Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin
Lactic acid (LA) and glycolic acid (GA), which are low-molecular-weight hydroxyacids, were identified in the particle and gas phases within the marine atmospheric boundary layer over the western subarctic North Pacific. A major portion of LA (81%) and GA (57%) was present in the particulate phase, w...
Main Authors: | , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2014-08-01
|
Series: | Biogeosciences |
Online Access: | http://www.biogeosciences.net/11/4407/2014/bg-11-4407-2014.pdf |
id |
doaj-198d7e6aaa3b4072a3307cdde43c05e9 |
---|---|
record_format |
Article |
spelling |
doaj-198d7e6aaa3b4072a3307cdde43c05e92020-11-24T22:03:04ZengCopernicus PublicationsBiogeosciences1726-41701726-41892014-08-0111164407441410.5194/bg-11-4407-2014Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial originY. Miyazaki0M. Sawano1K. Kawamura2Institute of Low Temperature Science, Hokkaido University, Sapporo, JapanInstitute of Low Temperature Science, Hokkaido University, Sapporo, JapanInstitute of Low Temperature Science, Hokkaido University, Sapporo, JapanLactic acid (LA) and glycolic acid (GA), which are low-molecular-weight hydroxyacids, were identified in the particle and gas phases within the marine atmospheric boundary layer over the western subarctic North Pacific. A major portion of LA (81%) and GA (57%) was present in the particulate phase, which is consistent with the presence of a hydroxyl group in these molecules leading to the low volatility of the compounds. The average concentration (±SD) of LA in more biologically influenced marine aerosols (33 ± 58 ng m<sup>−3</sup>) was substantially higher than that in less biologically influenced aerosols (11 ± 12 ng m<sup>−3</sup>). Over the oceanic region of phytoplankton blooms, the concentration of aerosol LA was comparable to that of oxalic acid, which was the most abundant diacid during the study period. A positive correlation was found between the LA concentrations in more biologically influenced aerosols and chlorophyll <i>a</i> in seawater (<i>r</i><sup>2</sup> = 0.56), suggesting an important production of aerosol LA possibly associated with microbial (e.g., lactobacillus) activity in seawater and/or aerosols. Our finding provides a new insight into the poorly quantified microbial sources of marine organic aerosols (OAs) because such low-molecular-weight hydroxyacids are key intermediates for OA formation.http://www.biogeosciences.net/11/4407/2014/bg-11-4407-2014.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Y. Miyazaki M. Sawano K. Kawamura |
spellingShingle |
Y. Miyazaki M. Sawano K. Kawamura Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin Biogeosciences |
author_facet |
Y. Miyazaki M. Sawano K. Kawamura |
author_sort |
Y. Miyazaki |
title |
Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin |
title_short |
Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin |
title_full |
Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin |
title_fullStr |
Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin |
title_full_unstemmed |
Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin |
title_sort |
low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin |
publisher |
Copernicus Publications |
series |
Biogeosciences |
issn |
1726-4170 1726-4189 |
publishDate |
2014-08-01 |
description |
Lactic acid (LA) and glycolic acid (GA), which are low-molecular-weight
hydroxyacids, were identified in the particle and gas phases within the
marine atmospheric boundary layer over the western subarctic North Pacific.
A major portion of LA (81%) and GA (57%) was present in the particulate
phase, which is consistent with the presence of a hydroxyl group in these
molecules leading to the low volatility of the compounds. The average
concentration (±SD) of LA in more biologically influenced marine
aerosols (33 ± 58 ng m<sup>−3</sup>) was substantially higher than that in
less biologically influenced aerosols (11 ± 12 ng m<sup>−3</sup>). Over the
oceanic region of phytoplankton blooms, the concentration of aerosol LA was
comparable to that of oxalic acid, which was the most abundant diacid during
the study period. A positive correlation was found between the LA
concentrations in more biologically influenced aerosols and chlorophyll <i>a</i> in
seawater (<i>r</i><sup>2</sup> = 0.56), suggesting an important production of aerosol
LA possibly associated with microbial (e.g., lactobacillus) activity in
seawater and/or aerosols. Our finding provides a new insight into the poorly
quantified microbial sources of marine organic aerosols (OAs) because such
low-molecular-weight hydroxyacids are key intermediates for OA formation. |
url |
http://www.biogeosciences.net/11/4407/2014/bg-11-4407-2014.pdf |
work_keys_str_mv |
AT ymiyazaki lowmolecularweighthydroxyacidsinmarineatmosphericaerosolevidenceofamarinemicrobialorigin AT msawano lowmolecularweighthydroxyacidsinmarineatmosphericaerosolevidenceofamarinemicrobialorigin AT kkawamura lowmolecularweighthydroxyacidsinmarineatmosphericaerosolevidenceofamarinemicrobialorigin |
_version_ |
1725833337078022144 |