厌氧条件下活性黑(KBR)染料脱色的批量投料研究

在厌氧条件下，进行了微生物降解染料活性黑（ＫＢＲ）的试验研究。试验中研究了氯离子浓度、染料浓度、生物量、特别是投加易降解物对染料降解的影响，并且对厌氧降解该染料的过程进行了分析，着重探讨了易降解物葡萄糖投加量对该染料脱色降解的作用     

双阳离子有机膨润土吸附处理水中有机物的性能

分别用长碳链季铵盐（ 如溴化十二烷基三甲铵、溴化十四烷基苄基二甲铵、溴化十六烷基三甲铵、溴化十八烷基三甲铵） 和短碳链季铵盐（ 如溴化四甲基铵） 按一定配比混合改性膨润土,制得一系列双阳离子有机膨润土．研究了双阳离子有机膨润土吸附水中对硝基苯酚、苯酚、苯胺的适宜条件、性能、作用机理．结果表明,双阳离子有机膨润土的层间距、有机碳含量和对有机物的吸附性能与改性时长、短碳链季铵盐的组成及配比有关,水中有机物的去除效果还与其本身的性质有关;所用的双阳离子有机膨润土对有机物的吸附符合 Freundlich或 Langmuir等温式,是表面吸附作用和分配作用共同作用的结果．     

纳米TiO2光催化脱色效果的影响研究

采用偶联剂法制备负载型纳米TiO2光催化剂，对染料废水进行脱色试验研究。结果发现，将废水pH值控制在10～11，通过曝气、添加H2O2、Fe^3 等措施能有效提高废水脱色效果，脱色率在95％以上。     

载铁沸石催化H2O2降解阳离子红X-GRL染料废水

以天然沸石为载体,FeSO₄·7H₂O溶液为浸渍液,采用浸渍蒸干法制备载铁沸石非均相类Fenton反应催化剂,并用其催化H₂O₂降解阳离子红X-GRL染料废水。结果表明,浸渍液浓度为0.18 mg/L、煅烧温度为300 ℃时制备的催化剂铁含量较高、催化效果和稳定性较好。当反应时间为120 min、溶液pH为3.0、催化剂投加量为20.0 g/L、H₂O₂投加量为30.0 mmol/L时,催化降解效果最佳,对染料废水TOC、色度、COD_Cr和TN的去除率分别为60.3%、99.4%、55.5%和49.9%;载铁沸石催化剂重复使用3次后,仍具有一定的催化效果。     

响应面法优化低频超声协同H2O2降解偶氮染料酸性绿B

以酸性绿B染料废水为研究对象,在单因素试验的基础上,选择染料废水初始pH和H₂O₂投加量及超声功率为自变量,以酸性绿B降解率为响应值,采用响应面分析法研究各自变量及其交互作用对酸性绿B超声降解的影响,并通过回归方程求解和响应曲面分析,得到二次多项式回归方程的预测模型. 结果表明,染料废水初始pH和H₂O₂投加量及超声功率与染料降解率存在显著的相关性. 确定酸性绿B废水超声降解优化条件:初始ρ(酸性绿B)为100 mg/L,初始pH和超声功率分别为4.43和216 W,H₂O₂投加量为1.77 mL. 在该优化条件下,酸性绿B的降解率可达93.34%.经试验验证,实际值与模型预测值拟合性良好,偏差仅为3.48%.      

染料探针技术对二级出水中优势污染物的定量检测

分别以刚果红和中性红为染料探针,建立了牛血清蛋白质(BSA)和海藻酸多糖(SA)含量与共振光散射(RLS)发射光谱强度间的线性关系;以甲苯胺蓝为染料探针,建立了腐殖酸(HA)含量与紫外吸光度间的线性关系;优化了3种标准物质的检测浓度范围及溶液p H值条件;考察了染料探针分析方法对标准物的二元和三元混合样品中的回收率.结果表明在适宜的浓度范围内,BSA、HA、SA浓度与染料探针光谱强度间的线性相关系数R0.98,3种标准物在混合样品中的回收率不小于95%,标准误差低于0.11%.以紫外光谱和3D-EEM光谱特征作为城市污水二级出水样品中蛋白质、多糖和腐殖酸的定性依据,确认了4种二级出水样品中的优势污染物.通过染料-探针技术与国标法测得的多糖和蛋白质质量浓度的相对偏差在1.2%~0.04%之间.     

