Soil uptake of VOCs exceeds production when VOCs are readily available

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Standard

Soil uptake of VOCs exceeds production when VOCs are readily available. / Jiao, Yi; Kramshøj, Magnus; Davie-Martin, Cleo L.; Albers, Christian Nyrop; Rinnan, Riikka.

I: Soil Biology and Biochemistry, Bind 185, 109153, 2023.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Jiao, Y, Kramshøj, M, Davie-Martin, CL, Albers, CN & Rinnan, R 2023, 'Soil uptake of VOCs exceeds production when VOCs are readily available', Soil Biology and Biochemistry, bind 185, 109153. https://doi.org/10.1016/j.soilbio.2023.109153

APA

Jiao, Y., Kramshøj, M., Davie-Martin, C. L., Albers, C. N., & Rinnan, R. (2023). Soil uptake of VOCs exceeds production when VOCs are readily available. Soil Biology and Biochemistry, 185, [109153]. https://doi.org/10.1016/j.soilbio.2023.109153

Vancouver

Jiao Y, Kramshøj M, Davie-Martin CL, Albers CN, Rinnan R. Soil uptake of VOCs exceeds production when VOCs are readily available. Soil Biology and Biochemistry. 2023;185. 109153. https://doi.org/10.1016/j.soilbio.2023.109153

Author

Jiao, Yi ; Kramshøj, Magnus ; Davie-Martin, Cleo L. ; Albers, Christian Nyrop ; Rinnan, Riikka. / Soil uptake of VOCs exceeds production when VOCs are readily available. I: Soil Biology and Biochemistry. 2023 ; Bind 185.

Bibtex

@article{e2ccfe127fd04069ba3dc38f2e9a0595,
title = "Soil uptake of VOCs exceeds production when VOCs are readily available",
abstract = "Volatile organic compounds (VOCs) are reactive gaseous compounds with significant impacts on air quality and the Earth's radiative balance. While natural ecosystems are known to be major sources of VOCs, primarily due to vegetation, soils, an important component of these ecosystems, have received relatively less attention as potential sources and sinks of VOCs. In this study, soil samples were collected from two temperate ecosystems: a beech forest and a heather heath, and then sieved, homogenized, and incubated under various controlled conditions such as different temperatures, oxic vs. anoxic conditions, and different ambient VOC levels. A dynamic flow-through system coupled to a proton transfer reaction-time of flight-mass spectrometry (PTR-ToF-MS) was used to measure production and/or uptake rates of selected VOCs, aiming to explore the processes and their controlling mechanisms. Our results showed that these soils were natural sources of a variety of VOCs, and the strength and profile of these emissions were influenced by soil properties (e.g. moisture, soil organic matter), oxic/anoxic conditions, and temperature. The soils also acted as sinks for most VOCs when VOC substrates at parts per billions levels (ranging between 0.18 and 68.65 ppb) were supplied to the headspace of the enclosed soils, and the size of the sink corresponded to the amount of VOCs available in the ambient air. Temperature-controlled incubations and glass bead simulations indicated that the uptake of VOCs by soils was likely driven by microbial metabolism, with a minor contribution from physical adsorption to soil particles. In conclusion, our study suggests that soil uptake of VOCs can mitigate the impact of other significant VOC sources in the near-surface environment and potentially regulate the net exchange of these trace gases in ecosystems.",
keywords = "Forest soil, Heath ecosystem, Production, Uptake, VOCs, Volatile organic compounds",
author = "Yi Jiao and Magnus Kramsh{\o}j and Davie-Martin, {Cleo L.} and Albers, {Christian Nyrop} and Riikka Rinnan",
note = "Publisher Copyright: {\textcopyright} 2023 The Authors",
year = "2023",
doi = "10.1016/j.soilbio.2023.109153",
language = "English",
volume = "185",
journal = "Soil Biology & Biochemistry",
issn = "0038-0717",
publisher = "Pergamon Press",

}

RIS

TY - JOUR

T1 - Soil uptake of VOCs exceeds production when VOCs are readily available

AU - Jiao, Yi

AU - Kramshøj, Magnus

AU - Davie-Martin, Cleo L.

