Evolution of Dissolved Organic Matter Properties in a Constructed Wetland of Xiao River, Hebei
MA Li-na1, 2, 3, ZHANG Hui2, 3, TAN Wen-bing2, 3, YU Min-da2, 3, HUANG Zhi-gang1, GAO Ru-tai2, 3*, XI Bei-dou2, 3, HE Xiao-song2, 3
1. Agricultural College of Guangxi University, Nanning 530004, China 2. State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China 3. Innovation Base of Ground Water & Environmental System Engineering, Chinese Research Academy of Environmental Science, Beijing 100012, China
Abstract：The evolution of water DOC and COD, and the source, chemical structure, humification degree and redox of dissolved organic matter (DOM) in a constructed wetland of Xiao River, Hebei, was investigated by 3D excitation–emission matrix fluorescence spectroscopy coupled with ultraviolet spectroscopy and chemical reduction, in order to explore the geochemical processes and environmental effects of DOM. Although DOC contributes at least 60% to COD, its decrease in the constructed wetland is mainly caused by the more extensive degradation of elements N, H, S, and P than C in DOM, and 65% is contributed from the former. DOM is mainly consisted of microbial products based on proxies f470/520 and BIX, indicating that DOM in water is apparently affected by microbial degradation. The result based on PARAFAC model shows that DOM in the constructed wetland contains protein-like and humus-like components, and Fulvic- and humic-like components are relatively easier to degrade than protein-like components. Fulvic- and humic-like components undergo similar decomposition in the constructed wetland. A common source of chromophoric dissolved organic matter (CDOM) and fluorescent dissolved organic matter (FDOM) exists; both CDOM and FDOM are mainly composed of a humus-like material and do not exhibit selective degradation in the constructed wetland. The proxies E2/E3，A240～400，r(A, C) and HIX in water have no changes after flowing into the constructed wetland, implying that the humification degree of DOM in water is hardly affected by wet constructed wetland. However, the constructed wetland environment is not only beneficial in forming the reduced state of DOM, but also facilitates the reduction of ferric. It can also improve the capability of DOM to function as an electron shuttle. This result may be related to the condition that the aromatic carbon of DOM can be stabilized well in the constructed wetland.
[1] Maie N, Yamashita Y, Cory R M, et al. Appl. Geochem., 2012, 27: 917. [2] Fu P, Wu F, Liu C, et al. Appl. Geochem., 2007, 22: 1668. [3] Nelson N B, Siegel D A. Annu. Rev. Mar. Sci., 2013, 5: 447. [4] Mariot M, Dudal Y, Furian S, et al. Sci. Total Environ., 2007, 388: 184. [5] Hijosa-Valsero M, Sidrach-Cardona R, Martín-Villacorta J, et al. Chemosphere, 2010, 81: 651. [6] Zhang H C, Weber E J. Environ. Sci. Technol., 2009, 43(4): 1042. [7] Guo W D, Stedmon C A, Han Y C, et al. Mar. Chem., 2007, 107: 357. [8] Vignudelli S, Santinelli C, Murru E, et al. Estuar. Coast. Shelf S., 2004, 60(1): 133. [9] Kimberly P W, Jason C N, George R A. Ecosystems, 2007, 10(8): 1323. [10] Ohno T. Environ. Sci. Technol., 2002, 36(4): 742. [11] Patel-Sorrentino N, Mounier S, Benaim J Y. Water Res., 2002, 36(10): 2571. [12] Wang L Y, Wu F C, Zhang R Y, et al. J. Environ. Sci-China, 2009, 21: 581. [13] Cory R M, Mcknight D M. Environ. Sci. Technol., 2005, 39: 8142. [14] Nurmi J T, Tratnyek P G. Environ. Sci. Technol., 2002, 36: 617. [15] Sposito G, Struyk Z. Geoderma, 2001, 102: 329.
