EGU25-18161, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-18161
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Monday, 28 Apr, 09:45–09:55 (CEST)
 
Room 0.11/12
Aerosol volatility over High-Altitude site in Western Ghats, India: Effect of semi-volatile organics coating
Subrata Mukherjee1, Rohit Dilip Patil1, Aslam Yusuf1, Ghuman Singh Meena1, Anil Kumar Vasudevan1, Anoop Sharad Mahajan1, Liselotte Tinel2, Vinayak Waghmare1, Sachin Suresh Patil1, and Pandithurai Govindan1
Subrata Mukherjee et al.
  • 1Indian Institute of Tropical M|eteorology, HACPL-PDTC, India (subrata.cat@tropmet.res.in)
  • 2IMT Nord Europe, Institut Mines-Télécom, University of Lille, Centre for Energy and Environment, F-59000, Lille, France

Sub-micron aerosols are primarily consisted of organics, sulfate, nitrate, ammonium etc. and among which organics have high complexity in its chemical and physical characteristics. In the present study, aerosol volatility of non-refractory sub-micron aerosol was extensively studied during 6th – 20th February of 2021 utilizing high-resolution Time of flight Aerosol Mass Spectrometer (HR-TOF AMS) coupled with Thermal denuder. The temperature was set to 150oC and the denuded and non-denuded ambient aerosol was then sampled utilizing a switching valve with 10 minute time interval. Nitrate and Ammonium possessed highest volatility (80% and 68%) which was followed by organics with volatility rate of 54%. Sulfate was observed to be the least volatile (26%).The volatility extent for organics was low in afternoon and night-early morning hours due to possible prevalence of oxygenated organic aerosols (secondary organic aerosol) during these time period. Further PMF was done on the denuded and non-denuded organics aerosol dataset and the analysis revealed 4 factors namely, Hydrocarbon like organic aerosol (HOA), Biomass burning organic aerosol (BBOA), semi-volatile oxygenated organic aerosol (SVOOA) and low-volatile oxygenated organic aerosol (LV-OOA). LV-OOA fractional contribution increased from 31% to 56% of total organics. SVOOA, HOA, BBOA being a primary aerosol, showed decreasing trend as they have higher volatility than LVOOA. Interestingly, of SV-OOA volatility was even higher than that of the other primary aerosols (HOA, BBOA). The possible reason may be SV-OOA is freshly formed and can be deposited on to pre-existing aerosols like inorganic aerosols, HOA, BBOA, LV-OOA etc which indicated the effect of possible coating.

How to cite: Mukherjee, S., Patil, R. D., Yusuf, A., Meena, G. S., Vasudevan, A. K., Mahajan, A. S., Tinel, L., Waghmare, V., Patil, S. S., and Govindan, P.: Aerosol volatility over High-Altitude site in Western Ghats, India: Effect of semi-volatile organics coating, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-18161, https://doi.org/10.5194/egusphere-egu25-18161, 2025.