固相微萃取模拟生物法用于养殖底泥多环芳烃污染监测的研究

本研究以养殖底泥中多环芳烃(PAHs)为研究对象,采用以聚二甲基硅氧烷(PDMS)为材料测定孔隙水中PAHs自由溶解态浓度(Cfree)的固相微萃取技术,以重要海水经济底栖生物菲律宾蛤仔(Ruditapes philippinarum)为参照生物,建立了PDMS中PAHs浓度与菲律宾蛤仔脂肪标化及底泥有机碳标化的PAHs浓度间的定量关系模型,进一步证明了基于固相微萃取的模拟生物法用于养殖区域中多环芳烃监测的可能性.结果表明,孔隙水中自由溶解态PAHs浓度(Cfree)显著低于孔隙水中总PAHs浓度(Cwater),且随着环数增加,两者间的差异越大,说明Cwater忽视了生物有效性,从而会高估孔隙水中PAHs的环境风险,因此,Cfree能更好地反映底泥孔隙水中PAHs的暴露水平;菲律宾蛤仔对PAHs的富集系数(BAF)及PDMS-水分配系数(KPDMS)均与辛醇-水分配系数(Kow)呈显著线性相关,且两者斜率相近,说明菲律宾蛤仔摄取PAHs的主要途径与PDMS相似,且PDMS中PAHs的浓度与生物体内PAHs的残留浓度和底泥有机碳标化的PAHs浓度间均呈现显著相关,说明当底泥孔隙水中和PDMS膜之间达到平衡时,固相微萃取模拟生物法可以用于计算底栖生物和沉积物中有机污染物,具有应用于养殖区域中多环芳烃监测的潜力,但有机污染物在生物体内转化和底泥性质对相关关系和监测应用的影响有待进一步研究.     

大亚湾浮游细菌的变性梯度凝胶电泳分析

于2010年12月以及2011年6月采集了大亚湾9个站点的表层水样,利用PCR-变性梯度凝胶电泳(PCR-DGGE)技术对浮游细菌DNA指纹进行了分析.结果显示,大亚湾海域浮游细菌DNA指纹比较丰富,冬季和夏季样品中分别共得到32条和33条条带,每个样品得到的条带数为18~25条.DNA指纹的Shannon-Weaver多样性指数(H')和Pielou均匀度(J)的变化范围分别为2.48~2.88和0.80~0.93.DNA指纹条带数与温度和盐度明显正相关,而与p H、DO、透明度呈明显负相关关系.结果说明PCR-DGGE技术可以在一定程度上反映细菌的群落结构和多样性,但需要与其他技术相结合方能较全面反映细菌的结构与功能.     

林州-安阳地区地下水三氮分布特征及其影响因素

本文分析了林州-安阳地区地下水的三氮分布特征,探讨了氮污染来源。运用Piper三线图、SPSS20软件,综合分析地下水化学特征,揭示氮循环作用机理。结果表明,研究区西北部主要为HCO_3-Ca-Mg型水,东部平原主要为HCO_3-Ca-Mg型水,其次为HCO_3-SO_4-Ca-Mg型、HCO_3-Cl-Ca型和HCO_3-Cl-Mg-Ca型水;氮污染源主要分布于林州市北部、安阳县北部、安阳市的东南部地区,其中农事活动、附近养殖场的畜禽排泄及污水排放是主要来源;地下水中存在着反硝化作用等氮的迁移转化现象,但是氮主要来源于附近的污染源。     

Reversibility of the structure and dewaterability of anaerobic digested sludge

The reversibility of the structure and dewaterability of broken anaerobic digested sludge(ADS)is important to ensure the efficiency of sludge treatment or management processes.This study investigated the effect of continuous strong shear(CSS)and multipulse shear(MPS)on the zeta potential,size(median size,d_(50)),mass fractal dimension(D_F),and capillary suction time(CST)of ADS aggregates.Moreover,the self-regrowth(SR)of broken ADS aggregates during slow mixing was also analyzed.The results show that raw ADS with d_(50) of 56.5μm was insensitive to CSS–SR or MPS–SR,though the size slightly decreased after the breakage phase.For conditioned ADS with d_(50) larger than 600μm,the breakage in small-scale surface erosion changed to large-scale fragmentation as the CSS strength increased.In most cases,after CSS or MPS,the broken ADS had a relatively more compact structure than before and d_(50) is at least 200μm.The CST of the broken fragments from optimally dosed ADS increased,whereas that corresponding to overdosed ADS decreased.MPS treatment resulted in larger and more compact broken ADS fragments with a lower CST value than CSS.During the subsequent slow mixing,the broken ADS aggregates did not recover their charge,size,and dewaterability to the initial values before breakage.In addition,less than 15%self-regrowth in terms of percentage of the regrowth factor was observed in broken ADS after CSS at average velocity gradient no less than 1905.6 sec~(-1).     

