Thermo-osmosis refers
to fluid migration due to the temperature
gradient. The mechanistic understanding of thermo-osmosis in charged
nano-porous media is still incomplete, while it is important for several
environmental and energy applications, such as low-grade waste heat
recovery, wastewater recovery, fuel cells, and nuclear waste storage.
This paper presents results from a series of molecular dynamics simulations
of thermo-osmosis in charged silica nanochannels that advance the
understanding of the phenomenon. Simulations with pure water and water
with dissolved NaCl are considered. First, the effect of surface charge
on the sign and magnitude of the thermo-osmotic coefficient is quantified.
This effect was found to be mainly linked to the structural modifications
of an aqueous electrical double layer (EDL) caused by the nanoconfinement
and surface charges. In addition, the results illustrate that the
surface charges reduce the self-diffusivity and thermo-osmosis of
interfacial liquid. The thermo-osmosis was found to change direction
when the surface charge density exceeds −0.03C · m–2. It was found that the thermo-osmotic flow and self-diffusivity
increase with the concentration of NaCl. The fluxes of solvent and
solute are decoupled by considering the Ludwig–Soret effect
of NaCl ions to identify the main mechanisms controlling the behavior.
In addition to the advance in microscopic quantification and mechanistic
understanding of thermo-osmosis, the work provides approaches to investigate
a broader category of coupled heat and mass transfer problems in nanoscale
space.