粉末活性炭的Fenton氧化再生

采用Fenton氧化法对吸附处理染料废水后的饱和粉末活性炭(饱和炭)进行再生,考察了饱和炭的再生效果及其主要影响因素。实验结果表明:饱和炭的最佳再生条件为H2O2投加量6.5 mmol/g、再生p H 3.0、H2O2与Fe2+的摩尔比10、再生时间1 h;最佳条件下的再生率(再生粉末活性炭(再生炭)与新粉末活性炭对废水COD去除率的百分比)约为60%;使用最佳再生条件下得到的再生炭对废水进行吸附处理,废水的COD去除率和脱色率分别约为27%和67%。     

新型类Fenton催化剂表征及其降解染料废水的试验研究

钴基和铜基类Fenton催化剂是近年来的研究热点,对新型类Fenton催化剂进行SEM,EDS,XPS表征,得知催化剂中的金属元素主要为钴和铜。通过单因素分析法,研究影响该催化剂处理甲基橙模拟废水效果的因素。结果表明:该催化剂在pH为3~9的范围内均表现出较好的催化降解能力;当双氧水的添加量达到20 mL/L时,催化降解能力不再增加;催化剂的投加量影响催化降解能力达到最大的时间;此外,双氧水的投加方式影响降解所需的时间而对最终的处理效果影响不大。     

可见光催化剂Ag_3PO_4/海泡石的制备及降解染料废水性能

以沉淀法、离子交换法和原位法制备了Ag_3PO_4/海泡石复合光催化剂,采用XRD、FTIR、UV-Vis-DRS对其结构进行了表征,以可见光驱动催化降解日落黄染料为探针反应,考察了制备方法对催化剂光催化性能的影响。结果表明:Ag_3PO_4与海泡石成功复合并产生了协同作用,催化剂中Ag_3PO_4均为立方晶型,部分Ag_3PO_4进入了海泡石层间,改变了其晶面有序性并拓宽了层间距,海泡石对Ag_3PO_4的复合提高了Ag_3PO_4的稳定性和光催化活性;其中,离子交换法制备的光催化剂中Ag_3PO_4与海泡石的复合程度最高,Ag_3PO_4稳定性最强,光催化活性最好,在可见光驱动下,该催化剂对50 mg/L的日落黄降解率可达97.16%,并且对其他3种50 mg/L的染料废水的降解率也在86%以上,此外,该催化剂再生2次后仍保持良好的活性和稳定性。     

纳米TiO_2光催化降解水溶性染料溶液的研究

研究了纳米ＴｉＯ２光催化剂对活性黄Ｘ６Ｇ、活性红Ｘ３Ｂ、活性蓝ＸＢＲ、碱性绿、碱性紫５ＢＮ、碱性品红等６种染料溶液的光解脱色效果。结果表明，在ｐＨ２的酸性溶液中，对浓度为６０ｍｇ／Ｌ的６种染料溶液的脱色率均超过９３．３％；即使对浓度达２００ｍｇ／Ｌ的活性蓝溶液，其脱色率仍可达７８．８％。染料溶液的ｐＨ值对纳米ＴｉＯ２光催化脱色效果影响较大     

天然矿物负载Fe/Co催化H2O2氧化降解阳离子红3R

类Fenton反应关键是催化剂的活性,利用浸渍法负载铁、钴双金属对天然矿物材料进行改性,提高其催化活性,并运用扫描式电子显微镜(SEM)、X射线能谱仪(EDS)、X射线衍射(XRD)等表征手段对负载前后的材料进行表征分析.结果表明负载后材料中生成Fe2O3和Co Fe2O4两种新物质.将合成的催化剂用于催化H2O2氧化阳离子红3R染料废水,在催化剂投加量3 g·L-1,H2O2投加量0.3 m L·L-1,反应时间1 h条件下,100 mg·L-1阳离子红3R废水脱色率可达99.8%,TOC去除率可达58.4%,催化剂中活性组分主要为表面负载的Fe2O3和Co Fe2O4,电子自旋共振(ESR)分析表明催化氧化过程中产生羟基自由基,阳离子红3R发色基团在1 min已被完全破坏,光谱分析表明反应过程中有小分子物质生成.催化氧化效果受染料废水初始p H值影响小,适应p H范围广,解决了传统Fenton反应p H条件苛刻的问题.研究结果为印染废水处理提供了具有工程应用潜力的技术方法.     

