In situ measurements of volatile organic compounds in a boreal forest

We present biogenic VOC, including sesquiterpenes, measurements at the SMEAR II station (Station For Measuring Forest Ecosystem-Atmosphere Relations) in Finland using an in situ gas chromatograph mass-spectrometer with 2 h time resolution. The measurements were conducted over the period October 2010...

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Main Authors: H. Hakola, H. Hellén, M. Hemmilä, J. Rinne, M. Kulmala
Format: Article
Language:English
Published: Copernicus Publications 2012-12-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/12/11665/2012/acp-12-11665-2012.pdf
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spelling doaj-e553ea6e0d054873afab842ff61945052020-11-24T22:22:30ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242012-12-011223116651167810.5194/acp-12-11665-2012In situ measurements of volatile organic compounds in a boreal forestH. HakolaH. HellénM. HemmiläJ. RinneM. KulmalaWe present biogenic VOC, including sesquiterpenes, measurements at the SMEAR II station (Station For Measuring Forest Ecosystem-Atmosphere Relations) in Finland using an in situ gas chromatograph mass-spectrometer with 2 h time resolution. The measurements were conducted over the period October 2010–October 2011, at least one week every month. To our knowledge there are no earlier species-speciated semi-continuous BVOC data also covering dormant periods. This was also the first time sesquiterpene mixing ratios were measured in a boreal forest. <br><br> During the winter months, and still in March, the mixing ratios of all biogenic compounds were very low, most of the time below detection limits. The monoterpene mixing ratios increased in April and started to show diurnal variability, with maximum mixing ratio at night and minima during the day. The diurnal variability continued until October, after which the mixing ratios decreased and then only occasional episodes took place. The diurnal variation was affected by boundary layer height. Sesquiterpene mixing ratios were very low, only a few ppt. The main sesquiterpenes were longifolene and isolongifolene. The diurnal variation of isoprene was opposite to the mono- and sesquiterpene diurnal curve due to isoprene's light dependent emissions. Due to its daytime maximum mixing ratios, isoprene also dominated hydroxyl radical reactivity in summer even though our isoprene measurements are underestimates due to a breakthrough in a cold trap.http://www.atmos-chem-phys.net/12/11665/2012/acp-12-11665-2012.pdf
collection DOAJ
language English
format Article
sources DOAJ
author H. Hakola
H. Hellén
M. Hemmilä
J. Rinne
M. Kulmala
spellingShingle H. Hakola
H. Hellén
M. Hemmilä
J. Rinne
M. Kulmala
In situ measurements of volatile organic compounds in a boreal forest
Atmospheric Chemistry and Physics
author_facet H. Hakola
H. Hellén
M. Hemmilä
J. Rinne
M. Kulmala
author_sort H. Hakola
title In situ measurements of volatile organic compounds in a boreal forest
title_short In situ measurements of volatile organic compounds in a boreal forest
title_full In situ measurements of volatile organic compounds in a boreal forest
title_fullStr In situ measurements of volatile organic compounds in a boreal forest
title_full_unstemmed In situ measurements of volatile organic compounds in a boreal forest
title_sort in situ measurements of volatile organic compounds in a boreal forest
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2012-12-01
description We present biogenic VOC, including sesquiterpenes, measurements at the SMEAR II station (Station For Measuring Forest Ecosystem-Atmosphere Relations) in Finland using an in situ gas chromatograph mass-spectrometer with 2 h time resolution. The measurements were conducted over the period October 2010–October 2011, at least one week every month. To our knowledge there are no earlier species-speciated semi-continuous BVOC data also covering dormant periods. This was also the first time sesquiterpene mixing ratios were measured in a boreal forest. <br><br> During the winter months, and still in March, the mixing ratios of all biogenic compounds were very low, most of the time below detection limits. The monoterpene mixing ratios increased in April and started to show diurnal variability, with maximum mixing ratio at night and minima during the day. The diurnal variability continued until October, after which the mixing ratios decreased and then only occasional episodes took place. The diurnal variation was affected by boundary layer height. Sesquiterpene mixing ratios were very low, only a few ppt. The main sesquiterpenes were longifolene and isolongifolene. The diurnal variation of isoprene was opposite to the mono- and sesquiterpene diurnal curve due to isoprene's light dependent emissions. Due to its daytime maximum mixing ratios, isoprene also dominated hydroxyl radical reactivity in summer even though our isoprene measurements are underestimates due to a breakthrough in a cold trap.
url http://www.atmos-chem-phys.net/12/11665/2012/acp-12-11665-2012.pdf
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