Molecular composition of dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls and fatty acids in atmospheric aerosols from Tanzania, East Africa during wet and dry seasons

Atmospheric aerosol samples of PM<sub>2.5</sub> and PM<sub>10</sub> were collected during the wet and dry seasons in 2011 from a rural site in Tanzania and analysed for water-soluble dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls, and...

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Main Authors: S. L. Mkoma, K. Kawamura
Format: Article
Language:English
Published: Copernicus Publications 2013-02-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/2235/2013/acp-13-2235-2013.pdf
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author S. L. Mkoma
K. Kawamura
author_facet S. L. Mkoma
K. Kawamura
author_sort S. L. Mkoma
collection DOAJ
description Atmospheric aerosol samples of PM<sub>2.5</sub> and PM<sub>10</sub> were collected during the wet and dry seasons in 2011 from a rural site in Tanzania and analysed for water-soluble dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls, and fatty acids using a gas chromatography/flame ionization detector (GC/FID) and GC/mass spectrometry. Here we report the molecular composition and sources of diacids and related compounds for wet and dry seasons. Oxalic acid (C<sub>2</sub>) was found as the most abundant diacid species followed by succinic and/or malonic acids whereas glyoxylic acid and glyoxal were the dominant ketoacid and α-dicarbonyl, respectively in both seasons in PM<sub>2.5</sub> and PM<sub>10</sub>. Mean concentration of C<sub>2</sub> in PM<sub>2.5</sub> (121 ± 47 ng m<sup>−3</sup>) was lower in wet season than dry season (258 ± 69 ng m<sup>−3</sup>). Similarly, PM<sub>10</sub> samples showed lower concentration of C<sub>2</sub> (169 ± 42 ng m<sup>−3</sup>) in wet season than dry season (292 ± 165 ng m<sup>−3</sup>). Relative abundances of C<sub>2</sub> in total diacids were 65% and 67% in PM<sub>2.5</sub> and 65% and 64% in PM<sub>10</sub> in the wet and dry seasons, respectively. Total concentrations of diacids (289–362 ng m<sup>−3</sup>), ketoacids (37.8–53.7 ng m<sup>−3</sup>), and α-dicarbonyls (5.7–7.8 ng m<sup>−3</sup>) in Tanzania are higher than those reported at a rural background site in Nylsvley (South Africa) but comparable or lower than those reported from sites in Asia and Europe. Diacids and ketoacids were found to be present mainly in PM<sub>2.5</sub> in both seasons (total α-dicarbonyls in the dry season), suggesting a production of organic acids from pyrogenic sources and photochemical oxidations. Averaged contributions of total diacids to aerosol total carbon were 1.4% in PM<sub>2.5</sub> and 2.1% in PM<sub>10</sub> during wet season and 3.3% in PM<sub>2.5</sub> and 3.9% in PM<sub>10</sub> during dry season whereas those to water-soluble organic carbon were 2.2% and 4.7% in PM<sub>2.5</sub> during wet season and 3.1% and 5.8% in PM<sub>10</sub> during dry season. The higher ratios in dry season suggest an enhanced photochemical oxidation of organic precursors probably via heterogeneous reactions on aerosols under strong solar radiation. Strong positive correlations were found among diacids and related compounds as well as good relations to source tracers in both seasons, suggesting a mixed source from natural biogenic emissions, biomass burning, biofuel combustion, and photochemical production.
