1,918
Views
29
CrossRef citations to date
0
Altmetric
Original Articles

Effects of temperature on the formation of secondary organic aerosol from amine precursors

, , , &
Pages 1216-1226 | Received 27 Feb 2016, Accepted 06 Sep 2016, Published online: 03 Oct 2016

Figures & data

Table 1. Environmental chamber experiments.

Figure 1. Mass concentration profiles (10 min averages) for the trimethylamine ( - circle), diethylamine ( - square), and butylamine (Δ - triangle) oxidation experiments (CHC = cold-hot-cold, HCH = hot-cold-hot).

Figure 1. Mass concentration profiles (10 min averages) for the trimethylamine ( - circle), diethylamine ( - square), and butylamine (Δ - triangle) oxidation experiments (CHC = cold-hot-cold, HCH = hot-cold-hot).

Table 2. Average density, volatility, and elemental ratio (HR-ToF-AMS) values at 10°C and 40°C for each of the amine oxidation experiments.

Figure 2. Correlation plots of the organic mass spectra (cold [initial] vs. hot, normalized to total mass) from the cold start (a) TMA + OH, (b) TMA + NO3, (c) DEA + OH, (d) DEA + NO3, (e) BA + OH, and (f) BA + NO3 oxidation experiments. The dashed lines indicate the 1:1 ratio.

Figure 2. Correlation plots of the organic mass spectra (cold [initial] vs. hot, normalized to total mass) from the cold start (a) TMA + OH, (b) TMA + NO3, (c) DEA + OH, (d) DEA + NO3, (e) BA + OH, and (f) BA + NO3 oxidation experiments. The dashed lines indicate the 1:1 ratio.

Figure 3. Time profiles for m/z 122 (unit mass resolution) and fragment ion C3H8NO4+ (high resolution) in the cold start (top) and hot start (bottom) trimethylamine with OH oxidation experiments.

Figure 3. Time profiles for m/z 122 (unit mass resolution) and fragment ion C3H8NO4+ (high resolution) in the cold start (top) and hot start (bottom) trimethylamine with OH oxidation experiments.

Figure 4. Proposed mechanism for the formation of temperature dependent aerosol with ion fragments at m/z 76 and m/z 122 observed by the HR-ToF-AMS (rH = hydrogen rearrangement).

Figure 4. Proposed mechanism for the formation of temperature dependent aerosol with ion fragments at m/z 76 and m/z 122 observed by the HR-ToF-AMS (rH = hydrogen rearrangement).
Supplemental material

UAST_1236182_Supplemental_File.zip

Download Zip (357 KB)

Reprints and Corporate Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

To request a reprint or corporate permissions for this article, please click on the relevant link below:

Academic Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

Obtain permissions instantly via Rightslink by clicking on the button below:

If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.