Changes in soil phosphorus in different forest residue management

We analyze the short term effect of the harvest residues management on the Phosphorus (P) fractions of the soil. Four trials were installed in Northeast Argentina on Vertisols (S1), Mollisols (S2) and Entisols (S3 and S4). In S1 and S2 harvest residues and forest fl oor were either (1) removed (R),...

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Autores principales: Lupi, Ana Maria, Quintero, Cesar, Boca, Rosa Teresa, Diaz, Diana, Boschetti, Graciela, Aparicio, Jorge Luis, Ingaramo, Luciana And
Formato: Artículo
Lenguaje:Inglés
Publicado: INIA Uruguay y Facultad de Agronomía, Universidad de la República 2021
Materias:
Acceso en línea:http://agrocienciauruguay.uy/ojs/index.php/agrociencia/article/view/655
http://hdl.handle.net/20.500.12123/9447
https://doi.org/10.31285/AGRO.16.655
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author Lupi, Ana Maria
Quintero, Cesar
Boca, Rosa Teresa
Diaz, Diana
Boschetti, Graciela
Aparicio, Jorge Luis
Ingaramo, Luciana And
author_browse Aparicio, Jorge Luis
Boca, Rosa Teresa
Boschetti, Graciela
Diaz, Diana
Ingaramo, Luciana And
Lupi, Ana Maria
Quintero, Cesar
author_facet Lupi, Ana Maria
Quintero, Cesar
Boca, Rosa Teresa
Diaz, Diana
Boschetti, Graciela
Aparicio, Jorge Luis
Ingaramo, Luciana And
author_sort Lupi, Ana Maria
collection INTA Digital
description We analyze the short term effect of the harvest residues management on the Phosphorus (P) fractions of the soil. Four trials were installed in Northeast Argentina on Vertisols (S1), Mollisols (S2) and Entisols (S3 and S4). In S1 and S2 harvest residues and forest fl oor were either (1) removed (R), (2) retained (RR), 3) burnt (BR), or (4) retained at double the normal quantity (DR). In S3 and S4 harvest residues where (1) removed (WTH), 2) retained (RR) or 3) burnt (BR). Soil samples were obtained at 0-5 cm and 5-10 cm depth layers at 18 (S1), 22(S2, S3) and 10 (S4) months after burnt treatments. P fractions were determined according to Hedley et al. (1982) methods. Soil orders showed different total P: in Mollisols P concentration (S2: 314,3 mg kg-1) tripled those in Entisols (S3 y S4: 118,4 mg P kg-1). Differences were even higher for Organic P (Po): the highest concentration was found in Mollisols (171,4 mg Po kg-1) related to its higher organic matter, and the lowest concentration was in Entisols (44,0 mg Po kg-1). Available P was between 14 mg kg-1 and 25 mg kg-1, enough to satisfy annual demands of forest plantations (Eucalyptus and Pinus). RR and DR did not show changes in the P fractions, although an increase in the P reserves (Po y Pt) could be expected for the middle term, due to the decomposition of the retained/added residues. R or WTH did not affect neither inorganic nor organic P fractions. The most important change was found in BR, where the available P and other mean and highly stable inorganic P fractions increased, due to the ashes; the Po was not modified. The fi re was an instant mechanism to transfer the nutrients from the biomass to the soil.
