Eutrophication development and its key regulating factors in a water-supply reservoir in North China

Yanghe Reservoir is an important source of drinking water for Qinhuangdao City,North China;however,in recent decades this water source has been eutrophic with recurrent summer cyanobacterial blooms.The trophic grade of the system in summer was mesotrophiceutrophic in 1990 and became hypertrophic in 2011.The nutrient availability is extremely high during the entire year,and the water temperature should be the primary driver of the summer blooms.In May-October of 2010 and 2011,abrupt variations were observed in the Secchi depth(SD) and chlorophyll a(Chl-a),and both the correlated analysis of Chl-a-SD and trophic status indices(TSI) deviation(TSI Chl-a-TSI SD) showed that algal cell density dominated light attenuation.During the algal bloom outbreak,the microcystin concentration was found to vary between 0.35-2.12 μg/L in 2010 and 0.11-1.86 μg/L in 2011.The maximum microcystin content was more than two times the safety limit required for drinking water.Inflow discharges were most concentrated in the summer,with periods of lower residence time and the largest water level fluctuation over the entire year.When a high availability of nutrients promoted a high Chl-a concentration in the whole system,it appeared that the instability caused by the decrease in residence time could not produce effective changes in the cyanobacterial abundance.The results indicated that nutrient enrichment in the aquatic systems of Yanghe Reservoir is the most serious problem and that the status would not been modified effectively by increasing hydrological fluctuations(e.g.,decreasing the residence time).Therefore,decreasing the nutrient concentrations is the only route to improve the water quality of this reservoir.     

溶解氧变化对底泥酶活性及微生物多样性的影响

采用室内静态实验考察了溶解氧变化对底泥酶活性影响,同时采用BIOLOG ECO微平板构造了不同溶解氧水平下底泥微生物多样性指数。结果表明:高溶解氧条件下,底泥多酚氧化酶及过氧化物酶活性显著高于缺氧条件及厌氧条件(P<0.01),脱氢酶活性高于背景值;厌氧条件下脱氢酶、脲酶及碱性磷酸酶活性显著高于高溶解氧组、缺氧组及背景值(P<0.05);缺氧条件下硝酸盐还原酶活性显著高于高溶解氧组及厌氧组(P<0.05);蛋白酶活性受溶解氧水平变化的影响较小。BIOLOG ECO微平板法分析表明,溶解氧变化对底泥微生物多样性有不同程度的负面影响,微生物多样性的降低程度从大到小依次为高溶解氧组>厌氧组>缺氧组。主成分分析结果表明:缺氧条件及厌氧条件下,底泥微生物对大分子有机物的利用出现不同程度的降低,相对地,高溶解氧条件下微生物对大分子有机物的利用程度呈现先下降后上升的趋势;高溶解氧组及缺氧组底泥微生物对碳水化合物利用程度升高,厌氧组对碳水化合物利用程度降低。总之,高溶解氧条件更有利于形成底泥有机物完整的代谢循环,提高大分子有机物的利用程度。     

无锡市大气中类二噁英多氯联苯污染水平

为了了解无锡市大气中类二噁英多氯联苯(Dioxin-like PCBs,DL-PCBs)水平,利用大流量空气采样器在无锡市分别采集了6个气相和6个颗粒相大气样品,气相色谱-质谱(GC-NCI-MS)测定样品中12种类二噁英多氯联苯。结果显示,大气样品中∑_(12)DL-PCBs的总浓度(气相+颗粒相)为1157～2 747 fg/m³,平均浓度为1759 fg/m3,平均浓度为1759 fg/m³。其中,气相的浓度为11 124～2 721 fg/m3。其中,气相的浓度为11 124～2 721 fg/m³,平均值为1 701fg/m3,平均值为1 701fg/m³;颗粒相的浓度为26～143 fg/m3;颗粒相的浓度为26～143 fg/m³,平均值为58fg/m3,平均值为58fg/m³。气相中∑_(12)DL-PCB含量占总量的97%,而颗粒相仅占3%。DL-PCBs的总毒性当量(气相+颗粒相)为2.16～4.47fg TEQ/m3。气相中∑_(12)DL-PCB含量占总量的97%,而颗粒相仅占3%。DL-PCBs的总毒性当量(气相+颗粒相)为2.16～4.47fg TEQ/m³,平均值为3.53fg TEQ/m3,平均值为3.53fg TEQ/m³。DL-PCBs单体中PCB-118的浓度最高,平均占总浓度的54%,其次是PCB-105和PCB-77,PCB+81在所有样品中均未检出。在所有DL-PCBs中,毒性当量浓度的主要贡献者为PCB-126,其平均贡献率为95%,其次为PCB-169,平均贡献率为3%。     

测定总氮中影响因素的探讨

本文研究了过硫酸钾氧化紫外分光光度法测定总氮的过程中,通过标准曲线、标准物质、具体试样的一系列测定探讨,发现试剂、实验用水、实验器皿、实验环境等对测定结果有很大影响。     

厦门石兜-坂头水库水体营养状态综合评价及变化趋势分析

以水质监测资料为基础,采用综合营养状态指数法（TLI法）和线性插值评分法（SCO法）2种模式,相互印证并综合评价2008．5—2011．6厦门石兜-坂头水库库区水体营养状态。应用Daniel的趋势检验,对评价时段内水库水体营养状态和水质参数（总氮、总磷以及氮磷浓度比）变化趋势进行分析。结果表明：2008年5月-2011年6月期间,石兜-坂头水库水体营养状态为中营养至轻-中度富营养;在此评价期内,总磷、总氮、氮磷比值趋势变化不显著;水体营养状态变化趋势也没有显著意义,始终在中营养至（轻-中度）富营养状态区间波动。水库周边环境及水质的监管措施能否及时到位是影响库区水体营养状态变化的关键。     

