fate of phosphorus of ash-rich biochars in a soil-plant system

AIMS: The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biochar-amended sandy soil; (ii) the transformation of biochar P in a soil-plant system. METHODS: Several methodologies (a bioassay test, soluble P extractions, a sequential P fractionation and successiv...

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Published inPlant and soil Vol. 375; no. 1-2; pp. 61 - 74
Main Authors Wang, Tao, Camps-Arbestain, Marta, Hedley, Mike
Format Journal Article
LanguageEnglish
Published Cham Springer-Verlag 01.02.2014
Springer
Springer International Publishing
Springer Nature B.V
Subjects
Acid soils
Agricultural and Veterinary sciences
Agricultural Sciences
Agricultural soils
Agrology
Agronomy. Soil science and plant productions
Animal, plant and microbial ecology
Annan lantbruksvetenskap
application timing
Bioassays
Bioavailability
Biochar
Biological and medical sciences
Biomedical and Life Sciences
Biosolids
calcium
Cattle manure
Charcoal
Ecology
Environmental aspects
Fertilizers
Flowers & plants
Forest soils
Fractionation
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
Lantbruksvetenskap och veterinärmedicin
Life Sciences
Other Agricultural Sciences
Phosphorus
Phosphorus content
phosphorus fertilizers
Plant Physiology
Plant Sciences
Plant-soil relationships
Plants
Regular Article
rock phosphate
Sand soils
Sandy soils
slow-release fertilizers
Sodium hydroxide
Soil pollution
Soil research
Soil Science & Conservation
Soil treatment
Soil-plant relationships. Soil fertility
Soil-plant relationships. Soil fertility. Fertilization. Amendments
Soils
New Zealand
Transformation
Bioavailability
Biochar
P fractionation
Carbonization
Fractionation
Phosphorus
Soil plant relation
Biological system
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Abstract AIMS: The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biochar-amended sandy soil; (ii) the transformation of biochar P in a soil-plant system. METHODS: Several methodologies (a bioassay test, soluble P extractions, a sequential P fractionation and successive P extractions via resin strips) were used to study the bioavailability and transformation of P in a sandy soil fertilised with either conventional P fertilisers [Ca(H₂PO₄)₂ (CaP) and Sechura phosphate rock (SPR)] or biochars produced from cattle manure (MAe) and alum-treated biosolids (BSe) at four temperatures (250, 350, 450, and 550 °C). RESULTS: Biochar P mainly contributed to increase soil resin-extractable P- and inorganic NaOH-extractable P-fractions, and thus to plant available P. The decrease in P concentrations of those fractions was caused by the uptake of P by plants rather than their transformations into more stable forms. P release rates diminished following the order: CaP > MAe > BSe > SPR, which indicates a decline in P availability from these P sources. CONCLUSIONS: Phosphorus-rich biochar can be used as a slow-release fertiliser. It is necessary to determine available P (either soil or fertiliser tests) in biochars prior to its application to soil, so that dose, frequency and timing of application are correctly established.
AbstractList Aims The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biocharamended sandy soil; (ii) the transformation of biochar P in a soil-plant system. Methods Several methodologies (a bioassay test, soluble P extractions, a sequential P fractionation and successive P extractions via resin strips) were used to study the bioavailability and transformation of P in a sandy soil fertilised with either conventional P fertilisers [Ca(H₂PO₄)₂ (CaP) and Sechura phosphate rock (SPR)] or biochars produced from cattle manure (MA e ) and alum-treated biosolids (BS e ) at four temperatures (250, 350, 450, and 550 °C). Results Biochar P mainly contributed to increase soil resin-extractable P-and inorganic NaOH-extractable P fractions, and thus to plant available P. The decrease in P concentrations of those fractions was caused by the uptake of P by plants rather than their transformations into more stable forms. P release rates diminished following the order: CaP > MAe > BSe > SPR, which indicates a decline in P availability from these P sources. Conclusions Phosphorus-rich biochar can be used as a slow-release fertiliser. It is necessary to determine available P (either soil or fertiliser tests) in biochars prior to its application to soil, so that dose, frequency and timing of application are correctly established.
