Please use this identifier to cite or link to this item: http://hdl.handle.net/11455/28220
標題: 腐植酸之化學組成與分子大小對Cr(VI)還原之影響
Influences of chemical compositions and molecular weights of humic acids on Cr (VI) reduction
作者: 黃詩文
Huang, Shih-Wen
關鍵字: 腐植酸
humic acid
連續萃取
超過濾
中空纖維管柱
TFF系統
六價鉻
光還原
repetitive extraction
ultrafiltration
hollow-fiber
TFF system
Cr (VI)
photo-reduction
aromaticity
functional groups
spectral analysis
出版社: 土壤環境科學系所
引用: Huang Y. Y. (2006), The Effects of Structural Characteristics of Repetitively Extracted Humic Acids on the Sorption of 2,4,6-Trichlorophenol, unpublished doctoral dissertation, Department of Soil & Environmental Science, NCHU, Taichung. Shen Y. S. (2009), Sorption and reductive transformation of hexavalent chromium on coconut-shell-derived black carbon, unpublished doctoral dissertation, Department of Soil & Environmental Science, NCHU, Taichung. Ssu Y. C. (2009), The photo-induced reduction of Cr(VI) as influenced by humic acids with various molecular weights and chemical compositions, unpublished doctoral dissertation, Department of Soil & Environmental Science, NCHU, Taichung. Amalfitano C., Quezada R.A., Wilson M.A., Hanna J.V. (1995), Chemical composition of Humic Acids: A Comparison With Precursor ''Light Fraction'' Litter From Different Vegetations Using Spectroscopic Techniques. Soil Science 159:391-401. Asakawa D., Kiyotak T., Yanagi Y., Fujitake N. (2008) Optimization of conditions for high-performance size-exclusion chromatography of different soil humic acids. Analytical Sciences 24:607-613. Christl I., Knicker H., Koegel-Knabner I., Kretzschmar R. (2000) Chemical heterogeneity of humic substances: characterization of size fractions obtained by hollow-fibreultrafiltration. European Journal of Soil Science 51:617-625. Christland I., Kretzschmar R. (2001) Relating ion binding byfulvic and humic acids to chemical composition and molecular size. 1. proton binding. Environmental Science & Technology 35:2505-2511. Conte P., Spaccini R., Piccolo A. (2006) Advanced CPMAS-13C NMR techniques for molecular characterization of size-separated fractions from a soil humic acid. Analytical and Bioanalytical Chemistry 386:382-390. Gallios G.P., Vaclavikova M. (2008) Removal of chromium (VI) from water streams: a thermodynamic study. Environmental Chemistry Letters 6:235-240. Garcia-Mina J.M. (2006) Stability, solubility and maximum metal binding capacity in metal-humic complexes involving humic substances extracted from peat and organic compost.Organic Geochemistry:1960-1972. Giovanela M., Crespo J.S., Antunes M., Adamatti D.S., Fernandes A.N., Barison A., da Silva C.W.P., Guegan R., Motelica-Heino M., Sierra M.M.D. (2010) Chemical and spectroscopic characterization of humic acids extracted from the bottom sediments of a Brazilian subtropical microbasin. Journal of Molecular Structure 981:111-119. Guertin J., Jacobs J., Avakian C., Group I.E.T.E. (2005) Chromium (VI) handbook CRC Press. Hsu L.C., Wang S.L., Lin Y.C., Wang M.K., Chiang P.N., Liu J.C., Kuan W.H., Chen C.C., Tzou Y.M. (2010) Cr(VI) Removal on Fungal Biomass of Neurospora crassa: the Importance of Dissolved Organic Carbons Derived from the Biomass to Cr(VI) Reduction. Environmental Science & Technology 44:6202-6208. Huang Y.Y., Wang S.L., Liu J.C., Tzou Y.M., Chang R.R., Chen J.H. (2008) Influences of preparative methods of humic acids on the sorption of 2,4,6-trichlorophenol. Chemosphere 70:1218-1227. Leenheer J.A., Wershaw R.L., Brown G.K., Reddy M.M. (2003) Characterization and diagenesis of strong-acid carboxyl groups in humic substances. Applied Geochemistry 18:471-482. Li L., Huang W., Peng P., Sheng G., Fu J. (2003) Chemical and molecular heterogeneity of humic acids repetitively extracted from a Peat. Soil Science Society of America journal 67:740-746. Li L., Zhao Z., Huang W., Peng P., Sheng G., Fu J. (2004) Characterization of humic acids fractionated by ultrafiltration. Organic Geochemistry 35:1025-1037. Mao J.D., Xing B.S., Schmidt-Rohr K. (2001) New structural information on a humic acid from two-dimensional H-1-C-13 correlation solid-state nuclear magnetic resonance. Environmental Science & Technology 35:1928-1934. Martyniuk H., Wieckowska J. (2003) Adsorption of metal ions on humic acids extracted from brown coals. Fuel Processing Technology 84:23-36. Maurer F., Christl I., Kretzschmar R. (2010) Reduction and Reoxidation of Humic Acid: Influence on Spectroscopic Properties and Proton Binding. Environmental Science & Technology 44:5787-5792. Perminova I.V., Frimmel F.H., Kudryavtsev A.V., Kulikova N.A., Abbt-Braun G., Hesse S., Petrosyan V.S. (2003) Molecular weight characteristics of humic substances from different environments as determined by size exclusion chromatography and their statistical evaluation. Environmental Science & Technology 37:2477-2485. Piccolo A., Conte P., Trivellone E., Lagen B.V., Buurman P. (2002) Reduced Heterogeneity of a Lignite Humic Acid by Preparative HPSEC Following Interaction with an Organic Acid. Characterization of Size-Separates by Pyr-GC-MS And 1H-NMR Spectroscopy. Environmental Science & Technology 36:76-84. Richard, F. C., and A. C. M. Bourg. 