融雪对土壤溶解性有机质溶析作用的影响

利用土壤浸提实验和土柱淋洗实验,考察了化学离子的种类与浓度对进入融雪径流的土壤溶解性有机物(DOM)的含量和光谱学特性的影响,以及不同化学特征的积雪融化过程中土壤DOM的释放规律.土壤浸提实验结果表明,随着Na~+、Mg~(2+)和Ca~(2+)浓度的升高,土壤浸提液中的溶解性有机碳(DOC)浓度显著降低;随着Cl~-、SO_4~(2-)、Mg~(2+)和Ca~(2+)浓度的升高,土壤浸提液中波长254 nm处的紫外吸光度(UV-254)逐渐降低;随着Na~+和Mg~(2+)浓度的升高,土壤浸提液中单位浓度DOC的紫外吸收值(SUVA)值逐渐升高.NO_3~-、SO_4~(2-)和Na~+的浓度过高或过低时,土壤浸提液中DOM的类腐殖酸和类富里酸荧光峰强度较低;随着Cl~-、Mg~(2+)和Ca~(2+)浓度的升高,土壤浸提液中DOM的类腐殖酸荧光峰强度逐渐降低.土柱淋溶实验结果表明,类腐殖酸和类富里酸荧光物质是土壤淋滤液中的主要荧光物质.与纯水相比,融雪水作为淋洗液导致土壤淋滤液中DOC浓度的降低,以及类微生物代谢产物荧光峰强度的增高.冻融交替抑制DOM自土壤解吸进入淋滤液,并且导致土壤淋滤液中芳香族化合物相对含量的降低.     

石化废水易降解成分对活性污泥耗氧抑制毒性评价的干扰因素

为评价某石化混合废水的毒性,采用活性污泥耗氧速率抑制试验研究不同φ(石化废水)对活性污泥中不同菌群的抑制及其影响因素. 结果表明,所用石化废水对活性污泥中的硝化细菌具有明显毒性,其EC₅₀(半抑制效应浓度,以φ计)为9%左右;同时,该废水对异养菌的耗氧具有较强的促进作用,φ(石化废水)为100%时I_H(异养菌耗氧速率抑制率,131%)最高,这种促进作用对R_T(总耗氧速率)测定有显著影响(R=0.991,P<0.05),因此,仅以R_T评价废水毒性容易造成对废水真实毒性的低估. 5种常见易降解基质(乙酸钠、葡萄糖、甲醇、生活污水、丙酸钠)中,ρ(甲醇)为15 mg/L时对异养菌促进效果显著(P<0.05),促进率达50%以上;而在高浓度条件下,乙酸钠、葡萄糖、甲醇、丙酸钠对异养菌均有显著促进作用(P<0.05),R_H(异养菌耗氧速率)最高提高了182%. 研究显示,石化废水中的乙酸盐等易降解成分是活性污泥耗氧速率抑制试验的重要干扰因素.      

