Metastable ionic cubic structure I clathrate hydrate formed with tetra-n-butylammonium bromide in the course of rapid cooling (30 K min−1) to −35 °C have been examined. An earlier unknown
metastable hydrate
Организация организации как условие метастабильности симбиоза организации и деятельностиOrganizational theory is currently in the
phase of active development. Taking a step from
Low-temperature dehydration of gypsum single crystals removal of water molecules occurs through the formation of an anhydrous
metastable phase. This phenomenon
Намагниченность пирротина состава Fe0.847S
в районе точки Кюри,
these pyrrhotites are in a
metastable phase condition and in due course (samples were observed
during 29 years
Structural transformations in the system of gypsum-anhydrite during sequential annealing up to 1000 ° c, this structural motif is retained in all
metastable mineral
phases with slight distortions in size and shape