1991. Aqueous Geochemistry of Chromium: A review. Water Research. 25:807-816. van Zomeren A., Comans R.N.J. (2007) Measurement of humic and fulvic acid concentrations and dissolution properties by a rapid batch procedure. Environmental Science & Technology 41:6755-6761. Wang J.N., Li A.M., Zhou Y., Xu L. (2009) Study on the influence of humic acid of different molecular weight on basic ion exchange resin''s adsorption capacity. Chinese Chemical Letters 20:1478-1482. World Health Organisation (2004) Guidelines for drinking waterquality, 3rd edn, vol 1. Recommendations. WHO Geneva, Switzerland Wittbrodt P.R., Palmer C.D. (1996) Reduction of Cr(V1) by soil humic acids. European Journal of Soil Science 47:151-162. Weber, J.H. 1988. Binding and transport of metals by humic materials. p. 165-178. In F.H. Frimmel and R.F. Christman (ed.) Humic substances and their role in the environment. John Wiley & Sons, Chichester, UK. Yau, W.W., Kirkland, J.J., Bly, D.D., 1979. Modern Size Exclusion Liquid Chromatography. John Wiley & Sons, New York. Zhilin D.M., Schmitt-Kopplin P., Perminova I.V. 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摘要: Humic acids (HAs) are one of the major components in soils which influence greatly the behavior and fate of heavy metals in the environment. Due to the high chemical and structural heterogeneities of HAs, of which domains in humic substances involved in Cr (VI) removal are barely understood. Thus, in the study, a repetitive extract and ultrafiltration techniques were used to fractionate HA into several fractions containing various proportions of aliphatic and aromatic carbons and molecular weights. Three fractions (denoted as F1, F2, and F3) and five molecular weights (MWs) of HAs (Bulk, >100kD, 50-100kD, <10kD) were obtained by a repetitive extraction method and by using a hollow-fiber tangential flow filtration (TFF) system, respectively, from a Yangming Mountain peat soil, Taiwan. In the study, the chemical properties of each HA fraction were characterized by FTIR and 13C-NMR spectroscopy before and after reaction with Cr(VI). Spectral analyses found that the contents of aromatic and oxygen-containing C decreased with a progressive extraction, and lower molecular weights of HAs contained more aromatic carbons and carboxyl groups. The interactions of each HA fractions with Cr(VI) showed that Cr (VI) removal could be enhanced under illumination, and the removal was attributed to Cr(VI) reduction. The redox product, i.e, Cr(III), was either adsorbed on residual HAs or released into the solution. A higher aromatic C content and a smaller molecular weight of humic acid exhibited a greater efficiency for Cr(VI) reduction, and the 13C NMR and FTIR results indicated that the carboxyl and phenolic groups enriched in these domains of HAs were responsible for the enhancement of Cr (VI) reduction. Time-dependent FTIR and 13C NMR spectra suggested that the activated sites on HA were rapidly consumed or dissolved into the solutions upon Cr(VI) oxidation. Thus, Cr(VI) may react directly with dissolved organic C (DOC) in the solution instead of on the surfaces of HA fractions. In conclusion, the O-containing groups of HAs were dominant sites for Cr(VI) reduction; however, the redox reactions proceeded very slowly unless the light participated to the reaction. With an increase of DOC concentrations upon Cr(VI) interactions with HAs, this study highlighted the possibilities that DOC derived from HAs may react with Cr(VI) much longer to complement the slow reactions between these two reactants. Thus, HAs may still have a profound effect to Cr(VI) reduction in a soil system.
URI: http://hdl.handle.net/11455/28220
其他識別: U0005-0802201111560600
文章連結: http://www.airitilibrary.com/Publication/alDetailedMesh1?DocID=U0005-0802201111560600
Appears in Collections:土壤環境科學系

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