Commercial
samples of strychnine sulfate were used as the starting
material in crystallization experiments accompanied by stability studies.
Eight hydrate forms (
HyA
–
HyG
), including
five novel hydrates, were verified. The crystal structures of
HyA
(“pentahydrate”) and
HyF
(“hexahydrate”)
were determined from single-crystal X-ray diffraction data.
HyF
was identified as the most stable hydrate at high water
activities at room temperature (RT), and
HyA
and
HyC
were also found to be stable at ambient conditions. Long-time
storage experiments over nearly two decades confirm that these three
hydrates are stable at ambient conditions (20–60% relative
humidity). The other five hydrates,
HyB
(“dihydrate”),
HyD
,
HyE
,
HyG
, and
HyH
, are only observable at the low(est) relative humidity (RH) levels
at RT. Some of these latter forms can only exist within a very narrow
RH range and are therefore intermediate phases. By applying a range
of complementary experimental techniques such as gravimetric moisture
sorption analysis, thermal analysis, moisture controlled PXRD measurements,
and variable temperature IR spectroscopy in combination with principal
component analysis, it was possible to identify the distinct hydrate
phases and elucidate their stability and dehydration pathways. The
observed (de)hydration routes,
HyA
↔
HyB
,
HyC
↔
HyD
↔
HyE
,
HyF
↔
HyG
↔
HyH
and
HyF
→
HyA
↔
HyB
, depended on the initial hydrate form, particle size, and atmospheric
conditions. In addition, a transformation from
HyC
/
HyA
to
HyF
occurs at high RH values at RT. The
specific moisture and temperature conditions of none of the applied
drying regimes yielded a crystalline water-free form, which highlights
the essential role of water molecules for the formation and stability
of the crystalline strychnine sulfate phases.