制革废水处理过程中磺胺类抗生素和抗性细菌的分布特征

针对两家制革厂废水处理过程中3种磺胺类抗生素和磺胺类抗性细菌的丰度和分布特性以及两个不同工艺污水处理厂对抗生素的去除规律做了相关研究.结果表明,3种抗生素在两家制革污水处理过程中均有检出,水样中3种抗生素的总质量浓度在59.1~706.7 ng·L~(-1)之间;两家制革厂废水处理剩余污泥中3种抗生素的总含量分别为4 388 ng·kg~(-1)和2 979.4ng·kg~(-1),与市政污水处理厂中的抗生素含量相差不大.不同的污水处理工段对3种抗生素去除效果不同,但去除效率均大于70%.生物处理单元对抗生素的去除率相对较高,而厌氧池是去除抗生素的主要阶段(去除率50%).两个制革厂的进出水和剩余污泥中共筛选出8株抗性细菌,这8个分离菌株可分为5个菌属.进出水中的抗性细菌含量介于9.37×10~3~5.08×10~5CFU·mL~(-1)之间,剩余污泥中的磺胺类抗性细菌含量较高分别为1.17×10`7CFU·g~(-1)和7.2×10~6CFU·g~(-1).两个制革污水处理厂对磺胺甲唑抗性细菌的去除率分别达到了1.34 log和2.15 log.     

基于稳定碳同位素技术的干旱区绿洲土壤有机碳向无机碳的转移

应用稳定碳同位素技术测定土壤无机碳稳定碳同位素组成(soil inorganic carbonδ13C,SICδ13C),并对干旱区绿洲土壤无机碳进行区分,结合土壤有机碳(soil organic carbon,SOC)与SIC含量关系进一步探讨SOC向SIC转移的碳量.结果表明,4种类型土壤SICδ13C值差异性极显著(P0.01),风沙土SICδ13C值最高且为正,均值为(0.32±0.04)‰,随土层深度增加而增加,说明风沙土原生性碳酸盐占绝对优势;灌漠土、棕漠土和盐碱土SIC的δ13C均值分别(-0.30±0.24)‰、(-1.96±0.66)‰和(-1.24±0.49)‰,随土层变化均呈先降低后逐渐增大的趋势,说明灌漠土原生性碳酸盐占优势,棕漠土和盐碱土发生性碳酸盐相对前者占优势.风沙土、灌漠土、棕漠土和盐碱土的发生性碳酸盐占SIC比例均值分别为1.33%、4.72%、15.01%、35.71%,均小于50%,说明干旱区绿洲土壤发生性碳酸盐比例总体水平较低.风沙土、灌漠土、棕漠土和盐碱土在土壤发生性碳酸盐形成或重结晶过程中固定土壤CO2的量分别为0.30、2.44、4.96、12.40 g·kg~(-1),其中固定来自大气CO2量平均为0.18、0.79、1.45、8.67 g·kg~(-1),来自SOC氧化分解转化为CO2的量分别为0.06、0.83、1.62、1.86g·kg~(-1),说明盐碱土、棕漠土SOC的贡献相对较高,灌漠土、风沙土较低;对土壤固定CO2量的来源比较发现,风沙土、盐碱土固定土壤CO2的量来自大气CO2量较高,SOC的贡献较低,而灌漠土、棕漠土固定来自SOC氧化分解CO2的量较高,大气贡献较低.研究区整体SOC向SIC的碳转移量介于0.03~2.38 g·kg~(-1)之间,平均每千克土壤固定1.09 g的CO2,说明干旱区绿洲土壤发生性碳酸盐所占比例较低,SOC的贡献较少.     

