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dc.contributor.authorGutiérrez-Jerez, F.-
dc.contributor.authorPérez-Méndez, J. A.-
dc.contributor.authorFernández-Caldas, E.-
dc.contributor.authorBorges-Pérez, Andrés-
dc.date.accessioned2010-02-10T10:56:05Z-
dc.date.available2010-02-10T10:56:05Z-
dc.date.issued1979-
dc.identifier.citationAnales de Edafología y Agrobiología 38(9-10): pp. 1479-1494 (1979)en_US
dc.identifier.issn0365-1797-
dc.identifier.urihttp://hdl.handle.net/10261/20898-
dc.description.abstractThe relationship of the several fractions of the inorganic phosphates, extracted by the Chang-Jackson method, with the weathering degree of the Canary Islands andosols show the following trend: 1. The fractions P-Ca and P-Al decrease as the weathering degree increase, giving the aluminium phosphate a maximum in the Evolued Vitrandepts. 2. The fraction P-Fe has not very much variation in the sequence, excluding the profil Manantiales, which has a very high values comparably to the other profiles. 3. The P-occluded tends to increase with the weathering degree. Chang-Jackson's hypothesis goes quite well to these soils, beacuse the differents forms of soil inorganic phosphates are related with the weathering degree according to the following tendence: P-Ca, P-Al, P-Fe, P-occluded.en_US
dc.format.extent427401 bytes-
dc.format.mimetypeapplication/pdf-
dc.language.isospaen_US
dc.publisherCSIC - Instituto Nacional de Edafología y Agrobiología José María Albaredaen_US
dc.rightsopenAccessen_US
dc.titleEstudio de los fosfatos inorgánicos en relación con el grado de evolución en andosolesen_US
dc.title.alternativeStudy of the relationship between the inorganic phospates and the weathering degree of the Canary Islands andosoilsen_US
dc.typeartículoen_US
dc.description.peerreviewedPeer revieweden_US
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