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institution Instituto Nacional de Tecnología Agropecuaria (INTA -Argentina)
language Inglés
publishDate 2021
publishDateRange 2021
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publisher INIA Uruguay y Facultad de Agronomía, Universidad de la República
publisherStr INIA Uruguay y Facultad de Agronomía, Universidad de la República
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spelling INTA94472021-05-28T16:38:52Z Changes in soil phosphorus in different forest residue management Lupi, Ana Maria Quintero, Cesar Boca, Rosa Teresa Diaz, Diana Boschetti, Graciela Aparicio, Jorge Luis Ingaramo, Luciana And Bosques Pinus Eucalyptus Fósforo Suelo Ordenación Forestal Forests Phosphorus Soil Forest Management We analyze the short term effect of the harvest residues management on the Phosphorus (P) fractions of the soil. Four trials were installed in Northeast Argentina on Vertisols (S1), Mollisols (S2) and Entisols (S3 and S4). In S1 and S2 harvest residues and forest fl oor were either (1) removed (R), (2) retained (RR), 3) burnt (BR), or (4) retained at double the normal quantity (DR). In S3 and S4 harvest residues where (1) removed (WTH), 2) retained (RR) or 3) burnt (BR). Soil samples were obtained at 0-5 cm and 5-10 cm depth layers at 18 (S1), 22(S2, S3) and 10 (S4) months after burnt treatments. P fractions were determined according to Hedley et al. (1982) methods. Soil orders showed different total P: in Mollisols P concentration (S2: 314,3 mg kg-1) tripled those in Entisols (S3 y S4: 118,4 mg P kg-1). Differences were even higher for Organic P (Po): the highest concentration was found in Mollisols (171,4 mg Po kg-1) related to its higher organic matter, and the lowest concentration was in Entisols (44,0 mg Po kg-1). Available P was between 14 mg kg-1 and 25 mg kg-1, enough to satisfy annual demands of forest plantations (Eucalyptus and Pinus). RR and DR did not show changes in the P fractions, although an increase in the P reserves (Po y Pt) could be expected for the middle term, due to the decomposition of the retained/added residues. R or WTH did not affect neither inorganic nor organic P fractions. The most important change was found in BR, where the available P and other mean and highly stable inorganic P fractions increased, due to the ashes; the Po was not modified. The fi re was an instant mechanism to transfer the nutrients from the biomass to the soil. Instituto de Suelos Fil: Lupi, Ana Maria. Instituto Nacional de Tecnología Agropecuaria (INTA). Instituto de Suelos; Argentina Fil: Quintero, César. Universidad Nacional de Entre Ríos. Facultad de Ciencias Agropecuarias; Argentina Fil: Boca, Rosa Teresa. Instituto Nacional de Tecnología Agropecuaria (INTA). Instituto de Clima y Agua; Argentina Fil: Diaz, Diana. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Concordia; Argentina Fil: Boschetti, Graciela. Universidad Nacional de Entre Ríos. Facultad de Ciencias Agropecuarias; Argentina Fil: Aparicio, Jorge Luis. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Bella Vista; Argentina Fil: Ingaramo, Luciana And. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Concordia; Argentina 2021-05-28T16:31:39Z 2021-05-28T16:31:39Z 2012 info:ar-repo/semantics/artículo info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://agrocienciauruguay.uy/ojs/index.php/agrociencia/article/view/655 http://hdl.handle.net/20.500.12123/9447 2730-5066 https://doi.org/10.31285/AGRO.16.655 eng info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) application/pdf INIA Uruguay y Facultad de Agronomía, Universidad de la República Agrociencia Uruguay 16 (3) : 128-134. (2012)
spellingShingle Bosques
Pinus
Eucalyptus
Fósforo
Suelo
Ordenación Forestal
Forests
Phosphorus
Soil
Forest Management
Lupi, Ana Maria
Quintero, Cesar
Boca, Rosa Teresa
Diaz, Diana
Boschetti, Graciela
Aparicio, Jorge Luis
Ingaramo, Luciana And
Changes in soil phosphorus in different forest residue management
title Changes in soil phosphorus in different forest residue management
title_full Changes in soil phosphorus in different forest residue management
title_fullStr Changes in soil phosphorus in different forest residue management
title_full_unstemmed Changes in soil phosphorus in different forest residue management
title_short Changes in soil phosphorus in different forest residue management
title_sort changes in soil phosphorus in different forest residue management
topic Bosques
Pinus
Eucalyptus
Fósforo
Suelo
Ordenación Forestal
Forests
Phosphorus
Soil
Forest Management
url http://agrocienciauruguay.uy/ojs/index.php/agrociencia/article/view/655
http://hdl.handle.net/20.500.12123/9447
https://doi.org/10.31285/AGRO.16.655
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