The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biochar-amended sandy soil; (ii) the transformation of biochar P in a soil-plant system. Several methodologies (a bioassay test, soluble P extractions, a sequential P fractionation and successive P extractions via resin strips) were used to study the bioavailability and transformation of P in a sandy soil fertilised with either conventional P fertilisers [Ca(H2PO4)(2) (CaP) and Sechura phosphate rock (SPR)] or biochars produced from cattle manure (MAe) and alum-treated biosolids (BSe) at four temperatures (250, 350, 450, and 550 A degrees C). Biochar P mainly contributed to increase soil resin-extractable P- and inorganic NaOH-extractable P-fractions, and thus to plant available P. The decrease in P concentrations of those fractions was caused by the uptake of P by plants rather than their transformations into more stable forms. P release rates diminished following the order: CaP > MAe > BSe > SPR, which indicates a decline in P availability from these P sources. Phosphorus-rich biochar can be used as a slow-release fertiliser. It is necessary to determine available P (either soil or fertiliser tests) in biochars prior to its application to soil, so that dose, frequency and timing of application are correctly established.
Aims The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biocharamended sandy soil; (ii) the transformation of biochar P in a soil-plant system. Methods Several methodologies (a bioassay test, soluble P extractions, a sequential P fractionation and successive P extractions via resin strips) were used to study the bioavailability and transformation of P in a sandy soil fertilised with either conventional P fertilisers [Ca([H.sub.2]P[O.sub.4])2 (CaP) and Sechura phosphate rock (SPR)] or biochars produced from cattle manure (MAe) and alum-treated biosolids (BSe) at four temperatures (250, 350, 450, and 550 °C). Results Biochar P mainly contributed to increase soil resin-extractable P- and inorganic NaOH-extractable Pfractions, and thus to plant available P. The decrease in P concentrations of those fractions was caused by the uptake of P by plants rather than their transformations into more stable forms. P release rates diminished following the order: CaP > MAe > BSe > SPR, which indicates a decline in P availability from these P sources. Conclusions Phosphorus-rich biochar can be used as a slow-release fertiliser. It is necessary to determine available P (either soil or fertiliser tests) in biochars prior to its application to soil, so that dose, frequency and timing of application are correctly established. Keywords P fractionation * Biochar * Bioavailability * Transformation
AIMS: The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biochar-amended sandy soil; (ii) the transformation of biochar P in a soil-plant system. METHODS: Several methodologies (a bioassay test, soluble P extractions, a sequential P fractionation and successive P extractions via resin strips) were used to study the bioavailability and transformation of P in a sandy soil fertilised with either conventional P fertilisers [Ca(H₂PO₄)₂(CaP) and Sechura phosphate rock (SPR)] or biochars produced from cattle manure (MAe) and alum-treated biosolids (BSe) at four temperatures (250, 350, 450, and 550 °C). RESULTS: Biochar P mainly contributed to increase soil resin-extractable P- and inorganic NaOH-extractable P-fractions, and thus to plant available P. The decrease in P concentrations of those fractions was caused by the uptake of P by plants rather than their transformations into more stable forms. P release rates diminished following the order: CaP > MAe > BSe > SPR, which indicates a decline in P availability from these P sources. CONCLUSIONS: Phosphorus-rich biochar can be used as a slow-release fertiliser. It is necessary to determine available P (either soil or fertiliser tests) in biochars prior to its application to soil, so that dose, frequency and timing of application are correctly established.
