Abstract. The oxidation of biogenic and anthropogenic compounds leads to the formation
of secondary organic aerosol mass (SOA). The present study aims to
investigate α-pinene, limonene, and m-cresol with regards to their SOA
formation potential dependent on relative humidity (RH) under night-
(NO3 radicals) and daytime conditions (OH radicals) and the resulting
chemical composition. It was found that SOA formation potential of limonene
with NO3 under dry conditions significantly exceeds that of the OH-radical reaction, with SOA yields of 15–30 % and 10–21 %,
respectively. Additionally, the nocturnal SOA yield was found to be very
sensitive towards RH, yielding more SOA under dry conditions. In contrast, the SOA formation potential of α-pinene with NO3
slightly exceeds that of the OH-radical reaction, independent from RH. On
average, α-pinene yielded SOA with about 6–7 % from NO3
radicals and 3–4 % from OH-radical reaction. Surprisingly, unexpectedly
high SOA yields were found for m-cresol oxidation with OH radicals (3–9 %), with the highest yield under elevated RH (9 %), which is most likely
attributable to a higher fraction of 3-methyl-6-nitro-catechol (MNC). While
α-pinene and m-cresol SOA was found to be mainly composed of
water-soluble compounds, 50–68 % of nocturnal SOA and 22–39 % of
daytime limonene SOA are water-insoluble. The fraction of SOA-bound peroxides
which originated from α-pinene varied between 2 and 80 % as a
function of RH. Furthermore, SOA from α-pinene revealed pinonic acid as the most
important particle-phase constituent under day- and nighttime conditions
with a fraction of 1–4 %. Other compounds detected are norpinonic acid
(0.05–1.1 % mass fraction), terpenylic acid (0.1–1.1 % mass
fraction), pinic acid (0.1–1.8 % mass fraction), and
3-methyl-1,2,3-tricarboxylic acid (0.05–0.5 % mass fraction). All
marker compounds showed higher fractions under dry conditions when formed
during daytime and showed almost no RH effect when formed during night.