Environmental controls over methanol emission from leaves

Methanol is found throughout the troposphere, with average concentrations second only to methane among atmospheric hydrocarbons. Proposed global methanol budgets are highly uncertain, but all agree that at least 60% of the total source arises from the terrestrial biosphere and primary emissions from...

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Main Authors: P. Harley, J. Greenberg, Ü. Niinemets, A. Guenther
Format: Article
Language:English
Published: Copernicus Publications 2007-12-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/4/1083/2007/bg-4-1083-2007.pdf
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spelling doaj-8b70d5d1228644e7989acda77cfc073b2020-11-25T01:50:27ZengCopernicus PublicationsBiogeosciences1726-41701726-41892007-12-014610831099Environmental controls over methanol emission from leavesP. HarleyJ. GreenbergÜ. NiinemetsA. GuentherMethanol is found throughout the troposphere, with average concentrations second only to methane among atmospheric hydrocarbons. Proposed global methanol budgets are highly uncertain, but all agree that at least 60% of the total source arises from the terrestrial biosphere and primary emissions from plants. However, the magnitude of these emissions is also highly uncertain, and the environmental factors which control them require further elucidation. <br><br> Using a temperature-controlled leaf enclosure, we measured methanol emissions from leaves of six plant species by proton transfer reaction mass spectrometry, with simultaneous measurements of leaf evapotranspiration and stomatal conductance. Rates of emission at 30°C varied from 0.2 to 38 μg g (dry mass)<sup>−1</sup> h<sup>−1</sup>, with higher rates measured on young leaves, consistent with the production of methanol via pectin demethylation in expanding foliage. On average, emissions increased by a factor of 2.3 for each 10°C increase in leaf temperature. At constant temperature, emissions were also correlated with co-varying incident photosynthetic photon flux density and rates of stomatal conductance. The data were analyzed using the emission model developed by Niinemets and Reichstein (2003a, b), with the incorporation of a methanol production term that increased exponentially with temperature. It was concluded that control of emissions, during daytime, was shared by leaf temperature and stomatal conductance, although rates of production may also vary diurnally in response to variations in leaf growth rate in expanding leaves. The model, which generally provided reasonable simulations of the measured data during the day, significantly overestimated emissions on two sets of measurements made through the night, suggesting that production rates of methanol were reduced at night, perhaps because leaf growth was reduced or possibly through a direct effect of light on production. Although the short-term dynamics of methanol emissions can be successfully modeled only if stomatal conductance and compound solubility are taken into account, emissions on longer time scales will be determined by rates of methanol production, controls over which remain to be investigated. http://www.biogeosciences.net/4/1083/2007/bg-4-1083-2007.pdf
collection DOAJ
language English
format Article
sources DOAJ
author P. Harley
J. Greenberg
Ü. Niinemets
A. Guenther
spellingShingle P. Harley
J. Greenberg
Ü. Niinemets
A. Guenther
Environmental controls over methanol emission from leaves
Biogeosciences
author_facet P. Harley
J. Greenberg
Ü. Niinemets
A. Guenther
author_sort P. Harley
title Environmental controls over methanol emission from leaves
title_short Environmental controls over methanol emission from leaves
title_full Environmental controls over methanol emission from leaves
title_fullStr Environmental controls over methanol emission from leaves
title_full_unstemmed Environmental controls over methanol emission from leaves
title_sort environmental controls over methanol emission from leaves
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2007-12-01
description Methanol is found throughout the troposphere, with average concentrations second only to methane among atmospheric hydrocarbons. Proposed global methanol budgets are highly uncertain, but all agree that at least 60% of the total source arises from the terrestrial biosphere and primary emissions from plants. However, the magnitude of these emissions is also highly uncertain, and the environmental factors which control them require further elucidation. <br><br> Using a temperature-controlled leaf enclosure, we measured methanol emissions from leaves of six plant species by proton transfer reaction mass spectrometry, with simultaneous measurements of leaf evapotranspiration and stomatal conductance. Rates of emission at 30°C varied from 0.2 to 38 μg g (dry mass)<sup>−1</sup> h<sup>−1</sup>, with higher rates measured on young leaves, consistent with the production of methanol via pectin demethylation in expanding foliage. On average, emissions increased by a factor of 2.3 for each 10°C increase in leaf temperature. At constant temperature, emissions were also correlated with co-varying incident photosynthetic photon flux density and rates of stomatal conductance. The data were analyzed using the emission model developed by Niinemets and Reichstein (2003a, b), with the incorporation of a methanol production term that increased exponentially with temperature. It was concluded that control of emissions, during daytime, was shared by leaf temperature and stomatal conductance, although rates of production may also vary diurnally in response to variations in leaf growth rate in expanding leaves. The model, which generally provided reasonable simulations of the measured data during the day, significantly overestimated emissions on two sets of measurements made through the night, suggesting that production rates of methanol were reduced at night, perhaps because leaf growth was reduced or possibly through a direct effect of light on production. Although the short-term dynamics of methanol emissions can be successfully modeled only if stomatal conductance and compound solubility are taken into account, emissions on longer time scales will be determined by rates of methanol production, controls over which remain to be investigated.
url http://www.biogeosciences.net/4/1083/2007/bg-4-1083-2007.pdf
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