On the chemical mechanism of kerogen thermal transformation. Study of the transformation of sporopollenin
Identifieur interne : 001720 ( Main/Exploration ); précédent : 001719; suivant : 001721On the chemical mechanism of kerogen thermal transformation. Study of the transformation of sporopollenin
Auteurs : M. A. Bestougeff [France] ; R. J. Byramjee [France] ; B. Pesneau [France]Source :
- Organic Geochemistry [ 0146-6380 ] ; 1985.
Abstract
Experiments were carried out on the thermal decomposition of sporopollenin, isolated from a marine algae (Lycopodium clavatum) at constant temperature (380°C) and pressure (around 200 atm), but for varying pyrolysis times.The decomposition products were separated into groups, analysed by chromatography and infra-red spectroscopy, and their elemental composition determined. The thermal evolution of sporopollenin proceeds in three distinct steps: first, a partial decomposition of the initial substance occurs with the formation of soluble materials. This is followed by a full decomposition of the sporopollenin and disappearance of the non-soluble residue. Finally, a non-soluble material reappears. It is proposed that, due to secondary reactions, the evolution of kerogen of the sapropelic type is similar to what has been observed in mild pyrolysis experiments.
Url:
DOI: 10.1016/0146-6380(85)90017-8
Affiliations:
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<front><div type="abstract" xml:lang="en">Experiments were carried out on the thermal decomposition of sporopollenin, isolated from a marine algae (Lycopodium clavatum) at constant temperature (380°C) and pressure (around 200 atm), but for varying pyrolysis times.The decomposition products were separated into groups, analysed by chromatography and infra-red spectroscopy, and their elemental composition determined. The thermal evolution of sporopollenin proceeds in three distinct steps: first, a partial decomposition of the initial substance occurs with the formation of soluble materials. This is followed by a full decomposition of the sporopollenin and disappearance of the non-soluble residue. Finally, a non-soluble material reappears. It is proposed that, due to secondary reactions, the evolution of kerogen of the sapropelic type is similar to what has been observed in mild pyrolysis experiments.</div>
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