Sheet erosion rates determined by using dendrogeomorphological analysis of exposed tree roots: Two examples from Central Spain

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dc.contributor.authorBodoque del Pozo, José María
dc.contributor.authorDíez Herrero, Andrés
dc.contributor.authorMartín Duque, José Francisco
dc.contributor.authorRubiales Jiménez, Juan Manuel
dc.contributor.authorGodfrey, Andrew E.
dc.contributor.authorDe Pedraza Gilsanz, Javier
dc.contributor.authorCarrasco González, Rosa María
dc.contributor.authorSanz Santos, Miguel Ángel
dc.date.accessioned2023-06-20T10:33:05Z
dc.date.available2023-06-20T10:33:05Z
dc.date.issued2005
dc.description.abstractThis paper describes the determination of sheet erosion rates by using dendrogeomorphological methods on exposed tree roots. Two sites on the northern slope of the Guadarrama Mountains, Central Spain, were studied: a popular trail in a Scots pine forest (Senda Schmidt, Valsaı´n) growing on granites and gneisses, and an open holm-oak forest on granitic slopes (Monterrubio). These sites were selected because they showed high denudation morphologies due to accelerated soil-erosion processes caused by human influence (trampling by continuous trekking and overgrazing), resulting in exposed roots. The method applied is based on the morphological pattern of roots, defined by the growth-ring series of the sampled roots. In order to confirm the validity of the criteria used and to make the estimations of erosion more accurate, several anatomical indicators of exposed and nonexposed Pinus sylvestris roots were characterized. The study entailed a statistical analysis of exposure time and erosion depth. The influence of environmental factors affecting the variation in velocity of the erosion processes was also examined. With a significance level of 95%, the mean erosion rates were in the range of 1.7–2.6 mm/year (29– 44 t/ha/year) on Senda Schmidt over the last 101 years, and 1.1–1.8 mm/year (19–31 t/ha/year) in Monterrubio over the last 42 years. Using a multifactor analysis of variance, we observed a change in the erosion rates as a function of position on the path along Senda Schmidt. In Monterrubio, however, we reached no significant conclusions, apart from an inverse relationship between erosion and slope gradient that was difficult to interpret. Climate conditions in Senda Schmidt and the accuracy of dating Scots pine indicate that the evaluation on P. sylvestris roots is fairly reliable, which is not the case for oak roots. Although this paper is based on the application of an existing method, its novelty lies in being the first attempt in Spain to estimate dacceleratedT sheet erosion rates (due to recreational activities and overgrazing) using dendrogeomorphological techniques, supplemented by anatomical indicators for P. sylvestris.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/20010
dc.identifier.doi10.1016/j.catena.2005.08.002
dc.identifier.issn0341-8162
dc.identifier.officialurlhttp://www.elsevier.com/wps/product/cws_home/524609/description
dc.identifier.urihttps://hdl.handle.net/20.500.14352/50455
dc.journal.titleCatena
dc.language.isoeng
dc.page.final102
dc.page.initial81
dc.publisherElsevier B.V.
dc.rights.accessRightsopen access
dc.subject.cdu551.4(234.1)
dc.subject.keywordTree ring
dc.subject.keywordTree root
dc.subject.keywordRill–interrill erosion
dc.subject.keywordDendrogeomorphology
dc.subject.keywordSierra de Guadarrama (Spain)
dc.subject.ucmGeodinámica
dc.subject.unesco2507 Geofísica
dc.titleSheet erosion rates determined by using dendrogeomorphological analysis of exposed tree roots: Two examples from Central Spain
dc.typejournal article
dc.volume.number64
dspace.entity.typePublication
relation.isAuthorOfPublication5f95937a-47b9-498e-a16c-44228acedd90
relation.isAuthorOfPublicationde984963-bc89-4562-a817-1e580b822107
relation.isAuthorOfPublicatione4817063-6685-4916-a5b0-91f54417a207
relation.isAuthorOfPublication.latestForDiscovery5f95937a-47b9-498e-a16c-44228acedd90
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