Por favor, use este identificador para citar o enlazar a este item:
http://hdl.handle.net/10261/54777
COMPARTIR / EXPORTAR:
SHARE BASE | |
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE | |
Título: | Interlamellar adsorption of a blackearth humic acid on Na-montmorillonite |
Autor: | Martín Martínez, Francisco; Pérez Rodríguez, José Luis | Fecha de publicación: | 1969 | Citación: | Zeitschrift für Pflanzenernährung und Bodenkunde 124 (1): 52-57 (1969) | Resumen: | Interaction between clay and organic compounds has been extensively studied and a considerable amount of literature is available. So, for example, reaction with glycerol (1), ethyleneglycol (7) and dimethylsulfoxide (3) are very well known. But there are not many papers dealing with the reaction between clay and organic matter of soil. Recently, Greenland (4) has made an interesting rewiew of this event. Reactions between clay minerals and fulvic acid have been reproduced in a number of publications, but there are very little papers about interaction between clay minerals and humic acid, probably due to the difficulty to get humic acid in solution. Schnitzer and Kodama (10) have been made an intensive study on the reaction between a Podzol fulvic acid and Na-Montmorillonite, and they have found that the fulvic acid was adsorbed in the interlamellar spaces of the clay. They found also, that the adsorption was dependent on pH, clay mineral/fulvic acid ratio and time of contact. | Descripción: | 6 pages, 4 figures, 2 tables, 11 references. | URI: | http://hdl.handle.net/10261/54777 |
Aparece en las colecciones: | (IRNAS) Artículos |
Ficheros en este ítem:
Fichero | Descripción | Tamaño | Formato | |
---|---|---|---|---|
Interlamellar adsorption of a blackearth humic.pdf | 207,58 kB | Adobe PDF | Visualizar/Abrir |
CORE Recommender
Page view(s)
293
checked on 19-abr-2024
Download(s)
207
checked on 19-abr-2024
Google ScholarTM
Check
NOTA: Los ítems de Digital.CSIC están protegidos por copyright, con todos los derechos reservados, a menos que se indique lo contrario.