The crystal and magnetic structure of Li-aegirine LiFe3+Si2O6:: a temperature-dependent study

被引:66
作者
Redhammer, GJ
Roth, G
Paulus, W
André, G
Lottermoser, W
Amthauer, G
Treutmann, W
Koppelhuber-Bitschnau, B
机构
[1] Rhein Westfal TH Aachen, Inst Kristallog, D-54056 Aachen, Germany
[2] CEA Saclay, Leon Brillouin Lab, F-91191 Gif Sur Yvette, France
[3] Salzburg Univ, Inst Mineral, A-5020 Salzburg, Austria
[4] Univ Marburg, Inst Mineral, D-35032 Marburg, Germany
[5] Graz Univ, Inst Phys Chem, A-8010 Graz, Austria
关键词
Li-aegirine; clinopyroxene; diffraction; phase transition; magnetism;
D O I
10.1007/s002690100159
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Single crystals of Li-aegirine LiFe3+Si2O6 were synthesized at 1573 K and 3 GPa, and a polycrystalline sample suitable for neutron diffraction was produced by ceramic sintering at 1223 K. LiFe3+Si2O6 is monoclinic, space group C2/c, a = 9.6641(2) Angstrom, b = 8.6612(3) Angstrom, c = 5.2924(2) Angstrom, beta = 110.12(1)degrees at 300 K as refined from powder neutron data. At 229 K Li-aegirine undergoes a phase transition from C2/c to P2(1)/ L. This is indicated by strong discontinuities in the temperature variation of the lattice parameters, especially for the monoclinic angle P and by the appearance of Bragg reflections (hkl) with h + k not equal 2n. In the low-temperature form two non-equivalent Si-sites with (SIA-O) = 1.622 Angstrom and (SiB-O) = 1.624 Angstrom at 100 K are present. The bridging angles of the SiO4 tetrahedra O3-O3-O3 are 193.55(8)degrees and 160.02(9)degrees at 100 K in the two independent tetrahedral chains in space group P2(1)/c, whereas it is 180.83(9)degrees at 300 K in the high-temperature C2/c phase, i.e. the chains are nearly fully expanded. Upon the phase transition the Li-coordination changes from six to five. At 100 K four Li-O bond lengths lie within 2.072(4)-2.172(3) Angstrom, the fifth Li-O bond length is 2.356(4) Angstrom, whereas the Li-O3 A bond lengths amount to 2.796(4) Angstrom. From Fe-57 Mossbauer spectroscopic measurements between 80 and 500 K the structural phase transition is characterized by a small discontinuity of the quadrupole splitting. Temperature-dependent neutron powder diffraction experiments show first occurrence of magnetic reflections at 16.5 K in good agreement with the point of inflection in the temperature-dependent magnetization of LiFe3+Si2O6. Distinct preordering phenomena can be observed up to 35 K, At the magnetic phase transition the unit cell parameters exhibit a pronounced magneto-striction of the lattice. Below T-N Li-aegirine shows a collinear antiferromagnetic structure. From our neutron powder diffraction experiments we extract a collinear antiferromagnetic spin arrangement within the a-c plane.
引用
收藏
页码:337 / 346
页数:10
相关论文
共 14 条
[1]  
[Anonymous], 1980, REVIEWSINMINERALOGYA
[2]  
Arlt T, 1997, EUR J MINERAL, V9, P953
[3]  
BAUM E, 1988, Z KRISTALLOGR, V183, P273
[4]   LOW-TEMPERATURE AND HIGH-TEMPERATURE CRYSTAL-STRUCTURES OF LIFEGE2O6, LIFESI2O6 AND LICRSI2O6 [J].
BEHRUZI, M ;
HAHN, T ;
PREWITT, CT ;
BALDWIN, K .
ACTA CRYSTALLOGRAPHICA SECTION A, 1984, 40 :C247-C247
[5]   A PROPOSED CRYSTALLOGRAPHIC NOMENCLATURE FOR CLINOPYROXENE STRUCTURES [J].
BURNHAM, CW ;
CLARK, JR ;
PAPIKE, JJ ;
PREWITT, CT .
ZEITSCHRIFT FUR KRISTALLOGRAPHIE KRISTALLGEOMETRIE KRISTALLPHYSIK KRISTALLCHEMIE, 1967, 125 (1-6) :109-&
[6]   CHOICE OF COLLIMATORS FOR A CRYSTAL SPECTROMETER FOR NEUTRON DIFFRACTION [J].
CAGLIOTI, G ;
PAOLETTI, A ;
RICCI, FP .
NUCLEAR INSTRUMENTS & METHODS, 1958, 3 (04) :223-228
[7]  
CLARK JR, 1969, MINERAL SOC AM SPEC, V0002
[8]   Single crystal Mossbauer and neutron powder diffraction measurements on the synthetic clinopyroxene Li-acmite LiFeSi2O6 [J].
Lottermoser, W ;
Redhammer, G ;
Forcher, K ;
Amthauer, G ;
Paulus, W ;
Andre, G ;
Treutmann, W .
ZEITSCHRIFT FUR KRISTALLOGRAPHIE, 1998, 213 (02) :101-107
[9]   A PROFILE REFINEMENT METHOD FOR NUCLEAR AND MAGNETIC STRUCTURES [J].
RIETVELD, HM .
JOURNAL OF APPLIED CRYSTALLOGRAPHY, 1969, 2 :65-&
[10]  
RODRIGUESCARVAJ.J, 1996, FULLPROF RIETVELD PR