Phase transitions and water dynamics of [Mn(H2O)(6)](ClO4)(2) studied by differential scanning calorimetry and neutron scattering methods

Citation
E. Mikuli et al., Phase transitions and water dynamics of [Mn(H2O)(6)](ClO4)(2) studied by differential scanning calorimetry and neutron scattering methods, Z NATURFO A, 55(9-10), 2000, pp. 759-764
Citations number
11
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
ZEITSCHRIFT FUR NATURFORSCHUNG SECTION A-A JOURNAL OF PHYSICAL SCIENCES
ISSN journal
09320784 → ACNP
Volume
55
Issue
9-10
Year of publication
2000
Pages
759 - 764
Database
ISI
SICI code
0932-0784(200009/10)55:9-10<759:PTAWDO>2.0.ZU;2-O
Abstract
DSC measurements performed at 95 - 290 K have shown that [Mn(H2O)6](ClO4)(2 ) possesses, besides a high-temperature phase, existing above 323 K, four l ow-temperature solid phases. The inelastic incoherent neutron scattering (I INS) spectra and neutron powder diffraction (NPD) patterns registered at 20 - 290 K have supported the DSC results and provided evidence that the inve stigated substance possesses even more than five solid phases. The IINS spe ctra have shown that in the room-temperature phase, water molecules perform fast stochastic reorientation at the picosecond scale. The orientational d isorder characteristic for the room-temperature phase can be easily overcoo led and frozen. Even by relatively slow cooling at ca. 40 K/hour a metastab le, orientational (protonic) glass phase is formed below ca. 160 K. Below c a. 100 K, a structural phase transition was observed by the NPD, however th e IINS spectra indicate existence of the pure ordered low-temperature phase only after annealing the sample for a few hours at 100 K. On heating, a st ructural phase transition takes place at ca. 120 K, and at ca. 225 K water molecules begin fast reorientation.