染料废水处理技术现状与发展

文章介绍了染料废水的物理、化学和生物处理技术,并分析了其去除原理和工艺优缺点,目的在于为染料废水处理工作提供理论基础和现实指导,并提出未来染料废水处理技术的发展走向———高效、经济、适应性强、清洁性的废水处理技术。     

铁阳极电解脱色直接黄11染料模拟废水

研究采用铁为阳极电化学法处理直接黄11染料模拟废水脱色性能的影响进行研究。影响因素包括:电流密度、pH值、染料浓度和电解质浓度。研究结果表明,电流密度大有利于染料废水脱色,但能耗消耗大;初始溶液在中性条件下不仅取得很好的处理效果,而且脱色能耗较低;随着染料初始浓度增加脱色率和脱色能耗降低的趋势;随着电解质浓度升高染料脱色率下降的趋势,脱色能耗先减少,然后缓慢增大。在染料初始浓度50 mg/L、pH值为7.11、电流密度2.083 mA/cm2、电解质Na2SO4浓度0.01 mol/L、温度20℃、搅拌速度600 r/min、电解时间60min条件下,脱色率达到92.2%,脱色能耗1.709 kW.h/kg染料。     

Dyes adsorption using a synthetic carboxymethyl cellulose-acrylic acid adsorbent

Removal of noxious dyes is gaining public and technological attention. Herein grafting polymerization was employed to produce a novel adsorbent using acrylic acid and carboxymethyl cellulose for dye removal. Scanning electron microscopy and Fourier-transform infrared spectroscopy verified the adsorbent formed under optimized reaction conditions. The removal ratio of adsorbent to Methyl Orange, Disperse Blue 2BLN and malachite green chloride reached to 84.2%, 79.6% and 99.9%, respectively. The greater agreement between the calculated and experimental results suggested that pseudo second-order kinetic model better represents the kinetic adsorption data. Equilibrium adsorptions of dyes were better explained by the Temkin isotherm. The results implied that this new cellulose-based absorbent had the universaiity for removal of dyes through the chemical adsorption mechanism.     

Identification of key factors governing chemistry in groundwater near the water course recharged by reclaimed water at Miyun County, Northern China

Reclaimed water was successfully used to recover the dry Chaobai River in Northern China, but groundwater may be polluted. To ensure groundwater protection, it is therefore critical to identify the governing factors of groundwater chemistry. Samples of reclaimed water, river and groundwater were collected monthly at Chaobai River from January to September in 2010. Fifteen water parameters were analyzed. Two kinds of reclaimed water were different in type (Na-Ca-Mg-Cl-HCO3 or Na-Ca-Cl-HCO3 ) and concentration of nitrogen. The ionic concentration and type in river were similar to reclaimed water. Some shallow wells near the river bed had the same type (Na-Ca-Mg-Cl-HCO3 ) and high concentration as reclaimed water, but others were consistent with the deep wells (Ca-Mg-HCO3 ). Using cluster analysis, the 9 months were divided into two periods (dry and wet seasons), and all samples were grouped into several spatial clusters, indicating different controlling mechanisms. Principal component analysis and conventional ionic plots showed that calcium, magnesium and bicarbonate were controlled by water-rock interaction in all deep and some shallow wells. This included the dissolution of calcite and carbonate weathering. Sodium, potassium, chloride and sulfate in river and some shallow wells recharged by river were governed by evaporation crystallization and mixing of reclaimed water. But groundwater chemistry was not controlled by precipitation. During the infiltration of reclaimed water, cation exchange took place between (sodium, potassium) and (calcium, magnesium). Nitrification and denitrification both happened in most shallow groundwater, but only denitrification in deep groundwater.