漆酶对染料废水脱色的应用研究

漆酶是一种含铜的多酚氧化酶,近年来在染料废水脱色领域的应用研究取得了长足发展.染料废水具有产生量大、危害性强、难于生物降解等特点,对印染废水脱色研究发现,漆酶是处理染料废水最具潜力的生物酶.当前研究最为广泛的是真菌漆酶与细菌漆酶.真菌漆酶具有作用pH偏酸性、适宜温度范围窄、培养周期长、易纯化等特点,细菌漆酶具有作用pH与适宜温度范围较广、培养周期短、不易纯化等特点.将漆酶在载体上进行固定化,可达到便捷高效、重复使用的目的,载体材料不断优化,推动漆酶实现更广泛的实际应用.     

Preparation and characterization of Fe2O3-CeO2-TiO2/γ-Al2O3 catalyst for degradation dye wastewater

In order to develop a catalyst with high activity for catalytic wet oxidation （CWO） process at room temperature and atmospheric pressure, Fe2O3-CeO2-TiO2/γ-Al2O3 catalyst was prepared by consecutive impregnation method and the prepared parameters were optimized. The structure of the catalyst was characterized by BET, XRF, SEM and XPS technologies, and the actual wastewater was used to investigate the catalytic activity of Fe2O3-CeO2-TiO2/γ-Al2O3 in CWO process. The experimental results showed that the prepared catalyst exhibited good catalytic activity when the doping amount of Ti was 1.0 wt% （the weight ratio of Ti to carriers）, and the middle product, Fe2O3-CeO2-TiO2/γ-Al2O3, was calcined in 450℃ for 2 h. The CWO experiment for treating actual dye wastewater indicated that the COD, color and TOC of actual wastewater were decreased by 62.23%, 50.12% and 41.26% in 3 h, respectively, and the ratio of BOD5/COD was increased from 0.19 to 0.30.     

絮凝—光氧化法处理染料废水的试验研究

以三氯化铁为絮凝剂，采用絮凝－光氧化二级串联法对模拟活性艳红Ｘ－３Ｂ染色料废水进行处理试验，取得了脱色率１００％、ＣＤＯＣＲ去除率８０％的效果。该方法具有一次性投药，投药量少，残渣少等优点。     

RHODAMINE WT DYE LOSSES IN A MOUNTAIN STREAM ENVIRONMENT1

ABSTRACT: A significant fraction of rhodamine WT dye was lost during a short term multitracer injection experiment in a mountain stream environment. The conservative anion chloride and the sorbing cation lithium were concurrently injected. In-stream rhodamine WT concentrations were as low as 45 percent of that expected, based on chloride data. Concentration data were available from shallow‘wells’dug near the stream course and from a seep of suspected return flow. Both rhodamine WT dye and lithium were nonconservative with respect to the conservative chloride, with rhodamine WT dye closely following the behavior of the sorbing lithium. Nonsorption and sorption mechanisms for rhodamine WT loss in a mountain stream were evaluated in laboratory experiments. Experiments evaluating nonsorption losses indicated minimal losses by such mechanisms. Laboratory experiments using sand and gravel size streambed sediments show an appreciable capacity for rhodamine WT sorption. The detection of tracers in the shallow wells and seep indicates interaction between the stream and the flow in the surrounding subsurface, intergravel water, system. The injected tracers had ample opportunity for intimate contact with materials shown in the laboratory experiments to be potentially sorptive. It is suggested that in the study stream system, interaction with streambed gravel was a significant mechanism for the attenuation of rhodamine WT dye (relative to chloride).