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Soil carbon stabilization pathways as reflected by the pyrolytic signature of humic acid in agricultural volcanic soils

dc.contributor.authorHernández, Zulimar
dc.contributor.authorAlmendros, Gonzalo
dc.contributor.authorÁlvarez, Ana María Tito
dc.contributor.authorFigueiredo, Tomás de
dc.contributor.authorCarral, Pilar
dc.date.accessioned2018-02-19T10:00:00Z
dc.date.accessioned2019-01-28T11:58:04Z
dc.date.available2018-01-19T10:00:00Z
dc.date.available2019-01-28T11:58:04Z
dc.date.issued2019
dc.description.abstractMolecular assessment of the origin and transformation processes of soil organic matter (SOM) was carried out based on information obtained from 13C NMR and analytical pyrolysis of humic acids (HAs) in soils from wine-growing regions in Tenerife (Canary Islands, Spain). Principal component analysis, using as variables pyrolysis products, shows different soil groups defined by the molecular assemblages released from the corresponding HAs, characterized by the predominance of: i) plant biomacromolecules (lignin) in soils on pumice substrate, ii) heterocyclic N-compounds and methoxyl-lacking aromatic structures, iii) a substantial domain of alkyl compounds in cultivated soils with active C turnover and finally, iv) polysaccharide and protein-derived compounds in soils developed on amorphous gels. The proportions of the pyrolytic compounds from soil HAs were represented by an upgraded graphical-statistical method (3D Van Krevelen plot) that was used to compare the major SOM structural domains in the different soils. The above results coincide with those suggested by the 13C NMR analysis, and were associated to two groups of local land management practices, in terms of their intensity respectively favoring either the transformation of plant-inherited macromolecular precursors from vascular plants, or the humification of aliphatic precursors in the presence of specific mineralogical substrates controlling microbial degradation and humification processes.
dc.description.sponsorshipThis research has been funded by the Spanish CICyT under grant CGL2013-43845-P . The authors wish to thank to three anonymous referees by their constructive comments that contributed to improving the final version of the paper.
dc.description.versioninfo:eu-repo/semantics/publishedVersionen_EN
dc.identifier.citationHernández, Z.; Almendros, G.; Álvarez, A.; Figueiredo, Tomás de; Carral, P. (2019). Soil carbon stabilization pathways as reflected by the pyrolytic signature of humic acid in agricultural volcanic soils. Journal of Analytical and Applied Pyrolysis. ISSN 0165-2370. 137, p. 14-28en_EN
dc.identifier.doi10.1016/j.jaap.2018.10.015en_EN
dc.identifier.issn0165-2370
dc.identifier.urihttp://hdl.handle.net/10198/12126
dc.language.isoeng
dc.peerreviewedyesen_EN
dc.subject13 C NMRen_EN
dc.subjectAllophaneen_EN
dc.subjectGC/MSen_EN
dc.subjectMethoxyphenolen_EN
dc.subjectSoil organic matteren_EN
dc.subjectVan Krevelen diagramen_EN
dc.titleSoil carbon stabilization pathways as reflected by the pyrolytic signature of humic acid in agricultural volcanic soilsen_EN
dc.typejournal article
dspace.entity.typePublication
person.familyNameFigueiredo
person.givenNameTomás d'Aquino
person.identifier1297327
person.identifier.ciencia-id961D-607D-51CC
person.identifier.orcid0000-0001-7690-8996
person.identifier.scopus-author-id54790554500
rcaap.rightsopenAccessen_EN
rcaap.typearticleen_EN
relation.isAuthorOfPublicationdb897e48-ecf7-4ce1-ba27-369260337510
relation.isAuthorOfPublication.latestForDiscoverydb897e48-ecf7-4ce1-ba27-369260337510

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