化颗粒污泥中微生物群落结构

在UASB成功运行同时产甲烷反硝化小试基础上,针对反应器内颗粒污泥,通过构建古菌和细菌的16SrDNA基因文库、RADAR遗传变异分型和测序比对等技术进行了微生物系统发育关系和群落结构分析.结果表明,在颗粒污泥的古菌中,产甲烷髦毛菌和产甲烷杆菌是主要菌群,随机选出的88个古菌克隆子,这两类古菌的16SrDNA序列分别占古菌总量71.59%和22.73%;而颗粒污泥中细菌的多样性要高于古菌,低GC革兰氏阳性菌和ε变型菌纲分支的细菌是细菌的主要菌群,在随机选出的133个细菌克隆子中,这2类细菌的16SrDNA序列分别占细菌总量的49.62%和12.03%.     

脱氮硫杆菌的分离鉴定和反硝化特性研究

从土壤中分离到1株高活性自养反硝化菌TD,并对其进行了鉴定和硝酸盐还原特性研究.该菌株为革兰氏阴性短杆菌,严格自养.16S rDNA序列分析表明.该菌株与ThiobaciUus denitrificans相似性为99.85%.结合生理生化特性和16S rDNA序列分析,确定菌株TD为脱氮硫杆菌.通过对该菌的生长特性和反硝化特性的研究表明,该菌在初始pH为6.85,32.8℃培养条件下脱氮效果最佳;在初始pH为6.90,29.5℃培养条件下生长最快.该菌生长比较缓慢,没有明显的稳定期,对数生长期阶段的反硝化能力最强,反硝化速率最快,达到了2.245 mg·(L·h)-1,在培养过程中培养基pH值明显下降.较高盐度对该菌株的反硝化活性有抑制作用.该菌株的急性毒性实验结果显示,脱氮硫杆菌对健康鱼体几乎无毒,属于无毒性菌株.     

改性煤矸石对上覆水磷及底泥磷代谢关键基因的影响

将热活化煤矸石和镧改性煤矸石应用于封闭水体除磷固磷试验,采用16SrRNA高通量测序技术分析底泥微生态群落结构、聚磷细菌和磷代谢功能基因的变化.结果表明：镧改性煤矸石对上覆水TP的去除能力最高,稳定期上覆水TP浓度为0.023~0.028mg/L,较对照组低83.5%以上,热活化煤矸石对上覆水TP的去除能力较差,稳定期上覆水TP浓度为0.15mg/L左右,略低于对照组.热活化煤矸石和镧改性煤矸石均提高了底泥中微生物多样性,变形菌门（Proteobacteria）和绿弯菌门（Chloroflexi）为底泥优势菌种.不同处理组底泥中聚磷细菌为Tetrasphaera和Candidatus_Accumulibacter,镧改性煤矸石显著降低了底泥中聚磷细菌的相对丰度.热活化煤矸石和镧改性煤矸石对多聚磷酸盐激酶（PPK）影响不大,但对外切聚磷酸酶（PPX）的抑制较大,热活化煤矸石抑制最大.     

Inhibition effect of magnetic field on nitrous oxide emission from sequencing batch reactor treating domestic wastewater at low temperature

This study aims to investigate the effect of a magnetic field on nitrous oxide(N_2O) emission from a sequencing batch reactor treating low-strength domestic wastewater at low temperature(10℃).After running for 124 days in parallel,results indicated that the conversion rate of N_2O for a magnetic field-sequencing batch reactor(MF-SBR) decreased by34.3% compared to that of a conventional SBR(C-SBR).Meanwhile,the removal efficiencies for total nitrogen(TN) and ammonia nitrogen(NH4-N) of the MF-SBR were 22.4% and 39.5% higher than those of the C-SBR.High-throughput sequencing revealed that the abundances of AOB(Nitrosomonas),NOB(Nitrospira) and denitrifiers(Zoogloea),which could reduce N_2O to N_2,were promoted significantly in the MF-SBR.Enzyme activities(Nir) and gene abundances(nos Z nir S and nir K) for denitrification in the MF-SBR were also notably higher compared to C-SBR.Our study shows that application of a magnetic field is a useful approach for inhibiting the generation of N_2O and promoting the nitrogen removal efficiency by affecting the microbial characteristics of sludge in an SBR treating domestic wastewater at low temperature.     

松花江表层沉积物中16种多环芳烃空间分布特征及生态风险评价

为揭示松花江干支流表层沉积物中16种PAHs（多环芳烃）的空间分布特征及其生态风险状况,采用气相色谱-质谱联用仪分析了2017年9月松花江干支流26个表层沉积物16种PAHs质量分数特征,并采用比值法对其污染来源进行解析,运用沉积物质量基准法和质量标准法评价其生态风险状况.结果表明:①松花江干支流表层沉积物中w（∑₁₆PAHs）为169.76~3 769.19 ng/g,以3~6环高环为主,并且支流w（∑₁₆PAHs）（范围为169.76~3 769.19 ng/g,平均值为1 598.41 ng/g）高于干流（范围为459.92~2 092.58 ng/g,平均值为1 173.67 ng/g）,呈从上游到下游逐渐降低的趋势.②松花江干支流表层沉积物中w（∑₁₆PAHs）主要来源于生物质燃烧和石油燃烧.③松花江干支流表层沉积物中w（∑₁₆PAHs）总体处于低生态风险水平,个别支流点位（3个）会发产生经常性生态风险.研究显示,松花江流域干支流表层沉积物中w（∑₁₆PAHs）呈从上游到下游逐渐降低的趋势,并且支流高于干流,但总体处于低生态风险水平.