Geomorphic dynamics of gullied developed in Sandy slopes of Central Spain

Gullies developed on sandy lithologies are scarce. Such landforms have developed in the sandy deposits of the Cretaceous ‘Utrillas’ facies within the Segovia province of Central Spain. They appear at the slopes of a group of mesas and cuestas located at the edge of the northern piedmont of the Guada...

Descripción completa

Detalles Bibliográficos
Autores: Lucía Vela, Ana, Martín Duque, J. F., Laronne, J. B., Sanz, M. A.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2011
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/128877
Acceso en línea:http://hdl.handle.net/10261/128877
Access Level:acceso abierto
Palabra clave:Sand
Gullies
Terrestrial Laser Scanner (TLS)
Reid bedload sampler
Erosion-runoff plots
Spain
id ES_5dbcb0ca5207035cade7c2aa28efeb4e
oai_identifier_str oai:digital.csic.es:10261/128877
network_acronym_str ES
network_name_str España
repository_id_str
spelling Geomorphic dynamics of gullied developed in Sandy slopes of Central SpainLucía Vela, AnaMartín Duque, J. F.Laronne, J. B.Sanz, M. A.SandGulliesTerrestrial Laser Scanner (TLS)Reid bedload samplerErosion-runoff plotsSpainGullies developed on sandy lithologies are scarce. Such landforms have developed in the sandy deposits of the Cretaceous ‘Utrillas’ facies within the Segovia province of Central Spain. They appear at the slopes of a group of mesas and cuestas located at the edge of the northern piedmont of the Guadarrama Mountains of the Spanish Central System. The activity of the different geomorphic processes acting in these gullies, as well as their connectivity, are being characterized and quantified. This study was preceded by reconnaissance methods, whereas presently technologically advanced and more accurate techniques are being utilized. The new methods are applied in an experimental catchment (1.26 ha). They include: i) an automatic Reid-type (formerly termed Birkbeck) slot bedload sampler for continuous monitoring of bedload flux and for continuous sampling of bedload; siphons for sampling the suspended load; and a Parshall flume to monitor water discharge. Jointly, these instruments allow to study the fluvial dynamics at the catchment mouth; ii) topographic surveys undertaken by a Terrestrial Laser Scanner (TLS) to quantify the activity of gravitational, overland flow and fluvial processes in different sediment source areas within the gully basin; iii) micro runoff and erosion plots to monitor the infiltration and erosive response of different Hydrologic Response Units (HRU) comprising the interior of the catchment. This ensemble of novel methods has started providing patterns of sediment movement within the gully system.Peer reviewedUniversity of SilesiaConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]201620162011info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Publisher's versioninfo:eu-repo/semantics/publishedVersionhttp://hdl.handle.net/10261/128877reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)InglésSíinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/1288772026-05-22T06:33:51Z
dc.title.none.fl_str_mv Geomorphic dynamics of gullied developed in Sandy slopes of Central Spain
title Geomorphic dynamics of gullied developed in Sandy slopes of Central Spain
spellingShingle Geomorphic dynamics of gullied developed in Sandy slopes of Central Spain
Lucía Vela, Ana
Sand
Gullies
Terrestrial Laser Scanner (TLS)
Reid bedload sampler
Erosion-runoff plots
Spain
title_short Geomorphic dynamics of gullied developed in Sandy slopes of Central Spain
title_full Geomorphic dynamics of gullied developed in Sandy slopes of Central Spain
title_fullStr Geomorphic dynamics of gullied developed in Sandy slopes of Central Spain
title_full_unstemmed Geomorphic dynamics of gullied developed in Sandy slopes of Central Spain
title_sort Geomorphic dynamics of gullied developed in Sandy slopes of Central Spain
dc.creator.none.fl_str_mv Lucía Vela, Ana
Martín Duque, J. F.
Laronne, J. B.
Sanz, M. A.
author Lucía Vela, Ana
author_facet Lucía Vela, Ana
Martín Duque, J. F.
Laronne, J. B.
Sanz, M. A.
author_role author
author2 Martín Duque, J. F.
Laronne, J. B.
Sanz, M. A.
author2_role author
author
author
dc.contributor.none.fl_str_mv Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]
dc.subject.none.fl_str_mv Sand
Gullies
Terrestrial Laser Scanner (TLS)
Reid bedload sampler
Erosion-runoff plots
Spain
topic Sand
Gullies
Terrestrial Laser Scanner (TLS)
Reid bedload sampler
Erosion-runoff plots
Spain
description Gullies developed on sandy lithologies are scarce. Such landforms have developed in the sandy deposits of the Cretaceous ‘Utrillas’ facies within the Segovia province of Central Spain. They appear at the slopes of a group of mesas and cuestas located at the edge of the northern piedmont of the Guadarrama Mountains of the Spanish Central System. The activity of the different geomorphic processes acting in these gullies, as well as their connectivity, are being characterized and quantified. This study was preceded by reconnaissance methods, whereas presently technologically advanced and more accurate techniques are being utilized. The new methods are applied in an experimental catchment (1.26 ha). They include: i) an automatic Reid-type (formerly termed Birkbeck) slot bedload sampler for continuous monitoring of bedload flux and for continuous sampling of bedload; siphons for sampling the suspended load; and a Parshall flume to monitor water discharge. Jointly, these instruments allow to study the fluvial dynamics at the catchment mouth; ii) topographic surveys undertaken by a Terrestrial Laser Scanner (TLS) to quantify the activity of gravitational, overland flow and fluvial processes in different sediment source areas within the gully basin; iii) micro runoff and erosion plots to monitor the infiltration and erosive response of different Hydrologic Response Units (HRU) comprising the interior of the catchment. This ensemble of novel methods has started providing patterns of sediment movement within the gully system.
publishDate 2011
dc.date.none.fl_str_mv 2011
2016
2016
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
Publisher's version
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/128877
url http://hdl.handle.net/10261/128877
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv University of Silesia
publisher.none.fl_str_mv University of Silesia
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
instname:Consejo Superior de Investigaciones Científicas (CSIC)
instname_str Consejo Superior de Investigaciones Científicas (CSIC)
reponame_str DIGITAL.CSIC. Repositorio Institucional del CSIC
collection DIGITAL.CSIC. Repositorio Institucional del CSIC
repository.name.fl_str_mv
repository.mail.fl_str_mv
_version_ 1869409050222919680
score 15,81155