Home > Research > Publications & Outputs > Phosphorus solubility changes following additio...

Electronic data

  • Ash and digestate_accepted_manuscript_PDF_29_Apr_2021

    Rights statement: This is the author’s version of a work that was accepted for publication in Geoderma. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Geoderma, 401, 2021 DOI: 10.1016/j.geoderma.2021.115150

    Accepted author manuscript, 586 KB, PDF document

    Available under license: CC BY-NC-ND: Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License

Links

Text available via DOI:

View graph of relations

Phosphorus solubility changes following additions of bioenergy wastes to an agricultural soil: implications for crop availability and environmental mobility  

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Published

Standard

Phosphorus solubility changes following additions of bioenergy wastes to an agricultural soil: implications for crop availability and environmental mobility  . / Richards, Samia; Marshall, Rachel; Lag Brotons, Alfonso et al.
In: Geoderma, Vol. 401, 115150, 01.11.2021.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

APA

Vancouver

Author

Bibtex

@article{e1dfe405f9164997bf75be6655658252,
title = "Phosphorus solubility changes following additions of bioenergy wastes to an agricultural soil: implications for crop availability and environmental mobility  ",
abstract = "Pathways for replacing chemical fertilisers (reliant on rock P resources) with alternative P-bearing materials require assessment of soil processes, crop nutrient acquisition and potential pollution consequences. We examined bioenergy waste materials, individually and as combined ash and anaerobic digestate in terms of plant P availability and mobility. We compared initial effects on mixing of amendments with a test soil and effects after 6-weeks pot trials, with and without wheat growth, against soil and chemical fertiliser controls. Chemical extractions, 31P NMR spectroscopic determination of P forms and phytase-labile P assays examined processes of P release. 31P NMR analysis revealed that ash comprised dominantly inorganic orthophosphate P with inherent low P solubility. Initial ash mixing with soils increased solution pH, soluble P in water (pure ash alone) and in citrate (ash alone and in blends). Digestate comprised a diverse array of orthophosphate and organically-complexed P forms, similar to the test soil P compositions, with limited P solubility on initial mixing. Following no plant incubations high water-soluble P with ash additions remained but all effects on citrate-soluble P were normalised. Incubations with plants increased water-soluble P in digestate only and blended amendment treatments relative to initial mixing. When comparing to chemical fertiliser the digestate plus ash blends led to smaller water-soluble P, but equal P in above-ground biomass after incubation. The ash-digestate C:N:P ratios and P form diversity appeared to promote microbial regulation of plant P availability versus potential leaching. The results suggest that the initial days-months are important periods for amendment interactions with soils during plant establishment and the lag before strong growth when system P mobility may induce polluted runoff. Biogeochemical P solubility controls require further study across differing soils and timescales to inform management of bioenergy wastes as fertilisers, particularly in terms of trade-offs such as crop nutrition versus system P losses.",
keywords = "Bioenergy waste, Soil P biogeochemistry, Anaerobic digestate, Ash",
author = "Samia Richards and Rachel Marshall and {Lag Brotons}, Alfonso and Kirk Semple and Marc Stutter",
note = "This is the author{\textquoteright}s version of a work that was accepted for publication in Geoderma. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Geoderma, 401, 2021 DOI: 10.1016/j.geoderma.2021.115150",
year = "2021",
month = nov,
day = "1",
doi = "10.1016/j.geoderma.2021.115150",
language = "English",
volume = "401",
journal = "Geoderma",
issn = "0016-7061",
publisher = "Elsevier Science B.V.",

}

RIS

TY - JOUR

T1 - Phosphorus solubility changes following additions of bioenergy wastes to an agricultural soil

T2 - implications for crop availability and environmental mobility  

AU - Richards, Samia

AU - Marshall, Rachel

AU - Lag Brotons, Alfonso

AU - Semple, Kirk

AU - Stutter, Marc

N1 - This is the author’s version of a work that was accepted for publication in Geoderma. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Geoderma, 401, 2021 DOI: 10.1016/j.geoderma.2021.115150

