分点进水高效除磷脱氮工艺工程应用研究

分点进水脱氮除磷新工艺以统一动力学理论、动力学负荷理论、污泥浓度优化理论、同步硝化反硝化理论、种群增殖速度的密度控制理论、种群增殖速度的营养工况控制理论等作为主要理论基础,具有脱碳、脱氮、除磷效率高,总停留时间短,运行费用较低的显著优点,在罗庄区污水深度处理工程改追中得到了成功应用,出水水质达到GB18918-2002<城镇污水处理厂排放标准>一级(A)标准.     

定襄县新老城区环境空气质量变化特征研究

为了掌握定襄县环境空气质量状况,根据定襄县新、老城区监测站点2009年的SO2,NO2和可吸入颗粒物(PM10)的浓度资料,对日、月、季节变化以及年内的整体特征进行了统计分析.结果表明,日尺度上,2009年定襄县老城区的污染较严重.月变化情况则是SO2的月均浓度变化范围较大,NO2浓度变化相对平缓,PM10的波动最频繁.4个季节中,SO2浓度的季节性最明显,NO2的变化相对平稳.从2009年的整体情况来看,定襄县的SO2是首要的大气污染物,其次是PM10,NO2污染最轻.     

UASB+双级好氧生物工艺处理豆奶制品废水

根据徐州市某豆奶制品企业废水水质分析,采用UASB+双级好氧生物法进行处理.运行结果表明,出水各项指标均能达到GB 8978-1996《污水综合排放标准》一级标准,工程投资和运行费用合理,运行效果稳定.     

好氧颗粒污泥处理青霉素废水研究

青霉素在其生产过中产生大量的废水,其COD值较高,生化性较差,成分复杂,微生物难以降解,其处理技术是世界性难题。文章采用以葡萄糖模拟废水培养的好氧颗粒污泥为接种体,经青霉素废水逐步驯化后,使其完全处理青霉素废水。实验结果表明,应用好氧颗粒污泥技术,处理青霉素废水,COD,NH3_N,TP去除率较高,具有很好的处理效果。     

数字

61.7%截至2010年12月底,这59条河流化学需氧量和氨氮平均浓度分别为23.7毫克/升和1.4毫克/升,比上年同期分别下降40.4%和61.7%。按常见鱼类能够稳定生存     

甘油基混合培养物合成PHA及其与OUR的关系

聚β羟基烷酸盐(PHA)以其较好的生物相容性、可生物降解性和再生性成为最有前途的生物高分子材料.本文基于甘油作为基质在饱食-饥饿模式下富集合成PHA的混培物,以乙酸、丙酸、丁酸、乳酸和葡萄糖作为基质考察混培物合成PHA的基质广谱性,结果表明乳酸和乙酸作为基质时PHA的产率系数较高;使用不同比例乙酸/丙酸混合基质时,PHA产量随着乙酸含量的增加而增大,乙酸/丙酸为3∶1时PHA产量最高.通过活性污泥同时贮存与生长模型模拟与线性回归两种方法证实,在单一基质或乙酸/丙酸混合基质情况下,PHA合成速率与OUR存在线性关系,因此,基于在线OUR测量数据可以实时估计PHA合成量.     

丙烯气体最小点火能研究

为研究丙烯气体最小点火能随温度的变化规律,首先采用最小点火能测试系对甲烷气体进行了测试和评估,得到了不同温度下的最小点火能及其随温度的变化趋势。结果表明,可燃气体(或液体蒸气)敏感浓度均略高于其当量浓度。气体最小点火能随温度升高而增大。     

准好氧填埋工艺垃圾重金属的污染特征

针对某准好氧填埋场,分析了填埋1~5年的陈垃圾及其浸出液中重金属的含量变化,并进行了污染风险评价,结果表明,垃圾中重金属含量随填埋时间的延长呈现一定的增加趋势,且导气管附近(0 m)垃圾样品重金属含量整体要高于距离导气管较远处(15 m)的样品中重金属含量。重金属As、Cd和Hg严重超过GB 15618—1995《土壤环境质量标准》三级标准限值,重金属Zn、Pb和Cr均未超过标准限值。垃圾浸出液中,重金属Zn、As、Cd、Pb和Cr含量均低于地表水环境质量标准的限值(Ⅱ类)。而Hg浓度超标,为标准限值的34倍~68倍(0 m)和38倍~90倍(15 m)。在污染指数评价中,内罗梅综合污染指数均大于3,为重度污染。     

Biostability in distribution systems in one city in southern China：Characteristics, modeling and control strategy

This study investigated the bacterial regrowth in drinking water distribution systems receiving finished water from an advanced drinking water treatment plant in one city in southem China. Thirteen nodes in two water supply zones with different aged pipelines were selected to monitor water temperature, dissolved oxygen （DO）, chloramine residual, assimilable organic carbon （AOC）, and heterotrophic plate counts （HPC）. Regression and principal component analyses indicated that HPC had a strong correlation with chloramine residual. Based on Chick-Watson＇s Law and the Monod equation, biostability curves under different conditions were developed to achieve the goal of HPC 100 CFU/mL. The biostability curves could interpret the scenario under various AOC concentrations and predict the required chloramine residual concentration under the condition of high AOC level. The simulation was also carded out to predict the scenario with a stricter HPC goal （≤50 CFU/mL） and determine the required chloramine residual. The biological regrowth control strategy was assessed using biostability curve analysis. The results indicated that maintaining high chloramine residual concentration was the most practical way to achieve the goal of HPC ≤ 100 CFU/mL. Biostability curves could be a very useful tool for biostability control in distribution systems. This work could provide some new insights towards biostability control in real distribution systems.     

Origin of major ions in monthly rainfall events at the Bamenda Highlands, North West Cameroon

Rainwater characteristics can reveal emissions from various anthropogenic and natural sources into the atmosphere. The physico-chemical characteristics of 44 monthly rainfall events （collected between January and December 2012） from 4 weather stations （Bamenda, Ndop plain, Ndawara and Kumbo） in the Bamenda Highlands （BH） were investigated. The purpose was to determine the sources of chemical species, their seasonal inputs and suitability of the rainwater for drinking. The mean pH of 5 indicated the slightly acidic nature of the rainwater. Average total dissolved solids （TDS） were low （6.7 mg/L）, characteristic of unpolluted atmospheric moisture/air. Major ion concentrations （mg/L） were low and in the order K＋ 〉 Ca2＋ 〉 Mg2~ 〉 Na＋ for cations and NO3 〉〉 HCO3 〉 SO] 〉 CI- 〉 PO3- 〉 F- for anions. The average rainwater in the area was mixed Ca-Mg-SO4-CI water type. The CI-/Na＋ ratio （1.04） was comparable to that of seawater （1.16）, an indication that N a＋ and CI originated mainly from marine （Atlantic Ocean） aerosols. High enrichments of Ca2＋, Mg2＋ and SO2- to Na＋ ratios relative to seawater ratios （constituting 44% of the total ions） demonstrated their terrigenous origin, mainly from Saharan and Sahelian arid dusts. The K＋/Na＋ ratio （2.24）, which was similar to tropical vegetation ash （2.38）, and NO3 was essentially from biomass burning. Light （〈 100 mm） pre-monsoon and post-monsoon convective rains were enriched in major ions than the heavy （〉 100 mm） monsoon rains, indicating a high contribution of major ions during the low convective showers. Despite the acidic nature, the TDS and major ion concentrations classified the rainwater as potable based on the WHO guidelines.