合肥市典型交通干道大气苯系物的特征分析

为研究合肥市交通干道大气苯系物污染状况,采用自主研制的差分吸收光谱(DOAS)系统,于2016年3月期间对合肥市交通主干道大气苯系物(苯、甲苯、间二甲苯和邻二甲苯)以及常规污染物NO_2、SO_2等进行了连续观测.观测结果显示,观测期间苯、甲苯、间二甲苯和邻二甲苯的平均浓度分别为:21.7、63.6、33.9和98.7μg·m~(-3).与国内外其它城市比较显示,合肥市交通干道大气苯和甲苯的污染处于中等水平,二甲苯的污染较为严重.结合观测期的间风速风向、T/B特征比值以及与CO等污染物的相关性,对上述苯系物来源进行了分析,结果显示观测期间T/B值为0.8~4.5,苯、甲苯与CO的相关性系数R分别为0.55和0.34.表明机动车尾气排放是观测区域苯和甲苯的主要排放源之一,同时也受到周边工业园区排放的影响,二甲苯的主要排放源为观测地点北偏东方向的涂料行业工业园区.苯和甲苯的夜间高浓度峰值分析结果表明,夜间的高浓度苯和甲苯可能主要来源于观测地点周边工业园区的排放.观测区域苯系物的臭氧生成潜势(OFP)表现为邻二甲苯间二甲苯甲苯苯,其中二甲苯的OFP占总OFP的85%,表明周边工业园区的排放对该地区臭氧生成的贡献较大.     

塔里木盆地北缘绿洲不同连作年限棉田土壤有机碳、无机碳含量与环境因子的相关性

农田土壤碳库是土壤碳库的重要组成部分,易受人类活动调节且固碳减排潜力巨大,研究土壤有机碳、无机碳含量特征及其与环境因子的关系有助于深入理解土壤生态过程,为全球碳收支平衡研究提供理论支持.本文以塔里木盆地北缘绿洲为靶区,分析土壤碳库特征,结合冗余分析、通径分析,探究土壤有机碳、无机碳含量及其与环境因子的相关关系.结果表明:(1)同一土层不同连作年限棉田土壤有机碳、无机碳含量存在显著差异(P0.05),随连作年限增加,有机碳含量呈先增加后减少趋势,而无机碳含量呈先减少后增加趋势;同一连作年限棉田不同土层土壤有机碳、无机碳含量存在显著差异(P0.05),有机碳含量均在0~20 cm层达到最大值,而无机碳含量均在20~50 cm层达到最大值.(2)通过冗余分析得出环境因子对土壤碳库特征影响的重要性排序为:磷酸酶活性p H值蔗糖酶活性过氧化氢酶活性全氮速效磷速效钾土壤含水量脲酶活性电导率;磷酸酶活性、p H值、蔗糖酶活性、过氧化氢酶活性、全氮、速效磷、速效钾与土壤有机碳、无机碳含量呈极显著相关关系(P0.01);土壤含水量、脲酶活性与土壤有机碳、无机碳含量表现为显著相关(P0.05).(3)通径分析表明,速效钾对有机碳含量直接作用显著,是影响有机碳含量的主要因素,而脲酶活性对无机碳含量直接作用显著,是影响无机碳含量的主要因素.干旱半干旱区土壤有机碳、无机碳含量研究是评价农田生态系统土壤碳的"源/汇"效应的基础数据,对研究全球碳收支平衡和陆地碳循环机制具有重要意义.     

长期侧流提取对EBPR系统除磷及其磷回收性能的影响

实验采用交替厌氧/好氧(An/O)运行模式的SBR反应器,考察310 d内分3个批次提取侧流比为0、1/4、1/3、1/2的厌氧放磷上清液后EBPR系统的脱氮除磷效果及相应的磷回收性能.结果表明,整个实验阶段系统对COD和氨氮的去除较为稳定,出水均能满足《城镇污水处理厂污染物综合排放标准》一级A标准,总氮去除因厌氧阶段反硝化不断增强有所提升,达标率由88.2%显著上升至98.6%.然而,随着厌氧上清液提取次数的增多,系统释磷能力整体下降,但前两个批次中系统除磷均稳定高效,去除率在90%以上,相应地出水磷达标率大于75%,仅第3批次实验中侧流比为1/2时系统除磷率出现大幅波动,最低降为54.2%,并贡献该批次出水磷不达标率的60%,说明长期提取1/2侧流比不利于主流工艺出水稳定维持.研究还发现,长期进行侧流磷回收实验有利于污泥减量,且对污泥沉降性能影响不大.因此,在EBPR系统内长期提取适当侧流比的厌氧上清液以进行磷回收与主流工艺同步高效脱氮除磷具有可行性.     

