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天然金红石光催化降解藏红T实验研究
引用本文:李巧荣,鲁安怀,李宁,李改云,杨欣.天然金红石光催化降解藏红T实验研究[J].矿物岩石地球化学通报,2003,22(3):215-218,223.
作者姓名:李巧荣  鲁安怀  李宁  李改云  杨欣
作者单位:1. 中国地质大学,材料科学与工程学院,北京,100083
2. 北京大学,地球与空间科学学院,北京,100871
基金项目:国家重大基础研究前期研究专项 (2 0 0 1CCA0 2 40 0 ),国家自然科学基金资助项目 (4 0 172 0 2 2 )
摘    要:以低压汞灯为光源研究了天然金红石悬浆体系中藏红T的脱色条件及其光催化反应动力学,讨论了溶液初始pH值、催化剂投入量、光强、气流量、催化剂粒径、反应气氛等实验条件对藏红T脱色速率的影响,阐述了实验过程中无机离子的生成情况。结果表明,该反应基本上符合一级反应动力学;在酸性条件下尤其是当溶液初始pH值为2.5时,藏红T的脱色速率要比在碱性和中性条件下快得多;增加光强度能较大地提高反应的降解速率;催化剂最佳投入量为1.3g/L;在氧化气氛下该反应比在非氧化气氛快得多;通入气体的流量在40L/h最合适;反应溶液中有氯离子溶出说明有机物中的含氯部分被降解。本研究为光催化作用降解有机污染物提供了新的途径。

关 键 词:天然金红石  光催化降解  藏红T  实验研究  脱色  无机离子  有机污染物  废水处理  TiO2  二氧化钛
文章编号:1007-2802(2003)03-0215-04

The Photocatalysis Oxidation of Safranine T by Natural Rutile
LI Qiao-rong ,LU An-huai ,LI Ning ,LI Gai -yun ,YANG Xin . School of Material Science and Engieering,China Unive rsity of Gescience,Beijing ,China, . Deparment of Geology and Space Sciences,Peking University,Beijing ,China.The Photocatalysis Oxidation of Safranine T by Natural Rutile[J].Bulletin of Mineralogy Petrology and Geochemistry,2003,22(3):215-218,223.
Authors:LI Qiao-rong  LU An-huai  LI Ning  LI Gai -yun  YANG Xin School of Material Science and Engieering  China Unive rsity of Gescience  Beijing  China  Deparment of Geology and Space Sciences  Peking University  Beijing  China
Institution:LI Qiao-rong 1,LU An-huai 2,LI Ning 2,LI Gai -yun 1,YANG Xin 1 1. School of Material Science and Engieering,China Unive rsity of Gescience,Beijing 100083,China, 2. Deparment of Geology and Space Sciences,Peking University,Beijing 100 871,China
Abstract:In natural rutile suspension sys te m, the decolorization of safranine T and its reaction kinetics were studied usin g a lowpressure mercury vapor lamp as the light source. The effect of initial p H value of safranine T solution, dosage of catalyst, intensity of UV irradiation , granularity of the catalyst, airflow rate and reaction atmosphere on photocata lytic degration rate were investigated. The development of inorganic irons in th e experiment was discussed. The results showed that the decolorization rate of s afranine T in acidic condition was much higher than in neut and alkaline conditi ons,especially,when the pH value is 2.5. Enhancing intensity of UV irradiation c an improve the reaction rate greatly. In addition, the favourable dosages of catalystx is 1.3g/L and the reaction rate is much higher in oxidative atmosp here than that in reductive atmosphere.The appropriate airflow rate is 40L/h.Fin ally we observed the existence of Cl - in the solution,which indicated that th e organic contaminants can be mineralized into inorganic molecules and ions.We p rovided a new way to mineralize organic contaminants using photo-catalyzed meth ods.
Keywords:natural rutile  degradation  decol orization  photocatalysis  dye
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