Changes in soil phosphorus (P) fractions and P bioavailability after 10 years of continuous P fertilization

Phosphorus fertilization modify soil P fractions differing in availability, but little is known about bioavailability of these pools for the crops when increasing P fertilizer rates in the medium term. Our objectives were to evaluate: i) changes in Bray-1 P content (extracted with 0,03 M NH4F and 0,...

Full description

Bibliographic Details
Main Authors: Biassoni, María Micaela, Vivas, Hugo, Gutierrez Boem, Flavio Hernán, Salvagiotti, Fernando
Format: info:ar-repo/semantics/artículo
Language:Inglés
Published: Elsevier 2023
Subjects:
Online Access:http://hdl.handle.net/20.500.12123/14637
https://www.sciencedirect.com/science/article/pii/S0167198723001447
https://doi.org/10.1016/j.still.2023.105777
_version_ 1855037153160986624
author Biassoni, María Micaela
Vivas, Hugo
Gutierrez Boem, Flavio Hernán
Salvagiotti, Fernando
author_browse Biassoni, María Micaela
Gutierrez Boem, Flavio Hernán
Salvagiotti, Fernando
Vivas, Hugo
author_facet Biassoni, María Micaela
Vivas, Hugo
Gutierrez Boem, Flavio Hernán
Salvagiotti, Fernando
author_sort Biassoni, María Micaela
collection INTA Digital
description Phosphorus fertilization modify soil P fractions differing in availability, but little is known about bioavailability of these pools for the crops when increasing P fertilizer rates in the medium term. Our objectives were to evaluate: i) changes in Bray-1 P content (extracted with 0,03 M NH4F and 0,1 M HCl) and soil P fractions as estimated by physical (Cambardella and Elliot method, POM-P) and chemical fractionation (Hedley method), ii) the relationship between these fractions and P bioavailability quantified in a test crop, and iii) the interaction with sulfur (S) fertilization after 10 years of continuous P and S fertilization. Soil samples were taken after 10 years in an experiment that followed a maize - full season-soybean - double-cropped wheat /soybean sequence that received P and S fertilization when cereals were sown. Treatments consisted of a factorial combination of three P rates (0, 20, and 40 kg P ha−1) and four S rates (0, 12, 24, and 36 kg S ha−1) applied to cereals from 2000 to 2010. After that, a maize used as a test crop was sown and P uptake was considered as bioavailable P. Soil samples were taken before sowing the test crop, and P in soil was fractionated chemically by the Hedley method and physically by wet sieving. After 10 years, when P fertilizer was not applied, soil Bray-1 P decreased 50 % respect to the initial P values, and increased up to 2.3 times when evaluating the highest P fertilizer rate. P fertilization did not change in POM-P. P soil labile (NaHCO3-Pi) and moderately labile (NaOH- Pi and HCl 1 M- Pi) inorganic fractions increased 83 %, 50 %, and 22 % in response to P addition, representing an increase of 4.2, 4.9, and 4.5 mg kg−1 of these fractions per 100 kg of applied P. Likewise, these fractions were related with P uptake in the maize test crop with 1.6, 1.5, and 1 kg of P uptake ha−1 in mg kg−1 increase in each of these fractions, respectively. Then, these fractions may be responsible for the legacy-P after 10 years of continuous fertilization in a Luvic Phaeozem of the Pampas region.
format info:ar-repo/semantics/artículo
id INTA14637
institution Instituto Nacional de Tecnología Agropecuaria (INTA -Argentina)
language Inglés
publishDate 2023
publishDateRange 2023
publishDateSort 2023
publisher Elsevier
publisherStr Elsevier
record_format dspace
spelling INTA146372024-11-07T15:02:47Z Changes in soil phosphorus (P) fractions and P bioavailability after 10 years of continuous P fertilization Biassoni, María Micaela Vivas, Hugo Gutierrez Boem, Flavio Hernán Salvagiotti, Fernando Suelo Fósforo Aplicación de Abonos Abonos Fosfatados Biodisponibilidad Soil Phosphorus Fertilizer Application Phosphate Fertilizers Bioavailability Phosphorus fertilization modify soil P fractions differing in availability, but little is known about bioavailability of these pools for the crops when increasing P fertilizer rates in the medium term. Our objectives were to evaluate: i) changes in Bray-1 P content (extracted with 0,03 M NH4F and 0,1 M HCl) and soil P fractions as estimated by physical (Cambardella and Elliot method, POM-P) and chemical fractionation (Hedley method), ii) the relationship between these fractions and P bioavailability quantified in a test crop, and iii) the interaction with sulfur (S) fertilization after 10 years of continuous P and S fertilization. Soil samples were taken after 10 years in an experiment that followed a maize - full season-soybean - double-cropped wheat /soybean