Biochar Chemistry in a Weathered Tropical Soil: Kinetics of Phosphorus Sorption

The phosphorus (P) chemistry of biochar (BC)-amended soils is poorly understood. This statement is based on the lack of published research attempting a comprehensive characterization of biochar’s influence on P sorption. Therefore, this study addressed the kinetic limitations of these processes. Thi...
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Autor*in:	Marina Moura Morales [verfasserIn] Nicholas Brian Comerford [verfasserIn] Maurel Behling [verfasserIn] Daniel Carneiro de Abreu [verfasserIn] Iraê Amaral Guerrini [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2021

Schlagwörter:	fast pyrolysis batch method P retention

Übergeordnetes Werk:	In: Agriculture - MDPI AG, 2012, 11(2021), 4, p 295
Übergeordnetes Werk:	volume:11 ; year:2021 ; number:4, p 295

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/agriculture11040295

Katalog-ID:	DOAJ05667838X

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520			\|a The phosphorus (P) chemistry of biochar (BC)-amended soils is poorly understood. This statement is based on the lack of published research attempting a comprehensive characterization of biochar’s influence on P sorption. Therefore, this study addressed the kinetic limitations of these processes. This was accomplished using a fast pyrolysis biochar made from a mix of waste materials applied to a highly weathered Latossolo Vermelho distrofico (Oxisol) from São Paulo, Brazil. Standard method (batch method) was used. The sorption kinetic studies indicated that P sorption in both cases, soil (S) and soil-biochar (SBC), had a relatively fast initial reaction between 0 to 5 min. This may have happened because adding biochar to the soil decreased P sorption capacity compared to the mineral soil alone. Presumably, this is a result of: (i) Inorganic phosphorus desorbed from biochar was resorbed onto the mineral soil; (ii) charcoal particles physically covered P sorption locations on soil; or (iii) the pH increased when BC was added SBC and the soil surface became more negatively charged, thus increasing anion repulsion and decreasing P sorption.
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source	In Agriculture 11(2021), 4, p 295 volume:11 year:2021 number:4, p 295
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authorswithroles_txt_mv	Marina Moura Morales @@aut@@ Nicholas Brian Comerford @@aut@@ Maurel Behling @@aut@@ Daniel Carneiro de Abreu @@aut@@ Iraê Amaral Guerrini @@aut@@
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callnumber-first	S - Agriculture
author	Marina Moura Morales
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topic_title	S1-972 Biochar Chemistry in a Weathered Tropical Soil: Kinetics of Phosphorus Sorption fast pyrolysis batch method P retention
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title	Biochar Chemistry in a Weathered Tropical Soil: Kinetics of Phosphorus Sorption
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title_full	Biochar Chemistry in a Weathered Tropical Soil: Kinetics of Phosphorus Sorption
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title_sort	biochar chemistry in a weathered tropical soil: kinetics of phosphorus sorption
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title_auth	Biochar Chemistry in a Weathered Tropical Soil: Kinetics of Phosphorus Sorption
abstract	The phosphorus (P) chemistry of biochar (BC)-amended soils is poorly understood. This statement is based on the lack of published research attempting a comprehensive characterization of biochar’s influence on P sorption. Therefore, this study addressed the kinetic limitations of these processes. This was accomplished using a fast pyrolysis biochar made from a mix of waste materials applied to a highly weathered Latossolo Vermelho distrofico (Oxisol) from São Paulo, Brazil. Standard method (batch method) was used. The sorption kinetic studies indicated that P sorption in both cases, soil (S) and soil-biochar (SBC), had a relatively fast initial reaction between 0 to 5 min. This may have happened because adding biochar to the soil decreased P sorption capacity compared to the mineral soil alone. Presumably, this is a result of: (i) Inorganic phosphorus desorbed from biochar was resorbed onto the mineral soil; (ii) charcoal particles physically covered P sorption locations on soil; or (iii) the pH increased when BC was added SBC and the soil surface became more negatively charged, thus increasing anion repulsion and decreasing P sorption.
abstractGer	The phosphorus (P) chemistry of biochar (BC)-amended soils is poorly understood. This statement is based on the lack of published research attempting a comprehensive characterization of biochar’s influence on P sorption. Therefore, this study addressed the kinetic limitations of these processes. This was accomplished using a fast pyrolysis biochar made from a mix of waste materials applied to a highly weathered Latossolo Vermelho distrofico (Oxisol) from São Paulo, Brazil. Standard method (batch method) was used. The sorption kinetic studies indicated that P sorption in both cases, soil (S) and soil-biochar (SBC), had a relatively fast initial reaction between 0 to 5 min. This may have happened because adding biochar to the soil decreased P sorption capacity compared to the mineral soil alone. Presumably, this is a result of: (i) Inorganic phosphorus desorbed from biochar was resorbed onto the mineral soil; (ii) charcoal particles physically covered P sorption locations on soil; or (iii) the pH increased when BC was added SBC and the soil surface became more negatively charged, thus increasing anion repulsion and decreasing P sorption.
abstract_unstemmed	The phosphorus (P) chemistry of biochar (BC)-amended soils is poorly understood. This statement is based on the lack of published research attempting a comprehensive characterization of biochar’s influence on P sorption. Therefore, this study addressed the kinetic limitations of these processes. This was accomplished using a fast pyrolysis biochar made from a mix of waste materials applied to a highly weathered Latossolo Vermelho distrofico (Oxisol) from São Paulo, Brazil. Standard method (batch method) was used. The sorption kinetic studies indicated that P sorption in both cases, soil (S) and soil-biochar (SBC), had a relatively fast initial reaction between 0 to 5 min. This may have happened because adding biochar to the soil decreased P sorption capacity compared to the mineral soil alone. Presumably, this is a result of: (i) Inorganic phosphorus desorbed from biochar was resorbed onto the mineral soil; (ii) charcoal particles physically covered P sorption locations on soil; or (iii) the pH increased when BC was added SBC and the soil surface became more negatively charged, thus increasing anion repulsion and decreasing P sorption.
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title_short	Biochar Chemistry in a Weathered Tropical Soil: Kinetics of Phosphorus Sorption
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Biochar Chemistry in a Weathered Tropical Soil: Kinetics of Phosphorus Sorption

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