English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/118152
Share/Impact:
Statistics
logo share SHARE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:
DC FieldValueLanguage
dc.contributor.authorFernandez-Cortes, Ángel-
dc.contributor.authorCuezva, Soledad-
dc.contributor.authorGarcía Antón, Elena-
dc.contributor.authorÁlvarez-Gallego, Miriam-
dc.contributor.authorBenavente, David-
dc.contributor.authorCalaforra, José María-
dc.contributor.authorSánchez Moral, Sergio-
dc.date.issued2015-
dc.identifier.citationHydrogeological and environmental investigations in karst systems: 523-531 (2015)es_ES
dc.identifier.isbn978-3-642-17434-6-
dc.identifier.isbn978-3-642-17435-3-
dc.identifier.urihttp://hdl.handle.net/10261/118152-
dc.description.abstractA comprehensive environmental monitoring programme has been recently launched in Ojo Guareña cave system (Burgos, Spain), one of the longest caves in Europe, aimed to assess the magnitude of the spatiotemporal changes of CO2 (g), on daily and synoptic timescales in the cave–soil–atmosphere profile. CO2 concentration of cave air is usually close to atmospheric background but huge daily oscillations of CO2 levels, ranging 680–1,900 ppm/day on average, have registered during periods when exterior air temperature oscillates every day around cave air temperature. These daily variations of CO2 content are hidden once the air temperature outside is continuously below cave temperature and a prevailing advective-renewal of cave air is established, so that daily-averaged concentrations of CO2 reach minimum values close to 500 ppm. The spatiotemporal pattern of CO2(g) provides evidence that the amounts of carbon that might be sequestered and then emitted (CO2) from subsurface air located in the uppermost part of the vadose zone could be noticeable at local or regional scale by considering long subterranean systems as Ojo Guareña karst.es_ES
dc.language.isoenges_ES
dc.publisherSpringeres_ES
dc.relation.ispartofseriesEnvironmental Earth Sciences-
dc.rightsclosedAccesses_ES
dc.titleClimate-driven changes on storage and sink of carbon dioxide in subsurface atmosphere of karst terrainses_ES
dc.typecapítulo de libroes_ES
dc.identifier.doi10.1007/978-3-642-17435-3_59-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1007/978-3-642-17435-3_59es_ES
dc.relation.csices_ES
Appears in Collections:(MNCN) Libros y partes de libros
Files in This Item:
File Description SizeFormat 
accesoRestringido.pdf15,38 kBAdobe PDFThumbnail
View/Open
Show simple item record
 


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