Hydration
forces play a crucial role in a wide range of phenomena
in physics, chemistry, and biology. Here, we study the hydration of
mica surfaces in contact with various alkali chloride solutions over
a wide range of concentrations and pH values. Using atomic force microscopy
and molecular dynamics simulations, we demonstrate that hydration
forces consist of a superposition of a monotonically decaying and
an oscillatory part, each with a unique dependence on the specific
type of cation. The monotonic hydration force gradually decreases
in strength with decreasing bulk hydration energy, leading to a transition
from an overall repulsive (Li+, Na+) to an attractive
(Rb+, Cs+) force. The oscillatory part, in contrast,
displays a binary character, being hardly affected by the presence
of strongly hydrated cations (Li+, Na+), but
it becomes completely suppressed in the presence of weakly hydrated
cations (Rb+, Cs+), in agreement with a less
pronounced water structure in simulations. For both aspects, K+ plays an intermediate role, and decreasing pH follows the
trend of increasing Rb+ and Cs+ concentrations.