dc.contributor.author
Batalla, Ramon J.
dc.contributor.author
Sala, Maria (Sala i Sanjaume)
dc.date.issued
2012-11-14T12:23:58Z
dc.date.issued
2012-11-14T12:23:58Z
dc.date.issued
2012-11-14T12:23:58Z
dc.identifier
https://hdl.handle.net/2445/32691
dc.description.abstract
A study of hydrochemical characteristics of the Arbúcies river (a seminatural mediterranean basin) has been undertaken during 1991. Mean solute yield for each ion has been determined using the correlation curves between discharge and concentration, and the flow duration curve. The hydrochemical budget of the Arbúcies drainage basin shows that the basin is a net source for al1 the elements. The cationic denudation rate obtained in this granitic basin is 5.24 keqhalyear. This high rate is due to the intensive chemical weathering of the granodionte, that delivers an important amount of cations which will release to be transported. The results demostrate clearly the strength of lithological control on stream loads, particulary on the dissolved component.
dc.format
application/pdf
dc.format
application/pdf
dc.publisher
Universitat de Barcelona (UB). Institut de Cièncias de la Terra Jaume Almera (ICTJA)
dc.relation
Reproducció del document publicat a: http://www.raco.cat/index.php/ActaGeologica/article/view/75436
dc.relation
Acta Geologica Hispanica, 1993, vol. 28, num. 1, p. 51-62
dc.rights
(c) Batalla, Ramon J. et al., 1993
dc.rights
info:eu-repo/semantics/openAccess
dc.source
Articles publicats en revistes (Geografia)
dc.subject
Meteorització química
dc.subject
Conques hidrogràfiques
dc.subject
Mediterrània (Regió)
dc.subject
Chemical weathering
dc.subject
Mediterranean Region
dc.title
Balanç hidroquímic d'una conca mediterrània en estat seminatural: el cas de la riera d'Arbúcies
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/publishedVersion
