Dew water serves as a temporary reservoir
of dissolved organic
molecules that are released in the morning when the dew evaporates.
Many locations allow for direct sunlight on the dew water in the morning,
raising the possibility for photolysis-driven chemical reactions.
The majority of prior works looking at dew water chemical composition
has targeted freshly deposited dew on clean surfaces like Teflon.
However, the dissolved organic material in dew is a mixture of compounds
deposited during the night, as well as water-soluble compounds already
present on the surface. Here, we analyzed six separate dew or frost
water samples collected off grass and bush leaf surfaces in Southeast
Virginia in the fall of 2020 and found evidence for a water-soluble
surface grime layer that we term biogrime. The chemical composition
and photoactivity of the mixtures were probed using Fourier transform
ion cyclotron resonance mass spectrometry, offline-aerosol mass spectrometry,
and UV/vis spectroscopy. Complex organic mixtures were found in all
the samples with a total of ∼9600 identified molecular formulae
containing C, H, N, O, S, and P. Many samples had strong absorption
in the visible region, and all showed an initially rapid photodecay.
The composition varied between samples with possible sources including
plant guttation and microbial waste as well as deposition of atmospheric
organic aerosol particles, soil particles, and fog droplets. The composition
of organic molecules, combined with their photoactivity, suggests
that dew water may be a complex source for water-soluble gases as
it evaporates.