Recycling of phosphorus from dredged lake sediment: Importance of iron-bound phosphates for plant growth

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Standard

Recycling of phosphorus from dredged lake sediment : Importance of iron-bound phosphates for plant growth. / Haasler, Sina; Kragh, Theis; Magid, Jakob; Gunnarsen, Klara Cecilia; Müller-Stöver, Dorette; Klamt, Anna Marie; Krogstrup, Kåre; Sorensen, Helle; Nielsen, Ulla Gro; Reitzel, Kasper.

I: Sustainable Environment, Bind 10, Nr. 1, 2362503, 2024.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Haasler, S, Kragh, T, Magid, J, Gunnarsen, KC, Müller-Stöver, D, Klamt, AM, Krogstrup, K, Sorensen, H, Nielsen, UG & Reitzel, K 2024, 'Recycling of phosphorus from dredged lake sediment: Importance of iron-bound phosphates for plant growth', Sustainable Environment, bind 10, nr. 1, 2362503. https://doi.org/10.1080/27658511.2024.2362503

APA

Haasler, S., Kragh, T., Magid, J., Gunnarsen, K. C., Müller-Stöver, D., Klamt, A. M., Krogstrup, K., Sorensen, H., Nielsen, U. G., & Reitzel, K. (2024). Recycling of phosphorus from dredged lake sediment: Importance of iron-bound phosphates for plant growth. Sustainable Environment, 10(1), [2362503]. https://doi.org/10.1080/27658511.2024.2362503

Vancouver

Haasler S, Kragh T, Magid J, Gunnarsen KC, Müller-Stöver D, Klamt AM o.a. Recycling of phosphorus from dredged lake sediment: Importance of iron-bound phosphates for plant growth. Sustainable Environment. 2024;10(1). 2362503. https://doi.org/10.1080/27658511.2024.2362503

Author

Haasler, Sina ; Kragh, Theis ; Magid, Jakob ; Gunnarsen, Klara Cecilia ; Müller-Stöver, Dorette ; Klamt, Anna Marie ; Krogstrup, Kåre ; Sorensen, Helle ; Nielsen, Ulla Gro ; Reitzel, Kasper. / Recycling of phosphorus from dredged lake sediment : Importance of iron-bound phosphates for plant growth. I: Sustainable Environment. 2024 ; Bind 10, Nr. 1.

Bibtex

@article{e382bf0206c448b5803ccafa9e25ec63,
title = "Recycling of phosphorus from dredged lake sediment: Importance of iron-bound phosphates for plant growth",
abstract = "Phosphorus (P) is critical for food production. However, it has been managed unsustainably for decades and geopolitical challenges complicate its availability. While accessible P-rock deposits are linearly exploited, excessive fertilization practices lead to P loss from land to water, and thus, eutrophication. The release of legacy P from sediments to the water column, i.e. internal P loading, sustains global eutrophication issues. Sediment removal and its subsequent reuse as soil amendment can simultaneously lower internal P loadings and create a new P resource. However, the plant bioavailability of sedimentary P, especially Fe-P, is rather controversial. In this study, the direct P fertilizer effect of fresh lake sediment, lake sediment after Fe-P removal, amorphous Fe-P, and the reduced Fe-P mineral vivianite on barley was investigated and compared to the conventional mineral P fertilizer triple superphosphate (TSP). Fresh sediment, amorphous Fe-P, and vivianite fertilization significantly increased biomass and P uptake compared to the 0-control, while the Fe-P removal from the sediment reduced both effects. The P use efficiency was generally lower than for TSP and decreased in the order amorphous Fe-P > fresh sediment > vivianite > sediment after Fe-P removal. In a parallel soil incubation without barley growth P diffusion from the tested alternative substrates was not observed. We conclude that fresh lake sediment has P fertilizer potential with amorphous Fe-P as a significant contributor. Further, fertilization with fresh sediment and Fe-P can increase soil adsorptive capacities potentially reducing leaching but also creating dependency of plant P bioavailability on plant-soil interactive mechanisms.",
keywords = "circularity, Fe phosphates, lake sediment, P bioavailability, P fertilizer, vivianite",
author = "Sina Haasler and Theis Kragh and Jakob Magid and Gunnarsen, {Klara Cecilia} and Dorette M{\"u}ller-St{\"o}ver and Klamt, {Anna Marie} and K{\aa}re Krogstrup and Helle Sorensen and Nielsen, {Ulla Gro} and Kasper Reitzel",
note = "Publisher Copyright: {\textcopyright} 2024 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group.",
year = "2024",
doi = "10.1080/27658511.2024.2362503",
language = "English",
volume = "10",
journal = "Sustainable Environment",
issn = "2765-8511",
publisher = "Taylor & Francis",
number = "1",

