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Physiological processes affecting methane transport by wetland vegetation - a review

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Physiological processes affecting methane transport by wetland vegetation - a review. / Vroom, RJE.; van den Berg, M.; Pangala, SR. et al.
In: Aquatic Botany, Vol. 182, 103547, 31.10.2022.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Vroom, RJE, van den Berg, M, Pangala, SR, van der Scheer, OE & Sorrell, BK 2022, 'Physiological processes affecting methane transport by wetland vegetation - a review', Aquatic Botany, vol. 182, 103547. https://doi.org/10.1016/j.aquabot.2022.103547

APA

Vroom, RJE., van den Berg, M., Pangala, SR., van der Scheer, OE., & Sorrell, BK. (2022). Physiological processes affecting methane transport by wetland vegetation - a review. Aquatic Botany, 182, Article 103547. https://doi.org/10.1016/j.aquabot.2022.103547

Vancouver

Vroom RJE, van den Berg M, Pangala SR, van der Scheer OE, Sorrell BK. Physiological processes affecting methane transport by wetland vegetation - a review. Aquatic Botany. 2022 Oct 31;182:103547. Epub 2022 Jul 21. doi: 10.1016/j.aquabot.2022.103547

Author

Vroom, RJE. ; van den Berg, M. ; Pangala, SR. et al. / Physiological processes affecting methane transport by wetland vegetation - a review. In: Aquatic Botany. 2022 ; Vol. 182.

Bibtex

@article{35b9dd989fe04e049e15c81901d61297,
title = "Physiological processes affecting methane transport by wetland vegetation - a review",
abstract = "Wetland plants transport oxygen to belowground tissues to survive in anoxic sediments, and simultaneously conduct methane (CH4) from the sediment to the atmosphere. Although plant-mediated transport is the main CH4 emission pathway in vegetated wetlands, the contribution of vegetated areas to total emissions in wetlands remains uncertain. To accurately quantify these emissions, understanding the physiological processes driving plant-mediated CH4 transport is crucial. This review describes the state of the art understanding of CH4 transport through trees, emergent, floating-leaved, and submerged freshwater macrophytes. Gas transport mechanisms in plants include diffusion, pressurized flow, and transpiration-driven flow. Pressurized flow in the gas-filled aerenchyma leads to higher gas transport rates than diffusion, and mostly occurs in plants standing in deeper water. Transpiration-driven flow occurs in the xylem tissue of trees, whereby dissolved CH4 is transported by sap flow. Pressurized flow and transpiration-driven flow both result in diel cycles in CH4 emission, with higher emissions during the day than at night. The total CH4 emission through a wetland plant depends on its growth stage, transport mechanisms and the balance between sediment and in-plant CH4 production and oxidation. Although plants contribute substantially to total CH4 emissions, soil carbon content, soil temperature, nutrient availability, and water depth are often stronger driving factors than plant species. Nevertheless, accurate quantification of emissions from vegetated wetlands requires standardization of measurement protocols which capture diurnal and seasonal variation in emissions. Knowledge on CH4 transport through trees and submersed and free-floating macrophytes is scarce and warrants further research.",
keywords = "Macrophytes, Methanogenesis, Methane oxidation, Plant-mediated fluxes, Greenhouse gases, Tree-mediated CH4 emissions",
author = "RJE. Vroom and {van den Berg}, M. and SR. Pangala and {van der Scheer}, OE. and BK. Sorrell",
year = "2022",
month = oct,
day = "31",
doi = "10.1016/j.aquabot.2022.103547",
language = "English",
volume = "182",
journal = "Aquatic Botany",
issn = "0304-3770",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Physiological processes affecting methane transport by wetland vegetation - a review

AU - Vroom, RJE.

AU - van den Berg, M.

AU - Pangala, SR.

AU - van der Scheer, OE.

AU - Sorrell, BK.

PY - 2022/10/31

Y1 - 2022/10/31

N2 - Wetland plants transport oxygen to belowground tissues to survive in anoxic sediments, and simultaneously conduct methane (CH4) from the sediment to the atmosphere. Although plant-mediated transport is the main CH4 emission pathway in vegetated wetlands, the contribution of vegetated areas to total emissions in wetlands remains uncertain. To accurately quantify these emissions, understanding the physiological processes driving plant-mediated CH4 transport is crucial. This review describes the state of the art understanding of CH4 transport through trees, emergent, floating-leaved, and submerged freshwater macrophytes. Gas transport mechanisms in plants include diffusion, pressurized flow, and transpiration-driven flow. Pressurized flow in the gas-filled aerenchyma leads to higher gas transport rates than diffusion, and mostly occurs in plants standing in deeper water. Transpiration-driven flow occurs in the xylem tissue of trees, whereby dissolved CH4 is transported by sap flow. Pressurized flow and transpiration-driven flow both result in diel cycles in CH4 emission, with higher emissions during the day than at night. The total CH4 emission through a wetland plant depends on its growth stage, transport mechanisms and the balance between sediment and in-plant CH4 production and oxidation. Although plants contribute substantially to total CH4 emissions, soil carbon content, soil temperature, nutrient availability, and water depth are often stronger driving factors than plant species. Nevertheless, accurate quantification of emissions from vegetated wetlands requires standardization of measurement protocols which capture diurnal and seasonal variation in emissions. Knowledge on CH4 transport through trees and submersed and free-floating macrophytes is scarce and warrants further research.

AB - Wetland plants transport oxygen to belowground tissues to survive in anoxic sediments, and simultaneously conduct methane (CH4) from the sediment to the atmosphere. Although plant-mediated transport is the main CH4 emission pathway in vegetated wetlands, the contribution of vegetated areas to total emissions in wetlands remains uncertain. To accurately quantify these emissions, understanding the physiological processes driving plant-mediated CH4 transport is crucial. This review describes the state of the art understanding of CH4 transport through trees, emergent, floating-leaved, and submerged freshwater macrophytes. Gas transport mechanisms in plants include diffusion, pressurized flow, and transpiration-driven flow. Pressurized flow in the gas-filled aerenchyma leads to higher gas transport rates than diffusion, and mostly occurs in plants standing in deeper water. Transpiration-driven flow occurs in the xylem tissue of trees, whereby dissolved CH4 is transported by sap flow. Pressurized flow and transpiration-driven flow both result in diel cycles in CH4 emission, with higher emissions during the day than at night. The total CH4 emission through a wetland plant depends on its growth stage, transport mechanisms and the balance between sediment and in-plant CH4 production and oxidation. Although plants contribute substantially to total CH4 emissions, soil carbon content, soil temperature, nutrient availability, and water depth are often stronger driving factors than plant species. Nevertheless, accurate quantification of emissions from vegetated wetlands requires standardization of measurement protocols which capture diurnal and seasonal variation in emissions. Knowledge on CH4 transport through trees and submersed and free-floating macrophytes is scarce and warrants further research.

KW - Macrophytes

KW - Methanogenesis

KW - Methane oxidation

KW - Plant-mediated fluxes

KW - Greenhouse gases

KW - Tree-mediated CH4 emissions

U2 - 10.1016/j.aquabot.2022.103547

DO - 10.1016/j.aquabot.2022.103547

M3 - Journal article

VL - 182

JO - Aquatic Botany

JF - Aquatic Botany

SN - 0304-3770

M1 - 103547

ER -