Adsorption isotherms on Na-SSZ-13,
a small-pore zeolite, for pure-component
adsorbates CO2, H2O, and C6H14 were measured using a gravimetric adsorption instrument
with a temperature range between 30 and 100 °C. These isotherm
data were fit to a multisite Langmuir adsorption model. Using the
same gravimetric adsorption instrument, binary adsorption isotherms
for the adsorbate pairs CO2–H2O and CO2–C6H14 were measured with a temperature
range between 30 and 80 °C. These data demonstrated that the
increasing loading of either H2O or C6H14 impacted the loading of CO2 on Na-SSZ-13. The
binary isotherm data were compared with ideal adsorbed solution theory
and showed relatively good agreement between the data and modeling.