Salt particles play
important roles in many atmospheric processes
due to their high hygroscopicity. Saline lakes and playas are sources
of salt particles, which are normally mixed with mineral dust that
can be transported over long distances. In this study, salt samples
collected from four saline lakes and surrounding playas in the Qaidam
Basin are studied for their physicochemical properties, focusing on
the chemical compositions and hygroscopicity. The salt samples include
brines, lakebed salts, crust salts, and crystallized brines. Thermodynamic
models are used to explain the precipitating and hygroscopic behaviors
based on ionic compositions of dissolved saline solutions. Regarding
the ionic compositions, the crystallized brines are similar to the
complex mineral compositions of brines, while the natural solid salts,
including lakebed salts and crust salts, show very distinct composition
differences. The main difference between brines and natural solid
salts is the presence of Mg2+ and SO4
2–, which are primarily found in brines but not in the solid phases.
Moreover, all the crust salts are dominated by NaCl regardless of
the chemical compositions of the nearby saline lakes. Positive matrix
factorization is applied to the ionic concentrations, and the results
show that solid salts and brines are governed by different factors.
The pH of brines correlates with Mg2+ concentrations and
is potentially influenced by ambient CO2 uptake. The hygroscopicity
experimental results and thermodynamic model outcomes show that the
water uptake of different salt types is controlled by different salt
components, that is, crystallized brines are controlled by MgCl2 and natural salts are governed by NaCl and KCl. The characterizations
of saline lake and playa salts improve the understandings of the roles
that surface salts potentially play in the climate systems of both
Planet Earth and Mars.