Urea is a critical nitrogen carrier molecule that is
abundant in
the environment due to its anthropogenic activity to enhance crop
growth. The intrinsic link between its high solubility and volatilization,
resulting in the reactive nitrogen species and CO2, especially
under excessive relative humidity (RH) conditions, suggests that the
urea hydrolysis-initiated decomposition reaction can be affecting
the global nitrogen balance. Fundamental analysis of water as RH adsorption
on urea particle surfaces was performed using a combination of dynamic
vapor sorption (DVS) experiments, in situ single-particle Raman spectroscopy,
and ab initio calculations. The DVS data acquired exhibited three
RH adsorption regimes with urea with 74% RH dramatically changing
adsorbate–urea interactions from monolayer- to multilayer-induced
deliquescence. Several empirical kinetic models were utilized to understand
the RH interaction with urea surfaces, and the Guggenheim–Anderson–de
Boer model provided a good description of the adsorption at <60%
RH values, while a Van Campen model was used to fit the data acquired
during the urea crystal deliquescence. The experimental water sorption
rate using the Van Campen model showed a gradual rise from 0.02 mg/min
at 80% to 0.08 mg/min at 95% in agreement with Van Campen’s
model of increasing trend, albeit at higher rates ranging from 0.03
mg/min at 80% to 0.1 mg/min at 95%. In situ Raman spectroscopy combined
with optical images of a single particle showed that the urea 1009
cm–1 peak full width at half-maximum can provide
in-depth information on the transient phenomena taking place on the
urea particle surface as well as in the partially liquefied environment.
Finally, density functional theory results suggested that Wulff’s
reconstruction of a single urea crystal depended on the presence of
higher crystalline planes; particularly, the (111) facet became significant
together with (101) and (110), while in the presence of bulk H2O, (101) became the dominant facet. The results presented
in this work will allow for a better understanding of urea–water
vapor interactions in the environment at the molecular level including
its potential for aerosol formation in the regions of high agricultural
activity. Further, this study will allow us to better understand urea
partitioning into soil pore volume where high RH is prevalent. Finally,
it will provide a microscopic, single-particle understanding of the
urea transformations in moist environments and pave the way for a
new, nitrogen-efficient material fertilizer design.