A lignite humic acid (HA) was fractionated by preparative high performance size-exclusion chromatography (HPSEC) in seven different size-fractions. The size-fractions were characterized by cross polarization (CP) magic angle spinning (MAS) 13C NMR spectroscopy and a further analytical HPSEC elution under UV and fluorescence detection. The alkyl hydrophobic components mainly distributed in the largest molecular-size-fraction, whereas the amount of oxidized carbons increased with decreasing size of fractions. Cross polarization time (TCH) and proton spin-lattice relaxation time in the rotating frame (T1ρ(H)) were measured from variable contact time (VCT) experiments. The bulk HA was characterized by the shortest TCH values and the longest T1ρ(H) values which suggested, respectively, one. an aggregation of components in a large conformation that favored a fast H–C cross polarization, and, two. consequent steric hindrances that prevented fast local molecular motions and decreased proton relaxation rates. Conversely, the separated size-fractions showed longer TCH values and shorter T1ρ(H) values than the bulk HA, thereby indicating that they were constituted by a larger number of mobile molecular conformations. The UV and fluorescence absorptions were both low in the large size-fractions that mainly contained alkyl carbons, whereas they increased in the olephinic- and aromatic-rich fractions with intermediate molecular-size, and decreased again in the smaller fractions which were predominantly composed by oxidized carbons. These results support the supramolecular structure of humic substances and indicate that the observed variation in conformational distribution in humic association may be used to explain environmental processes with additional precision.

CONTE P, R SPACCINI, D SMEJKALOVA, A NEBBIOSO, A PICCOLO (2007). Spectroscopic and conformational properties of size-fractions separated from a lignite humic acid. CHEMOSPHERE, 69(7), 1032-1039 [10.1016/j.chemosphere.2007.04.043].

Spectroscopic and conformational properties of size-fractions separated from a lignite humic acid

CONTE, Pellegrino;
2007-01-01

Abstract

A lignite humic acid (HA) was fractionated by preparative high performance size-exclusion chromatography (HPSEC) in seven different size-fractions. The size-fractions were characterized by cross polarization (CP) magic angle spinning (MAS) 13C NMR spectroscopy and a further analytical HPSEC elution under UV and fluorescence detection. The alkyl hydrophobic components mainly distributed in the largest molecular-size-fraction, whereas the amount of oxidized carbons increased with decreasing size of fractions. Cross polarization time (TCH) and proton spin-lattice relaxation time in the rotating frame (T1ρ(H)) were measured from variable contact time (VCT) experiments. The bulk HA was characterized by the shortest TCH values and the longest T1ρ(H) values which suggested, respectively, one. an aggregation of components in a large conformation that favored a fast H–C cross polarization, and, two. consequent steric hindrances that prevented fast local molecular motions and decreased proton relaxation rates. Conversely, the separated size-fractions showed longer TCH values and shorter T1ρ(H) values than the bulk HA, thereby indicating that they were constituted by a larger number of mobile molecular conformations. The UV and fluorescence absorptions were both low in the large size-fractions that mainly contained alkyl carbons, whereas they increased in the olephinic- and aromatic-rich fractions with intermediate molecular-size, and decreased again in the smaller fractions which were predominantly composed by oxidized carbons. These results support the supramolecular structure of humic substances and indicate that the observed variation in conformational distribution in humic association may be used to explain environmental processes with additional precision.
2007
Settore AGR/13 - Chimica Agraria
CONTE P, R SPACCINI, D SMEJKALOVA, A NEBBIOSO, A PICCOLO (2007). Spectroscopic and conformational properties of size-fractions separated from a lignite humic acid. CHEMOSPHERE, 69(7), 1032-1039 [10.1016/j.chemosphere.2007.04.043].
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/10447/19201
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