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核磁共振证实干腐殖质中不存在可移动碳水化合物结构域及其对有机污染物吸附模型的影响。

Absence of mobile carbohydrate domains in dry humic substances proven by NMR, and implications for organic-contaminant sorption models.

作者信息

Mao J D, Schmidt-Rohr K

机构信息

Department of Chemistry, Gilman Hall, Iowa State University, Iowa 50011, USA.

出版信息

Environ Sci Technol. 2006 Mar 15;40(6):1751-6. doi: 10.1021/es0511467.

DOI:10.1021/es0511467
PMID:16570593
Abstract

The mobility and domain structure of various standard humic substances have been investigated by 1H and 1H-13C solid-state nuclear magnetic resonance (NMR) experiments. In four dry humic acids, a fulvic acid, a natural organic matter sample, and a whole peat sample, segments that undergo fast, large-amplitude motions account for <9% of the sample. This disproves a previous suggestion, based on 1H NMR data, that flexible domains, presumably carbohydrates, make up >40% of various humic acids; these putative mobile domains were also linked to dual-mode sorption. In particular, neither the polar alkyl (carbohydrate) nor the aromatic components show any fast, large-amplitude mobility. A small fraction of mobile nonpolar alkyl segments identified by us before is the only component undergoing large-amplitude motions, apart from absorbed water that we observe in humic acids exposed to ambient air. 1H-13C wide-line separation NMR shows that, contrary to previous suggestions, the dipolar couplings in the aromatic regions are smaller than in the polar alkyl segments, most likely due to differences in local 1H densities. Series of 1H-13C heteronuclear correlation experiments with 1H spin diffusion reveal close proximity of aromatic and polar alkyl segments in several humic acids, precluding carbohydrate domains on a scale of > 1-nm diameter. In the standard peat humic acid, nonpolar aromatic segments also do not form sorption domains of significant size, while nonpolar aliphatic domains, which we had previously shown to correlate with sorption capacity, have been confirmed.

摘要

通过1H和1H-13C固态核磁共振(NMR)实验研究了各种标准腐殖质的流动性和域结构。在四种干腐殖酸、一种富里酸、一个天然有机物样品和一个完整泥炭样品中,经历快速、大幅度运动的片段占样品的比例不到9%。这反驳了先前基于1H NMR数据提出的观点,即柔性域(可能是碳水化合物)占各种腐殖酸的比例超过40%;这些假定的移动域也与双模式吸附有关。特别是,极性烷基(碳水化合物)和芳香族成分均未表现出任何快速、大幅度的流动性。除了在暴露于环境空气中的腐殖酸中观察到的吸附水外,我们之前确定的一小部分可移动非极性烷基片段是唯一经历大幅度运动的成分。1H-13C宽线分离NMR表明,与先前的观点相反,芳香族区域的偶极耦合小于极性烷基片段,这很可能是由于局部1H密度的差异。一系列具有1H自旋扩散的1H-13C异核相关实验表明,几种腐殖酸中芳香族和极性烷基片段紧密相邻,排除了直径大于1 nm尺度上的碳水化合物域。在标准泥炭腐殖酸中,非极性芳香族片段也不会形成显著大小的吸附域,但我们之前已证明与吸附能力相关的非极性脂肪族域得到了证实。

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