The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biochar-amended sandy soil; (ii) the transformation of biochar P in a soil-plant system. Several methodologies (a bioassay test, soluble P extractions, a sequential P fractionation and successive P extractions via resin strips) were used to study the bioavailability and transformation of P in a sandy soil fertilised with either conventional P fertilisers [Ca(H2PO^sub 4^)^sub 2^ (CaP) and Sechura phosphate rock (SPR)] or biochars produced from cattle manure (MAe) and alum-treated biosolids (BSe) at four temperatures (250, 350, 450, and 550 °C). Biochar P mainly contributed to increase soil resin-extractable P- and inorganic NaOH-extractable P-fractions, and thus to plant available P. The decrease in P concentrations of those fractions was caused by the uptake of P by plants rather than their transformations into more stable forms. P release rates diminished following the order: CaP > MAe > BSe > SPR, which indicates a decline in P availability from these P sources. Phosphorus-rich biochar can be used as a slow-release fertiliser. It is necessary to determine available P (either soil or fertiliser tests) in biochars prior to its application to soil, so that dose, frequency and timing of application are correctly established.[PUBLICATION ABSTRACT]
Aims The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biochar-amended sandy soil; (ii) the transformation of biochar P in a soil-plant system. Methods Several methodologies (a bioassay test, soluble P extractions, a sequential P fractionation and successive P extractions via resin strips) were used to study the bioavailability and transformation of P in a sandy soil fertilised with either conventional P fertilisers [Ca(H 2 PO 4 ) 2 (CaP) and Sechura phosphate rock (SPR)] or biochars produced from cattle manure (MAe) and alum-treated biosolids (BSe) at four temperatures (250, 350, 450, and 550 °C). Results Biochar P mainly contributed to increase soil resin-extractable P- and inorganic NaOH-extractable P-fractions, and thus to plant available P. The decrease in P concentrations of those fractions was caused by the uptake of P by plants rather than their transformations into more stable forms. P release rates diminished following the order: CaP > MAe > BSe > SPR, which indicates a decline in P availability from these P sources. Conclusions Phosphorus-rich biochar can be used as a slow-release fertiliser. It is necessary to determine available P (either soil or fertiliser tests) in biochars prior to its application to soil, so that dose, frequency and timing of application are correctly established.
Audience Academic
Author Camps-Arbestain, Marta
Hedley, Mike
Wang, Tao
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ISSN 0032-079X
1573-5036
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IsPeerReviewed true
IsScholarly true
Issue 1-2
Keywords Transformation
Bioavailability
Biochar
P fractionation
Carbonization
Fractionation
Phosphorus
Soil plant relation
Biological system
Language English
License http://www.springer.com/tdm
CC BY 4.0
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PublicationSubtitle An International Journal on Plant-Soil Relationships
PublicationTitle Plant and soil
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Publisher Springer-Verlag
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Snippet AIMS: The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biochar-amended sandy soil; (ii) the transformation of biochar...
Aims The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biocharamended sandy soil; (ii) the transformation of biochar P...
Aims The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biochar-amended sandy soil; (ii) the transformation of biochar...
The objectives were to investigate (i) the forms and release pattern of P from an ash-rich biochar-amended sandy soil; (ii) the transformation of biochar P in...
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StartPage 61
SubjectTerms Acid soils
Agricultural and Veterinary sciences
Agricultural Sciences
Agricultural soils
Agrology
Agronomy. Soil science and plant productions
Animal, plant and microbial ecology
Annan lantbruksvetenskap
application timing
Bioassays
Bioavailability
Biochar
Biological and medical sciences
Biomedical and Life Sciences
Biosolids
calcium
Cattle manure
Charcoal
Ecology
Environmental aspects
Fertilizers
Flowers & plants
Forest soils
Fractionation
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
Lantbruksvetenskap och veterinärmedicin
Life Sciences
Other Agricultural Sciences
Phosphorus
Phosphorus content
phosphorus fertilizers
Plant Physiology
Plant Sciences
Plant-soil relationships
Plants
Regular Article
rock phosphate
Sand soils
Sandy soils
slow-release fertilizers
Sodium hydroxide
Soil pollution
Soil research
Soil Science & Conservation
Soil treatment
Soil-plant relationships. Soil fertility
Soil-plant relationships. Soil fertility. Fertilization. Amendments
Soils
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Title fate of phosphorus of ash-rich biochars in a soil-plant system
URI https://www.jstor.org/stable/42952756
https://link.springer.com/article/10.1007/s11104-013-1938-z
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oai:portal.research.lu.se:publications/807570db-9c21-44b6-9c73-534fb9a13f93
Volume 375
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