Effect of DOM derived from straw in West Sichuan plain on fine mineral particle adsorbing SMX
LI Ming1,2, WANG Bin1,2, ZHU Jing-ping1, CHEN Shu1,2, BAI Ying-chen3, WANG You-zhi1,4, TAN Jiang-yue1, FU Xin-mei1
1. School of Environment and Resource, Southwest University of Science and Technology, Mianyang 621010, China;
2. Key Laboratory of Solid Waste Treatment and Resource Recycle, Ministry of Education, Southwest University of Science and Technology, Mianyang 621010, China;
3. State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environment Sciences, Beijing 100012, China;
4. Chengdu Shude Huaiyuan middle school, Chengdu 611237, China
Effect mechanism of the dissolved organic matter (DOM) extracted from crop straw to adsorption processes of sulfamethoxazole (SMX) on the mineral fine particles was tracked. Under the effect of DOM, the adsorption kinetics of SMX on those particles were compared. The fourier transform infrared spectroscopy (FI-IR) characteristics of mineral particles in processes were analyzed. The adsorption kinetics of SMX on the minerals was well fitted by the two-compartment first order kinetic model, implying that the adsorption processes occurred with the adsorption of the multi-domains or multiple sites. Adsorption quantity of SMX with DOM on montmorillonite, albite and calcite, to a certain extent, had the increase of 28.94, 28.34 and 2.40μg/g. However, the fitting degrees of the two-compartment first order kinetic model were decreased. Base on the FI-IR analysis, the peak values of montmorillonite around 3700, 1600 and 1000cm-1of the wave numbers and the wide range of 3600~3000cm-1 were weakened. Moreover, the FI-IR characteristics with the DOM effect were similar. The relatively high capacity was related with the supplemental adsorption sites of montmorillonite because of the interaction between Al3+ and DOM. The spectral features of the albite in adsorption processes had slight fluctuation. However, the peak values in the DOM-albite-SMX adsorption system decreased significantly around the 1013, 781 and 460cm-1 of wave numbers. The phenomenon indicated that the adsorbing capacity of albite increased constantly via the common and/or continuous adsorption. Moreover, the spectral characteristics of calcite in the interaction processes of calcite-SMX and DOM-calcite-SMX were analogous, implying little or no effect of DOM. Nevertheless, the increments in the complex matrices could be related to the combination between DOM and SMX.
黎明, 王彬, 朱静平, 谌书, 白英臣, 王有志, 谭江月, 付新梅. 川西平原还田秸秆DOM对矿物细颗粒吸附SMX的影响[J]. 中国环境科学, 2016, 36(11): 3441-3448.
LI Ming, WANG Bin, ZHU Jing-ping, CHEN Shu, BAI Ying-chen, WANG You-zhi, TAN Jiang-yue, FU Xin-mei. Effect of DOM derived from straw in West Sichuan plain on fine mineral particle adsorbing SMX. CHINA ENVIRONMENTAL SCIENCECE, 2016, 36(11): 3441-3448.
Mader B T, Uwe-Goss K, Eisenreich S J. Sorption of nonionic, hydrophobic organic chemicals to mineral surfaces[J]. Environmental Science & Technology, 1997,31(4):1079-1086.
[3]
Schwarzenbach R P, Westall J. Transport of nonpolar organic compounds from surface water to groundwater. Laboratory sorption studies[J]. Environmental Science & Technology, 1981,15(11):1360-1367.
Chen W, Westerhoff P, Leenheer J, et al. Fluorescence excitation-emission matrix regional integration to quantify spectra for dissolved organic matter[J]. Environmental Science & Technology, 2003,37(24):5701-5710.
[6]
Chen M, Jin H. Pre-treatments, characteristics, and biogeochemical dynamics of dissolved organic matter in sediments:A review[J]. Water Research, 2015,79:10-25.
[7]
Philippe A, Schaumann G E. Interactions of dissolved organic matter with natural and engineered inorganic colloids:a review[J]. Environmental Science & Technology, 2014,48(16):8946-62.
Marschner B, Brodowski S, Dreves A, et al. How relevant is recalcitrance for the stabilization of organic matter in soils?[J]. Journal of Plant Nutrition & Soil Science, 2008,171(1):91-110.
Qu X, Xie L, Lin Y, et al. Quantitative and qualitative characteristics of dissolved organic matter from eight dominant aquatic macrophytes in Lake Dianchi, China[J]. Environmental Science & Pollution Research, 2013,20(10):7413-7423.
[12]
Wang L Y, Wu F C, Zhang R Y, et al. Characterization of dissolved organic matter fractions from Lake Hongfeng,Southwestern China Plateau[J]. 环境科学学报(英文版), 2009, 21(5):581-8.
Nebbioso A, Piccolo A. Molecular characterization of dissolved organic matter (DOM):a critical review[J]. Analytical & Bioanalytical Chemistry, 2013,405(1):109-24.
[16]
Chen G, Chao L, Liang C, et al. Effect of size-fractionation dissolved organic matter on the mobility of prometryne in soil[J]. Chemosphere, 2010,79(11):1046-55.
[17]
Jiang L, Huang J, Liang L, et al. Mobility of prometryne in soil as affected by dissolved organic matter[J]. Journal of Agricultural & Food Chemistry, 2008,56(24):11933-40.
[18]
Ning H, Liang C, Hong Y. Effect of dissolved organic matter on mobility and activation of chlorotoluron in soil and wheat[J]. Geoderma, 2008,146(1/2):344-352.
[19]
Hou J, Bo P, Niu X, et al. Sulfamethoxazole sorption by sediment fractions in comparison to pyrene and bisphenol A[J]. Environmental Pollution, 2010,158(9):2826-32.
[20]
Pan B, Xing B S, Xu J M, et al. Adsorption kinetics of 17α-ethinyl estradiol and bisphenol A on carbon nanomaterials. I. Several concerns regarding pseudo-first order and pseudo-second order models[J]. Journal of Soils & Sediments Protection Risk Assessment & Rem, 2010,10(5):838-844.
[21]
Ding Q, Wu H L, Xu Y, et al. Impact of low molecular weight organic acids and dissolved organic matter on sorption and mobility of isoproturon in two soils[J]. Journal of Hazardous Materials, 2011,190(1-3):823-32.
Shi K, Wang X, Guo Z, et al. Se(IV) sorption on TiO2:Sorption kinetics and surface complexation modeling[J]. Colloids & Surfaces A Physicochemical & Engineering Aspects, 2009, 349(1-3):90-95.