日本污水脱氮除磷深度处理工艺分析

为提高进入琵琶湖水体水质和有效恢复并保持琵琶湖流域水生态环境,日本滋贺县10家下水道污水处理厂全部采用脱氮除磷深度处理工艺。湖南中部净化中心目前规模为26.85万t/d,采用缺氧-好氧循环硝化/反硝化(AO)、厌氧-缺氧-好氧(AAO)和多段进水多级缺氧-好氧硝化/反硝化(SMAO)3种深度处理工艺。AAO工艺是国内城镇污水处理厂广泛采用的二级生化工艺,AO、SMAO工艺在国内还没有应用实例。AO、AAO工艺采用内循环硝化/反硝化反应脱氮,SMAO工艺采用无内循环的多段进水多级硝化/反硝化反应脱氮。AO、SMAO工艺采用化学方式除磷,PAC添加浓度约50 mg/L。AAO工艺采用化学和生物组合方式除磷,PAC添加浓度降低到约30 mg/L。AO、AAO工艺出水BOD、CODMn、SS、TN和TP均值分别约为0.9 mg/L、5.2 mg/L、99.5%、78.0%和98.1%。SMAO工艺出水TN约为2.5 mg/L,TN去除率提高到91.6%,其他指标和AO、AAO工艺基本相同。     

生物表面活性剂合成条件的优化及提取方法

利用油平板筛选法和排油圈法从辽河某油田的土壤样品中分离筛选高效的生物表面活性剂产生菌, 通过16S rRNA基因序列分析对所筛选菌株进行鉴定。采用L16(45)正交实验对所筛选菌株合成生物表面活性剂的条件进行优化。比较5种提取方法对发酵液中生物表面活性剂的提取效果。共分离得到17株菌,其中菌株A3、As和Y产表面活性剂的能力最强。16S rRNA基因序列分析表明,这3株菌均为假单胞菌属(Pseudomonas)。菌株A3、As、Y和 A3-As混合菌的生物表面活性剂提取量较优化前有明显的提高,其产量分别是优化前的8.4倍、6.4倍、5.6倍和5.7倍,其中,菌株As的生物表面活性剂产量最高,可达20.55 g/L。对于3种纯菌和A3-As混合菌而言,5种提取方法中均以CHCl3萃取的量最高;而对其他混合菌,5种提取方法的差别并不显著。菌株A3、As、Y均属于高效的生物表面活性剂产生菌,具有很好的应用前景。     

MFC-MBR耦合系统运行效果及产电性能

为了解决膜生物反应器（MBR）运行成本高、膜污染的问题,本研究建立了一个微生物燃料电池（MFC）-MBR耦合系统,通过MFC回收污水中的能量,同时控制膜污染。研究结果表明,耦合系统对COD和NH3-N的去除率分别为（94.6±3.0）%和（90.9±6.9）%,出水水质稳定。由于MFC的耦合作用,使MBR的运行周期由18 d延长至36 d,膜污染得到了明显的减缓。耦合系统中MFC产电性能稳定,电流密度稳定在5.7 A/m3,最大功率密度达到了928.0 mW/m3,循环伏安法（CV）表明,阴极附着的微生物具有良好的电化学催化作用。MFC-MBR耦合系统将污水中的化学能转化为电能从而实现了膜污染的减缓及能量的回收,显示出巨大的发展前景。     

牡丹江流域水质变化趋势及水环境污染特征研究

通过对牡丹江近10年水质监测、评价及变化趋势研究,采用单项污染指数评价法、环境功能区达标评价法,评价牡丹江丰水期、平水期、枯水期水质现状,给出超标项目与超标倍数,计算污染分担率、污染负荷比,绘制主要污染物各断面浓度变化图,总结牡丹江污染特点和水质变化趋势,得出牡丹江水环境污染特征,为环境管理提供科学依据。     

Detection of tritium sorption on four soil materials

In order to measure groundwater age and design nuclear waste disposal sites, it is important to understand the sorption behavior of tritium on soils. In this study, batch tests were carried out using four soils from China: silty clays from An County and Jiangyou County in Sichuan Province, both of which could be considered candidate sites for Very Low Level Waste disposal; silty sand from Beijing; and loess from Yuci County in Shanxi Province, a typical Chinese loess region. The experimental results indicated that in these soil media, the distribution coefficient of tritium is slightly influenced by adsorption time, water/solid ratio, initial tritium specific activity, pH, and the content of humic and fulvic acids. The average distribution coefficient from all of these influencing factors was about 0.1-0.2 mL/g for the four types of soil samples. This relatively modest sorption of tritium in soils needs to be considered in fate and transport studies of tritium in the environment.     

