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1.
Mössbauer parameters (internal magnetic field, quadrupole splitting and isomer shift) of both α-(Fe1-x Cr x )2O3 (x=0, 0.2 and ≈1.0) doped and undoped with57Co are in good agreement at room temperature and 77 K, except internal magnetic fields of both α-Cr2O3 doped with57Co and enriched57Fe. It is thus concluded that57Fe produced from57Co occupies the octahedral sites as Fe3+ with small distortion from cubic symmetry. Different internal magnetic field of doped α-Cr2O3 may be explained by the difference of canting of the spin against the [111] axis. By adding zinc ions, the adsorption of Co2+ ions on α-Fe2O3 particles in aqueous solution is decreased considerably in the pH range of 6.5–9.5 at 303 K, but the internal magnetic field of57Co adsorbed on α-Fe2O3 does not change, although the internal magnetic fields of both samples with and without zinc ions are smaller than that of bulk α-Fe2O3 doped with57Co. This suggests that densities of57Co ions on the surface of α-Fe2O3 may be decreased by the addition of zinc ions and57Co ions adsorbed on α-Fe2O3 are weakly bound on the substrate.  相似文献   

2.
LiTaO3 single crystals were doped with57Co. Heat treatments of the crystals in the various atmospheres (Ar, Ar/H2 etc.) very sensitively influenced the charge states of iron formed after the EC of57Co. Fe2+ Fe3+ and metallic clusters are formed depending on the treatments in the various atmospheres. The observed effects were found reversible by changing the reducing and oxidising atmospheres.  相似文献   

3.
The57Co emission Mössbauer spectra from YBa2Cu3O6.92 (1-2-307) and YBa2Cu3O6.00 (1-2-306) have been measured and compared with the57Fe absorption spectra from YBa2Cu2.95Fe0.05O7?δ in order to clarify decisively the site assignments for the57Fe quadrupole-split doublets in these compounds. Mössbauer spectra obtained from both specimens consist of four components whose hyperfine interaction parameters well agree with each other. It is shown that the Co and Fe atoms mainly substitute at Cu1 chain sites in 1-2-307, but in 1-2-306 the Co atoms occupy randomly the Cu2 plane sites and indicate magnetically-split sextet which converts to a paramagnetic doublet of S-state Fe3+ in 1-2-307 by a post-annealing in O2 gas.  相似文献   

4.
Powder samples of57Fe2O3 and56Fe2O3 were implanted with56Fe and57Fe ions, respectively. By the use of Conversion Electron Mössbauer Spectroscopy it was possible to observe the local states of implanted ions (57Fe in56Fe2O3) or the states of iron atoms from the target which were displaced during implantation due to the ballistic processes (56Fe in57Fe2O3). The implanted and displaced iron atoms appear in three different states: (i) in regular substitutional positions of Fe2O3, (ii) as magnetite Fe3O4-type structures and (iii) paramagnetic FeO1?x state. The observed fractions of each state agree rather well with the calculated values obtained from the local iron atom enrichment at the surface as well as from the analysis of the equilibrium phase diagram for the binary Fe?O system. However, in57Fe implanted samples some enhancement of the FeO1?x fraction was found in comparison with the56Fe implanted hematite.  相似文献   

5.
YAG and YIG crystals implanted respectively with 100 keV57Fe2+ ions (1 × 1017 ions.cm?2) and 50 keV27Al ions (1.1 × 1017 ions.cm?2) have been studied by conversion electron Mössbauer spectroscopy (CEMS) directly after implantation and after annealings in air at temperatures up to 1100°C. In both as-implanted samples iron is found mainly in three states: Fe2+, Fe3+ and small metallic precipitates. Annealing behaviour is divided into two stages: (i) up to 400°C the iron has become completely oxidized and (ii) between 400 and 850°C the epitaxial regrowth of the implanted layer takes place. During this process a part of iron ions are incorporated into octahedral and tetrahedral sites, thus making a Y3 (Al Fe)5 O12 compound. The remaining iron part precipitates in the form of Fe2O3 particles.  相似文献   

6.
The analysis of room temperature and4.2 K Mössbauer spectra of NdCo12B6 doped with57Fe is presented. A clear preference of the57Fe atoms for the 18h sites, of increased number of Co near neighbour atoms compared with the 18g site, is obtained in good agreement with recent studies of related 1:12:6 compounds.  相似文献   

