左氧氟沙星的超声/H2O2联合降解研究

采用超声/H2O2高级氧化技术对喹诺酮类抗生素左氧氟沙星进行降解,考察了H2O2浓度、超声功率、溶液初始pH值对反应过程的影响.结果表明,与单独超声和H2O2氧化相比,超声/H2O2对左氧氟沙星具有明显的协同降解作用. H2O2 添加浓度在3.0~20.0mmol/L范围, 左氧氟沙星的降解率随其添加浓度的增加而增加;超声功率在260W时降解效果最佳;左氧氟沙星初始浓度在10~30mg/L范围内,左氧氟沙星的降解量随其初始浓度的增加而增加;超声/H2O2降解左氧氟沙星在未调节(pH 7.14)效果最佳. HPLC分析发现降解过程主要有2种产物生成, 产物的生成和分布受体系pH的影响较大.     

TiO2-Fe3+可见光催化H2O2降解阿特拉津的协同效应

以内分泌干扰物阿特拉津为模型污染物,研究了TiO2-Fe3+可见光催化H2O2降解阿特拉津的协同效应.结果表明,在H2O2存在条件下,金红石TiO2经可见光激发可持续稳定地产生.OH自由基,在Fe3+协同作用下,.OH自由基生成量急剧增加;TiO2能可见光催化H2O2降解阿特拉津,金红石TiO2显示出较锐钛矿TiO2及混晶TiO2(TiO2P25)更高的催化活性,反应60 min,阿特拉津的降解率可达40%;以Fe3+协同TiO2可见光催化H2O2降解阿特拉津时,反应效率显著加快,反应5 min即对阿特拉津的降解率达到100%,而金红石TiO2显示出更为明显的协同效应.     

电化学方法现场产生H2O2的影响因素及其废水处理应用

建立了以石墨碳棒为阴极,Pt为阳极,饱和甘汞电极为参比电极,Na2SO4为支持电解质溶液的H2O2制备三电极体系。对电流密度、pH值、通氧流量、支持电解质浓度和极间距等主要参数对生成H2O2的影响进行了单因素轮换试验研究,并采用正交试验方法对这些因素进行了分析。结果发现,pH值对生成H2O2的影响最为显著,支持电解质浓度和通氧流量也具有较大影响,极间距影响不明显,电流密度则存在着最佳值。通过试验获得的最优参数组合为:pH=2.00,电流密度=1.02mA·cm-2,通氧流量=0.4L·min-1,支持电解质浓度=0.1mol·L-1,极间距=6cm。在该参数组合条件下,采用电-Fenton法对活性染料RedMX-5B进行脱色和矿化试验,初始Fe2 投量为0.25mmol·L-1,电解180min,脱色率可达90%以上,但矿化率不高(<25%)。因此,提高矿化率是染料废水处理在未来的主要课题。     

O3／H2O2高级氧化技术H2O2加入量的简易控制方法

对与臭氧有着不同反应活性的3类有机污染物，探讨并建立了O3／H2O2高级氧化技术H2O2较优投加量的简易控制方法。结果表明，水中存在溶解臭氧是H2O2与臭氧降解效率具有协同作用的必要条件，另外，H2O2的较优加入量直接依赖于目标有机污染物与臭氧的反应活性。对于不同的有机物及在常规的臭氧化水处理时间内，H2O2加入量控制在单独臭氧化处理时水中溶解臭氧的20-30倍（质量比）之间为宜。这种简易控制H2O2加入量的方法对推广O3／H2O2技术在实际废水处理中的应用具有重要的意义。     

对环境空气氯化氢浓度限值的探讨

通过对环境空气中氯化氢的毒理作用,各类标准比较、标准来源、评价标准的计算方法等,对现有的环境空气质量标准进行了探讨,提出了需要对现行标准进行修订的建议.     

天然水中过氧化氢生成及其光化学反应的研究进展

在综合近４０年来国外对天然水（地表水、大气水滴及降水）中过氧化氢研究成果的基础上，重点从天然水中过氧化氢的含量和分布、生成机理以及光化学反应三方面，对这一领域的研究进展作了综述。     

Kinetics of hydrogen peroxide-sulfur (IV) reaction in atmospheric precipitation

The kinetics of the reaction of dissolved S(IV) with H2O2 was studied on 59 precipitation samples collected in Southwestern China, during the period of June 1988 to October 1989, from which the oxidation rates of the reaction were measured. The extent of reaction was followed by continuous amperometric measurement of the concentrations of the reagents. The two systems (i. e. rainwater and purified water) have been studied with the same methodology under identical reaction conditions (e. g. reagent concentrations, ionic strength and temperature). The kinetics was studied in no buffer solutions. The effect of formaldehyde on the reaction has also been studied, including kinetic studies in laboratory and model calculations, and it is indicated that formaldehyde with typical atmospheric concentration exerts no influence on the reaction of dissolved S(IV) with H2O2. In addition, the activation energy of the reaction was also measured in purified water as reaction medium for temperature range 0-50℃ at pH 4.0     

