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StructuraI correlation between soil humins and kerogens as seen by analyticaI pyrolysis

Abstract

3 pages, 1 figure, 1 table, 10 references. Publicación incluida en: Select papers from the 17th International Meeting on Organic Geochemistry. 4-8/09/1995, San Sebastián, España.The possibility of the accumulation in soils of stable aliphatic materials has been postulated as a non-exclusive altemative to classical models for humus formation, based on the selective preservation of aromatic biomacromolecules. Such a hypothesis represents an actualistic approach to the formation process of fossil organic sediments and conforms to recent findings regarding the humification process in specific compartments in active terrestrial soils. In order to bring sorne light into this possible connection we investigated the pyrolytic behaviour of humin preparations isolated by two physical methods.Peer reviewe

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