Tracing TiO₂ photocatalytic degradation of humic acid in the presence of clay particles by excitation-emission matrix (EEM) fluorescence spectra

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• 作者：Sibel Sen Kavurmaci ; ^{sibel.sen@boun.edu.tr" class="auth_mail} ; ^{sibel.sen@gmail.com" class="auth_mail} ; Miray Bekbolet
• 关键词：EEM fluorescence spectra ; Humic acid ; Kaolinite ; Montmorillonite ; Photocatalysis ; TiO2
• 刊名：Journal of Photochemistry and Photobiology A: Chemistry
• 出版年：15 May, 2014
• 年：2014
• 卷：282
• 期：Complete
• 页码：53-61
• 全文大小：3616 K

文摘

Excitation-emission matrix (EEM) fluorescence spectral features were evaluated for the elucidation of the photocatalytic degradation of sole humic acid (HA) and HA in the presence of clay minerals. Montmorillonite (Mt) or kaolinite (Kt) was selected to represent two different types of clay minerals. EEM fluorescence signatures displayed irradiation time dependent transformation of humic-like fluorophores to fulvic-like fluorophores in accordance with the photocatalytic mineralization of HA. The role of Ca²⁺ ions on the photocatalytic degradation of HA could also be visualized through EEM under the specified conditions. Upon photocatalytic treatment, the role of Mt was more pronounced with respect to the effects observed in the presence of Kt in comparison to the results achieved for sole HA. Under prolonged irradiation conditions (m>tm>_irr = 180 min) almost complete removal of fluorophoric groups was detected in relation to a substantial degree of mineralization (>75% removal of dissolved organic carbon, DOC). As a correlative approach, fluorescence-derived index defined as fluorescence intensity (FI) represented by the ratio of the emission intensity at m>位m>_emis = 450 nm to that at m>位m>_emis = 500 nm, following excitation at m>位m>_exc = 370 nm was successfully employed. FI values were correlated to specified UV parameters (UV₂₅₄ and UV₂₈₀) revealing an inverse relationship. Moreover, through normalization of the specified UV parameters to DOC contents, the derived specific UV parameters (SUVA₂₅₄ and SUVA₂₈₀) could also be successfully correlated to FI. The obtained results indicated that besides photocatalytic mineralization efficiencies, UV-vis and fluorescence spectroscopic properties could also be employed to gain further information on the humic structural changes attained through non-selective oxidation mechanism in comparison to the data obtained under non-oxidative conditions.