The
calcium sulfate–water vapor system is of great scientific
and technological importance due to its applications in several fields
such as the construction materials industry, geology, and planetary
sciences. While much effort has been concentrated during the past
decades on characterizing the crystallographic structure of the different
calcium sulfate polymorphs, some questions concerning their thermodynamic
aspects as phase equilibria and their capability to increase their
overall water content continuously beyond structural water content
seem to have been left aside. Nevertheless, the comprehension of these
aspects is of the utmost importance if we want to understand this
chemical system fully. The present two-part work investigates these
phenomena experimentally and by a thermodynamic modeling approach.
In this first part, we develop a rigorous experimental protocol by
thermogravimetric analysis under controlled temperature and water
vapor partial pressure. We use this protocol to obtain thermodynamic
equilibrium values for the overall water content of calcium sulfate
hydrates. To ensure that the equilibrium was reached, we verified
that these values could be obtained by distinct thermodynamic paths.
With the equilibrium data, we were able to propose an updated equilibrium
curve between soluble anhydrite AIII-CaSO4 and CaSO4·0.5H2O and estimate the thermodynamic parameters
Δr
H° = (35.5 ± 1.0) kJ·mol–1 and Δr
S° =
(80.0 ± 2.8) J·mol–1·K–1. After that, we were able to quantify the extent of water adsorption
as a function of (T, P
H2O), and we observed that it could represent a significant
part of the overall water content of calcium sulfates.