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Spectroscopic and molecular characterization of humic substances (HS) from soils and sediments in a watershed: comparative study of HS chemical fractions and the origins

机译:流域土壤和沉积物中腐殖质(HS)的光谱和分子表征:HS化学分数的比较研究及起源

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摘要

Optical properties and molecular composition of humic substances (HS) can provide valuable information on the sources and the history of the associated biogeochemical processes. In this study, many well-known spectral and molecular characteristics were examined in eight different HS samples, which were extracted from soils and sediments located in a forested watershed, via two advanced tools including fluorescence excitation emission matrix-parallel factor analysis (EEM-PARAFAC) and high-resolution Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS). Two humic-like (C1 and C2) and one protein-like (C3) components were identified from EEM-PARAFAC. Irrespective of the origins, humic acid (HA) fractions were distinguished from fulvic acid (FA) fractions by the HS characteristics of specific UV absorbance (SUVA), the number of formulas, maximum fluorescence intensities of C1 and C2, condensed aromatics, tannins, and CHON, CHOS, and CHONS classes. In contrast, only five HS indices, including C3 intensity, H%, modified aromatic index (AI(mod)), the percentages of carbohydrates, and unsaturated hydrocarbons, were found to be significant factors in discriminating between the two HS origins (i.e., soils and sediments). The ordination of the Bray-Curtis dissimilarity matrix further confirmed that the HS chemical fraction (i.e., HA or FA) was the more important factor to determine the measured HS characteristics than the HS origin. Our results provided an in-depth insight into the chemical and structural heterogeneity of bulk HS, which could be even beyond the differences observed along the two HS origins. This study also delivers a cautious message that the two operationally defined HS chemical fractions should be carefully considered in tracking the origins of different HS samples.
机译:腐殖质物质(HS)的光学性质和分子组成可以提供有关相关生物地球化学过程的源和历史的有价值的信息。在这项研究中,在八种不同的HS样品中检查了许多众所周知的光谱和分子特性,该样品从位于森林流域的土壤和沉积物中提取,通过两个先进的工具,包括荧光激发发射矩阵平行因子分析(EEM-Parafacac )和高分辨率傅里叶变换离子回旋谐振质谱(FT-ICR MS)。从EEM-PARAFAC中鉴定出两个腐殖质(C1和C2)和一种蛋白质(C3)组分。与起源而言,通过特异性UV吸光度(SUVA)的HS特征,腐殖酸(HA)级分与特定UV吸光度(SUVA)的特征区分开,所述公式的数量,C1和C2的最大荧光强度,所述浓缩芳烃,单宁,Tannins,和chon,chos和chons课程。相反,仅发现五个HS指数,包括C3强度,H%,改性的芳族指数(AI(MOD)),碳水化合物和不饱和烃的百分比,是在两个HS起源之间区分的重要因素(即,土壤和沉积物)。 Bray-Curtis异化基质的序列进一步证实HS化学级分(即HA或Fa)是确定比HS原点的测量的HS特性更重要的因素。我们的结果介绍了对散装HS的化学和结构异质性的深入深入了解,这甚至可以超出沿两个HS起源观察到的差异。本研究还提供了一种谨慎的消息,即应仔细考虑跟踪不同HS样品的起源的两种操作定义的HS化学分数。

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