the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
28 Jan 2021
28 Jan 2021
Interactions of organosulfates with water vapor under sub- and supersaturated conditions
- 1State Key Laboratory of Organic Geochemistry, Guangdong Key Laboratory of Environmental Protection and Resources Utilization, and Guangdong-Hong Kong-Macao Joint Laboratory for Environmental Pollution and Control, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
- 2CAS Center for Excellence in Deep Earth Science, Guangzhou 510640, China
- 3Department of Chemistry and Biochemistry, College of Computer, Mathematical and Natural Sciences, University of Maryland, College Park, MD 20742, USA
- 4Department of Chemical and Biomolecular Engineering, A. James Clark School of Engineering, University of Maryland, College Park, MD 20742, USA
- 5State Key Laboratory for Structural Chemistry of Unstable and Stable Species, Beijing National Laboratory for Molecular Sciences, CAS Research/Education Center for Excellence in Molecular Sciences, Institute of Chemistry, Chinese Academy of Sciences, Beijing 100190, China
- 6Key Laboratory of Aerosol Chemistry and Physics, State Key Laboratory of Loess and Quaternary Geology, Institute of Earth and Environment, Chinese Academy of Sciences, Xi'an 710061, China
- 7University of Chinese Academy of Sciences, Beijing 100049, China
- 1State Key Laboratory of Organic Geochemistry, Guangdong Key Laboratory of Environmental Protection and Resources Utilization, and Guangdong-Hong Kong-Macao Joint Laboratory for Environmental Pollution and Control, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
- 2CAS Center for Excellence in Deep Earth Science, Guangzhou 510640, China
- 3Department of Chemistry and Biochemistry, College of Computer, Mathematical and Natural Sciences, University of Maryland, College Park, MD 20742, USA
- 4Department of Chemical and Biomolecular Engineering, A. James Clark School of Engineering, University of Maryland, College Park, MD 20742, USA
- 5State Key Laboratory for Structural Chemistry of Unstable and Stable Species, Beijing National Laboratory for Molecular Sciences, CAS Research/Education Center for Excellence in Molecular Sciences, Institute of Chemistry, Chinese Academy of Sciences, Beijing 100190, China
- 6Key Laboratory of Aerosol Chemistry and Physics, State Key Laboratory of Loess and Quaternary Geology, Institute of Earth and Environment, Chinese Academy of Sciences, Xi'an 710061, China
- 7University of Chinese Academy of Sciences, Beijing 100049, China
Abstract. Organosulfates (OS) are important constituents of secondary organic aerosols, but their hygroscopic properties and cloud condensation nucleation (CCN) activities have not been well understood. In this work we employed three complementary techniques to characterize interactions of several OS with water vapor under sub- and supersaturated conditions. A vapor sorption analyzer was used to measure mass changes of OS samples with RH (0–90 %); among the 11 organosulfates examined, only sodium methyl sulfate (methyl-OS), sodium ethyl sulfate (ethyl-OS), sodium octyl sulfate (octyl-OS) and potassium hydroxyacetone sulfate were found to deliquesce as RH increased, and their mass growth factors at 90 % RH were determined to be 3.652 ± 0.064, 3.575 ± 0.024, 1.591 ± 0.004 and 2.202 ± 0.031. Hygroscopic growth of methyl-, ethyl- and octyl-OS aerosols was also studied using a humidity tandem differential mobility analyzer (H-TDMA); continuous hygroscopic growth was observed, and their growth factors at 90 % RH were determined to be 1.83 ± 0.03, 1.79 ± 0.02 and 1.21 ± 0.02. We further investigated CCN activities of methyl-, ethyl- and octyl-OS aerosols, and their single hygroscopicity parameters (κccn) were determined to be 0.459 ± 0.021, 0.397 ± 0.010 and 0.206 ± 0.008. For methyl- and ethyl-OS aerosols, κccn values agree reasonably well with those derived from H-TDMA measurements (κgf), whereas κccn was found to be significantly larger than κgf for octyl-OS, likely due to both solubility limit and surface tension reduction.
- Preprint
(688 KB) -
Supplement
(110 KB) - BibTeX
- EndNote
Chao Peng et al.
