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...

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Published in:Biogeosciences
Main Authors: Miyazaki, Y., Sawano, M., Kawamura, K.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications
Subjects:
519
Online Access:http://hdl.handle.net/2115/56848
https://doi.org/10.5194/bg-11-4407-2014
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spelling fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/56848 2023-05-15T18:28:25+02:00 Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin Miyazaki, Y. Sawano, M. Kawamura, K. http://hdl.handle.net/2115/56848 https://doi.org/10.5194/bg-11-4407-2014 eng eng Copernicus Publications http://hdl.handle.net/2115/56848 Biogeosciences, 11(16): 4407-4414 http://dx.doi.org/10.5194/bg-11-4407-2014 http://creativecommons.org/licenses/by/3.0/ CC-BY 519 article fthokunivhus https://doi.org/10.5194/bg-11-4407-2014 2022-11-18T01:03:16Z 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−3) was substantially higher than that in less biologically influenced aerosols (11 ± 12 ng m−3). 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 a in seawater (r2 = 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. Article in Journal/Newspaper Subarctic Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Pacific Biogeosciences 11 16 4407 4414
institution Open Polar
collection Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP)
op_collection_id fthokunivhus
language English
topic 519
spellingShingle 519
Miyazaki, Y.
Sawano, M.
Kawamura, K.
Low-molecular-weight hydroxyacids in marine atmospheric aerosol: evidence of a marine microbial origin
topic_facet 519
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−3) was substantially higher than that in less biologically influenced aerosols (11 ± 12 ng m−3). 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 a in seawater (r2 = 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.
format Article in Journal/Newspaper
author Miyazaki, Y.
Sawano, M.
Kawamura, K.
author_facet Miyazaki, Y.
Sawano, M.
Kawamura, K.
author_sort Miyazaki, Y.
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
url http://hdl.handle.net/2115/56848
https://doi.org/10.5194/bg-11-4407-2014
geographic Pacific
geographic_facet Pacific
genre Subarctic
genre_facet Subarctic
op_relation http://hdl.handle.net/2115/56848
Biogeosciences, 11(16): 4407-4414
http://dx.doi.org/10.5194/bg-11-4407-2014
op_rights http://creativecommons.org/licenses/by/3.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.5194/bg-11-4407-2014
container_title Biogeosciences
container_volume 11
container_issue 16
container_start_page 4407
op_container_end_page 4414
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