Pathway of the ozonation of 2,4,6-trichlorophenol in aqueous solution

The reaction mechanism and pathway of the ozonation of 2,4,6-trichlorophenol (2,4,6-TCP) in aqueous solution were investigated. The removal efficiency and the variation of H₂O₂, Cl⁻ formic acid, and oxalic acid were studied during the semi-batch ozonation experiments (continuous for ozone gas supply, fixed volume of water sample). The results showed that when there was no scavenger, the removal efficiency of 0.1 mmol/L 2,4,6-TCP could reach 99% within 6 min by adding 24 mg/L ozone. The reaction of molecular ozone with 2,4,6-TCP resulted in the formation of H₂O₂. The maximal concentration of H₂O₂ detected during the ozonation could reach 22.5% of the original concentration of 2,4,6-TCP. The reaction of ozone with H₂O₂ resulted in the generation of a lot of OH• radicals. Therefore, 2,4,6-TCP was degraded to formic acid and oxalic acid by ozone and OH• radicals together. With the inhibition of OH• radicals, ozone molecule firstly degraded 2,4,6-TCP to form chlorinated quinone, which was subsequently oxidized to formic acid and oxalic acid. Two reaction pathways of the degradation of 2,4,6-TCP by ozone and O₃/OH• were proposed in this study. Translated from Acta Scientiae Circumstantiae, 2005, 25(12): 1619–1623 [译自: 环境科学学报]     

A theoretical study of hydrogen-bonded molecular clusters of sulfuric acid and organic acids with amides

Amides, a series of significant atmospheric nitrogen-containing volatile organic compounds (VOCs), can participate in new particle formation (NPF) throught interacting with sulfuric acid (SA) and organic acids. In this study, we investigated the molecular interactions of formamide (FA), acetamide (AA), N-methylformamide (MF), propanamide (PA), N-methylacetamide (MA), and N,N-dimethylformamide (DMF) with SA, acetic acid (HAC), propanoic acid (PAC), oxalic acid (OA), and malonic acid (MOA). Global minimum of clusters were obtained through the association of the artificial bee colony (ABC) algorithm and density functional theory (DFT) calculations. The conformational analysis, thermochemical analysis, frequency analysis, and topological analysis were conducted to determine the interactions of hydrogen-bonded molecular clusters. The heterodimers formed a hepta or octa membered ring through four different types of hydrogen bonds, and the strength of the bonds are ranked in the following order: SOH???O > COH???O > NH???O > CH???O. We also evaluated the stability of the clusters and found that the stabilization effect of amides with SA is weaker than that of amines with SA but stronger than that of ammonia (NH₃) with SA in the dimer formation of nucleation process. Additionally, the nucleation capacity of SA with amides is greater than that of organic acids with amides.     

Formation control of bromate and trihalomethanes during ozonation of bromide-containing water with chemical addition: Hydrogen peroxide or ammonia?

To ensure the safety of drinking water, ozone (O₃) has been extensively applied in drinking water treatment plants to further remove natural organic matter (NOM). However, the surface water and groundwater near the coastal areas often contain high concentrations of bromide ion (Br^?). Considering the risk of bromate (BrO₃^?) formation in ozonation of the sand-filtered water, the inhibitory efficiencies of hydrogen peroxide (H₂O₂) and ammonia (NH₃) on BrO₃^? formation during ozonation process were compared. The addition of H₂O₂ effectively inhibited BrO₃^? formation at an initial Br^? concentration amended to 350 µg/L. The inhibition efficiencies reached 59.6 and 100% when the mass ratio of H₂O₂/O₃ was 0.25 and > 0.5, respectively. The UV₂₅₄ and total organic carbon (TOC) also decreased after adding H₂O₂, while the formation potential of trihalomethanes (THMsFP) increased especially in subsequent chlorination process at a low dose of H₂O₂. To control the formation of both BrO₃^? and THMs, a relatively large dose of O₃ and a high ratio of H₂O₂/O₃were generally needed. NH₃ addition inhibited BrO₃^? formation when the background ammonia nitrogen (NH₃N) concentration was low. There was no significant correlation between BrO₃^? inhibition efficiency and NH₃ dose, and a small amount of NH₃N (0.2 mg/L) could obviously inhibit BrO₃^? formation. The oxidation of NOM seemed unaffected by NH₃ addition, and the structure of NOM reflected by synchronous fluorescence (SF) scanning remained almost unchanged before and after adding NH₃. Considering the formation of BrO₃^? and THMs, the optimal dose of NH₃ was suggested to be 0.5 mg/L.