Soil mineralogy-controlled phosphorus availability in soils mixed with phosphate fertiliser and biochar.

he biochar amendment to soil proved to be beneficial to improve soil quality and provide nutrients. However, the effect of biochar on the availability of P is still controversial. We aim to study the effect of adding phosphate fertiliser and biochar on the P bioavailability in soils of different mineralogies. Eight biochars derived from biomass (rice husk and coffee husk), soil (sandy and clayey), and phosphate fertiliser (triple superphosphate) were produced. The biochar enrichment process with superphosphate was carried out before and after pyrolysis. Thus, we tested two biochar groups: (1) enriched biochars prior to pyrolysis; (2) enriched biochars after pyrolysis. These biochars were tested as P sources in soils of three mineralogies (kaolinite/oxide, kaolinite, and smectite). Batch sorption-desorption experiments were conducted. The sorbed P was fractionated to examine the factors controlling the retention of applied P. In the three soil mineralogies the use of enriched biochars prior to pyrolysis results in lower availability of P. In contrast, the enriched biochars after pyrolysis increase the bioavailability of P. The coffee husk biochar is more suitable than rice husk biochar to protect P from soil retention reactions. The use of sandy soil rather than clayey soil in enriched biochars compositions results in higher P content availability when applied to soils. The factor that controls the retention of P is the reaction between P, organic compounds, and Fe and Al compounds. The greater the relationship between biochar and soluble P in the fertiliser, the higher the increase of P retention.

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Main Authors: MATOSO, S. C. G., WADT, P. G. S., SOUZA JÚNIOR, V. S. de, PÉREZ, X. L. O.
Other Authors: PAULO GUILHERME SALVADOR WADT, CPAF-RO.
Format: Artigo de periódico biblioteca
Language:Ingles
English
Published: 2022-06-06
Subjects:Enriched biochar, Organo-mineral associations, Phosphorus availability, Biochar, Soil mineralogy,
Online Access:http://www.alice.cnptia.embrapa.br/alice/handle/doc/1143745
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spelling dig-alice-doc-11437452022-06-07T13:19:46Z Soil mineralogy-controlled phosphorus availability in soils mixed with phosphate fertiliser and biochar. MATOSO, S. C. G. WADT, P. G. S. SOUZA JÚNIOR, V. S. de PÉREZ, X. L. O. PAULO GUILHERME SALVADOR WADT, CPAF-RO. Enriched biochar Organo-mineral associations Phosphorus availability Biochar Soil mineralogy he biochar amendment to soil proved to be beneficial to improve soil quality and provide nutrients. However, the effect of biochar on the availability of P is still controversial. We aim to study the effect of adding phosphate fertiliser and biochar on the P bioavailability in soils of different mineralogies. Eight biochars derived from biomass (rice husk and coffee husk), soil (sandy and clayey), and phosphate fertiliser (triple superphosphate) were produced. The biochar enrichment process with superphosphate was carried out before and after pyrolysis. Thus, we tested two biochar groups: (1) enriched biochars prior to pyrolysis; (2) enriched biochars after pyrolysis. These biochars were tested as P sources in soils of three mineralogies (kaolinite/oxide, kaolinite, and smectite). Batch sorption-desorption experiments were conducted. The sorbed P was fractionated to examine the factors controlling the retention of applied P. In the three soil mineralogies the use of enriched biochars prior to pyrolysis results in lower availability of P. In contrast, the enriched biochars after pyrolysis increase the bioavailability of P. The coffee husk biochar is more suitable than rice husk biochar to protect P from soil retention reactions. The use of sandy soil rather than clayey soil in enriched biochars compositions results in higher P content availability when applied to soils. The factor that controls the retention of P is the reaction between P, organic compounds, and Fe and Al compounds. The greater the relationship between biochar and soluble P in the fertiliser, the higher the increase of P retention. Online First. 2022-06-07T13:19:38Z 2022-06-07T13:19:38Z 2022-06-06 2022 Artigo de periódico Environmental Technology, 2022. http://www.alice.cnptia.embrapa.br/alice/handle/doc/1143745 Ingles en openAccess
institution EMBRAPA
collection DSpace
country Brasil
countrycode BR
component Bibliográfico
access En linea
databasecode dig-alice
tag biblioteca
region America del Sur
libraryname Sistema de bibliotecas de EMBRAPA
language Ingles
English
topic Enriched biochar
Organo-mineral associations
Phosphorus availability
Biochar
Soil mineralogy
Enriched biochar
Organo-mineral associations
Phosphorus availability
Biochar
Soil mineralogy
spellingShingle Enriched biochar
Organo-mineral associations
Phosphorus availability
Biochar
Soil mineralogy
Enriched biochar
Organo-mineral associations
Phosphorus availability
Biochar
Soil mineralogy
MATOSO, S. C. G.
