The formation of crystals under physicochemical and flow
dynamic
conditions in constrained dimensions is ubiquitous in nature and of
great interest to different disciplines in science. In this report,
using a physicochemical approach, we investigated the spatiotemporal
precipitation of calcium oxalate (CaOx) crystals, the most common
chemical compound found in kidney stones, at the dynamic interface
generated by the interdiffusion of oxalate and calcium ions in a microchannel.
Spatiotemporal crystal habit distributions were mapped and analyzed
using scanning electron microscopy, and their formation was correlated
to a numerical model that accounts for supersaturation and gravity.
We show that while monohydrated CaOx crystals are the most frequent
with random distribution in the channel, the dihydrated CaOx phase
crystals are mainly formed at the contact line between oxalate and
calcium at the oxalate side, where gradients are large and supersaturation
is low. In addition, the size of the crystals correlates well with
the supersaturation with increasing monodispersity over time. These
results are supported by the numerical model. The simulations also
show that nucleation can occur everywhere in the channel; however,
with time, nucleation is limited to the upper level of the channel,
while crystals on the bottom continue to grow from the reactants.