人工湿地处理农村生活污水

采用无动力厌氧生化池+人工湿地模式处理某农村生活污水,运行结果表明,CODcr的去除率为80％,BOD5的去除率为85％,SS去除率为77％,出水水质均达到了《污水综合排放标准》(GB8978-1996)一级排放标准的要求.该工艺具有运行费用低、出水水质好、操作方便等优点.     

序批式移动床生物膜反应器富集反硝化聚磷菌及其在单污泥系统中的应用

本文介绍了在单污泥系统中选择和富集反硝化聚磷菌的国内外研究进展,对不同研究者提出的选择和富集反硝化聚磷菌的方法进行了分析和评价,并提出将反硝化聚磷菌与移动床生物膜反应器工艺结合起来,在序批式移动床生物膜反应器悬浮填料上选择和富集反硝化聚磷菌,进一步认识了反硝化聚磷菌的生化特征,使其成为反应器中优势菌群,以及该工艺今后的研究重点。     

崇明东滩夏季沉积物厌氧氨氧化菌群落结构与空间分布特征

为探索长江口崇明东滩表层沉积物中是否存在厌氧氨氧化菌以及厌氧氨氧化菌的群落结构与空间分布特征,以崇明东滩高、中、低潮滩夏季表层沉积物中总DNA为模板,PCR扩增沉积物样品中厌氧氨氧化菌特异性16S rDNA片段,通过克隆、测序,构建相应基因文库,将文库中有效克隆序列分别提交到GenBank中进行相似序列搜索,并利用MEGA5绘制系统发育树.分析结果发现,克隆序列CM-L-7和CM-L-18与已发现厌氧氨氧化菌Candidatus"Scalindua sp."同源性达98%,CM-L-13与Candidatus"Scalindua wagneri"同源性达94%,CM-M-6与Candidatus"Kuenenia sp."同源性达94%,CM-M-22与Anaerobicammonium-oxidizing planctomycete JMK-1的同源性达95%,CM-H-15与Candidatus"Kuenenia stuttgartiensis"的同源性达94%.表明,崇明东滩高、中、低潮滩表层沉积物中均存在厌氧氨氧化菌,但所属菌属不同,低潮滩以Candidatus"Scalindua"为主,中、高潮滩以Candidatus"Kuenenia"为主.相比之下,中潮滩厌氧氨氧化菌群落结构较为复杂.部分克隆序列与已发现厌氧氨氧化菌存在较大进化距离,表明崇明东滩可能还存在其他具有潜在厌氧氨氧化功能的细菌.     

沈阳市降雪中PFOS和PFOA污染现状调查

通过调查降雪中PFOS和PFOA的浓度,阐明了沈阳市大气中PFOS和PFOA的污染状况和污染规律.2006-02-06采集沈阳市区和郊区共计36个采样点的降雪样品,2006-02-25在其中5个采样点再次采集降雪样品.固相萃取融雪水中的PFOS和PFOA,利用LC-MS-SIM法测定样品中PFOS和PFOA浓度.全部样品中均检出PFOS和PFOA.2006-02-06降雪中PFOS和PFOA的浓度几何平均值分别为2.0 ng·L^-1（范围：0.4～46.2 ng·L^-1）和3.6 ng·L^-1（范围：1.6～22.4 ng·L^-1）,95%置信区间分别为1.5～2.8 ng·L^-1和3.1～4.2 ng·L^-1.PFOS和PFOA的最高浓度同时出现在郊区采样点朱尔屯,市中心区2种物质的浓度呈显著正相关.2006-02-25的5个采样点降雪中PFOS和PFOA的浓度几何平均值均为2.2 ng·L^-1.2次降雪中PFOS浓度差异不显著,2006-02-25降雪中PFOA浓度高于2006-02-06.结果表明,沈阳市区和郊区降雪中广泛存在PFOS和PFOA污染,局部区域可能存在共同的PFOS和PFOA污染来源;沈阳地区有较稳定的PFOS来源持续向大气中输送该类物质;PFOS和PFOA的环境行为可能不同.     

沸石强化生化装置脱氮功能的效果及机理初探

针对石化工业废水开展沸石强化脱氮处理试验研究,通过比较沸石浓度25mg/L与空白,以及沸石浓度25 mg/L与50mg/L两阶段脱氮效果,探讨沸石促进脱氮功能的机理,结果表明,曝气池中投加沸石可明显提高氨氮和总氮的去除率,硝化细菌总数和硝化功能也得到增强。与空白对照组相比, 沸石浓度25mg/L的试验组运行稳定后,氨氮去除率提高约10%~13%,总氮去除率约提高13%,出水中NO3--N含量约提高100%,氨氮与总氮之比下降6%,内源硝化耗氧呼吸速率可提高138%,硝化细菌总数是空白对照组2.2folds。沸石浓度提高到50mg/L后,试验组的脱氮效果略有增加,但效果不明显。通过对试验结果的关联分析,认为沸石提高系统脱氮能力的原因一方面是因为沸石对NH4+及硝态氮的交换吸附,另一方面NH4+离子富集于沸石表面及内部、沸石颗粒独特的好氧-缺氧微环境,以及沸石离解出CO32- 或HCO3-增加碱度等条件,促进了硝化细菌和反硝化细菌的生长,从而提高了系统脱氮能力。     

大气气溶胶中碘形态研究进展

大气中的碘直接影响对流层中多种光化学反应并间接影响全球气候变化,因而碘的大气化学机制研究受到越来越多关注.气溶胶中的碘是其大气化学反应的最终产物,通过其赋存形态可以推测和了解碘的大气化学过程.大气碘化学理论一直认为IO3-是大气碘沉降中最主要的碘形态,但近年来的各地实测数据发现大气气溶胶中的碘形态大多以可溶性有机碘或I-为主.这种分歧说明目前的大气碘化学理论尚有待完善.本文详细介绍了近年来碘的大气化学以及气溶胶颗粒物中碘形态的研究进展.     

