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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     

高氨氮废水短程硝化的影响因素

工业废水中,氨和氮的含量较高,而且全程硝化的工艺很难满足对这些废水的处理要求,因而,高氨氮废水的短程硝化工艺越来越被重视起来.文章将阐述高氨氮废水短程硝化的原理,并着重分析影响高氨氮废水短程硝化的各种因素.     

冶金高含盐废水处理工艺实践应用

某黄金冶炼厂根据云南当地的实际情况,在废水处理工程中采用太阳能预热-刮板式薄膜蒸法工艺处理黄金深加工过程中产生的高含盐废水,处理效果好,出水稳定,是一种非常有效的处理工艺。氯化物及重金属到达GB5749—2006生活饮用水卫生标准。     

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.     

不同基质的人工湿地去除猪场沼液中磷的性能

以猪场沼液为研究对象,通过静态吸附试验研究沸石、硅藻土、煤渣、铁粉、石英砂5种基质对磷的等温吸附特征,并采用一级和二级动力学模型分析吸附动力学过程。根据试验结果,构建了4种人工湿地单元研究人工湿地对猪场沼液处理效果及对高浓度沼液的抗冲击能力。结果表明,5种基质对总磷的吸附更符合非线性Langmuir方程。准二级动力学方程更能描述各种基质对总磷的动力学吸附过程。沸石对磷的最大饱和吸附量1.868 mg/g,对磷去除率最高,可达到96.01%。沸石-垂直流人工湿地在构建的4种人工湿地单元中具有最强抗冲击能力。     

市政污泥深度脱水滤液水质特性研究

以武汉市五座污水处理厂剩余污泥经Ⅰ、Ⅱ、Ⅲ三种污泥调理方法调理及脱水的污泥深度脱水滤液为研究对象,分析测定了水样的常规水质指标。结果表明,配方Ⅰ所得脱水滤液pH为12.8左右,呈强碱性,配方Ⅱ、Ⅲ所得脱水滤液pH=3.0~6.2,呈酸性。污泥深度脱水滤液的水质随脱水污泥的来源、污泥调理方法不同而异,稳定、氧化程度高的污泥其深度脱水滤液水质较好。经调理后的深度脱水滤液ρ(COD)为180~1200 mg/L,为中低浓度有机废水;BOD5/COD=0.49~0.66,可生化性良好;氨氮浓度为20~200 mg/L,差异较大,但普遍较高,C/N在2.2~13.4,属低C/N比废水;TP在0.4~5.5 mg/L,C∶N∶P对微生物生长来说并不协调。污泥调理剂中的破胞试剂对污泥脱水滤液水质影响较大,配方Ⅱ、Ⅲ调理剂中含破胞试剂,调理后的污泥深度脱水滤液COD和氨氮值较大。最后,建议对氨氮负荷过高而不适合回流的深度脱水滤液采用高效的生物脱氮工艺进行处理。     

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.     

Characteristics of atmospheric particles and heavy metals in winter in Chang-Zhu-Tan city clusters, China

To understand the pollution characteristics of atmospheric particles and heavy metals in winter in Chang-Zhu-Tan city clusters, China, total suspended particulate(TSP) and PM10samples were collected in cities of Changsha, Zhuzhou and Xiangtan from December 2011 to January 2012, and heavy metals of Cd, Pb, Cr, and As were analyzed. It shows that the average TSP concentration in Changsha, Zhuzhou and Xiangtan were(183 ± 73),(201 ± 84) and(190 ± 66) μg/m3respectively, and the average PM10 were(171 ± 82),(178 ± 65) and(179 ± 55) μg/m3respectively. The lowest TSP and PM10concentrations occurred at the background Shaping site of Changsha. The average ratio of ρ(PM10)/ρ(TSP) was 91.9%, ranging from 81.3% to 98.9%. Concerning heavy metals, in TSP samples, the concentration of Cr, As, Cd and Pb were 28.8–56.5, 18.1–76.3, 3.9–26.1 and 148.0–460.9 ng/m3, respectively, while in PM10samples, were 16.4–42.1, 15.5–67.9, 3.3–22.2 and 127.9–389.3 ng/m3, respectively. The enrichment factor of Cd was the highest, followed by Pb and As, while that of Cr was the lowest.     

Nitrogen mass balance in a constructed wetland treating piggery wastewater effluent

The nitrogen changes and the nitrogen mass balance in a free water surface flow constructed wetland （CW） using the four-year monitoring data from 2008 to 2012 were estimated. The CW was composed of six cells in series that include the first settling basin （Cell 1）, aeration pond （Cell 2）, deep marsh （Cell 3）, shallow marsh （Cell 4）, deep marsh （Cell 5） and final settling basin （Cell 6）. Analysis revealed that the NH4＋-N concentration decreased because of ammonification which was then followed by nitrification. The NO4＋-N and NO4＋-N were also further reduced by means of microbial activities and plant uptake during photosynthesis. The average nitrogen concentration at the influent was 37,819 kg/year and approximately 45% of that amount exited the CW in the effluent. The denitrification amounted to 34% of the net nitrogen input, whereas the accretion of sediment was only 7%. The biomass uptake of plants was able to retain only 1% of total nitrogen load. In order to improve the nutrient removal by plant uptake, plant coverage in four cells （i.e., Cells 1, 3, 4 and 5） could be increased.