PY - 2021/11/1

Y1 - 2021/11/1

N2 - Pathways for replacing chemical fertilisers (reliant on rock P resources) with alternative P-bearing materials require assessment of soil processes, crop nutrient acquisition and potential pollution consequences. We examined bioenergy waste materials, individually and as combined ash and anaerobic digestate in terms of plant P availability and mobility. We compared initial effects on mixing of amendments with a test soil and effects after 6-weeks pot trials, with and without wheat growth, against soil and chemical fertiliser controls. Chemical extractions, 31P NMR spectroscopic determination of P forms and phytase-labile P assays examined processes of P release. 31P NMR analysis revealed that ash comprised dominantly inorganic orthophosphate P with inherent low P solubility. Initial ash mixing with soils increased solution pH, soluble P in water (pure ash alone) and in citrate (ash alone and in blends). Digestate comprised a diverse array of orthophosphate and organically-complexed P forms, similar to the test soil P compositions, with limited P solubility on initial mixing. Following no plant incubations high water-soluble P with ash additions remained but all effects on citrate-soluble P were normalised. Incubations with plants increased water-soluble P in digestate only and blended amendment treatments relative to initial mixing. When comparing to chemical fertiliser the digestate plus ash blends led to smaller water-soluble P, but equal P in above-ground biomass after incubation. The ash-digestate C:N:P ratios and P form diversity appeared to promote microbial regulation of plant P availability versus potential leaching. The results suggest that the initial days-months are important periods for amendment interactions with soils during plant establishment and the lag before strong growth when system P mobility may induce polluted runoff. Biogeochemical P solubility controls require further study across differing soils and timescales to inform management of bioenergy wastes as fertilisers, particularly in terms of trade-offs such as crop nutrition versus system P losses.

AB - Pathways for replacing chemical fertilisers (reliant on rock P resources) with alternative P-bearing materials require assessment of soil processes, crop nutrient acquisition and potential pollution consequences. We examined bioenergy waste materials, individually and as combined ash and anaerobic digestate in terms of plant P availability and mobility. We compared initial effects on mixing of amendments with a test soil and effects after 6-weeks pot trials, with and without wheat growth, against soil and chemical fertiliser controls. Chemical extractions, 31P NMR spectroscopic determination of P forms and phytase-labile P assays examined processes of P release. 31P NMR analysis revealed that ash comprised dominantly inorganic orthophosphate P with inherent low P solubility. Initial ash mixing with soils increased solution pH, soluble P in water (pure ash alone) and in citrate (ash alone and in blends). Digestate comprised a diverse array of orthophosphate and organically-complexed P forms, similar to the test soil P compositions, with limited P solubility on initial mixing. Following no plant incubations high water-soluble P with ash additions remained but all effects on citrate-soluble P were normalised. Incubations with plants increased water-soluble P in digestate only and blended amendment treatments relative to initial mixing. When comparing to chemical fertiliser the digestate plus ash blends led to smaller water-soluble P, but equal P in above-ground biomass after incubation. The ash-digestate C:N:P ratios and P form diversity appeared to promote microbial regulation of plant P availability versus potential leaching. The results suggest that the initial days-months are important periods for amendment interactions with soils during plant establishment and the lag before strong growth when system P mobility may induce polluted runoff. Biogeochemical P solubility controls require further study across differing soils and timescales to inform management of bioenergy wastes as fertilisers, particularly in terms of trade-offs such as crop nutrition versus system P losses.

KW - Bioenergy waste

KW - Soil P biogeochemistry

KW - Anaerobic digestate

KW - Ash

U2 - 10.1016/j.geoderma.2021.115150

DO - 10.1016/j.geoderma.2021.115150

M3 - Journal article

VL - 401

JO - Geoderma

JF - Geoderma

SN - 0016-7061

M1 - 115150

ER -