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spelling doaj.art-ea61b69fd29940c0b51434a287ea5ad52022-12-22T03:43:36ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-02-011342235225110.5194/acp-13-2235-2013Molecular composition of dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls and fatty acids in atmospheric aerosols from Tanzania, East Africa during wet and dry seasonsS. L. MkomaK. KawamuraAtmospheric aerosol samples of PM<sub>2.5</sub> and PM<sub>10</sub> were collected during the wet and dry seasons in 2011 from a rural site in Tanzania and analysed for water-soluble dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls, and fatty acids using a gas chromatography/flame ionization detector (GC/FID) and GC/mass spectrometry. Here we report the molecular composition and sources of diacids and related compounds for wet and dry seasons. Oxalic acid (C<sub>2</sub>) was found as the most abundant diacid species followed by succinic and/or malonic acids whereas glyoxylic acid and glyoxal were the dominant ketoacid and α-dicarbonyl, respectively in both seasons in PM<sub>2.5</sub> and PM<sub>10</sub>. Mean concentration of C<sub>2</sub> in PM<sub>2.5</sub> (121 ± 47 ng m<sup>−3</sup>) was lower in wet season than dry season (258 ± 69 ng m<sup>−3</sup>). Similarly, PM<sub>10</sub> samples showed lower concentration of C<sub>2</sub> (169 ± 42 ng m<sup>−3</sup>) in wet season than dry season (292 ± 165 ng m<sup>−3</sup>). Relative abundances of C<sub>2</sub> in total diacids were 65% and 67% in PM<sub>2.5</sub> and 65% and 64% in PM<sub>10</sub> in the wet and dry seasons, respectively. Total concentrations of diacids (289–362 ng m<sup>−3</sup>), ketoacids (37.8–53.7 ng m<sup>−3</sup>), and α-dicarbonyls (5.7–7.8 ng m<sup>−3</sup>) in Tanzania are higher than those reported at a rural background site in Nylsvley (South Africa) but comparable or lower than those reported from sites in Asia and Europe. Diacids and ketoacids were found to be present mainly in PM<sub>2.5</sub> in both seasons (total α-dicarbonyls in the dry season), suggesting a production of organic acids from pyrogenic sources and photochemical oxidations. Averaged contributions of total diacids to aerosol total carbon were 1.4% in PM<sub>2.5</sub> and 2.1% in PM<sub>10</sub> during wet season and 3.3% in PM<sub>2.5</sub> and 3.9% in PM<sub>10</sub> during dry season whereas those to water-soluble organic carbon were 2.2% and 4.7% in PM<sub>2.5</sub> during wet season and 3.1% and 5.8% in PM<sub>10</sub> during dry season. The higher ratios in dry season suggest an enhanced photochemical oxidation of organic precursors probably via heterogeneous reactions on aerosols under strong solar radiation. Strong positive correlations were found among diacids and related compounds as well as good relations to source tracers in both seasons, suggesting a mixed source from natural biogenic emissions, biomass burning, biofuel combustion, and photochemical production.http://www.atmos-chem-phys.net/13/2235/2013/acp-13-2235-2013.pdf
spellingShingle S. L. Mkoma
K. Kawamura
Molecular composition of dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls and fatty acids in atmospheric aerosols from Tanzania, East Africa during wet and dry seasons
Atmospheric Chemistry and Physics
title Molecular composition of dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls and fatty acids in atmospheric aerosols from Tanzania, East Africa during wet and dry seasons
title_full Molecular composition of dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls and fatty acids in atmospheric aerosols from Tanzania, East Africa during wet and dry seasons
title_fullStr Molecular composition of dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls and fatty acids in atmospheric aerosols from Tanzania, East Africa during wet and dry seasons
title_full_unstemmed Molecular composition of dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls and fatty acids in atmospheric aerosols from Tanzania, East Africa during wet and dry seasons
title_short Molecular composition of dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls and fatty acids in atmospheric aerosols from Tanzania, East Africa during wet and dry seasons
title_sort molecular composition of dicarboxylic acids ketocarboxylic acids α dicarbonyls and fatty acids in atmospheric aerosols from tanzania east africa during wet and dry seasons
url http://www.atmos-chem-phys.net/13/2235/2013/acp-13-2235-2013.pdf
work_keys_str_mv AT slmkoma molecularcompositionofdicarboxylicacidsketocarboxylicacidsadicarbonylsandfattyacidsinatmosphericaerosolsfromtanzaniaeastafricaduringwetanddryseasons
AT kkawamura molecularcompositionofdicarboxylicacidsketocarboxylicacidsadicarbonylsandfattyacidsinatmosphericaerosolsfromtanzaniaeastafricaduringwetanddryseasons