The iron chalcogenides FeSe and FeS are superconductors composed of
two-dimensional sheets held together by van der Waals interactions, which makes
them prime candidates for the intercalation of various guest species. We review
the intercalation chemistry of FeSe and FeS superconductors and discuss their
synthesis, structure, and physical properties. Before we review the latest work
in this area, we provide a brief background on the intercalation chemistry of
other inorganic materials that exhibit enhanced superconducting properties upon
intercalation, which include the transition metal dichalcogenides, fullerenes,
and layered cobalt oxides. From past studies of these intercalated
superconductors, we discuss the role of the intercalates in terms of charge
doping, structural distortions, and Fermi surface reconstruction. We also
briefly review the physical and chemical properties of the host
materials---mackinawite-type FeS and $\beta$-FeSe. The three types of
intercalates for the iron chalcogenides can be placed in three categories: 1.)
alkali and alkaline earth cations intercalated through the liquid ammonia
technique; 2.) cations intercalated with organic amines such as
ethylenediamine; and 3.) layered hydroxides intercalated during hydrothermal
conditions. A recurring theme in these studies is the role of the intercalated
guest in electron doping the chalcogenide host and in enhancing the
two-dimensionality of the electronic structure by spacing the FeSe layers
apart. We end this review discussing possible new avenues in the intercalation
chemistry of transition metal monochalcogenides, and the promise of these
materials as a unique set of new inorganic two-dimensional systems