Sorption and Fractionation of a Peat Derived Humic Acid by Kaolinite, Montmorillonite, and Goethite

被引:62
|
作者
Ghosh, S. [1 ]
Wang Zhen-Yu [2 ]
Kang, S. [1 ]
Bhowmik, P. C. [1 ]
Xing, B. S. [1 ,2 ]
机构
[1] Univ Massachusetts, Dept Plant Soil & Insect Sci, Amherst, MA 01003 USA
[2] Ocean Univ China, Coll Environm Sci & Engn, Qingdao 266100, Peoples R China
关键词
carboxylic group; DRIFT; hydrophobic; NMR; sequential coating; DISSOLVED ORGANIC-CARBON; MINERAL SURFACES; MATTER FRACTIONS; CLAY-MINERALS; ADSORPTION; SOIL; SUBSTANCES; PHENANTHRENE; ALUMINUM; NMR;
D O I
10.1016/S1002-0160(08)60080-6
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Sorption of humic acid (HA) oil mineral surfaces has a profound interest regarding the fate of hydrophobic organic contaminants (HOCs) and carbon sequestration in soils. The objective of our study is to determine the fractionation behavior of HA upon sorption oil mineral surfaces with varying surface properties. HA was coated sequentially oil kaolinite (1:1 clay), montmorillonite (2:1 clay), and goethite (iron oxide) for four times. The unadsorbed HA fractions were characterized by elemental analysis, diffuse reflectance infrared Fourier transform spectroscopy (DRIFT), and solid state C-13 nuclear magnetic resonance spectroscopy (NMR). The mineral-HA complexes were characterized by DRIFT. Polarity index [(N+O)/C] revealed higher polarity of the unadsorbed HA fractions after coating oil kaolinite, reflecting that relatively higher polarity fractions of HA remain unadsorbed. Sorption of aliphatic alcohol fraction along with carbohydrate was prominent on kaolinite surface. DRIFT results of the unadsorbed HA fractions indicated more sorption of aliphatic moieties oil both kaolinite and montmorillonite. DRIFT results of the unadsorbed HA fractions after sorption oil kaolinite and goethite showed the sorption of the proteinaccous fractions of HA. The HA fractions obtained after coating on goethite showed significant sorption of carboxylic moieties. The results mentioned above comply reasonably well with the DRIFT spectra of the mineral-HA complexes. 13C NMR results showed higher sorption of anomeric C oil kaolinite surface. Higher sorption of paraffinic fraction was observed oil montmorillonite. NMR data inferred the sorption of carboxylic moieties on goethite surface. Overall, this study showed that aliphatic moieties of HA preferentially sorbed oil kaolinite and montmorillonite. while carboxylic functional groups play a significant role in sorption of HA oil goethite. The sorbed fractions of HA may modify the mineral surface properties, and thus, the interaction with organic contaminants.
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页码:21 / 30
页数:10
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