Structural characterization of charcoal size-fractions from a burnt Pinus pinea forest by FT-IR, Raman and surface-enhanced Raman spectroscopies

Charcoal is mainly composed by aromatic C but is characterized by several degrees of aromaticity, which complicate its identification and quantification in natural environments by conventional analyses. Charcoal is an almost ubiquitous component of soil, although often occurring in minor amounts. He...

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Veröffentlicht in:Journal of molecular structure 2011-05, Vol.994 (1), p.155-162
Hauptverfasser: Francioso, Ornella, Sanchez-Cortes, Santiago, Bonora, Sergio, Roldán, Maria Lorena, Certini, Giacomo
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Sanchez-Cortes, Santiago
Bonora, Sergio
Roldán, Maria Lorena
Certini, Giacomo
description Charcoal is mainly composed by aromatic C but is characterized by several degrees of aromaticity, which complicate its identification and quantification in natural environments by conventional analyses. Charcoal is an almost ubiquitous component of soil, although often occurring in minor amounts. Hence, there is a great interest in studying the charcoal structure and understanding the behavior of charcoal in soils. In soil, it has been demonstrated that the chemical structure of charcoal is also dependant on its particle-size. In this paper we have applied infrared, normal Raman, SERS and SEF spectroscopies to study four size-fractions of charcoal (>2 mm, 2–1 mm, 1–0.5 mm and 2 mm). The presence of organic N was well evidenced by the vibration of iso-cyanate and cyanamide groups in the fractions. This result is of great environmental importance because N may be immobilized in form of stable molecules like N-heterocyclic poliaromatic structures, and so persists in soils. The soluble organic C (SOC) extracted from charcoal size-fractions did not differ from the bulk charcoal in terms of IR and Raman spectra. Instead SERS and SEF provided further information regarding the ratio between the aromatic component and the aliphatic cross-linking one in studied fractions.
doi_str_mv 10.1016/j.molstruc.2011.03.011
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Charcoal is an almost ubiquitous component of soil, although often occurring in minor amounts. Hence, there is a great interest in studying the charcoal structure and understanding the behavior of charcoal in soils. In soil, it has been demonstrated that the chemical structure of charcoal is also dependant on its particle-size. In this paper we have applied infrared, normal Raman, SERS and SEF spectroscopies to study four size-fractions of charcoal (&gt;2 mm, 2–1 mm, 1–0.5 mm and &lt;0.5 mm) and their alkaline extracts from a burnt Pinus pinea forest. Second derivative FT-IR in agreement with the normal Raman spectroscopy have given information about the size of aromatic rings and the nature of substituted groups in size-fractions of charcoal. Carbon cluster size progressively decreased in the smallest fractions suggesting that higher graphitization and crystallization occurred in the coarsest fraction (&gt;2 mm). The presence of organic N was well evidenced by the vibration of iso-cyanate and cyanamide groups in the fractions. This result is of great environmental importance because N may be immobilized in form of stable molecules like N-heterocyclic poliaromatic structures, and so persists in soils. The soluble organic C (SOC) extracted from charcoal size-fractions did not differ from the bulk charcoal in terms of IR and Raman spectra. 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The presence of organic N was well evidenced by the vibration of iso-cyanate and cyanamide groups in the fractions. This result is of great environmental importance because N may be immobilized in form of stable molecules like N-heterocyclic poliaromatic structures, and so persists in soils. The soluble organic C (SOC) extracted from charcoal size-fractions did not differ from the bulk charcoal in terms of IR and Raman spectra. 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subjects Carbon
Charcoal
Derivatives
Forests
FT-IR
Molecular structure
Normal Raman spectroscopy
Organic matter
Raman spectroscopy
Soil (material)
Surface-enhanced fluorescence
Surface-enhanced Raman scattering
Vibration
title Structural characterization of charcoal size-fractions from a burnt Pinus pinea forest by FT-IR, Raman and surface-enhanced Raman spectroscopies
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