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Linear erosion in mountain scrublands of North and Centre Portugal: the case studies of Seirós and Corgo gullies

dc.contributor.authorMartins, Bruno
dc.contributor.authorLourenço, Luciano
dc.contributor.authorFonseca, Felícia
dc.contributor.authorFigueiredo, Tomás de
dc.contributor.authorFerreira, Carmen
dc.date.accessioned2018-02-22T10:25:25Z
dc.date.available2018-02-22T10:25:25Z
dc.date.issued2016
dc.description.abstractGully occurrence is particularly common in the mountain areas of North and Central Portugal, dominantly covered by forests and scrublands. In many of these regions, linear erosion is a very important process, contributing to significant soil loss and land degradation. In rural areas, land degradation may be responsible for limiting the options for territory occupation and development, reducing farmland quality and suitable area. Driven by climatic conditions as long and intense rainfalls, gully formation is related to topographical factors such as hill‐slope gradient, length and shape, to physical, chemical and mineralogical properties of the soils. The variety of physical factors associated with gully formation hinders straightforward interpretations and requires well grounded analysis based on local observation. Also, anthropogenic factors significantly contribute to gully formation and development and for the associated soil loss rates. Deforestation, forest fires, overgrazing, vegetation removal, as well as road building, are the most important ones. In most cases, they reduce infiltration and promote runoff water concentration. Two case studies are presented in this paper, aiming at discussing interpretations on gully formation factors and their contribution to soil loss. Both correspond to scrubland over colluvial hillslope deposits, located in Seirós (Ribeira de Pena, Northern Portugal) and Corgo (Oliveira do Hospital, Central Portugal). Field surveys were performed to assess gully volume and the corresponding soil loss by linear erosion, consisting in measurements of cross‐sectional area at regular intervals along the gully, and their integration up to gully cross‐sections with less than 900 cm2 area. Samples were taken on gully walls for bulk density (100 cm3 cylinders). Field surveys also allow the collection of samples for granulometric analysis in the tentative to assert relationship to the gullies geometry and understanding the most significant driven factors in gullies formation.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationMartins, Bruno; Lourenço, Luciano; Fonseca, Felícia; Figueiredo, Tomás de; Ferreira, Cármen (2016). Linear erosion in mountain scrublands of North and Centre Portugal: the case studies of Seirós and Corgo gullies. In Mountains 2016: I Conferência Internacional sobre Investigação e Desenvolvimento Sustentável em Regiões de Montanha. Bragança: Instituto Politécnico. ISBN 978‐972‐745‐214‐9pt_PT
dc.identifier.isbn978‐972‐745‐214‐9
dc.identifier.urihttp://hdl.handle.net/10198/15914
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherInstituto Politécnico de Braganapt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.titleLinear erosion in mountain scrublands of North and Centre Portugal: the case studies of Seirós and Corgo gulliespt_PT
dc.typeconference object
dspace.entity.typePublication
oaire.citation.conferencePlaceInstituto Politécnico de Bragança, Portugal.pt_PT
oaire.citation.titleI Conferência Internacional sobre Investigação e Desenvolvimento Sustentável em Regiões de Montanhapt_PT
person.familyNameFonseca
person.familyNameFigueiredo
person.givenNameFelícia
person.givenNameTomás d'Aquino
person.identifier1297327
person.identifier.ciencia-id961D-607D-51CC
person.identifier.orcid0000-0001-7727-071X
person.identifier.orcid0000-0001-7690-8996
person.identifier.scopus-author-id36970960500
person.identifier.scopus-author-id54790554500
rcaap.rightsopenAccesspt_PT
rcaap.typeconferenceObjectpt_PT
relation.isAuthorOfPublication4f6f8be1-73c1-45bb-b159-ce3f8ff96c84
relation.isAuthorOfPublicationdb897e48-ecf7-4ce1-ba27-369260337510
relation.isAuthorOfPublication.latestForDiscovery4f6f8be1-73c1-45bb-b159-ce3f8ff96c84

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