Abstract:[1] Humic-like substances (HULIS) in the atmosphere are ubiquitous macromolecular substances that comprise a major fraction of the organic component of atmospheric aerosols. In this study we report that HULIS extracted from collected wood burning and urban pollution atmospheric particles enhance aqueous phase oxidation of model organic contaminants (pyrene and phenol), by promoting the dark Fenton reaction under atmospherically relevant conditions. The paucity of radical sources at night makes this reaction, w… Show more
“…Because HULIS encompasses a complex and varying suite of molecules in different locations, it is difficult to predict the impact of HULIS photochemistry on Barrow snow grains. However, past work has identified a number of the (photo)chemical pathways involving HULIS in ice and surface waters, including water assisted cooperative sorption of organic compounds onto HULIS, changing their structure [ Taraniuk et al , 2009], contribution of atmospheric HULIS to (nighttime) oxidation of organic pollutants in cloud water via the dark (and photo‐) Fenton reaction [ Moonshine et al , 2008], oxidative photodegradation of HULIS and formation of aryl aldehydes [ Cowen and Al‐Abadleh , 2009], light‐induced ozone depletion by HULIS [ D ' Anna et al , 2009], and its possibly essential role in HONO production from photochemical reactions of NO 3 − in snowpacks [ Beine et al , 2008]. Finally, unknown chromophores (i.e., not NO 3 − , NO 2 − , H 2 O 2 , or HULIS) are responsible for approximately half of sunlight absorption by Barrow snows, implying that there is a significant amount of uncharacterized photochemistry that is occurring in these samples, with possible implications for snowpack cycling of carbon, nitrogen, halogens, and oxidants.…”
As part of the international multidisciplinary Ocean ‐ Atmosphere ‐ Sea Ice ‐ Snowpack (OASIS) program we analyzed more than 500 terrestrial (melted) snow samples near Barrow, AK between February and April 2009 for light absorption, as well as H2O2 and inorganic anion concentrations. For light absorption in the photochemically active region (300–450 nm) of surface snows, H2O2 and NO3− make minor contributions (combined < 9% typically), while HUmic LIke Substances (HULIS) and unknown chromophores each account for approximately half of the total absorption. We have identified four main sources for our residual chromophores (i.e., species other than H2O2 or NO3−): (1) vegetation and organic debris impact mostly the lowest 20 cm of the snowpack, (2) marine inputs, which are identified by high Cl− and SO42− contents, (3) deposition of diamond dust to surface snow, and (4) gas‐phase exchange between the atmosphere and surface snow layers. The snow surfaces, and accompanying chromophore concentrations, are strongly modulated by winds and snowfall at Barrow. However, even with these physical controls on light absorption, we see an overall decline of light absorption in near‐surface snow during the 7 weeks of our campaign, likely due to photo‐bleaching of chromophores. While HULIS and unknown chromophores dominate light absorption by soluble species in Barrow snow, we know little about the photochemistry of these species, and thus we as a community are probably overlooking many snowpack photochemical reactions.