7.
Using diamond anvil cell, the57Fe Mössbauer spectra of pure iron foil and α-Fe2O3 powder under high pressure have been measured at room temperature.57Fe Mössbauer spectra of α-Fe were measured from 15 GPa to 45 GPa. Isomer shift value decreased and the quadrupole splitting slightly increased as the pressure increased.57Fe Mössbauer spectra of Fe2O3 under high pressure up to 72 GPa were observed. Above 52 GPa, the new lines appeared at the center portion of the spectrum corresponding to the new high pressure phase. The spectrum of new high pressure phase consisted of 6-line splitting and doublet, suggesting the existence of the two different kinds of iron states in it.  相似文献   

8.
Conclusions Different charge states of57Fe are identified in the57Co implanted SiO2 matrix.It is interesting to see that the states appearing in solid oxygen [2 ] also appear in the SiO2 matrix, although in neither of the matrices a preferential interpretation of the S1-line being Fe+ 6 or Fe0, can be achieved.Further, implantation of57Fe in SiO2 could reveal whether the states appearing in the57Co implanted SiO2 are really after decay effects or part of a (57Fe-SiO2)-structure.The authors wish to thank Prof. P. Boolchand for the SiO2 samples and L. Verwilst for the ion implantation.  相似文献   

9.
Lithium iron phosphates LiFe1-y Co y PO4 (y = 0, 0.1, 0.2) exposed to a charging process were studied by 57Fe Mössbauer spectroscopy taking into account XRD and SEM data. Hyperfine parameters of the spectra were determined above and below the magnetic ordering temperature for all the samples. It was shown that the presence of Co impurity atoms in lithium phosphates gives no effect on the hyperfine interaction of 57Fe2+ cations. However, Co atoms in the nearest cation environment of Fe atoms lead to a significant change of the hyperfine interactions of 57Fe3+ cations. The Co impurity atoms distribution over the positions of the iron atoms in the structure is found not to be statistical,but correlated.  相似文献   

10.
57Fe emission Mössbauer spectroscopy has been applied to study the lattice location and properties of Fe in gadolinium gallium garnet Gd3Ga5O12 (GGG) single crystals in the temperature interval 300 – 563 K within the extremely dilute (<10?4 at.%) regime following the implantation of57Mn (T1/2= 1.5 min.) at ISOLDE/CERN. These results are compared with earlier Mössbauer spectroscopy study of Fe-doped gadolinium gallium garnet Gd3Ga5O12(GGG), with implantation fluences between 8×1015 and 6×1016 atoms cm?2. Three Fe components are observed in the emission Mössbauer spectra: (i) high spin Fe2+ located at damage sites due to the implantation process, (ii) high spin Fe3+ at substitutional tetrahedral Ga sites, and (iii) interstitial Fe, probably due to the recoil imparted on the daughter57?Fe nucleus in the β? decay of57Mn. In contrast to high fluence57Fe implantation studies the Fe3+ ions are found to prefer the tetrahedral Ga site over the octahedral Ga site. No annealing stages are evident in the temperature range investigated. Despite the very low concentration, high-spin Fe3+ shows fast spin relaxation, presumably due to an indirect interaction between nearby gadolinium atoms.  相似文献   

11.
Bi, In, Pb, Sb, α- and β-Sn were implanted with57Co and57Fe. The results of the analysis suggested strongly hybridized bonds between the iron and the host atoms. An upturn of the isomer shift (δ) values relative to the δ values in hosts with completed d-shell was not justified. Charge states of Fe2+ or Fe+ also appeared. The possible role of the native surface oxide layers in the formation of these states was investigated.  相似文献   

12.
In addition to spectral components due to Fe2?+? and Fe3?+?, a single line is observed in emission Mössbauer spectra following low fluence (<1015 cm???2) implantation of 57Fe*, 57Mn and 57Co in α-Al2O3. For the 57Co and 57Mn implantations, the intensity of the single line is found to depend on the emission angle relative to the crystal symmetry axis. This angular dependence can be explained by a non-isotropic f-factor and/or motion of the Fe ion between sites in an interstitial cage. It is argued that interstitial cage motion is a more likely explanation, as this can account for the lack of quadrupole splitting of the line.  相似文献   

13.
Emission Mössbauer Spectroscopy following the implantation of radioactive precursor isotope 57Mn+ (T 1/2= 1.5 min) into ZnO single crystals at ISOLDE/CERN shows that a large fraction of 57Fe atoms produced in the 57Mn beta decay is created as paramagnetic Fe3+ with relatively long spin-lattice relaxation times. Here we report on ZnO pre-implanted with 56Fe to fluences of 2×1013, 5×10 13 and 8 × 1013 ions/cm2 in order to investigate the dependence of the paramagnetic relaxation rate of Fe3+ on fluence. The spectra are dominated by magnetic features displaying paramagnetic relaxation effects. The extracted spin-lattice relaxation rates show a slight increase with increasing ion fluence at corresponding temperatures and the area fraction of Fe3+ at room temperature reaches a maximum contribution of 80(3)% in the studied fluence range.  相似文献   

