Temperate food forest soil and dead organic matter carbon content relative to adjacent land

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Standard

Temperate food forest soil and dead organic matter carbon content relative to adjacent land. / Hald, Lisa Mølgaard; Schafer, Luke J.

I: Agrosystems, Geosciences & Environment, Bind 6, Nr. 4, e20433, 2023.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Hald, LM & Schafer, LJ 2023, 'Temperate food forest soil and dead organic matter carbon content relative to adjacent land', Agrosystems, Geosciences & Environment, bind 6, nr. 4, e20433. https://doi.org/10.1002/agg2.20433

APA

Hald, L. M., & Schafer, L. J. (2023). Temperate food forest soil and dead organic matter carbon content relative to adjacent land. Agrosystems, Geosciences & Environment, 6(4), [e20433]. https://doi.org/10.1002/agg2.20433

Vancouver

Hald LM, Schafer LJ. Temperate food forest soil and dead organic matter carbon content relative to adjacent land. Agrosystems, Geosciences & Environment. 2023;6(4). e20433. https://doi.org/10.1002/agg2.20433

Author

Hald, Lisa Mølgaard ; Schafer, Luke J. / Temperate food forest soil and dead organic matter carbon content relative to adjacent land. I: Agrosystems, Geosciences & Environment. 2023 ; Bind 6, Nr. 4.

Bibtex

@article{9c7788c6f2ca4e14a678b815707852a4,
title = "Temperate food forest soil and dead organic matter carbon content relative to adjacent land",
abstract = "Soil is identified as the terrestrial carbon (C) pool with the highest potential for C sequestration. This study therefore examined the soil organic carbon (SOC) under four different but adjacent land-use systems in the temperate climate zone: a food forest, redwood forest, pasture land and agricultural field in Dartington, UK. Soil samples were collected at 0- to 20-cm and 20- to 40-cm depth at all four sites. Two soil fractionation methodologies were applied as well as analysis for C content. Additionally, carbon content from dead organic matter (DOM) was estimated from the woody and non-woody litter in the food forest and redwood forest. Similar total SOC was found between all four systems. However, due to the difference in turnover rates of C in different soil fractions, the food forest soil exhibited a similar long-term storage of C as the redwood forest, while pasture land and agricultural field stored less C in the long term. The redwood forest exhibited a higher non-woody litter C content than the food forest, but similar amounts of coarse and fine woody litter.",
author = "Hald, {Lisa M{\o}lgaard} and Schafer, {Luke J.}",
year = "2023",
doi = "10.1002/agg2.20433",
language = "English",
volume = "6",
journal = "Agrosystems, Geosciences & Environment",
issn = "2639-6696",
publisher = "Wiley",
number = "4",

}

RIS

TY - JOUR

T1 - Temperate food forest soil and dead organic matter carbon content relative to adjacent land

AU - Hald, Lisa Mølgaard

AU - Schafer, Luke J.

PY - 2023

Y1 - 2023

N2 - Soil is identified as the terrestrial carbon (C) pool with the highest potential for C sequestration. This study therefore examined the soil organic carbon (SOC) under four different but adjacent land-use systems in the temperate climate zone: a food forest, redwood forest, pasture land and agricultural field in Dartington, UK. Soil samples were collected at 0- to 20-cm and 20- to 40-cm depth at all four sites. Two soil fractionation methodologies were applied as well as analysis for C content. Additionally, carbon content from dead organic matter (DOM) was estimated from the woody and non-woody litter in the food forest and redwood forest. Similar total SOC was found between all four systems. However, due to the difference in turnover rates of C in different soil fractions, the food forest soil exhibited a similar long-term storage of C as the redwood forest, while pasture land and agricultural field stored less C in the long term. The redwood forest exhibited a higher non-woody litter C content than the food forest, but similar amounts of coarse and fine woody litter.

AB - Soil is identified as the terrestrial carbon (C) pool with the highest potential for C sequestration. This study therefore examined the soil organic carbon (SOC) under four different but adjacent land-use systems in the temperate climate zone: a food forest, redwood forest, pasture land and agricultural field in Dartington, UK. Soil samples were collected at 0- to 20-cm and 20- to 40-cm depth at all four sites. Two soil fractionation methodologies were applied as well as analysis for C content. Additionally, carbon content from dead organic matter (DOM) was estimated from the woody and non-woody litter in the food forest and redwood forest. Similar total SOC was found between all four systems. However, due to the difference in turnover rates of C in different soil fractions, the food forest soil exhibited a similar long-term storage of C as the redwood forest, while pasture land and agricultural field stored less C in the long term. The redwood forest exhibited a higher non-woody litter C content than the food forest, but similar amounts of coarse and fine woody litter.

U2 - 10.1002/agg2.20433

DO - 10.1002/agg2.20433

M3 - Journal article

VL - 6

JO - Agrosystems, Geosciences & Environment

JF - Agrosystems, Geosciences & Environment

SN - 2639-6696

IS - 4

M1 - e20433

ER -

ID: 369468290