Sorption Selectivity in Natural Organic Matter Probed with Fully Deuterium-Exchanged and Carbonyl-13C-Labeled Benzophenone and 1H-13C NMR Spectroscopy

被引:20
作者
Cao, Xiaoyan [2 ]
Lattao, Charisma [3 ]
Pignatello, Joseph J. [3 ]
Mao, Jingdong [1 ,2 ]
Schmidt-Rohr, Klaus [4 ]
机构
[1] Nanjing Agr Univ, Coll Sci, Dept Chem, Nanjing 210095, Jiangsu, Peoples R China
[2] Old Dominion Univ, Dept Chem & Biochem, Norfolk, VA 23529 USA
[3] Connecticut Agr Expt Stn, Dept Environm Sci, New Haven, CT 06504 USA
[4] Iowa State Univ, Dept Chem, Ames, IA 50011 USA
基金
美国国家科学基金会;
关键词
DISTRIBUTED REACTIVITY MODEL; STATE C-13 NMR; HUMIC SUBSTANCES; PHENANTHRENE SORPTION; SOIL; DOMAINS; SEDIMENTS; HETEROGENEITY; CONTAMINANT; SITES;
D O I
10.1021/es501129f
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Specific functional-group or domain interactions of fully deuterium-exchanged, carbonyl-C-13-labeled benzophenone and different types of natural organic matter (NOM) were investigated through two-dimensional H-1-C-13 heteronuclear correlation NMR spectroscopy. The sorbents included Beulah-Zap lignite, type II kerogen (IL-6), Pahokee peat, Amherst humic acid, and a polystyrenepoly(vinylmethyl ether) (PS-PVME) blend. PS-PVME consists of PS and PVME chains that are mixed on a scale of <5 nm. The NOM sorbents all consist predominantly of a mixed aromatic-alkyl or aromatic-O-alkyl matrix that is homogeneous on the 3 nm scale, as evidenced by fast equilibration of aromatic and alkyl H-1 magnetization. In addition, Beulah lignite and IL-6 kerogen exhibit small fractions of distinct polymethylene (CH2)(n) domains, and Pahokee peat contains significant fractions of polar and nonpolar alkyl domains. Benzophenone-(C-13=O)-d(10) shows proximity to both aromatic rings and alkyl segments in all samples but preferentially interacts with aromatic rings in PS-PVME and Beulah lignite, possibly due to pi-pi electron donor-acceptor interactions. The data for IL-6 kerogen are also compatible with preferential location of benzophenone near the alkyl-substituted edges of aromatic rings, while in Pahokee peat, clear signatures of benzophenone affinity to both aromatic-rich and nonpolar alkyl domains have been detected. Amherst humic acid shows evidence of some affinity to polar alkyl segments but which is weaker than that to aromatic rings. Our results indicate that specific interactions of the sorbate and the presence of domains in the sorbent influence the magnitude and selectivity of sorption.
引用
收藏
页码:8645 / 8652
页数:8
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