Low-temperature Mössbauer study of heterosite, (Fe, Mn)PO4.
The heterosite phase occurring in a pegmatitic rock sample was characterized by X-ray diffraction, by energy-dispersive X-ray spectroscopy and by Mössbauer spectroscopy. The orthorhombic unit-cell parameters, expressed in Å, were found as a=9.733 (1), b=5.837 (1) and c=4.776 (1). The composition was determined to be (Fe(0.54)Mn(0.43)Mg(0.04))PO(4). Mössbauer spectra recorded at temperatures T of 65 K and higher consist of two broadened quadrupole doublets. Their isomer shifts δ are both diagnostic for the ferric state. The dominant doublet (~60% of total area) exhibits an average quadrupole splitting ΔE(Q,av) of 1.62 mm/s at room temperature, while the weaker broader doublet has ΔE(Q,av)=0.68 mm/s. For temperatures T≤60 K the spectra are composed of a broad sextet and a central quadrupole doublet. The doublet persists down to the lowest applied temperature of 17 K. It is concluded that this doublet is due to an Fe-bearing phase other than heterosite and which gives rise to the inner doublet appearing in the spectra recorded at T≥65 K. The broad sextets, attributable to the heterosite phase, were fitted with model-independent hyperfine-field distributions. However, it was consistently experienced that using the common Lorentzian-shaped elementary sextets composing the distribution, could not adequately reproduce the observed line shapes. Instead, the calculations had to be based on the diagonalization of the complete hyperfine-interaction Hamiltonian. This is due to the unusually strong quadrupole interaction. The as-such calculated hyperfine parameters of the heterosite phase at 17 K may be summarized as follows: maximum-probability hyperfine field B(hf,m)=473 kOe, isomer shift δ(Fe)=0.54 mm/s, average quadrupole coupling constant ½e(2)qQ=1.50 mm/s, asymmetry parameter of the EFG η=0.80, and polar angles of the hyperfine field with respect to the EFGs principal axes frame Ω=40° and Ψ=90°. The temperature variation of the hyperfine field was interpreted in terms of the Bean-Rodbell (BR) model. The BR parameter, η(BR), was found to be 0.90, indicating a first-order magnetic transition at T(N)=59.7 K. The temperature variation of the isomer shift is explained by the second-order Doppler shift δ(SOD). Using the Debye model for the lattice vibrational spectrum for calculating δ(SOD), the characteristic Mössbauer temperature Θ(M) was found to be 400 K, which is unusually low for a ferric compound.
Department of Physics and Astronomy, University of Ghent, B-9000 Gent, Belgium. eddy.degrave@Ugent.be
Eddy
E
De Grave
Geraldo Magela
GM
da Costa
Antoine
A
Van Alboom
Robert Emile
RE
Vandenberghe
D019015:Geologic Sediments / Q000737:chemistry; D058085:Iron Compounds / Q000737:chemistry*; D008903:Minerals / Q000737:chemistry*; D010710:Phosphates / Q000737:chemistry*; D012432:Rwanda; D015204:Spectroscopy, Mossbauer / Q000379:methods*; D013696:Temperature
D058085:Iron Compounds; D008903:Minerals; D010710:Phosphates