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...
| Autores: | , , , |
|---|---|
| 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 |
Sí |
| 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 |