AU - Albers, Christian Nyrop

AU - Rinnan, Riikka

N1 - Publisher Copyright: © 2023 The Authors

PY - 2023

Y1 - 2023

N2 - Volatile organic compounds (VOCs) are reactive gaseous compounds with significant impacts on air quality and the Earth's radiative balance. While natural ecosystems are known to be major sources of VOCs, primarily due to vegetation, soils, an important component of these ecosystems, have received relatively less attention as potential sources and sinks of VOCs. In this study, soil samples were collected from two temperate ecosystems: a beech forest and a heather heath, and then sieved, homogenized, and incubated under various controlled conditions such as different temperatures, oxic vs. anoxic conditions, and different ambient VOC levels. A dynamic flow-through system coupled to a proton transfer reaction-time of flight-mass spectrometry (PTR-ToF-MS) was used to measure production and/or uptake rates of selected VOCs, aiming to explore the processes and their controlling mechanisms. Our results showed that these soils were natural sources of a variety of VOCs, and the strength and profile of these emissions were influenced by soil properties (e.g. moisture, soil organic matter), oxic/anoxic conditions, and temperature. The soils also acted as sinks for most VOCs when VOC substrates at parts per billions levels (ranging between 0.18 and 68.65 ppb) were supplied to the headspace of the enclosed soils, and the size of the sink corresponded to the amount of VOCs available in the ambient air. Temperature-controlled incubations and glass bead simulations indicated that the uptake of VOCs by soils was likely driven by microbial metabolism, with a minor contribution from physical adsorption to soil particles. In conclusion, our study suggests that soil uptake of VOCs can mitigate the impact of other significant VOC sources in the near-surface environment and potentially regulate the net exchange of these trace gases in ecosystems.

AB - Volatile organic compounds (VOCs) are reactive gaseous compounds with significant impacts on air quality and the Earth's radiative balance. While natural ecosystems are known to be major sources of VOCs, primarily due to vegetation, soils, an important component of these ecosystems, have received relatively less attention as potential sources and sinks of VOCs. In this study, soil samples were collected from two temperate ecosystems: a beech forest and a heather heath, and then sieved, homogenized, and incubated under various controlled conditions such as different temperatures, oxic vs. anoxic conditions, and different ambient VOC levels. A dynamic flow-through system coupled to a proton transfer reaction-time of flight-mass spectrometry (PTR-ToF-MS) was used to measure production and/or uptake rates of selected VOCs, aiming to explore the processes and their controlling mechanisms. Our results showed that these soils were natural sources of a variety of VOCs, and the strength and profile of these emissions were influenced by soil properties (e.g. moisture, soil organic matter), oxic/anoxic conditions, and temperature. The soils also acted as sinks for most VOCs when VOC substrates at parts per billions levels (ranging between 0.18 and 68.65 ppb) were supplied to the headspace of the enclosed soils, and the size of the sink corresponded to the amount of VOCs available in the ambient air. Temperature-controlled incubations and glass bead simulations indicated that the uptake of VOCs by soils was likely driven by microbial metabolism, with a minor contribution from physical adsorption to soil particles. In conclusion, our study suggests that soil uptake of VOCs can mitigate the impact of other significant VOC sources in the near-surface environment and potentially regulate the net exchange of these trace gases in ecosystems.

KW - Forest soil

KW - Heath ecosystem

KW - Production

KW - Uptake

KW - VOCs

KW - Volatile organic compounds

U2 - 10.1016/j.soilbio.2023.109153

DO - 10.1016/j.soilbio.2023.109153

M3 - Journal article

AN - SCOPUS:85168427030

VL - 185

JO - Soil Biology & Biochemistry

JF - Soil Biology & Biochemistry

SN - 0038-0717

M1 - 109153

ER -

ID: 363510667