WADT, P. G. S.
SOUZA JÚNIOR, V. S. de
PÉREZ, X. L. O.
Soil mineralogy-controlled phosphorus availability in soils mixed with phosphate fertiliser and biochar.
description he biochar amendment to soil proved to be beneficial to improve soil quality and provide nutrients. However, the effect of biochar on the availability of P is still controversial. We aim to study the effect of adding phosphate fertiliser and biochar on the P bioavailability in soils of different mineralogies. Eight biochars derived from biomass (rice husk and coffee husk), soil (sandy and clayey), and phosphate fertiliser (triple superphosphate) were produced. The biochar enrichment process with superphosphate was carried out before and after pyrolysis. Thus, we tested two biochar groups: (1) enriched biochars prior to pyrolysis; (2) enriched biochars after pyrolysis. These biochars were tested as P sources in soils of three mineralogies (kaolinite/oxide, kaolinite, and smectite). Batch sorption-desorption experiments were conducted. The sorbed P was fractionated to examine the factors controlling the retention of applied P. In the three soil mineralogies the use of enriched biochars prior to pyrolysis results in lower availability of P. In contrast, the enriched biochars after pyrolysis increase the bioavailability of P. The coffee husk biochar is more suitable than rice husk biochar to protect P from soil retention reactions. The use of sandy soil rather than clayey soil in enriched biochars compositions results in higher P content availability when applied to soils. The factor that controls the retention of P is the reaction between P, organic compounds, and Fe and Al compounds. The greater the relationship between biochar and soluble P in the fertiliser, the higher the increase of P retention.
author2 PAULO GUILHERME SALVADOR WADT, CPAF-RO.
author_facet PAULO GUILHERME SALVADOR WADT, CPAF-RO.
MATOSO, S. C. G.
WADT, P. G. S.
SOUZA JÚNIOR, V. S. de
PÉREZ, X. L. O.
format Artigo de periódico
topic_facet Enriched biochar
Organo-mineral associations
Phosphorus availability
Biochar
Soil mineralogy
author MATOSO, S. C. G.
WADT, P. G. S.
SOUZA JÚNIOR, V. S. de
PÉREZ, X. L. O.
author_sort MATOSO, S. C. G.
title Soil mineralogy-controlled phosphorus availability in soils mixed with phosphate fertiliser and biochar.
title_short Soil mineralogy-controlled phosphorus availability in soils mixed with phosphate fertiliser and biochar.
title_full Soil mineralogy-controlled phosphorus availability in soils mixed with phosphate fertiliser and biochar.
title_fullStr Soil mineralogy-controlled phosphorus availability in soils mixed with phosphate fertiliser and biochar.
title_full_unstemmed Soil mineralogy-controlled phosphorus availability in soils mixed with phosphate fertiliser and biochar.
title_sort soil mineralogy-controlled phosphorus availability in soils mixed with phosphate fertiliser and biochar.
publishDate 2022-06-06
url http://www.alice.cnptia.embrapa.br/alice/handle/doc/1143745
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AT wadtpgs soilmineralogycontrolledphosphorusavailabilityinsoilsmixedwithphosphatefertiliserandbiochar
AT souzajuniorvsde soilmineralogycontrolledphosphorusavailabilityinsoilsmixedwithphosphatefertiliserandbiochar
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