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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    European journal of soil science 49 (1998), S. 0 
    ISSN: 1365-2389
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Ilmenite-rich samples were obtained by chemical extraction methods from materials collected from a soil developing on an amphibolite and from its altered parent rock. The soil ilmenite of this mantle was found to be inherited from the rock, but its composition varied significantly from one soil fraction to another and according to its mineralogical association. Unit cell parameters are smaller than those of pure ilmenite: the a-dimension of the hexagonal structure varies from 0.5076 ± 0.0004 to 0.5083 ± 0.0007 nm. Mössbauer patterns at room temperature reveal that this mineral, which is most often associated with the iron-rich spinel phase, actually corresponds to a member of the haematite–ilmenite series having the general formula xFeTiO3.(1-x)Fe2O3, with 0.83 ≤x≤ 0.95. There is a correlation (r= 0.95) between x, the molar fraction of FeTiO3, and the a-dimension of the unit cell.
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Journal of materials science 27 (1992), S. 6116-6122 
    ISSN: 1573-4803
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Abstract The haematites obtained by dehydration of three synthetic goethites of different sizes have been characterized by X-ray diffraction, Mössbauer spectroscopy and transmission electron microscopy. The transformation itself has been studied by thermogravimetric analysis and differential scanning calorimetry. Samples (24) obtained by annealing the goethites for 30 min at several temperatures up to 900°C were analysed. All samples had a tabular shape. The variation of the internal magnetic field, as well as of the line widths of the spectra at room temperature, indicate growth of the particle size. The constant value for the quadrupole splitting and the absence of a distribution of hyperfine interactions of the spectra at 80 K excluded the presence of iron ions out of their normal positions. No strain was detected by X-ray diffraction. The results also showed a differential line broadening in the haematite pattern, but there was no shift in the position of the lines. This broadening was present in all lines, including those wihl=3n (n=0,1,2,...). Increasing the treatment temperature made all lines sharp. The relative integrated intensities,l(1 1 0)/l(1 0 4), of each series remained unaltered, but the relative intensities did not. The above results lead to the conclusion that the differential X-ray line broadening of haematites derived from goethite occurs only in tabular (or acicular) haematites with small size. For small spherical particles, the broadening should be uniform for all lines.
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Hyperfine interactions 67 (1991), S. 501-505 
    ISSN: 1572-9540
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Several synthetic hematites have been analysed by X-ray diffraction and Mössbauer spectroscopy. They have tabular shape and their Morin transition at 85 K show a dependence on the ratio (R) of the sizes inc anda directions. The Morin transition has been observed for samples withR=0.43±0.05.
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Hyperfine interactions 70 (1992), S. 961-964 
    ISSN: 1572-9540
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract The thermally induced oxidation of Fe2+ in talc has been investigated by Mössbauer spectroscopy. The heating temperature range of the samples was from 600°C to 750°C with variable times of treatment going from 6 hours up to 192 hours. The obtained isothermals could be well fitted by a first order kinetic model. The activation energy deduced from an Arrhenius plot is 178 kJ/mol.
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Hyperfine interactions 53 (1990), S. 379-383 
    ISSN: 1572-9540
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract A series of organophosphorus tin complexes was prepared and studied by several chemical and physical methods. The tin moiety was PhnSnCl4-n , where 0⪯n⪯4. Whenn was different from zero or from 4 the complexes showed unusual behaviour, with more than one Mössbauer site. Other studies were then undertaken in order to determine the nature of this behaviour.
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  • 6
    ISSN: 1572-9540
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Seven different samples obtained from the Petrobras Oil Well 1-ICA-1BA from depths down to 1872 m have been studied by Mössbauer spectroscopy, X-ray diffraction and neutron activation analysis. The X-ray diffraction showed the presence of clay minerals, feldspar, calcite, pyrite, quartz, dolomite, andrite and others. The neutron activation analysis has been used to obtain the iron concentration in the samples. The Mössbauer spectra were obtained both at room and liquid nitrogen temperatures. Spectra are complex in nature indicating multiple sites or mixture of iron containing minerals. The spectra at 85 K could be least squares fitted are resolved up to four doublets with typical values of IS(Fe)=1.4, 1.21, 1.16, 0.40 and QS=3.62, 2.82, 2.37, 0.61 mm/s respectively. They have slightly large line widths except for the first doublet. Two samples also showed the presence of hematite.
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Hyperfine interactions 67 (1991), S. 459-462 
    ISSN: 1572-9540
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Four samples of a wall containing rock paintings have been studied by Mössbauer spectroscopy in combination with optical microscopy analysis and X-ray diffraction. Hematite and goethite were identified as the pigments responsible for the colors and the mineral tinsleyite, as the principal component of a light pink layer that is present in some parts of the wall.
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Hyperfine interactions 67 (1991), S. 437-442 
    ISSN: 1572-9540
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Steatite mineral rocks, soapstone, have been studied by X-ray diffraction, optical microscopic analysis (modal analysis), electron probe micro analysis and Mössbauer spectroscopy for characterization, mineral percentages and chemical composition. Mössbauer spectra show both, magnetic interactions corresponding to magnetite and doublets corresponding to talc. chlorite, dolomite and tremolite. The temperature dependence of the quadrupole splitting in dolomite has been explained in terms of crystal field interaction.
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Hyperfine interactions 94 (1994), S. 2011-2015 
    ISSN: 1572-9540
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Iron-yttrium mixed oxides in varying ratios (Y∶Fe 9∶1, 3∶1, 1∶1, 1∶2, 1∶3, and 1∶9) annealed to different temperatures (850, 1000 and 1250
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Hyperfine interactions 91 (1994), S. 771-775 
    ISSN: 1572-9540
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract A natural ilmenite was extracted from the silt fraction of a soil developed from basalt of Minas Gerais State, Brazil. The sample was characterized by chemical analysis, X-ray diffraction, magnetic measurements and Mössbauer spectroscopy. The Mössbauer spectrum at 293 K shows two doublets: a major subspectrum of Fe2+ (relative area 74%) and a minor one of Fe3+ (26%). An incipient magnetic structure appears at 85 K, with a broadline sextet. These results may be explained by supposing that the separate is a solid solutionxFeTiO3 · (1−x)Fe2O3, withx=0.85, which is magnetically ordered at low temperature. The lattice parameters for this hexagonal structure area=0.5082±0.0001 nm andc=1.398±0.001 nm.
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