南京市城市生活垃圾分类收集问卷调查

围绕南京市城市生活垃圾分类收集的问卷调查展开，揭示了南京市生活垃圾收集开展的现状，分析了其间存在的问题及成因，提出了相应的改进意见和解决办法，为生活垃圾分类收集在全国的推广提供了依据。     

城市供水中藻类去除技术的研究进展

日趋严重的水体富营养化已成为全球性的环境问题,藻类及其副产物给传统净水工艺带来了诸多不利影响,增加了水处理难度。本文对饮用水中藻类各种去除技术进行了具体的论述,并系统分析各技术去除效果、局限性,展望了藻类去除技术发展前景。指出目前控制饮用水中藻类污染必须将水源污染综合治理、强化预氧化工艺、优化常规工艺结合起来。     

粉煤灰增钙渣水泥试验研究

提出了粉煤灰增钙渣水泥的最佳配合比及工艺技术参数。并介绍了该品种水泥的物理力学性能，为粉煤灰增钙渣水泥的生产与应用提供了一定的依据     

杭州湾表层海水营养盐分布特征及富营养化状况研究

根据2015年3月和8月杭州湾的海水质量监测数据,分析了该海域的营养盐分布特征以及富营养化状况,结果表明:杭州湾表层海水无机氮变化范围为0.36~4.22 mg/L,活性磷酸盐的含量范围为0.014~1.51 mg/L,化学需氧量含量范围为0.56~3.18 mg/L.该海域无机氮和活性磷酸盐超标严重,表层海水已处于重度富营养化状态,调查站位EI均大于1.该海域表层海水无机氮、活性磷酸盐、化学需氧量和富营养化指数高值区均与陆源入海口、养殖区、排污口等人类活动影响较大的区域有关.     

Reassessment of the Ocean-To-Atmosphere Flux of Carbon Monoxide

Carbon monoxide (CO) in the surface sea waters is produced predominantly by photochemical processes, oxidized by micro-organisms and outgassed to the atmosphere. to assess carbon monoxide flux from the oceans to the atmosphere, the photochemical production and microbial oxidation of carbon monoxide in the oceanic mixed-layer was investigated during several oeanographic cruises and in the laboratory. the photoproduction rate of carbon monoxide was found to be well correlated to the concentration of dissolved organic carbon (DOC) in coastal and open ocean surface waters. Taking a global average carbon monoxide production rate of 10 ± 2 nmole litre^-1 (mg DOC hr)^-1 in the surface open ocean water, and 25 ± 7 nmole litre^-1 (mg DOC hr)^-1 in coastal sea water, at cloud-free summer solar noon, the photochemical production of carbon monoxide in the global oceans is estimated to be at a rate of 1200 ± 200 Tg CO y^-1. the microbial carbon monoxide turnover time in the mixed-layer was observed to range from hours in a coastal estuary to 16 days in the Pacific along 1057deg; W in dark incubations. Natural sunlight can largely inhibit the microbial consumption of carbon monoxide in surface water. On a global scale, microbial consumption is responsible for the loss of less than 10% of photochemical produced carbon monoxide in the surface ocean. Field measurements have shown that the net transport of carbon monoxide from the euphotic zone to the underlying deeper ocean water is limited and that the overall life time in surface sea waters is less than 3-4 hours. When combined, these field measurements with the photoproduction and microbial consumption rates obtained, we estimate the oceanic flux to the atmosphere is about 1000 ± 200 Tg CO y^-1, which represents the largest single source of atmospheric carbon monoxide.