14.
A Mössbauer study of nano-TiO2 doped with Fe is presented. The samples are prepared by sol-gel method, doping Fe by 5, 10 and 15 wt.%, respectively, which are measured with XRD, TEM and Raman spectra. Especially, Mössbauer spectra are emphasized in this study. The anatase phase is major in both doped and no-doped sample. The α-Fe2O3 phase is also in the doped samples. The grain size of doped sample is in 5–20 nm range, the major grains are about 13 nm. And the grain size of no-doped sample is about 8 nm. Studying Mössbauer spectra and Raman spectra, we concluded that in the doping process the Fe3+ ions entered anatase lattice and substituted Ti4+ ions. However, the amount of Fe ions in the site is limited to about 1.5 wt.%. It does not increase as the doping Fe increase. The more Fe doped, the more α-Fe2O3 formed. For comparing conveniently, it also can be described as (Ti0.98Fe0.02)O2 by atomic percent.  相似文献   

15.
Emission Mössbauer spectroscopy is used to investigate the physico-chemical state of57Fe atoms generated by57Co2+ clectron capture in57Co: FeSO4xH2O (x=0,1,4,7). The spectra of all the hydrates show at least three main components, the normal bivalent state, Fe2+(N), an aliovalent state, Fe3+, and one (or several) anomalous ferrous species in which the coordination sphere has been perturbated by the self-radiolysis. No Fe3+ is observed in the anhydrous compound whereas the intensity of this component increases as a function of the hydration number, reaching a saturation value of 36% for x=4 and 7.  相似文献   

16.
Si(111) single crystals were implanted with57Fe in a broad dose range in order to overlap the concentration range of bulk amorphous Fe x Si1−x samples. At high (≥1016 atoms/cm2) doses the measured hyperfine interaction values were found to be the same as in the bulk amorphous samples, suggesting the same Fe−Si bonding and a very similar structure for the two amorphous phases produced by different methods. A comparison of the isomer shift (δ) and quadrupole splitting (ΔE) values with the values of the stoichiometric crystalliine phases showed the same δ but different δE values indicating similar Fe−Si bonding but different atomic arrangement around the iron atom.  相似文献   

17.
Sintered plates of alumina have been implanted at room temperature with 110 keV57Fe+ at a dose of 1.2×1017 ions.cm?2. The analysis of the Conversion Electron Mössbauer Spectrum indicated that implantation introduces iron in alumina in three charge state: Fe2+ (two components), Fe4+ and Fe0 (metallic clusters). The evolution of the iron depth distribution during annealings in oxiding or in neutral atmosphere has been followed using the Rutherford backscattering spectroscopy. Up to 800°C the profile as well as the charge states of iron evolve very slowly. A drastic change occurs' for annealing temperature around 1000°C. The total amount of iron is distributed among α-Fe2O3 and α-(Fe1?x Al x )2O3 precipitates. Some scanning electron micrographs have allowed to locate these precipitates. For highest temperature anneals, up to 1600°C, only substitutional iron remain.  相似文献   

18.
The in-beam Mössbauer spectroscopy using a short-lived 57Mn (T 1/2=1.5 min) beam was carried out to study the production of the exotic chemical species of 57Fe atoms arising from 57Mn implanted into solid oxygen. The obtained spectra can be analyzed by four components of doublets at least, which are assigned to be novel Fe species of FeO, Fe(O2), (O2)FeO2, and Fe(O2)2, on the basis of ab initio molecular orbital calculations.  相似文献   

19.
The lattice dynamics of an α-Al2O3 crystal with vacancies in various charge states is simulated using the recursive method in the shell model. The frequencies of resonant vibrations induced by defects in various directions are calculated. Characteristic features in vibrational spectra of anion-nonstoichiometric α-Al2O3 crystals, mostly associated with changes in the effective interaction between vacancies and the nearest neighbor atoms, are analyzed and explained.  相似文献   

20.
Mössbauer spectra of amorphous LiNbO3 doped with57Fe2+ ions were measured atT≥4.2 K in external magnetic fields up toH=5.5 T. It was found that the oxygen octahedra around the high-spin Fe2+ ions are randomly distorted obeying no symmetry at all. The correlation of isomer shift and quadrupole splitting is probably due to T2g distortions.  相似文献   

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