Ketones
are major oxygen-containing compounds in low-temperature
coal tars (LTCTs); however, the molecular composition of these compounds
is not well characterized as a result of the complexity of itself
and the interference of the coal tar matrix. In this study, ketones
were separated from a LTCT and characterized by Fourier transform
ion cyclotron resonance mass spectrometry (FT-ICR MS), Orbitrap mass
spectrometry (Orbitrap MS), and gas chromatography–mass spectrometry
(GC–MS). Isolation of ketones was carried out by a chemical
derivatization process with Girard T reagent and followed by a hydrolysis
process of the derivatives. The Girard T reagent reacted with ketones
under weakly acidic conditions and introduced a charged quaternary
ammonium moiety on carbonyl to form water-soluble hydrazones, which
can be separated from a complex matrix through an extrography separation
and have a strong response in a positive-ion electrospray ionization
(ESI) source for mass spectrometric analysis. The isolated derivatives
were reversibly turned into the original ketones to selectively separate
long alkyl ketones from aromatic ketones with alkyl substituents of
C0–C4. The ketones were assigned to 12
class species by high-resolution MS analysis: O1–5 (refers that there are 1–5 oxygen atoms in the molecules),
O1S1, N1O1–4, and
N2O1–2, among which the O1 class species was the most abundant. The long-chain alkyl ketones,
such as aliphatic 2-, 3-, and 4-ketones, alkylcyclopentanones, alkyl
phenyl ketones, and aromatic ketones (such as indanone, cyclopentenone,
tetralone, acetonaphthone, dihydrophenanthrenone, benzophenone, fluorenone,
fluorenyl formaldehyde, anthrone, anthracene formaldehyde, acetylanthracene,
acetylphenanthrene, acetylfluorene, benzofluorenone, etc.), were detected
by GC–MS. In addition, C18-isoprenoid methyl ketone
and tricyclic terpenoids and steroids with one or two oxygen atoms
were found in the coal tar.