共查询到20条相似文献,搜索用时 46 毫秒
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采用Fenton试剂氧化—活性炭吸附工艺处理炼油厂循环水排污水,考察了各种因素对处理效果的影响.通过实验得出最佳处理条件为:室温,H2O2加入量600 mg/L,m(H2O2):m(Fe2+)=4,水样pH5.0~5.5,Fenton试剂氧化反应时间1h,活性炭选择8~30目的无烟煤破碎炭,水样在吸附柱的停留时间约为30 min.当循环水排污水COD低于150 mg/L时,经该联合工艺处理后出水COD低于50 mg/L,达到GB8978-1996《污水综合排放标准》中的二级排放标准. 相似文献
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采用三级厌氧柱串联形成的递进式强化厌氧处理工艺协同Fenton氧化工艺处理某印染厂的印染废水(COD 1 418 mg/L、色度400倍)。三级厌氧柱的运行参数为:以陶粒为填料,进水p H为7.0,3个厌氧柱的HRT均为16 h,柱温(33±2)℃。厌氧柱2的强化条件为投加280 mg/L钙离子和30 mg/L PAM,厌氧柱3的强化条件为投加350 mg/L煤质活性炭。三级厌氧柱强化前后的COD去除率分别为70.38%和84.13%,色度去除率分别为50.00%和62.50%。Fenton氧化处理的最佳条件为H2O2投加量450 mg/L、Fe SO4投加量450 mg/L、反应p H 3.5、反应时间0.5 h。整个工艺的总COD去除率达96.12%、总色度去除率达78.75%,处理后出水的COD为55 mg/L、色度为85倍,满足GB 4287—2012《纺织染整工业水污染物排放标准》中的直排标准。 相似文献
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采用分步化学沉淀法分别脱除并回收磷酸铁生产废水中的高浓度磷酸根和硫酸根。实验结果表明:在以n(Fe~(3+))∶n(PO_4~(3-))=1.0的比例加入硫酸铁、反应时间为40 min、反应温度为25℃、废水初始p H为8.17、反应30 min时二次调节废水p H至5.50的条件下,磷酸根去除率可达98%以上,所得沉淀中Fe和P的质量分数分别为36.77%和18.81%,成分简单,回收价值高;采用氢氧化钙作为沉淀剂,在n(Ca~(2+))∶n(SO_4~(2-))=1.0的条件下可将废水中硫酸根质量浓度由78.62 g/L降至2.16 g/L,硫酸根去除率为97.3%,硫酸钙回收量为120.2 g/L;最终出水的磷酸根质量浓度小于0.5 mg/L,满足GB 8978—1996《污水综合排放标准》的一级标准。 相似文献
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臭氧催化氧化法处理焦化废水中氰化物 总被引:1,自引:0,他引:1
采用臭氧催化氧化法处理焦化废水中的氰化物,采用合理的试验设计方案,应用响应曲面法讨论了O3的投加量、催化剂加入量以及溶液初始p H值对总氰去除率影响,从而优化了总氰去除工艺条件。试验结果表明,O3投加量、催化剂用量和溶液初始p H值对总氰的去除率影响极为显著;回归分析和验证试验表明,应用响应曲面法优化试验合理可行;O3投加量为84.35 mg/L、催化剂用量为120 mg/L、p H值为9.26、总氰去除率为91.38%,此时溶液中残留的总氰浓度为0.884 mg/L,可以实现达标排放。 相似文献
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《再生资源与循环经济》2017,(1)
以农药毒死蜱有机磷废水为处理对象,研究了湿式氧化加磷酸镁铵与生化组全处理工艺对废水COD、三氯吡啶酚钠及有机磷的处理效果,结果表明,该工艺的处理效率主要受反应温度、反应时间、p H值的影响。在200℃,氧分压为1.2 MPa,反应时间为2 h,进水p H值为2.0时,COD去除率达65%以上,再经过镁盐沉淀除磷后,TP去除率达99.7%以上,预处理后废水B/C比值提高到0.5以上,与其他低盐废水混合后可生化处理达标,同时产生的磷酸镁铵作为肥料可进行综合利用。 相似文献
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采用O_3-H_2O_2-催化剂氧化体系对某石化企业含盐废水的二级生化出水进行处理,考察了不同反应体系下的反应时间、O_3流量、H_2O_2投加量对COD去除效果的影响。实验结果表明:O_3-H_2O_2-催化剂氧化体系对石化含盐废水的处理效果最好;在臭氧流量为40 m L/min、H_2O_2投加量为50 mg/L、催化剂投加量为300 g/L、反应时间为60 min的条件下,COD去除率为51.4%,出水COD为52.0 mg/L,达到GB31570—2015《石油炼制工业污染物排放标准》的要求。 相似文献
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分别采用次氯酸钙单一体系和盐酸-次氯酸钙复合体系对贫泥磷中的黄磷进行氧化处理,重点考察了盐酸浓度、次氯酸钙加入量、反应温度和反应时间等因素对贫泥磷中黄磷去除率的影响。实验结果表明:与单一次氯酸钙体系相比,盐酸的加入有效地破除了贫泥磷中的胶质结构,盐酸-次氯酸钙复合体系能有效地去除贫泥磷中的黄磷;在反应温度为60℃、盐酸浓度为2.4 mol/L、破胶反应时间为30 min、次氯酸钙加入量为250 g/L、氧化反应时间为3 h的最佳条件下,黄磷的去除率达到99.6%以上。 相似文献
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Morphometric, hydrological and basic physico-chemicalcharacteristics of three deep Alpine lakes, Traunsee,Hallstättersee and Attersee as well as their long-termbahaviour are presented. The deep Alpine lakesHallstättersee and Traunsee have been influenced by saltmining and the traditional salt industry for over 100 years. Waste products from these activities, entering the lakes, have mainlyaffected the chemistry of these water bodies, especially bysubstantially increasing the chloride concentrations up to 