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Control of the chemical structure of perhydrous coals. FTIR and Py-GC/MS investigations

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dc.contributor European Commission
dc.creator Iglesias, María José
dc.creator Río Andrade, José Carlos del
dc.creator Laggoun-Défarge, Fatima
dc.creator Cuesta, María José
dc.creator Suárez Ruiz, Isabel
dc.date 2007-12-26T13:42:52Z
dc.date 2007-12-26T13:42:52Z
dc.date 2002
dc.date.accessioned 2017-01-31T00:59:32Z
dc.date.available 2017-01-31T00:59:32Z
dc.identifier Journal of Analytical and Applied Pyrolysis 62 (2002) 1-34.
dc.identifier 0165-2370
dc.identifier http://hdl.handle.net/10261/2606
dc.identifier 10.1016/S0165-2370(00)00209-6
dc.identifier.uri http://dspace.mediu.edu.my:8181/xmlui/handle/10261/2606
dc.description This work analyses a set of perhydrous coals (mainly composed of huminite/vitrinite maceral group) in order to determine the inter-relations between the hydrogen content and the modifications in the coal structure at a molecular level. The study involves the direct solid state characterisation of the coal combined with the analysis of representative fragments of the coal network obtained through flash-pyrolysis. The perhydrous character of the coals is not reflected either in the aliphatic hydrogen concentration (from FTIR data) or by the presence of straight-chain aliphatic moieties in the pyrolysates. This structural study shows that perhydrous coals contain mainly aromatic structures with 1–2 rings and a very small concentration of aromatic rings of large size. In agreement with this, phenol and alkyl phenols are the most prominent degradation products whereas other aromatic compounds (mainly benzene and naphthalene derivatives) are minor and probably evaporative compounds. The major structural elements in the samples studied are simple phenols with a preponderance of substituted para alkyl. The results obtained show that the processes of hydrogen enrichment affect the reactions of aromatisation and condensation. During the natural evolution of the perhydrous coals the transformations of the oxygenated functionalities in the lignin precursor seem to have taken place without the parallel structural reorganisation of the lignin framework responsible for the formation of polycyclic aromatic systems. As a result, the chemical structure of perhydrous vitrinites in coals is substantially modified with respect to that described in ‘normal' coals. The results obtained also indicate that the source of hydrogen content and the effect that it has during the subsequent evolution process of the coals, affects the chemical structure of the perhydrous vitrinite and hence its properties and behaviour.
dc.description Financial support for this work was provided through a contract with the European Community (No. 7220/EC-769).
dc.description Peer reviewed
dc.format 550539 bytes
dc.format application/pdf
dc.language eng
dc.publisher Elsevier
dc.relation http://dx.doi.org/10.1016/S0165-2370(00)00209-6
dc.rights openAccess
dc.subject Coal
dc.subject Perhydrous vitrinites
dc.subject Reflectance suppression
dc.subject Chemical structure
dc.subject Coal structure
dc.subject FTIR
dc.subject Py-GC/MS
dc.title Control of the chemical structure of perhydrous coals. FTIR and Py-GC/MS investigations
dc.type Artículo


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