1980
DOI: 10.1007/bf02061277
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Phase transformation in the cupric magnesium oxide system

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1982
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Cited by 13 publications
(5 citation statements)
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“…The proximity of the lattice parameter values of the samples of different compositions at low temperatures is probably explained by the fact that under these conditions the rocksalt phase is predominantly comprised of magnesia, which is saturated with Co 2+ only during the thermal decomposition of the spinel, forming a solid solution with a composition corresponding to the initial cobalt loading. The higher value of the lattice parameter of low-temperature MgO relative to the theoretical value (4.2112 Å) is confirmed in [35] and is explained by the paracrystalline structure of anion-modified low-temperature oxide systems [36]; this phenomenon can also be explained by the presence of microstresses and strain in the structure [28,29]. The characteristic decrease of the lattice parameter values of both the spinel phase in the 400-750 °C range and the rocksalt phase formed during spinel thermal decomposition in the 900-1100 °C range is presumably explained by the stress relaxation together with decomposition of anionic residues in the phase structure.…”
Section: Phase Composition and Structure Of Samplessupporting
confidence: 53%
“…The proximity of the lattice parameter values of the samples of different compositions at low temperatures is probably explained by the fact that under these conditions the rocksalt phase is predominantly comprised of magnesia, which is saturated with Co 2+ only during the thermal decomposition of the spinel, forming a solid solution with a composition corresponding to the initial cobalt loading. The higher value of the lattice parameter of low-temperature MgO relative to the theoretical value (4.2112 Å) is confirmed in [35] and is explained by the paracrystalline structure of anion-modified low-temperature oxide systems [36]; this phenomenon can also be explained by the presence of microstresses and strain in the structure [28,29]. The characteristic decrease of the lattice parameter values of both the spinel phase in the 400-750 °C range and the rocksalt phase formed during spinel thermal decomposition in the 900-1100 °C range is presumably explained by the stress relaxation together with decomposition of anionic residues in the phase structure.…”
Section: Phase Composition and Structure Of Samplessupporting
confidence: 53%
“…This may indicate the presence of additional ruthenium valence states in spectrum. This could be RuO 2 or Ru 3+ and Ru 4+ ions dissolved in the MgO lattice . However, the Ru3d spectra are fairly symmetric and can be described well by a single peak.…”
Section: Resultsmentioning
confidence: 98%
“…This could be RuO 2 or Ru 3+ and Ru 4+ ions dissolved in the MgO lattice. 20 However, the Ru3d spectra are fairly symmetric and can be described well by a single peak. So, it is impossible to make an unambiguous conclusion on the presence or absence of additional ruthenium states different from Ru 0 based only on these data.…”
Section: Resultsmentioning
confidence: 99%
“…The red brick color of the sample after this treatment allows supposing Cu 2 O phase formation and XRD proves decomposition of Cu-Mg oxide solid solution and formation of two individual oxide phases-Cu 2 O and MgO. One should note that the decomposition of Cu 0.15 Mg 0.85 O in air wasn't observed even at significantly higher temperature (up to 1,100°C) in [11]. The lower temperature of decomposition in the inert gas flow (i.e.…”
Section: Resultsmentioning
confidence: 94%
“…In earlier publications (see e.g. [11]), it was shown that the binary hydroxide system of Cu(OH) 2 and Mg(OH) 2 has limited solubility range. According to our data, the solubility limit of Cu 2?…”
Section: Resultsmentioning
confidence: 98%