}

RIS

TY - JOUR

T1 - Recycling of phosphorus from dredged lake sediment

T2 - Importance of iron-bound phosphates for plant growth

AU - Haasler, Sina

AU - Kragh, Theis

AU - Magid, Jakob

AU - Gunnarsen, Klara Cecilia

AU - Müller-Stöver, Dorette

AU - Klamt, Anna Marie

AU - Krogstrup, Kåre

AU - Sorensen, Helle

AU - Nielsen, Ulla Gro

AU - Reitzel, Kasper

N1 - Publisher Copyright: © 2024 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group.

PY - 2024

Y1 - 2024

N2 - Phosphorus (P) is critical for food production. However, it has been managed unsustainably for decades and geopolitical challenges complicate its availability. While accessible P-rock deposits are linearly exploited, excessive fertilization practices lead to P loss from land to water, and thus, eutrophication. The release of legacy P from sediments to the water column, i.e. internal P loading, sustains global eutrophication issues. Sediment removal and its subsequent reuse as soil amendment can simultaneously lower internal P loadings and create a new P resource. However, the plant bioavailability of sedimentary P, especially Fe-P, is rather controversial. In this study, the direct P fertilizer effect of fresh lake sediment, lake sediment after Fe-P removal, amorphous Fe-P, and the reduced Fe-P mineral vivianite on barley was investigated and compared to the conventional mineral P fertilizer triple superphosphate (TSP). Fresh sediment, amorphous Fe-P, and vivianite fertilization significantly increased biomass and P uptake compared to the 0-control, while the Fe-P removal from the sediment reduced both effects. The P use efficiency was generally lower than for TSP and decreased in the order amorphous Fe-P > fresh sediment > vivianite > sediment after Fe-P removal. In a parallel soil incubation without barley growth P diffusion from the tested alternative substrates was not observed. We conclude that fresh lake sediment has P fertilizer potential with amorphous Fe-P as a significant contributor. Further, fertilization with fresh sediment and Fe-P can increase soil adsorptive capacities potentially reducing leaching but also creating dependency of plant P bioavailability on plant-soil interactive mechanisms.

AB - Phosphorus (P) is critical for food production. However, it has been managed unsustainably for decades and geopolitical challenges complicate its availability. While accessible P-rock deposits are linearly exploited, excessive fertilization practices lead to P loss from land to water, and thus, eutrophication. The release of legacy P from sediments to the water column, i.e. internal P loading, sustains global eutrophication issues. Sediment removal and its subsequent reuse as soil amendment can simultaneously lower internal P loadings and create a new P resource. However, the plant bioavailability of sedimentary P, especially Fe-P, is rather controversial. In this study, the direct P fertilizer effect of fresh lake sediment, lake sediment after Fe-P removal, amorphous Fe-P, and the reduced Fe-P mineral vivianite on barley was investigated and compared to the conventional mineral P fertilizer triple superphosphate (TSP). Fresh sediment, amorphous Fe-P, and vivianite fertilization significantly increased biomass and P uptake compared to the 0-control, while the Fe-P removal from the sediment reduced both effects. The P use efficiency was generally lower than for TSP and decreased in the order amorphous Fe-P > fresh sediment > vivianite > sediment after Fe-P removal. In a parallel soil incubation without barley growth P diffusion from the tested alternative substrates was not observed. We conclude that fresh lake sediment has P fertilizer potential with amorphous Fe-P as a significant contributor. Further, fertilization with fresh sediment and Fe-P can increase soil adsorptive capacities potentially reducing leaching but also creating dependency of plant P bioavailability on plant-soil interactive mechanisms.

KW - circularity

KW - Fe phosphates

KW - lake sediment

KW - P bioavailability

KW - P fertilizer

KW - vivianite

U2 - 10.1080/27658511.2024.2362503

DO - 10.1080/27658511.2024.2362503

M3 - Journal article

AN - SCOPUS:85195517537

VL - 10

JO - Sustainable Environment

JF - Sustainable Environment

SN - 2765-8511

IS - 1

M1 - 2362503

ER -

ID: 396637029