Phosphate desorption in luvisols and solonetz from a Mediterranean region

Bibliographic Details
Main Author: Monteiro, M.C.H.
Publication Date: 2010
Other Authors: Monteiro, Fernando, Madeira, Manuel
Language: eng
Source: Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
Download full: http://hdl.handle.net/10400.11/539
Summary: Transfer of P from soil to water is controlled by the P retention capacity in the solid phase, namely by the equilibrium between adsorbed and precipitated forms. Desorption of P and/or phosphate dissolution govern the amount of P released into drainage water, runoff or freshwater. Soil P evaluated by Olsen method showed a strong correlation with the capacity of soil to desorb P and, within certain limits, to the transfer of P to water. This transfer of P relates to losses that occur either in surface horizons, or in subsurface horizons (to drainage water, to runoff or by soil erosion to freshwater).
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spelling Phosphate desorption in luvisols and solonetz from a Mediterranean regionPhosphorusDesorptionOlsen methodTransfer of P from soil to water is controlled by the P retention capacity in the solid phase, namely by the equilibrium between adsorbed and precipitated forms. Desorption of P and/or phosphate dissolution govern the amount of P released into drainage water, runoff or freshwater. Soil P evaluated by Olsen method showed a strong correlation with the capacity of soil to desorb P and, within certain limits, to the transfer of P to water. This transfer of P relates to losses that occur either in surface horizons, or in subsurface horizons (to drainage water, to runoff or by soil erosion to freshwater).IPW6Repositório Científico do Instituto Politécnico de Castelo BrancoMonteiro, M.C.H.Monteiro, FernandoMadeira, Manuel2011-02-18T17:42:34Z20102010-01-01T00:00:00Zconference objectinfo:eu-repo/semantics/publishedVersionapplication/pdfhttp://hdl.handle.net/10400.11/539enginfo:eu-repo/semantics/openAccessreponame:Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiainstacron:RCAAP2025-02-26T14:22:40Zoai:repositorio.ipcb.pt:10400.11/539Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireinfo@rcaap.ptopendoar:https://opendoar.ac.uk/repository/71602025-05-28T21:36:52.585100Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) - FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiafalse
dc.title.none.fl_str_mv Phosphate desorption in luvisols and solonetz from a Mediterranean region
title Phosphate desorption in luvisols and solonetz from a Mediterranean region
spellingShingle Phosphate desorption in luvisols and solonetz from a Mediterranean region
Monteiro, M.C.H.
Phosphorus
Desorption
Olsen method
title_short Phosphate desorption in luvisols and solonetz from a Mediterranean region
title_full Phosphate desorption in luvisols and solonetz from a Mediterranean region
title_fullStr Phosphate desorption in luvisols and solonetz from a Mediterranean region
title_full_unstemmed Phosphate desorption in luvisols and solonetz from a Mediterranean region
title_sort Phosphate desorption in luvisols and solonetz from a Mediterranean region
author Monteiro, M.C.H.
author_facet Monteiro, M.C.H.
Monteiro, Fernando
Madeira, Manuel
author_role author
author2 Monteiro, Fernando
Madeira, Manuel
author2_role author
author
dc.contributor.none.fl_str_mv Repositório Científico do Instituto Politécnico de Castelo Branco
dc.contributor.author.fl_str_mv Monteiro, M.C.H.
Monteiro, Fernando
Madeira, Manuel
dc.subject.por.fl_str_mv Phosphorus
Desorption
Olsen method
topic Phosphorus
Desorption
Olsen method
description Transfer of P from soil to water is controlled by the P retention capacity in the solid phase, namely by the equilibrium between adsorbed and precipitated forms. Desorption of P and/or phosphate dissolution govern the amount of P released into drainage water, runoff or freshwater. Soil P evaluated by Olsen method showed a strong correlation with the capacity of soil to desorb P and, within certain limits, to the transfer of P to water. This transfer of P relates to losses that occur either in surface horizons, or in subsurface horizons (to drainage water, to runoff or by soil erosion to freshwater).
publishDate 2010
dc.date.none.fl_str_mv 2010
2010-01-01T00:00:00Z
2011-02-18T17:42:34Z
dc.type.driver.fl_str_mv conference object
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dc.identifier.uri.fl_str_mv http://hdl.handle.net/10400.11/539
url http://hdl.handle.net/10400.11/539
dc.language.iso.fl_str_mv eng
language eng
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