sequence that received P and S fertilization when cereals were sown. Treatments consisted of a factorial combination of three P rates (0, 20, and 40 kg P ha−1) and four S rates (0, 12, 24, and 36 kg S ha−1) applied to cereals from 2000 to 2010. After that, a maize used as a test crop was sown and P uptake was considered as bioavailable P. Soil samples were taken before sowing the test crop, and P in soil was fractionated chemically by the Hedley method and physically by wet sieving. After 10 years, when P fertilizer was not applied, soil Bray-1 P decreased 50 % respect to the initial P values, and increased up to 2.3 times when evaluating the highest P fertilizer rate. P fertilization did not change in POM-P. P soil labile (NaHCO3-Pi) and moderately labile (NaOH- Pi and HCl 1 M- Pi) inorganic fractions increased 83 %, 50 %, and 22 % in response to P addition, representing an increase of 4.2, 4.9, and 4.5 mg kg−1 of these fractions per 100 kg of applied P. Likewise, these fractions were related with P uptake in the maize test crop with 1.6, 1.5, and 1 kg of P uptake ha−1 in mg kg−1 increase in each of these fractions, respectively. Then, these fractions may be responsible for the legacy-P after 10 years of continuous fertilization in a Luvic Phaeozem of the Pampas region. EEA Oliveros Fil: Biassoni, María Micaela. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Oliveros; Argentina Fil: Biassoni, María Micaela. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Biassoni, María Micaela. Universidad Nacional de Rosario. Facultad de Ciencias Agrarias. Cátedra de Edafología; Argentina Fil: Vivas, H. Actividad privada; Argentina Fil: Gutiérrez Boem, Flavio Hernán. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Gutiérrez Boem, Flavio Hernán. Universidad de Buenos Aires. Facultad de Agronomía. Cátedra de Fertilidad y Fertilizantes; Argentina. Fil: Salvagiotti, Fernando. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Oliveros; Argentina Fil: Salvagiotti, Fernando. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina 2023-06-16T16:32:51Z 2023-06-16T16:32:51Z 2023-08 info:ar-repo/semantics/artículo info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://hdl.handle.net/20.500.12123/14637 https://www.sciencedirect.com/science/article/pii/S0167198723001447 0167-1987 1879-3444 https://doi.org/10.1016/j.still.2023.105777 eng info:eu-repograntAgreement/INTA/PNCYO-1127033/AR./Manejo nutricional de cereales y oleaginosas para la intensificación sustentable de los sistemas productivos info:eu-repograntAgreement/INTA/2019-PE-E1-I011-001/2019-PE-E1-I011-001/AR./Intensificacion Sustentable de la Agricultura en la Region Pampeana info:eu-repo/semantics/restrictedAccess 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 Elsevier Soil and Tillage Research 232 : 105777. (August 2023)
spellingShingle Suelo
Fósforo
Aplicación de Abonos
Abonos Fosfatados
Biodisponibilidad
Soil
Phosphorus
Fertilizer Application
Phosphate Fertilizers
Bioavailability
Biassoni, María Micaela
Vivas, Hugo
Gutierrez Boem, Flavio Hernán
Salvagiotti, Fernando
Changes in soil phosphorus (P) fractions and P bioavailability after 10 years of continuous P fertilization
title Changes in soil phosphorus (P) fractions and P bioavailability after 10 years of continuous P fertilization
title_full Changes in soil phosphorus (P) fractions and P bioavailability after 10 years of continuous P fertilization
title_fullStr Changes in soil phosphorus (P) fractions and P bioavailability after 10 years of continuous P fertilization
title_full_unstemmed Changes in soil phosphorus (P) fractions and P bioavailability after 10 years of continuous P fertilization
title_short Changes in soil phosphorus (P) fractions and P bioavailability after 10 years of continuous P fertilization
title_sort changes in soil phosphorus p fractions and p bioavailability after 10 years of continuous p fertilization
topic Suelo
Fósforo
Aplicación de Abonos
Abonos Fosfatados
Biodisponibilidad
Soil
Phosphorus
Fertilizer Application
Phosphate Fertilizers
Bioavailability
url http://hdl.handle.net/20.500.12123/14637
https://www.sciencedirect.com/science/article/pii/S0167198723001447
https://doi.org/10.1016/j.still.2023.105777
work_keys_str_mv AT biassonimariamicaela changesinsoilphosphoruspfractionsandpbioavailabilityafter10yearsofcontinuouspfertilization
AT vivashugo changesinsoilphosphoruspfractionsandpbioavailabilityafter10yearsofcontinuouspfertilization
AT gutierrezboemflaviohernan changesinsoilphosphoruspfractionsandpbioavailabilityafter10yearsofcontinuouspfertilization
AT salvagiottifernando changesinsoilphosphoruspfractionsandpbioavailabilityafter10yearsofcontinuouspfertilization