- Volumes 84-95 (2024)
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Volumes 72-83 (2023)
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Volume 83
Pages 1-258 (December 2023)
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Volume 82
Pages 1-204 (November 2023)
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Volume 81
Pages 1-188 (October 2023)
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Volume 80
Pages 1-202 (September 2023)
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Volume 79
Pages 1-172 (August 2023)
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Volume 78
Pages 1-146 (July 2023)
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Volume 77
Pages 1-152 (June 2023)
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Volume 76
Pages 1-176 (May 2023)
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Volume 75
Pages 1-228 (April 2023)
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Volume 74
Pages 1-200 (March 2023)
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Volume 73
Pages 1-138 (February 2023)
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Volume 72
Pages 1-144 (January 2023)
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Volume 83
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Volumes 60-71 (2022)
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Volume 71
Pages 1-108 (December 2022)
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Volume 70
Pages 1-106 (November 2022)
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Volume 69
Pages 1-122 (October 2022)
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Volume 68
Pages 1-124 (September 2022)
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Volume 67
Pages 1-102 (August 2022)
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Volume 66
Pages 1-112 (July 2022)
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Volume 65
Pages 1-138 (June 2022)
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Volume 64
Pages 1-186 (May 2022)
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Volume 63
Pages 1-124 (April 2022)
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Volume 62
Pages 1-104 (March 2022)
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Volume 61
Pages 1-120 (February 2022)
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Volume 60
Pages 1-124 (January 2022)
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Volume 71
- Volumes 54-59 (2021)
- Volumes 48-53 (2020)
- Volumes 42-47 (2019)
- Volumes 36-41 (2018)
- Volumes 30-35 (2017)
- Volumes 24-29 (2016)
- Volumes 18-23 (2015)
- Volumes 12-17 (2014)
- Volume 11 (2013)
- Volume 10 (2012)
- Volume 9 (2011)
- Volume 8 (2010)
- Volume 7 (2009)
- Volume 6 (2008)
- Volume 5 (2007)
- Volume 4 (2006)
- Volume 3 (2005)
- Volume 2 (2004)
- Volume 1 (2003)
• HULIS-n is the main component in winter in contrast to HULIS-a in summer.
• Neutral HULIS plays a major role in light absorption of WSOC.
• Aromatic content has a crucial effect on light absorption of WSOC.
• Winter HULIS has higher molecular weight and light absorption than summer.
Humic-like substances (HULIS) are a major component of brown carbon and consequently play a major role in climate change. In this study, 70 PM2.5 samples were collected from Xi'an in winter 2019 and summer 2020. Neutral HULIS (HULIS-n), acidic HULIS (HULIS-a), and high-polarity water-soluble organic compounds (HP–WSOC) were analyzed to determine their carbon concentrations and measure their ultraviolet–visible absorption and infrared spectra. Of the three components, HULIS-n had the highest carbon content in both winter (3.29 ± 1.45 μg m−3) and in summer (1.38 ± 1.10 μg m−3). The semiquantitative results for the functional groups revealed that HP-WSOC was rich in carboxylic acids and had high aromaticity in winter, whereas HULIS-n was rich in carboxylic acids in summer. Moreover, HULIS-a was richer in nitrate esters and saturated aliphatic hydrocarbons in summer than in winter. The results for specific ultraviolet absorbance (SUVA) and E250/E365 revealed that HULIS had higher molecular weight and aromaticity in winter than in summer. HULIS-n dominated in the total light absorption of HULIS + HP-WSOC in both winter (73.08%) and summer (48.57%). Overall, the results on the carbon content, optical properties, and functional groups of WSOCs with differing polarity can improve understanding of environmental and climatic effects.