鄱阳湖沉积物有机磷形态及对水位变化响应

选取鄱阳湖枯水期不同高程出露表层沉积物,通过研究有机磷含量及形态差异,试图揭示江湖关系变化引起的水位下降对鄱阳湖沉积物有机磷潜在释放风险的影响.结果表明:1鄱阳湖枯水期表层沉积物有机磷含量(115.2~448.3 mg·kg-1)占总磷的19.3%~45.1%,有机磷含量空间分布呈"五河"入湖尾闾区高于湖心区和北部湖区.2鄱阳湖表层沉积物各形态有机磷含量大小顺序为:残渣态有机磷盐酸提取有机磷胡敏酸有机磷碳酸氢钠提取有机磷富里酸有机磷.3水位下降引起的沉积物出露时间延长是引起鄱阳湖不同高程沉积物有机磷形态变化的重要原因.沉积物出露时间越长,碳酸氢钠提取有机磷、盐酸提取有机磷与富里酸有机磷的含量越低,而胡敏酸有机磷和残渣态有机磷含量越高.同时,水位下降引起的沉积物出露时间延长致使活性有机磷和中活性有机磷占总有机磷比例下降,而非活性有机磷占总有机磷比例增加,反映了沉积物出露时间延长可能会促进有机磷形态由活性向非活性转化,在一定程度上能够降低沉积物有机磷的潜在性风险.     

超声辅助生物淋滤废旧Zn-C电池锌锰溶出的研究

以氧化硫硫杆菌(A.thiooxidans)为淋滤菌株对废旧Zn-C电池电极材料中的Zn、Mn进行了生物浸提,比较研究了化学浸提、生物淋滤和不同超声辅助方法生物淋滤体系下的Zn、Mn的溶出效率及溶出动力学.结果表明:不同超声辅助方法中,超声+生物淋滤体系Zn、Mn溶出最优,Zn、Mn的最大溶出率分别为94.2%和65.5%,并提高了溶释速率.此外,对于Mn的溶出,化学淋滤体系符合边界层扩散控制模型,生物淋滤和超声+生物淋滤体系符合收缩核Stoke's regime模型,而Zn的溶出均符合化学反应控制模型.     

Microbial bioavailability of dissolved organic nitrogen (DON) in the sediments of Lake Shankou, Northeastern China

Dissolved organic nitrogen(DON)extracted from Lake Shankou sediments using KCl was isolated into hydrophobic and hydrophilic fractions.The bioavailabilities of the hydrophobic and hydrophilic fractions to three types of bacterial communities collected from sediments,activated sludge and compost products were examined.The DON recoveries obtained by DAX-8 and cation exchange resins treatment were 96.17% ± 1.58% and 98.14% ±0% for the samples obtained from N4 and N14 stations,respectively.After 25 days of incubation at 25°C,most DON(59% to 96%)was degraded.Hydrophilic DON exhibited a higher reduction rate than hydrophobic DON during the growth phase.Untreated wastewater from Changshuihe town was the main degradable DON source to station N4,and 93% of hydrophilic DON and 80% of hydrophobic DON were degraded.Station N14 received a large amount of refractory DON from forest soils and exhibited DON degradation rates of 82% and 71% for the hydrophilic and hydrophobic fractions,respectively.Amino acid contents and fluorescence intensities were also analyzed.Approximately 27% to 74% of amino acids were taken up by day 5,and their concentration gradually increased in the following days due to the decomposition of dissolved proteins.Parallel factor analysis resulted in identification of tryptophan-like proteins,tyrosine-like proteins and FA-like substances.During the growth phase,40%–51% of the tryptophan-like proteins were taken up by bacteria,and the accumulation of tyrosine-like proteins was attributed to the release of biotic substances.The concentration of the FA-like substances decreased due to microbial decomposition.     

珠江口沉积物中重金属分布、形态特征及风险分析

为了解珠江口沉积物中重金属的污染现状及潜在生态危害,于2012年5月在珠江口海域采集29个站位表层沉积物,对6种重金属(Cr、Cu、Zn、As、Cd、Pb)的含量、形态特征、影响因素以及潜在生态风险进行了研究。本研究采用改进BCR提取法分析重金属赋存形态,并运用酸提取态百分含量风险评估法对重金属潜在生态风险进行评价。结果表明,珠江口沉积物中重金属总量呈现西北向东南逐渐减小的分布特征,西岸的浓度普遍高于东岸区域,重金属含量高值区主要分布于虎门、磨刀门、鸡啼门附近,陆源人为污染影响明显;重金属赋存形态中Cr、Cu、Zn、As主要以残渣态存在,Pb主要以可还原态存在,Cd主要以酸提取态存在,各重金属非残渣态所占比例以Cd最高,表明Cd的迁移性最强;以酸提取态百分含量为依据进行的珠江口沉积物重金属的风险评价,结果显示虽然Cd的绝对含量不高,但其潜在危害等级为高风险,其余重金属为中-低-无风险等级。