Carbonaceous and nitrogenous disinfection byproduct precursor variation during the reversed anaerobic–anoxic–oxic process of a sewage treatment plant

Disinfection byproduct(DBP)precursors in wastewater during the reversed anaerobic–anoxic–oxic(A~2/O)process,as well as their molecular weight(MW)and polarity-based fractions,were characterized with UV scanning,fluorescence excitation emission matrix,Fourier transform infrared and nuclear magnetic resonance spectroscopy.Their DBP formation potentials(DBPFPs)after chlorination were further tested.Results indicated that the reversed A~2/O process could not only effectively remove the dissolved organic carbon(DOC)and dissolved total nitrogen in the wastewater,but also affect the MW distribution and hydrophilic–hydrophobic properties of dissolved organic matter(DOM).The accumulation of low MW and hydrophobic(HPO)DOM was possibly due to the formation of soluble microbial product-like(SMP-like)matters in the reversed A~2/O treatment,especially in the anoxic and aerobic processes.Moreover,DOM in the wastewater displayed a high carbonaceous disinfection byproduct formation potential(C-DBPFP)in the fractions of MW100 k Da and MW5 k Da,and revealed an increasing tendency of nitrogenous disinfection byproduct formation potential(N-DBPFP)with decrease of MW.For polarity-based fractions,the HPO fraction of wastewater showed significantly higher C-DBPFP and N-DBPFP than hydrophilic and transphilic fractions.Therefore,although the reversed A~2/O process could remove most DBP precursors by DOC reduction,it led to the enhancement of DBPFP with the formation and accumulation of low MW and HPO DOM.In addition,strong correlations between C-DBPFPs and SUVA,and between N-DBPFPs and DON/DOC,were observed in the wastewater,which might be helpful for DBPFP prediction in wastewater and reclaimed water chlorination.     

Concurrent catalytic removal of typical volatile organic compound mixtures over Au-Pd/α-MnO2 nanotubes

α-MnO_2 nanotubes and their supported Au-Pd alloy nanocatalysts were prepared using hydrothermal and polyvinyl alcohol-protected reduction methods, respectively. Their catalytic activity for the oxidation of toluene/m-xylene, acetone/ethyl acetate, acetone/m-xylene and ethyl acetate/m-xylene mixtures was evaluated. It was found that the interaction between Au-Pd alloy nanoparticles and α-MnO_2 nanotubes significantly improved the reactivity of lattice oxygen, and the 0.91 wt.% Au0.48 Pd/α-MnO_2 nanotube catalyst outperformed the α-MnO_2 nanotube catalyst in the oxidation of toluene, m-xylene, ethyl acetate and acetone. Over the0.91 wt.% Au0.48 Pd/α-MnO_2 nanotube catalyst,(i) toluene oxidation was greatly inhibited in the toluene/m-xylene mixture, while m-xylene oxidation was not influenced;(ii) acetone and ethyl acetate oxidation suffered a minor impact in the acetone/ethyl acetate mixture; and(iii) m-xylene oxidation was enhanced whereas the oxidation of the oxygenated VOCs(volatile organic compounds) was suppressed in the acetone/m-xylene or ethyl acetate/m-xylene mixtures. The competitive adsorption of these typical VOCs on the catalyst surface induced an inhibitive effect on their oxidation, and increasing the temperature favored the oxidation of the VOCs. The mixed VOCs could be completely oxidized into CO_2 and H_2 O below 320°C at a space velocity of 40,000 m L/(g·hr). The 0.91 wt.% Au0.48 Pd/α-MnO_2 nanotube catalyst exhibited high catalytic stability as well as good tolerance to water vapor and CO_2 in the oxidation of the VOC mixtures. Thus, the α-MnO_2 nanotube-supported noble metal alloy catalysts hold promise for the efficient elimination of VOC mixtures.     

