Analysis of asphaltenic ketones in fossil material
Asphaltenes, defined as the fraction of petroleum that is insoluble in n-pentane or n-heptane but soluble in toluene or benzene, are a very complex mixture of polycyclic aromatic hydrocarbons (PAHs) variably substituted with alkyl groups, heteroatoms (N, S, and O), and metals (Ni and V).
Earlier studies have identified oxygen in carboxylic, phenolic, and ketonic structures. The oxygen in asphaltenes may be present as acidic hydroxyl groups. This was confirmed by the poor interaction of phenol solution with asphaltenes. Asphaltenes contain ester and ether bonds in which alcohols and carboxylic acids are bonded to the core by C-O and also C-C bonds.
Of the limited data available, there are indications that oxygen in asphaltenes can exist as nonhydrogen-bonded phenolic hydroxyl groups. Other information on the presence and nature of oxygen in asphaltenes has been derived from infrared spectroscopic examination of the products after interaction of the asphaltenes with acetic anhydride. This has produced evidence for the presence of ketones and/or quinones as well as indications that a considerable portion of the hydroxyl groups present in asphaltenes may exist as collections of two or more hydroxyl functions on the same aromatic ring, or on adjacent peripheral sites on a condensed ring system.
Via selective derivatization reactions the type of oxygen containing functional group within the asphaltenes can be identified