Cargando…
Stoichiometric and Nonstoichiometric Hydrates of Brucine
[Image: see text] The complex interplay of temperature and water activity (a(w))/relative humidity (RH) on the solid form stability and transformation pathways of three hydrates (HyA, HyB, and HyC), an isostructural dehydrate (HyA(dehy)), an anhydrate (AH), and amorphous brucine has been elucidated...
Autores principales: | , |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
American Chemical
Society
2016
|
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5486439/ https://www.ncbi.nlm.nih.gov/pubmed/28670204 http://dx.doi.org/10.1021/acs.cgd.6b01231 |
Sumario: | [Image: see text] The complex interplay of temperature and water activity (a(w))/relative humidity (RH) on the solid form stability and transformation pathways of three hydrates (HyA, HyB, and HyC), an isostructural dehydrate (HyA(dehy)), an anhydrate (AH), and amorphous brucine has been elucidated and the transformation enthalpies quantified. The dihydrate (HyA) shows a nonstoichiometric (de)hydration behavior at RH < 40% at 25 °C, and the removal of the water molecules results in an isomorphic dehydrate structure. The metastable dehydration product converts to AH upon storage at the driest conditions or to HyA if exposed to moisture. HyB is a stoichiometric tetrahydrate. The loss of the water molecules causes HyB to collapse to an amorphous phase. Amorphous brucine transforms to AH at RH < 40% RH and a mixture of hydrated phases at higher RH values. The third hydrate (HyC) is only stable at RH ≥ 55% at 25 °C and contains 3.65–3.85 mol equiv of water. Dehydration of HyC occurs in one step at RH < 55% at 25 °C or upon heating, and AH is obtained. The AH is the thermodynamically most stable phase of brucine at RH < 40% at 25 °C. Depending on the conditions, temperature, and a(w), each of the three hydrates becomes the thermodynamically most stable form. This study demonstrates the importance of applying complementary analytical techniques and appropriate approaches for understanding the stability ranges and transition behavior between the solid forms of compounds with multiple hydrates. |
---|