the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Size-resolved hygroscopicity and volatility properties of ambient urban aerosol particles measured by the VH-TDMA system in the autumn of 2023
Abstract. Hygroscopicity, volatility and the hygroscopicity of the non-volatile core of submicron aerosols with diameters of 50 nm, 80 nm, 110 nm and 150 nm were measured using a Volatility Hygroscopicity Tandem Differential Mobility Analyzer (VH-TDMA) system with a relative humidity of 90 % and a thermal denuder temperature of 270 °C from 11 October to 6 November 2023 in Beijing. The mean hygroscopic growth factor (HGF) for particles ranging from 50 nm to 150 nm was 1.15 ± 0.07, 1.24 ± 0.08, 1.30 ± 0.09, and 1.36 ± 0.10, respectively, while the mean volatile shrink factor (VSF) was 0.51 ± 0.05, 0.55 ± 0.04, 0.56 ± 0.05, and 0.56 ± 0.07, respectively. Both the HGF probability density function (HGF-PDF) and the VSF probability density function (VSF-PDF) for all particle sizes exhibited a pronounced bimodal distribution, indicating that the particles were primarily in an external mixing state. Hygroscopicity was observed to increase with particle size in both clean and pollution periods, while volatility decreased slightly with particle size during the clean period, without apparent trend during the pollution period. Additionally, a positive correlation was identified between hygroscopicity and volatility, as well as between the number fraction of nearly hydrophobic (NH) and non-volatile (NV) particles, which was higher correlation during the pollution period. Furthermore, this study measured the HGF of the non-volatile core (HGFcore) of submicron aerosols heated at 270 °C and derived the HGF of the volatile coating (HGFcoating). The mean HGFcoating for particles ranging from 50 nm to 150 nm particles was 1.17 ± 0.08, 1.27 ± 0.10, 1.35 ± 0.10 and 1.41 ± 0.10, respectively, which is 2 % to 7 % higher than the mean HGF for the same particle sizes. The mean HGFcore for particles ranging from 50 nm to 150 nm was 1.08 ± 0.03, 1.07 ± 0.03, 1.07 ± 0.03 and 1.09 ± 0.04, respectively. Notably, the HGFcore values were influenced by marine aerosols during air mass passages through and originating from the Bohai Sea.
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RC1: 'Comment on egusphere-2024-2232', Anonymous Referee #1, 16 Oct 2024
The manuscript is presents volatility and hygroscopicity data from urban ambient measurements in a clear manner and with good scientific quality. I would like to propose that this manuscript would be accepted with minor revisions. The first comment is related to the volatility measurement temperature that was chosen to be 300 Celsius. All the references given in the introduction are from measurements using 270 Celsius temperature. What lead to this decision? How to compare results with pre-existing data I there is a clear difference in the temperature used? Please add some text about this issue / decision. Second comment is about the experimental setup used: did you use PSM2.5 cut for the sampling, or a cyclone? A couple of typos or inaccurate phrases:
- First sentence: replace "aerosols" with ambient aerosol particles
- 3 Data analysis, first sentence: add "electrical" before "mobility"
- Page 14 row 332: "peaked" should be "peak" right?
Citation: https://doi.org/10.5194/egusphere-2024-2232-RC1 - RC2: 'Comment on egusphere-2024-2232', Anonymous Referee #2, 18 Oct 2024
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