Por favor, use este identificador para citar o enlazar a este item:
http://hdl.handle.net/10261/35212
COMPARTIR / EXPORTAR:
SHARE CORE BASE | |
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE | |
Campo DC | Valor | Lengua/Idioma |
---|---|---|
dc.contributor.author | Molina Ballesteros, Eloy | - |
dc.contributor.author | García Talegón, Jacinta | - |
dc.contributor.author | Iñigo, Adolfo C. | - |
dc.contributor.author | Sánchez, M. G. | - |
dc.contributor.author | Herrero Fernández, Hernando | - |
dc.date.issued | 2011 | - |
dc.identifier.citation | Environmental Earth Science. (2011) Online First™ | es_ES |
dc.identifier.issn | 1866-6280 | - |
dc.identifier.uri | 10261/35212 | - |
dc.description | 14 p. | es_ES |
dc.description.abstract | Some physical properties (bulk and free porosity, pore size distribution), and the chemical composition and mass balance of two deeply weathered profiles one developed on Hercynian granodiorite and the other on pre-Cambrian slates were studied. Hydric and mercury porosimetry, nitrogen adsorption techniques, chemical analyses and XRD techniques were used. On granodiorite, weathering has created increased porosity with a pore diameter \5 lm, whereas on slates the weathering has produced of ca. 1 lm in diameter. These pore sizes have played an important role in the weathering processes. Assuming that weathering preserves volumes, except in the uppermost part of the profiles, it brought about a loss of matter of more than 12% (*300 kg/m3) on granodiorite and ca. 30% (*800 kg/m3) on slates. These changes are related to shifts in the mineralogical evolution, with the appearance of new 2:1 and 1:1 phyllosilicates and Fe oxyhydroxides as the main authigenic minerals. The release of matter, at least since the upper Neogene until the present, has led to the lowering of relief in a more or less homogeneous way, giving rise to gentle hillsides and flat surfaces below which the current river networks are incised. Porosity studies have the potential to explain several specific landforms as well as affecting landscape development in general. | es_ES |
dc.description.sponsorship | The authors acknowledged the interesting suggestions of Prof. C. R. TWIDALE. We also thank the Ministerio de Educacio´n y Ciencia of Spain and the Junta de Castilla y Leo´n for financial support under Projects CGL2007-62168/BTE (funds FEDER) and Project SA024A07, respectively. | es_ES |
dc.description.uri | 10261/35212 | - |
dc.language.iso | eng | es_ES |
dc.publisher | Springer Nature | es_ES |
dc.rights | openAccess | es_ES |
dc.subject | Weathering | es_ES |
dc.subject | Porosity | es_ES |
dc.subject | Mass balance | es_ES |
dc.subject | Granodiorite | es_ES |
dc.subject | Slates | es_ES |
dc.subject | Piedmont surfaces | es_ES |
dc.title | Importance of porosity and transfer of matter in the rock weathering processes: two examples in Central Spain. | es_ES |
dc.type | artículo | es_ES |
dc.identifier.doi | 10.1007/s12665-011-1015 | - |
dc.description.peerreviewed | Peer reviewed | es_ES |
dc.relation.publisherversion | http://www.springerlink.com/content/wr145h43q2981u57/ | es_ES |
local.message.claim | 2023-11-27T12:17:52.564+0100|||rp15164|||submit_approve|||dc_contributor_author|||None | * |
dc.type.coar | http://purl.org/coar/resource_type/c_6501 | es_ES |
item.openairetype | artículo | - |
item.grantfulltext | open | - |
item.cerifentitytype | Publications | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
item.languageiso639-1 | en | - |
Aparece en las colecciones: | (IRNASA) Artículos |
Ficheros en este ítem:
Fichero | Descripción | Tamaño | Formato | |
---|---|---|---|---|
Environ Earth Sciadol2011.pdf | 1,58 MB | Adobe PDF | Visualizar/Abrir |
CORE Recommender
Page view(s)
255
checked on 18-abr-2024
Download(s)
193
checked on 18-abr-2024
Google ScholarTM
Check
Altmetric
Altmetric
NOTA: Los ítems de Digital.CSIC están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.