English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/20882
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:
Title

Disolución diferencial de Si, Al Y Fe. II. Secuencia climática: S. ferralíticos, S. fersialíticos y vertisoles

Other TitlesSelective dissolution of Si Al and Fe. II. Climatic sequence: vertisol., ferrallitic and fersiallitic soils
AuthorsFernández-Caldas, E.; Tejedor-Salguero, M. L.; Hernández-Moreno, J. M.
Issue Date1979
PublisherCSIC - Instituto Nacional de Edafología y Agrobiología José María Albareda
CitationAnales de Edafología y Agrobiología 38(9-10): pp. 1591-1606 (1979)
AbstractSi, Al and Fe dissolution by acid-base technique of Segralen is studied in a climatic sequence of volcanic soils of thje Island of Tenerife (Vertisol, Ferrellitic and fersiallitic Soils). The results are correlated with the effect of the treatment in different crystalline compounds by means of X-ray analysis before and after the treatment. In some cases the dissolution of certain minerals (hallosyte and smectite) can be characterised. Fe dissolution kinetics can differentiate "free" forms from Fe as constituent in the clay minerals.
URIhttp://hdl.handle.net/10261/20882
ISSN0365-1797
Appears in Collections:(CAB) Artículos
Files in This Item:
File Description SizeFormat 
ANEA-1979-38-1591.pdf350,49 kBAdobe PDFThumbnail
View/Open
Show full item record
Review this work
 


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