Status: open (until 25 Mar 2021)
-
RC1: 'Comment on acp-2021-30', Anonymous Referee #1, 17 Feb 2021
reply
This work measures the hygroscopic properties and cloud condensation nucleation (CCN) activities of model organosulfate aerosols and allow us to better understand the environmental fates and impacts of these compounds. This work fits the scope of Atmospheric Chemistry and Physics. I have the following comments and suggestions for the authors' consideration.
Comments
Line 72, “As OS are ubiquitous and abundant in the troposphere, it is important to understand their hygroscopic properties and CCN activities in order to assess their environmental and climatic effects.” As mentioned by the authors, the atmospheric abundance of organosulfates investigated in this work is in order of ng/m3. Can the authors further elaborate or comment the atmospheric significances of these investigated organosulfates? For instance, how the presence of these organosulfates would affect the physiochemical properties of atmospheric aerosols such as surface tension, hygroscopicity and CCN studied in this work?
Line 127, “As shown in Figure 2, the mass of OS samples at different RH was determined by the VSA using the following method.” In figure 2, only the results of sodium methyl sulfate were shown. What would be the VSA results for other species?
Line 197, “the increase in sample mass at 50% and 60% RH may be because ethyl-OS were partially deliquesced at this stage.” What causes the ethyl-OS partially deliquesce? Why other OSs do not deliquesce partially?
Line 276, “Figure 4 shows that obvious deliquescence transitions were observed for methyl-, ethyl-, and octyl-OS in the VSA experiments; in contrast, as revealed by Figure 5, continuous hygroscopic growth without obvious phase transitions was observed for methyl-, ethyl- and octyl-OS aerosol particles in H-TDMA measurements, suggesting that these aerosol particles may exist in amorphous state.” Can the authors discuss why methyl OS, ethyl-OS and octyl OS exhibited different deliquescence behaviours in H-TDMA and VSA measurements?
Figure 6, at the same RH the GFs of methyl-, ethyl- and octyl-OS derived from VSA measurements were found to be consistently smaller than those measured using H-TDMA. Can the authors elaborate this observation?
Line 351, “Such underestimation at 70% and 75% RH is likely to due to that inorganic compounds (AS, in our work) may dissolve partially in the organics/water solution (which can be formed at much lower RH due to continuous water uptake of organics) before the mixed particle is completely deliquesced (Svenningsson et al., 2006; Zardini et al., 2008; Wu et al., 2011);” Can the authors comment if the amount of AS partially dissolved could be estimated based on their assumption and the hygroscopic data?
Line 392, “No significant difference was observed between κgf and κccn for five types of aerosol particles, and the relative differences between κccn and κgf values do not exceed 25%. However, octyl-OS appears to be an exception, and the average κccn value (0.206) was ~1.4 times larger than the average κgf value (0.086).” Given the differences between κgf and κccn were larger than the error bars (Figure 8), can the authors discuss why they would like to claim there is no significant difference between κgf and κccn.
Line 403, “Petters and Kreidenweis. (2008) demonstrated that cloud droplet activation was highly sensitive to the solubility for sparingly soluble compounds in the range of 5×10-4-2×10-1, expressed as volume of solute per unit volume of water (Petters and Kreidenweis, 2008). Compared to the highly soluble methyl- and ethyl-OS, the solubility of octyl-OS (8.43×10-4-4.26×10-2) (Chemistry Dashboard, 2021) is rather limited.” What are the estimated water solubility for methyl- OSand ethyl-OS? Are they highly soluble or sparingly soluble?
Line 408, “incomplete dissolution at subsaturated condition in H-TDMA measurements may lead to underestimation of κgf values for octyl-OS; as a result, the solubility limit may explain the observed difference between κgf and κccn for octyl-OS.” As mentioned by the authors, shall the authors estimate the κgf values for octyl-OS with solubility limit and surface tension correction?
Chao Peng et al.
Chao Peng et al.
Viewed
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 224 | 75 | 5 | 304 | 15 | 3 | 7 |
- HTML: 224
- PDF: 75
- XML: 5
- Total: 304
- Supplement: 15
- BibTeX: 3
- EndNote: 7
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1