The aerosol mass
spectrometer (AMS) has significantly expanded
our understanding of aerosol chemical composition over the past few
decades. However, most studies have made limited use of the high molecular
weight (HMW) signals in the mass spectra due to their low intensities
and multiple overlapping peaks. Using long time-of-flight (LTOF) AMS
measurements at a boreal forest site in Finland, we utilize the high
resolution of the LTOF and the newly developed binPMF approach to
explore the potential of the HMW range to improve source identification.
During our measurements, inorganics (primarily sulfate) contributed
∼30% and oxygenated organic aerosol (OOA) contributed ∼60%
to aerosol mass. The remaining ∼10% were attributed to specific
organic aerosol types: hydrocarbon-like OA (HOA) ∼3%, biomass
burning OA (BBOA) ∼0.06%, and a pollution plume from the Kola
Peninsula ∼5%. None of these factors were separated using traditional
unit-mass resolution PMF (m/z 12–150
Th). The small BBOA factor was only extracted using binPMF on the
100–225 amu m/z range, and
using this BBOA temporal profile, we could constrain the BBOA factor
for the lower masses, revealing a prominent signal at m/z 60 (a tracer for levoglucosan). We encourage
AMS users to experiment with the presented approach with their own
datasets