English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/20923
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. I. Secuencia climática: andosoles, suelos pardos

Other TitlesSelective diccolution of Si At and Fe. I. Climatic sequence: andosols and brown and Brown soils
AuthorsCabezas-Viaño, O.; Fernández-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. 1573-1589 (1979)
AbstractSi, Al and Fe dissolution by acid-base technique of Segalen is studied in a climatic sequence of volcanic soils of Tenerife Island (Andosols and Brown Soils). X-ray analysis before and after the treatment reveals that amorphous forms are not differentiated from very soluble crystalline ones (gibbsite, imogolite). Hallosyte shows two types of solubility depending it occurs in the hydrated form or metahalloysite. Fe-dissolution kinetics is quite uniform in all soils of the sequence.
URIhttp://hdl.handle.net/10261/20923
ISSN0365-1797
Appears in Collections:(CAB) Artículos
Files in This Item:
File Description SizeFormat 
ANEA-1979-38-1573.pdf325,71 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.