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首页> 外文期刊>Geoderma: An International Journal of Soil Science >CHARACTERIZATION OF THE ORGANIC COMPONENTS OF AN ALFISOL AND A VERTISOL IN ADJACENT LOCATIONS IN INDIAN SEMI-ARID TROPICS USING OPTICAL SPECTROSCOPY, C-13 NMR SPECTROSCOPY, AND C-14 DATING
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CHARACTERIZATION OF THE ORGANIC COMPONENTS OF AN ALFISOL AND A VERTISOL IN ADJACENT LOCATIONS IN INDIAN SEMI-ARID TROPICS USING OPTICAL SPECTROSCOPY, C-13 NMR SPECTROSCOPY, AND C-14 DATING

机译:利用光谱学,C-13 NMR光谱学和C-14约会表征印度半干旱热带地区邻近地点的Alfisol和VERTISOL的有机成分

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Organic components of an Alfisol and a Vertisol in adjacent locations in Indian semi-arid tropics were characterized using chemical analysis, photometric and high resolution solid-state C-13 nuclear magnetic resonance (NMR) spectroscopies, and C-14 dating. The organic carbon contents of the Alfisol (0.50-0.25%) were about half the ones of the Vertisol (0.69-0.48%). Among the organic components, fulvic acids were found to be the major constituents, about 80-90% in the Alfisol and 70% in the Vertisol. These figures suggested faster organic decomposition in the Alfisol. The color intensities (K-600/C) of humic acids of the Alfisol increased from the surface through deeper layers, while those of the Vertisol remained constant in all the layers. The C-13 NMR measurements on the humic acids of both soils suggested the presence of polymethylene-, methyl-, N-methyl-, O-methyl-, dioxygenated-, O-alkyl-, aromatic-, phenolic or quaternary-, and carboxyl carbons. The Alfisol humic acid samples were characterized by a higher content of unsaturated (110-0 ppm) carbons and a lower content of quaternary (145-120 ppm) carbons than those of the Vertisol, Radiocarbon dating showed that the humic acids of the Alfisol were of modern (10 cm) through 2520 yr BP (40 cm) years old, while those of the Vertisol were in a narrower range of 4650 yr BP (10 cm) through 5440 yr BP (40 cm), Close relationships among radiocarbon dating, photometric, and NMR spectrometric characteristics of humic acids were suggested.
机译:使用化学分析,光度和高分辨率固态C-13核磁共振(NMR)光谱学和C-14测年,对印度半干旱热带地区邻近地点的Alfisol和Vertisol的有机成分进行了表征。 Alfisol(0.50-0.25%)的有机碳含量约为Vertisol(0.69-0.48%)的一半。在有机成分中,富里酸是主要成分,在Alfisol中约为80-90%,在Vertisol中为70%。这些数字表明在Alfisol中有机物分解更快。 Alfisol的腐殖酸的色强度(K-600 / C)从表面到更深的层增加,而Vertisol的色强度在所有层中保持恒定。在两种土壤的腐殖酸上进行的C-13 NMR测量表明,存在多亚甲基,甲基,N-甲基,O-甲基,双加氧,O-烷基,芳族,酚或季铵盐,以及羧基碳。 Alfisol腐殖酸样品的特征在于其不饱和碳(110-0 ppm)碳含量较高,而季铵盐(145-120 ppm)碳含量则低于Vertisol。放射性碳测年表明Alfisol的腐殖酸为(10 cm)到2520年BP(40 cm)岁之间的距离,而Vertisol的范围则在4650 yr BP(10 cm)到5440 yr BP(40 cm)的较窄范围内,放射性碳测年之间的密切关系,提出了腐殖酸的光度和核磁共振光谱特征。

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