1995
DOI: 10.1016/0009-2614(94)01465-8
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Absorption and luminescence spectroscopy of Cr4+-doped Ca2GeO4. A potential near infrared laser material

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Cited by 31 publications
(23 citation statements)
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“…Conversion to the crystalline orthorhombic phase changes the oxidation state and coordination of the chromium dopant. EPR spectra of Cr-doped Ca 2 SiO 4 and Ca 2 GeO 4 (Figure ) show a single resonance with g = 2.05 ± 0.02 and a half-width of 200 G. Although the half-width is significantly larger, the g value is within experimental error of that reported for aluminates, alkyls, , and oxide glasses , containing tetrahederally coordinated Cr 4+ and is attributed to tetrahedrally coordinated Cr 4+ . These resonances also resemble those observed in forsterite where Cr 4+ formation has been attributed to a reaction between Cr 3+ and excess oxygen defect centers. , In addition to the resonance attributed to tetrahederal Cr 4+ , all Cr-doped forsterite samples prepared in these experiments exhibit an additional resonance with g ≈ 5 and g ≈ 1.96 that are (Figure ) assigned to octahederally coordinated Cr 3+ . , …”
Section: Discussionsupporting
confidence: 64%
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“…Conversion to the crystalline orthorhombic phase changes the oxidation state and coordination of the chromium dopant. EPR spectra of Cr-doped Ca 2 SiO 4 and Ca 2 GeO 4 (Figure ) show a single resonance with g = 2.05 ± 0.02 and a half-width of 200 G. Although the half-width is significantly larger, the g value is within experimental error of that reported for aluminates, alkyls, , and oxide glasses , containing tetrahederally coordinated Cr 4+ and is attributed to tetrahedrally coordinated Cr 4+ . These resonances also resemble those observed in forsterite where Cr 4+ formation has been attributed to a reaction between Cr 3+ and excess oxygen defect centers. , In addition to the resonance attributed to tetrahederal Cr 4+ , all Cr-doped forsterite samples prepared in these experiments exhibit an additional resonance with g ≈ 5 and g ≈ 1.96 that are (Figure ) assigned to octahederally coordinated Cr 3+ . , …”
Section: Discussionsupporting
confidence: 64%
“…Forsterite and other olivine systems have been prepared by high-temperature processing techniques, coprecipitation, and different sol−gel routes. Systems that are isostructural with forsterite, Mg 2 SiO 4 , also exhibit near-IR emissions. ,, Forsterite, Mg 2 SiO 4 has an orthorhombic structure with the space group Pbnm and contains four formula units per unit cell. In the unit cell, Mg 2+ ions occupy two distinct octahedral coordination sites, M 1 with inversion symmetry ( C i ) and M 2 with mirror symmetry ( C s ), while Si 4+ occupies a tetrahedral coordination site .…”
Section: Introductionmentioning
confidence: 99%
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“…These four excellent optical-function oxides with d 10 electron configuration are probably applied in water splitting and the photoluminescent field [9,10,[18][19][20]. Subsequently, structures and morphologies of these oxides were confirmed by X-ray powder diffraction, scanning electron microscopy, Raman spectroscopy and infrared spectroscopy, respectively.…”
Section: Introductionmentioning
confidence: 95%
“…Isoelectronic d cations Cr'4, Mn4, and Fe4' in various oxide ceramics have been subject to extensive studies, both experimental and theoretical, because of their remarkable luminescence properties (1)(2)(3)(4)(5)(6)(7)(8)(9)(10)(11)(12) and applications, in the case of Cr'4, in tunable lasers in the near infrared (13)(14)(15)(16). The oxidation states of tetrahedrally coordinated Cr'4, Mn4, and Fe4' ions are rather unstable when compared to those of Cr''', Cr4', Mn'', Mn''', Mn'4, Mn4'', and Fe'''.…”
Section: Introductionmentioning
confidence: 99%