TY - JOUR
T1 - Orbital ordering as the determinant for ferromagnetism in biferroic BiMnO3
AU - Moreira dos Santos, A.
AU - Cheetham, A. K.
AU - Atou, T.
AU - Syono, Y.
AU - Yamaguchi, Y.
AU - Ohoyama, K.
AU - Chiba, H.
AU - Rao, C. N.R.
PY - 2002/8/1
Y1 - 2002/8/1
N2 - The ferromagnetic structure of BiMnO3, Tc = 105 K, has been determined from powder neutron-diffraction data collected at 20 K on a sample synthesized at high pressures using a cubic anvil press. BiMnO3 is a distorted perovskite that crystallizes in the monoclinic space group C2 with unit-cell parameters a = 9.5317(7) Å, b = 5.6047(4) Å, c = 9.8492(7) Å, and β = 110.60(1)° (Rp = 6.78%, wRp = 8.53%, reduced X2 = 1.107). Data analysis reveals a collinear ferromagnetic structure with the spin direction along [010] and a magnetic moment of 3.2μB. There is no crystallographic phase transition on cooling the polar room-temperature structure to 20 K, lending support to the belief that ferromagnetism and ferroelectricity coexist in BiMnO3. Careful examination of the six unique Mn-O-Mn superexchange pathways between the three crystallographically independent Mn3+ sites shows that four are ferromagnetic and two are antiferromagnetic, thereby confirming that the ferromagnetism of BiMnO3 stems directly from orbital ordering.
AB - The ferromagnetic structure of BiMnO3, Tc = 105 K, has been determined from powder neutron-diffraction data collected at 20 K on a sample synthesized at high pressures using a cubic anvil press. BiMnO3 is a distorted perovskite that crystallizes in the monoclinic space group C2 with unit-cell parameters a = 9.5317(7) Å, b = 5.6047(4) Å, c = 9.8492(7) Å, and β = 110.60(1)° (Rp = 6.78%, wRp = 8.53%, reduced X2 = 1.107). Data analysis reveals a collinear ferromagnetic structure with the spin direction along [010] and a magnetic moment of 3.2μB. There is no crystallographic phase transition on cooling the polar room-temperature structure to 20 K, lending support to the belief that ferromagnetism and ferroelectricity coexist in BiMnO3. Careful examination of the six unique Mn-O-Mn superexchange pathways between the three crystallographically independent Mn3+ sites shows that four are ferromagnetic and two are antiferromagnetic, thereby confirming that the ferromagnetism of BiMnO3 stems directly from orbital ordering.
UR - http://www.scopus.com/inward/record.url?scp=0036696987&partnerID=8YFLogxK
U2 - 10.1103/PhysRevB.66.064425
DO - 10.1103/PhysRevB.66.064425
M3 - Article
AN - SCOPUS:0036696987
SN - 0163-1829
VL - 66
SP - 644251
EP - 644254
JO - Physical Review B - Condensed Matter and Materials Physics
JF - Physical Review B - Condensed Matter and Materials Physics
IS - 6
M1 - 064425
ER -