The uptake of water
vapor by various organic aerosols is important
in a number of applications ranging from medical delivery of pharmaceutical
aerosols to cloud formation in the atmosphere. The coefficient that
describes the probability that the impinging gas-phase molecule sticks
to the surface of interest is called the mass accommodation coefficient,
αM. Despite the importance of this coefficient for
the description of water uptake kinetics, accurate values are still
lacking for many systems. In this Feature Article, we present various
experimental techniques that have been evoked in the literature to
study the interfacial transport of water and discuss the corresponding
strengths and limitations. This includes our recently developed technique
called photothermal single-particle spectroscopy (PSPS). The PSPS
technique allows for a retrieval of αM values from
three independent, yet simultaneous measurements operating close to
equilibrium, providing a robust assessment of interfacial mass transport.
We review the currently available data for αM for
water on various organics and discuss the few studies that address
the temperature and relative humidity dependence of αM for water on organics. The knowledge of the latter, for example,
is crucial to assess the water uptake kinetics of organic aerosols
in the Earth’s atmosphere. Finally, we argue that PSPS might
also be a viable method to better restrict the αM value for water on liquid water.