Insights into the formation of secondary organic carbon in the summertime in urban Shanghai

To investigate formation mechanisms of secondary organic carbon(SOC) in Eastern China,measurements were conducted in an urban site in Shanghai in the summer of 2015. A period of high O_3 concentrations(daily peak 120 ppb) was observed, during which daily maximum SOC concentrations exceeding 9.0 μg/(C·m~3). Diurnal variations of SOC concentration and SOC/organic carbon(OC) ratio exhibited both daytime and nighttime peaks. The SOC concentrations correlated well with O_x(= O_3+ NO_2) and relative humidity in the daytime and nighttime, respectively, suggesting that secondary organic aerosol formation in Shanghai is driven by both photochemical production and aqueous phase reactions. Single particle mass spectrometry was used to examine the formation pathways of SOC. Along with the daytime increase of SOC, the number fraction of elemental carbon(EC) particles coated with OC quickly increased from 38.1% to 61.9% in the size range of 250–2000 nm, which was likely due to gas-to-particle partitioning of photochemically generated semi-volatile organic compounds onto EC particles. In the nighttime, particles rich in OC components were highly hygroscopic, and number fraction of these particles correlated well with relative humidity and SOC/OC nocturnal peaks. Meanwhile, as an aqueous-phase SOC tracer, particles that contained oxalate-Fe(III) complex also peaked at night. These observations suggested that aqueous-phase processes had an important contribution to the SOC nighttime formation. The influence of aerosol acidity on SOC formation was studied by both bulk and single particle level measurements, suggesting that the aqueous-phase formation of SOC was enhanced by particle acidity.     

金属软管爆裂失效分析

某厂压缩机出口管线处金属软管的设计压力为6.3 MPa,试压时金属软管接头与接头套处发生爆裂,爆裂压力为4.2 MPa。通过对金属软管爆裂处进行宏观检查与测厚、化学成分分析、断口分析、X射线能谱分析以及焊接形式分析,判定金属软管爆裂的主要原因是活套法兰侧接头与波纹管连接焊缝结构不合理导致焊缝承载能力不足,焊缝存在严重未焊透、焊材选用不合理,进一步导致了焊缝承载能力的下降。最后,提出了针对性预防措施。     

13C脉冲标记法定量冬小麦光合碳分配及其向地下的输入

研究冬小麦生长向地下部分的输入对于土壤固碳和作物生产具有重要意义.分别在分蘖期、拔节期、花期和灌浆期,用~(13)CO2对冬小麦进行脉冲标记7 h,标记结束后28 d(示踪期)破坏性取样,测定冬小麦地上部、根、土壤和土壤呼吸中的~(13)C含量等指标.研究结果表明,在各标记时期,冬小麦光合固定的~(13)C大部分保留在地上部(51.6%~90.8%),且随小麦生长的进行而逐渐向地上部分配,向地下部分(根系、土壤和根际呼吸)的转移随生长进程的延续而降低.转移到地下部的~(13)C中,有22.9%~65.3%被根际呼吸消耗,24.3%~59.3%在根部保存,10.4%~17.8%通过根际沉积转化为土壤有机碳.示踪期28d内最后2 d呼吸产生的~(13)C只占整个示踪期根际呼吸~(13)C量的0.7%~2.7%,说明28 d的示踪期可以确保光合碳在各系统分配完全.在整个生育期内,冬小麦净吸收的光合碳分配到地上部、根部、土壤有机碳和根际呼吸的比例分别为78.5%、6.0%、3.1%和12.4%.结合当地生产方式估算,冬小麦在整个生育期内输入到地下的总碳量为1.72 t·hm~(-2),其中有0.99t·hm~(-2)被根际呼吸消耗,根部固持碳量为0.48 t·hm~(-2),0.25 t·hm~(-2)以有机碳沉积的形式进入土壤.