核电可持续发展与低中放固体废物安全管理

核事故与放射性废物安全管理是核电可持续发展的两大制约因素。本文针对目前核电厂面临的积存的低中放固体废物超出暂存库设计容量和时间的困境,分析核电持续发展带来的放射性固体废物的处置需求和放射性风险,深入探讨了我国低中放固体废物处置现状和存在的问题,认为问题存在的深层原因主要是废物处置责任划分不明确、核电发展与放射性废物管理的国家职能存在割离,在此基础上提出加快出台放射性固体废物处置选址规划、建立独立的放射性固体废物贮存和处置公司、建立和完善放射性废物管理基金制度等政策建议。     

水位变化对湖泊沉积物营养释放的影响

水位波动可有效调节湖泊生态系统的结构与功能,干湿交替过程引起的沉积物生物地球化学循环途径的改变是其重要机制之一。大量研究结果表明,干湿交替将加速沉积物有机碳的分解,强化沉积物硝化与硝化作用的偶联,促进沉积物磷的酶促水解和厌氧解离,从而增加再度淹没之后水中溶解有机碳和生物可利用性磷的浓度,并减少溶解无机态氮的浓度。有机质的分解是上述过程的关键步骤。因此,必须系统描述湖泊水陆界面土壤和沉积物基本理化性状与水生生物特征,分析干旱过程中沉积物生物地球化学循环途径的变化,了解淹没过程中水柱营养状态与浮游生物群落对沉积物营养释放的响应,从而揭示水位波动调控富营养化过程的机制,即诱发营养脉冲或维系其持续补给,改变营养阈值,进而导致稳态转换。     

全氟辛烷磺酸(PFOS)对斑马鱼卵黄蛋白原mRNA水平的影响

为了研究环境低剂量全氟辛烷磺酸（perfluorooctane sulfonate,PFOS）对水生生物的内分泌干扰效应和可能的作用机制,测定了PFOS对斑马鱼（Brachydanio rerio）肝脏中卵黄蛋白原（vitellogenin,VTG）mRNA水平的影响.将斑马鱼暴露于4个PFOS的环境低剂量浓度组（0.1、1、10、100μg.L-1）中进行21d毒性试验,收集肝脏样品,提取RNA,采用荧光定量PCR（qRT-PCR）分别检测VTG1和VTG3的mRNA水平.结果表明：①PFOS暴露引起雄性斑马鱼肝脏VTG1和VTG3 mRNA水平升高,VTG1 mRNA水平升高与剂量呈正相关,在100μg.L-1暴露浓度处与对照组呈现显著性差异;VTG3的mRNA水平变化与剂量呈倒U型曲线,呈现典型的毒物刺激荷尔蒙效应,在10和100μg.L-1暴露浓度处与对照组呈现显著性差异;②PFOS暴露引起雌性斑马鱼肝脏中VTG1 mRNA水平升高,在10μg.L-1暴露浓度处与对照组呈现显著性差异,但在高浓度（10和100μg.L-1）处试验结果误差较大;VTG3 mRNA水平只在10μg.L-1暴露浓度处升高,但相比于对照组均没有显著性差异.试验结果表明PFOS暴露对斑马鱼的内分泌干扰作用明显,其毒性作用机制可能是类雌激素效应,而肝脏中VTG1和VTG3mRNA水平可能作为PFOS内分泌干扰效应评价的敏感生物标志物,但VTG1和VTG3 mRNA水平的响应曲线呈现基因亚型和性别差异.     

石油化工行业可接受风险水平研究

石油化工行业存在着巨大的潜在风险,为了明确该行业的风险可接受水平,制定一个合理可行的可接受风险准则极为必要.本文在对国内外风险可接受水平研究的基础上,系统分析了国内外有关标准,对生命风险水平、经济风险水平和环境风险水平确定的基本思想进行了详尽阐述,分别给出了3种风险的可接受水平公式,提出了确定石化行业可接受风险水平的方法,需同时满足可接受生命风险、经济风险和环境风险.     

Emissions of SO2, NO and N2O in a circulating fluidized bed combustor during co-firing coal and biomass

This paper presents the experimental investigations of the emissions of SO2, NO and N2O in a bench scale circulating fluidized bed combustor for coal combustion and co-firing coal and biomass. The thermal capacity of the combustor is 30 kW. The setup is electrically heated during startup. The influence of the excess air, the degree of the air staging, the biomass share and the feeding position of the fuels on the emissions of SO2, NO and N2O were studied. The results showed that an increase in the biomass shares resulted in an increase of the CO concentration in the flue gas, probably due to the high volatile content of the biomass. In co-firing, the emission of SO2 increased with increasing biomass share slightly, however, non-linear increase relationship between SO2 emission and fuel sulfur content was observed. Air staging significantly decreased the NO emission without raising the SO2 level. Although the change of the fuel feeding position from riser to downer resulted in a decrease in the NO emission level, no obvious change was observed for the SO2 level. Taking the coal feeding position R as a reference, the relative NO emission could significantly decrease during co-firing coal and biomass when feeding fuel at position D and keeping the first stage stoichiometry greater than 0.95. The possible mechanisms of the sulfur and nitrogen chemistry at these conditions were discussed and the ways of simultaneous reduction of SO2, NO and N2O were proposed.