170 mg L-1. As a consequence of the increased density, mixing conditions of the lakes were altered. The resulting incomplete mixing led to oxygen depletionin deeper layers. In addition, increased nutrientload from the catchment rised the trophic level in the 70s and 80sof the last century in turn, affecting the oxygen content in thehypolimnion. Finally a situation developed where the risk becamehigh for these lakes to become meromictic induced by humanactivity. In fact, Hallstättersee became facultativelymeromictic. This process was interrupted by increased chlorideinput of more than 30 mg L-1 due to accidental wash outfrom an upstream salt mine rendering Hallstätterseehomogenous in 1978 to 1980 resulting in complete over-turn. Conditions substantially improved in both lakes after miningpractices were altered and restoration measures againsteutrophication were initiated. Chloride and phosphorusconcentrations declined, while oxygen conditions substantiallyimproved in the following years. Conditions in Traunseesubstantially improved and chloride levels near the sedimentdecreased to less than 140 mg L-1. The third lakeconsidered here, Attersee, always remained in a near-naturalstate although some signs of increased nutrient levels becamevisible in the late 1970s. Chloride concentrations of around 3 mgL-1 in this lake can be considered as background levels.Attersee can now serve as a reference site for deep Alpine lakesbecause of its ultra-oligotrophic and pristine nature. 相似文献
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Cootes Paradise is a coastal wetland, adjacent to Hamilton Harbour at the western tip of Lake Ontario. The marsh has been
considerably degraded due to the excessive sediment and nutrient input from sewage treatment plants (STPs), marsh tributaries
and Combined Sewer Overflows (CSOs). Although there has been reduction in nutrient loadings from external sources, high nutrient
levels, and a prolific algal growth remain a problem in Cootes Paradise. To assess the importance of external versus internal nutrient loadings to the marsh, nutrient fluxes from sediments were estimated using porewater profiles at three
locations from 2001 and five additional sites from 2002. The fluxes varied between 0.27 and 5.25 mg P m−2 day−1, with sites receiving outfalls of STP and CSO having highest fluxes (∼5 mg P m−2 day−1). Mean phosphorus release rate of 2.02 mg P m−2 day−1 was calculated from the spatial distribution of the non-apatite inorganic phosphorus (NAI-P) in sediments, employing a relationship
between the NAI-P and P fluxes. The results confirm that sediment P geochemistry is important in regulating the P pool in
porewater which, consequently, governs the P fluxes from sediments. 相似文献
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活性污泥生物除磷数学模型研究进展 总被引:1,自引:0,他引:1
概述了活性污泥生物除磷过程的Comeau/Wentzel模式和Mino模式,以及以Wentzel和Smolders为代表的两类生物除磷数学模型,提出结合Smolders模型与ASM2、ASM2D模型的优点建立结构完整、参数较少、辨识简单的模型,是生物除磷数学模型发展的方向。 相似文献
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