羊草草原和贝加尔针茅草原生态系统呼吸的差异分析

应用静态暗箱-气相色谱法对羊草草原和贝加尔针茅草原的生态系统呼吸CO2通量进行了测算,分析了生态系统呼吸的影响因素,比较了2种草原生态系统呼吸的差异并分析了产生差异的原因.观测期间羊草草原生态系统呼吸CO2通量平均为(12.03±2.10)mg·(m2·min)-1,显著低于贝加尔针茅草原[(20.09±4.41)mg·(m2·min)-1];而羊草草原生物量显著大于贝加尔针茅草原(p0.001).羊草草原和贝加尔针茅草原生态系统呼吸都与温度(箱内气温、5cm和15cm地温)具有显著的指数函数关系.通过偏相关分析发现,在地温作为控制变量时,生态系统呼吸与土壤Eh、pH间不再具有显著的相关性,Eh、pH对CO2通量的影响可能是由地温变化间接引起的,而CO2通量与活体生物量呈现出了一定的相关性,与凋落物生物量无显著相关性.2种草原的CO2通量都可以用温度指数模型进行很好地模拟,基于地温的模拟效果(R2为0.568～0.639)显著好于基于箱内气温的(R2为0.323～0.426).地温是2种草原生态系统呼吸最重要的影响因素,它掩盖了地上部植物体对生态系统呼吸的影响.在该区域,土壤呼吸占生态系统呼吸比例较高,贝加尔针茅草原较高的有机质含量导致了其生态系统呼吸CO2通量较高.     

Effect of platinum on the photocatalytic degradation of chlorinated organic compound

TiO2 nanoparticles, doped with di erent Pt contents, were prepared by a modified photodeposition method using Degussa P-25 TiO2, H2PtCl6 6H2O and methanol as the solvents. The physicochemical properties of Pt/TiO2 were investigated by the nitrogen adsorption and desorption isotherm measurement technique, X-ray di raction analysis and photoluminescence spectra, respectively. Reaction rates from photocatalytic removal of dichloromethane over Degussa P-25 TiO2 and Pt/TiO2 were evaluated. The average diameter and BET surface area of the TiO2 catalyst particles were 300 nm and 50 m2/g, respectively. The degradation e ciency was 99.0%, 82.7%, 55.2%, and 57.9% with TiO2 at inlet concentrations of 50, 100, 200, and 300 ppm, respectively. And the degradation e ciency was 99.3%, 79.7%, 76.5%, and 73.4% with a 0.005 wt.% Pt/TiO2 at inlet concentrations of 50, 100, 200, and 300 ppm, respectively. In addition, we found that the photoluminescence emission peak intensities decreased with increases in the doping amount of Pt, which indicates that the irradiative recombination was weakened. Furthermore, the results showed that the UV/0.005 wt.% Pt/TiO2 process was capable of e ciently decomposing gaseous DCM in air.     

Removal of copper ions from aqueous solution by calcium alginate immobilized kaolin

Kaolin has been widely used as an adsorbent to remove heavy metal ions from aqueous solutions. However, the lower heavy metal adsorption capacity of kaolin limits its practical application. A novel environmental friendly material, calcium alginate immobilized kaolin (kaolin/CA), was prepared using a sol-gel method. The e ects of contact time, pH, adsorbent dose, and temperature on Cu2+ adsorption by kaolin/CA were investigated. The Langmuir isotherm was used to describe the experimental adsorption, the maximum Cu2+ adsorption capacity of the kaolin/CA reached up to 53.63 mg/g. The thermodynamic studies showed that the adsorption reaction was a spontaneous and endothermic process.     

Historical trends of heavy metal contamination and their sources in lacustrine sediment from Xijiu Lake, Taihu Lake Catchment, China

Concentrations of Cd, Cr, Cu, Pb, Zn and Hg in Xijiu Lake sediment from the Taihu Lake catchment, China, were analyzed. Their contamination state was investigated based on the geoaccumulation index and enrichment factors. Statistical analysis was used to differentiate the anthropogenic versus natural sources of heavy metals (HMs), and the anthropogenic accumulation fluxes were calculated to quantify anthropogenic contribution to HMs. The results indicated that the lake sediment had been heavily contaminated by Cd, enrichment of Zn and Hg was at a relatively high level, while that of Cu and Pb was in the lower-to-moderate level and Cr was in the low enrichment level. Sources of Cr in the sediment were mainly from natural inputs, while other metals, especially Cd, were predominantly derived from anthropogenic sources. In the past century, anthropogenic accumulation fluxes of Pb, Zn and Hg increased by 0.1-47.3 mg/(cm².yr), 2.4-398.1 mg/(cm².yr), and 3.7-110.3 ng/(m².yr), respectively, accounting for most inputs of HMs entering the sediment. The contamination state of HMs varied with industrial development of the catchment, which demonstrated that contamination started in the early 20th century, reached the maximal level between the mid-1970s and mid-1990s, and decreased a little after the implementation of constraints on high contamination industries, although the contamination of some HMs, such as Cd, Zn and Hg, is still at high levels.