The
low-pressure gas in the vacuum plume produced by the chemical
thrusters contaminates the spacecraft when adsorbed on the low-temperature
surface. To provide theoretical support for further research on gaseous
plume pollutants, the adsorption isotherms of low-pressure H
2
O were measured by a quartz crystal microbalance (QCM) at temperatures
ranging from 233 to 273 K. The measured isotherms are similar to the
type-I and type-II isotherms and have been correlated by various models
(e.g., the Langmuir, Dubinin–Radushkevich, Brunauer–Emmett–Teller
(BET), and universal models). It shows that the universal model has
a great advantage in predicting the adsorption at a specific temperature
point in our study. To estimate the adsorption at the continuous temperature
range, the critical parameters of the multi-Langmuir model were expressed
in semiempirical formulas. Since the normalized isotherms of H
2
O at different temperatures converge well, a simplified multi-Langmuir
(SML) model was proposed. The experimental results at the temperature
and pressure ranges we explored are consistent with the results predicted
by the SML model, suggesting that the SML model is more suitable and
convenient to predict the low-pressure adsorption of H
2
O for a continuous low-temperature range. Moreover, the low-pressure
adsorption behaviors of H
2
O and CO
2
on the low-temperature
surface are compared and discussed.