TY - JOUR
T1 - A comprehensive variable temperature study of the layered oxide, Ca2Mn3O8
AU - Stimpson, Laura
AU - McNulty, Jason Allan
AU - Morrison, Finlay D.
AU - Mahjan, Amit
AU - McCabe, Emma
AU - Gibbs, Alexandra
AU - Stenning, Gavin
AU - Jura, Marek
AU - Arnold, Donna
N1 - The authors acknowledge the ISIS Neutron and Muon User Source for access to beamtime on HRPD (RB1520166 and RB1720182) [39,40]. We are also thankful for access to the instrumentation in the ISIS Materials Characterisation laboratory. We are grateful to Professor Mike Reece at Queen Mary University London for access to the spark plasma sintering (SPS) instrumentation and for assistance preparing pellets. LJV and JAM are grateful for the award of EPSRC DTA studentships.
PY - 2020/11/30
Y1 - 2020/11/30
N2 - Ca2Mn3O8 forms a delafossite-related layered structure, which crystallises with monoclinic C2/m symmetry. Compared with the delafossite-structure, the MnO6 layers in Ca2Mn3O8 exhibit an ordered cation void which forms a magnetic ‘bow-tie’ like connectivity of Mn4+ ion layers separated by Ca2+ ions. In-situ
variable temperature diffraction data demonstrates that the structure
is robust up to a temperature of approximately 1173 K before the
material decomposes into the perovskite, CaMnO3 and marokite, CaMn2O4
phases. Simultaneous thermal analysis suggests that a very small amount
of water remains within the layers post synthesis. Impedance
spectroscopy indicates that Ca2Mn3O8 is an electronic conductor in the range ∼400–700 K with an activation energy of 0.50 ± 0.01 eV.
AB - Ca2Mn3O8 forms a delafossite-related layered structure, which crystallises with monoclinic C2/m symmetry. Compared with the delafossite-structure, the MnO6 layers in Ca2Mn3O8 exhibit an ordered cation void which forms a magnetic ‘bow-tie’ like connectivity of Mn4+ ion layers separated by Ca2+ ions. In-situ
variable temperature diffraction data demonstrates that the structure
is robust up to a temperature of approximately 1173 K before the
material decomposes into the perovskite, CaMnO3 and marokite, CaMn2O4
phases. Simultaneous thermal analysis suggests that a very small amount
of water remains within the layers post synthesis. Impedance
spectroscopy indicates that Ca2Mn3O8 is an electronic conductor in the range ∼400–700 K with an activation energy of 0.50 ± 0.01 eV.
KW - Layered oxides
KW - Neutron diffraction
KW - Electronic measurements
UR - https://www.scopus.com/pages/publications/85087429146
U2 - 10.1016/j.jallcom.2020.155633
DO - 10.1016/j.jallcom.2020.155633
M3 - Article
SN - 0925-8388
VL - 843
JO - Journal of Alloys and Compounds
JF - Journal of Alloys and Compounds
M1 - 155633
ER -