Accelerated salt-induced
deterioration occurs by frequent changes
across the equilibrium relative humidity (RH
eq
). Therefore,
knowledge of the actual RH
eq
of a salt mixture has a major
impact on preventive conservation to ensure that the relative humidity
(RH) does not cause a salt-phase transition. In addition, knowledge
of the RH
eq
is essential in relation to in situ desalination
as the dissolution of salt is an essential criterion to enable transport
of salt (ions) in materials. For decades, it has been possible to
determine the RH
eq
in salt mixtures with thermodynamic-based
ECOS-Runsalt software. However, the ECOS-Runsalt model is challenged
by the influence of kinetics along with some limitations in regard
to possible ion types and combinations. A dynamic vapor sorption (DVS)
instrument is used for the direct measurement of RH
eq
and
to deduce knowledge on the physicochemical nonequilibrium process
related to the phase changes in salt mixtures. The experimentally
measured RH
eq
values in this study of NaCl–Na
2
SO
4
–NaNO
3
, NaNO
3
–Na
2
SO
4
, NaCl–NaNO
3
, NaCl–Na
2
SO
4
, and (NH
4
)
2
SO
4
–Na
2
SO
4
are in agreement with values
from the literature. A comparison with thermodynamically calculated
results makes it probable that the phase transition for some salts
is significantly influenced by nonequilibrium conditions. The present
work bridges some of the existing gaps in regard to improving the
accuracy of ECOS-Runsalt, including the effects of kinetics and the
possible ions and combinations that may be found in situ. The proposed
method makes it possible to determine a more representative RH
eq
in relation to real conditions for the improved treatment
of salt-infected constructs.