Hygroscopic properties and chemical
reactivity of secondary organic
aerosols (SOA) influence their overall contribution to the indirect
effect on the climate. In this study, we investigate the hygroscopic
properties of organic and organometallic polymeric particles, namely
polycatechol, polyguaiacol, Fe-polyfumarte, and Fe-polymuconate. These
particles efficiently form in iron-catalyzed reactions with aromatic
and aliphatic dicarboxylic acid compounds detected in field-collected
SOA. The structure of surface water was studied using diffuse reflectance
infrared Fourier transform spectroscopy (DRIFTS), and the uptake of
gas water was quantified using quartz crystal microbalance (QCM) as
a function of relative humidity. Spectroscopic data show that water
bonding with organic functional groups acting as hydrogen bond acceptors
causes shifts in their vibrational modes. Analysis of the hydroxyl
group stretching region revealed weak and strong hydrogen bonding
networks that suggest cluster formation reflecting water–water
and water–organics interactions, respectively. A modified Type
II multilayer Brunauer–Emmett–Teller adsorption model
described the adsorption isotherm on the nonporous materials, polycatechol,
polyguaiacol, and Fe-polymuconate. However, water adsorption on porous
Fe-polyfumarate was best described using a Type V adsorption model,
namely the Langmuir–Sips model that accounts for condensation
in pores. The data revealed that organometallic polymers are more
hygroscopic than organic polymers. The implications of these investigations
are discussed in the context of the chemical reactivity of these particles
relative to known SOA.