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Influence of aeolian deposits on the pedogenesis process of the Costa da Morte soils (NW Spain)

dc.contributor.authorArán, Diego
dc.contributor.authorMacías, Felipe
dc.date.accessioned2024-07-19T10:48:11Z
dc.date.available2024-07-19T10:48:11Z
dc.date.issued2023-11
dc.description.abstractAeolian deposition in coastal system can modify pedogenic processes or provide parent material for new pedogenesis cycles. In Galicia region (NW Spain), as in other regions of the world, the pedogenic processes associated with aeolian deposits under coastal conditions are little know. These processes are also conditioned by the development time from the formation of the sedimentary deposits, which in the case of the Galician coast is highly variable. The main objective was to identify the effect of aeolian deposits on coastal soils, through the characterization and classification of several soil profiles, and the identification of the main pedogenic process that contributed to their formation or modification. The studied soils presented one and two pedogenic cycles as well as in each one different level of pedogenic evolution. The soils with one pedogenic cycle were Endoleptic Umbrisol (Loamic, Hyperdystric, Hyperhumic, Pachic) from Xuxurantes and Haplic Umbrisol (Arenic, Humic, Pachic) from Cabo Vilano. The soils with two cycles were found in Muxia (Aeolic Calcaric Arenosol (Ochric- Novic) over Haplic Phaeozems (Endoloamic)) and Cementerio de los Ingleses (Albic Umbric Podzol (Pantoar- enic)). This last type of soil constituted one more step in the evolution of aeolian deposits (first cycle of pedo- genesis in the Muxia profile). Thus, changes in the pedogenesis processes and mechanisms were conditioned by the presence of a superficial aeolian deposition as well as the proximity to the coast and determine a chro- nosequence of the processes in the aeolian sediments.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationArán, D., Macías, F. “Influence of aeolian deposits on the pedogenesis process of the Costa da Morte soils (NW Spain)”. Catena, vol. 232, Nov. 2023, p.107465pt_PT
dc.identifier.doi10.1016/j.catena.2023.107465pt_PT
dc.identifier.urihttp://hdl.handle.net/10400.5/31330
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherElsevierpt_PT
dc.relation.publisherversionwww.elsevier.com/locate/catenapt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectAeolian materialspt_PT
dc.subjectCarbonatizationpt_PT
dc.subjectPodzolizationpt_PT
dc.subjectPedogenesispt_PT
dc.subjectOrganic matterpt_PT
dc.subjectUmbrisolspt_PT
dc.titleInfluence of aeolian deposits on the pedogenesis process of the Costa da Morte soils (NW Spain)pt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.startPage107465pt_PT
oaire.citation.titleCatenapt_PT
oaire.citation.volume232pt_PT
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT

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