Chem. J. Chinese Universities ›› 2011, Vol. 32 ›› Issue (5): 1077.

• Preface • Previous Articles     Next Articles

Photoconversion of p-Chlorphenol in Photo-Fe3+-oxalic Acid System in Ice

XUE Hong-Hai, PENG Fei, ZHAO Xu-Hui, KANG Chun-Li*, LI Lin-Lin, LI Zhe, LIU Han-Fei   

  1. Key Laboratory of Groundwater Resources and Environment of the Ministry of Education, College of Environment and Resources,  Jilin University,  Changchun 130012, China
  • Received:2010-09-10 Revised:2011-03-01 Online:2011-05-10 Published:2011-04-11
  • Contact: KANG Chun-Li E-mail:kangcl@jlu.edu.cn
  • Supported by:

    国家自然科学基金(批准号:   41073063)资助.

Abstract: This work investigated the photoconversion of para-chlorphenol (4-CP) in simulated sunlight - Fe3+ - oxalic acid system in ice using self-made low temperature device. The results showed that in the presence of Fe3+ and oxalic acid, the photoconversion of 4-CP was accelerated in ice. The initial concentration of Fe3+ and oxalic acid, the ratio of the initial concentration of Fe3+ and oxalic acid, and the initial pH value had significant influence on the photoconversion of 4-CP. The photoconversion rate of 4-CP reached 39.1% after irradiation for 7.5 h when the initial pH value was 6.5, the ratio of the initial concentration of Fe3+ and oxalic acid was 1/5, and the initial concentration of oxalic acid was 0.8mmol/L. During irradiation, the conversion rate of TOC was lower than that of 4-CP. The photoconversion of 4-CP obeyed the first order kinetics equation. The photoproduct of 4-CP were enriched through direct extraction and derivatization respectively, and then analyzed by GC-MS. Accroding to the outcome, the photoconversion mechanism was deduced in the simulated sunlight - Fe3+ - oxalic acid system in ice.

Key words: para-chlorphenol, photoconvertion, ice, oxalic acid, Fe3+

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