“…Because HULIS encompasses a complex and varying suite of molecules in different locations, it is difficult to predict the impact of HULIS photochemistry on Barrow snow grains. However, past work has identified a number of the (photo)chemical pathways involving HULIS in ice and surface waters, including water assisted cooperative sorption of organic compounds onto HULIS, changing their structure [ Taraniuk et al , 2009], contribution of atmospheric HULIS to (nighttime) oxidation of organic pollutants in cloud water via the dark (and photo‐) Fenton reaction [ Moonshine et al , 2008], oxidative photodegradation of HULIS and formation of aryl aldehydes [ Cowen and Al‐Abadleh , 2009], light‐induced ozone depletion by HULIS [ D ' Anna et al , 2009], and its possibly essential role in HONO production from photochemical reactions of NO 3 − in snowpacks [ Beine et al , 2008]. Finally, unknown chromophores (i.e., not NO 3 − , NO 2 − , H 2 O 2 , or HULIS) are responsible for approximately half of sunlight absorption by Barrow snows, implying that there is a significant amount of uncharacterized photochemistry that is occurring in these samples, with possible implications for snowpack cycling of carbon, nitrogen, halogens, and oxidants.…”
As part of the international multidisciplinary Ocean ‐ Atmosphere ‐ Sea Ice ‐ Snowpack (OASIS) program we analyzed more than 500 terrestrial (melted) snow samples near Barrow, AK between February and April 2009 for light absorption, as well as H2O2 and inorganic anion concentrations. For light absorption in the photochemically active region (300–450 nm) of surface snows, H2O2 and NO3− make minor contributions (combined < 9% typically), while HUmic LIke Substances (HULIS) and unknown chromophores each account for approximately half of the total absorption. We have identified four main sources for our residual chromophores (i.e., species other than H2O2 or NO3−): (1) vegetation and organic debris impact mostly the lowest 20 cm of the snowpack, (2) marine inputs, which are identified by high Cl− and SO42− contents, (3) deposition of diamond dust to surface snow, and (4) gas‐phase exchange between the atmosphere and surface snow layers. The snow surfaces, and accompanying chromophore concentrations, are strongly modulated by winds and snowfall at Barrow. However, even with these physical controls on light absorption, we see an overall decline of light absorption in near‐surface snow during the 7 weeks of our campaign, likely due to photo‐bleaching of chromophores. While HULIS and unknown chromophores dominate light absorption by soluble species in Barrow snow, we know little about the photochemistry of these species, and thus we as a community are probably overlooking many snowpack photochemical reactions.
“…HULIS is characterized to contain a high density of quinoid units and carboxylate groups. As a result, HULIS may enhance the aqueous phase oxidation of organic pollutants in the atmosphere via its ability to promote the Fenton reaction (Moonshine, Rudich, Katsman, & Graber, 2008).…”
“…Laboratory studies have shown that HULIS can be important in Published by Copernicus Publications on behalf of the European Geosciences Union. P. Lin et al: Humic-like substances in fresh emissions of rice straw burning the troposphere in issues such as hygroscopic growth and cloud condensation nuclei formation of aerosols (Dinar et al, 2006;Gysel et al, 2004), light extinction (Hoffer et al, 2006;Lukacs et al, 2007), atmospheric chemistry processes such as aqueous-phase oxidation of organic pollutants (Moonshine et al, 2008) and ozone depletion on aerosol surfaces (D'Anna et al, 2009).…”
HUmic-LIke Substances (HULIS) are an abundant unresolved mixture of organic compounds present in atmospheric samples. Biomass burning (BB) has been recognized as an important primary source of HULIS, but measurements of HULIS in various fresh BB particles are lacking. In this work, HULIS in emissions of rice straw burning was measured in a number of field and chamber experiments. The average HULIS/OC ratio was 0.34±0.05 in μg/μgC, showing small variance among emissions under different burning conditions. The influence of BB on ambient HULIS levels was investigated by examining the spatial and temporal variation of HULIS and other aerosol constituents and interspecies relations in ambient PM<sub>2.5</sub>. The PM<sub>2.5</sub> samples were collected at an urban and a suburban location in the Pearl River Delta (PRD), China over a period of one year. The HULIS concentrations in the ambient PM<sub>2.5</sub> were significantly higher in air masses originating from regions influenced by BB. Significant correlations between HULIS and water-soluble K<sup>+</sup> concentrations at both sites further support that BB was an important source of HULIS. Ambient concentrations of HULIS also correlated well with those of sulfate, oxalate, and oxidant (the sum of O<sub>3</sub> and NO<sub>2</sub>). The HULIS/OC ratios in BB-influenced ambient aerosols (~0.6) were much higher than those in the fresh BB emissions (0.34), implying that secondary formation was also an important source of HULIS in the atmosphere. The annual average HULIS concentrations were 4.9 μg m<sup>−3</sup> at the urban site and 7.1 μg m<sup>−3</sup> at the suburban site while the annual average concentrations of elemental carbon were 3.3 μg m<sup>−3</sup> and 2.4 μg m<sup>−3</sup>, respectively. The urban-suburban spatial gradient of HULIS was opposite to that of elemental carbon, negating vehicular exhaust as a significant primary emission source of HULIS
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.