English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/90243
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE
Exportar a otros formatos:

DC FieldValueLanguage
dc.contributor.authorNord, Guillaume-
dc.contributor.authorGallart Gallego, Francesc-
dc.contributor.authorGratiot, N.-
dc.contributor.authorSoler Roig, M.-
dc.contributor.authorReid, Ian-
dc.contributor.authorVachtman, Dina-
dc.contributor.authorLatron, Jérôme-
dc.contributor.authorMartín-Vide, J. P.-
dc.contributor.authorLaronne, J. B.-
dc.date.accessioned2014-01-31T10:43:56Z-
dc.date.available2014-01-31T10:43:56Z-
dc.date.issued2014-
dc.identifier.citationJournal of Hydrology 509 : 504-518 (2014)es_ES
dc.identifier.issn0022-1694-
dc.identifier.urihttp://hdl.handle.net/10261/90243-
dc.description15 páginas, 8 figuras, 4 tablas, 1 apéndice con 2 tablas.es_ES
dc.description.abstractAcoustic Doppler devices (Unidata Starflow) have been deployed for velocity measurements and discharge estimates in five contrasted open-channel flow environments, with particular attention given to the influence of sediment transport on instrument performance. The analysis is based on both field observations and flume experiments. These confirm the ability of the Starflow to provide reliable discharge time-series, but point out its limitations when sediment is being transported. (i) After calibration of the instrument by the Index Velocity Method, the deviation from reference discharge measurements was < 20% at the 95% confidence level. (ii) In ungauged conditions at high flows, the Starflow was particularly useful in providing velocity data for approximating measurements of discharge. (iii) However, channel and flume experiments revealed the effects of mobilised sediment on velocity estimates: coarse particles (P 150 lm) transported by way of saltation or as bedload caused a significant underestimation of velocity by as much as 50%; a slight underestimation (10–15%) was also observed when significant quantities of fine particles (6150 lm) were transported in suspension; this underestimation was shown to reach 20–30% when suspended sediment concentrations were very high (c. 50–100 g L 1).es_ES
dc.description.sponsorshipThis research was supported by the PROBASE (CGL2006-11619/ HID) and RespHiMed (CGL2010-18374) projects funded by the Spanish Ministry of Science and Innovation and by the agreement (RESEL) between the CSIC and the Spanish Ministry of Environment.es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsopenAccesses_ES
dc.subjectSuspended sediment concentrationes_ES
dc.subjectBedloades_ES
dc.subjectAcoustic Doppleres_ES
dc.subjectSediment transportes_ES
dc.subjectDischargees_ES
dc.subjectVelocityes_ES
dc.titleApplicability of acoustic Doppler devices for flow velocity measurements and discharge estimation in flows with sediment transportes_ES
dc.typeartículoes_ES
dc.identifier.doi10.1016/j.jhydrol.2013.11.020-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1016/j.jhydrol.2013.11.020es_ES
Appears in Collections:(CEAB) Artículos
Files in This Item:
There are no files associated with this item.
Show simple item record
 

Related articles:


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.