2016
DOI: 10.1016/j.jcrysgro.2016.04.046
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Single crystal growth of CuFe1−Ga O2 by the optical floating-zone method

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Cited by 11 publications
(5 citation statements)
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“…If stoichiometric source material would be used, the peritectic Cu 2 O–Fe 2 O 3 phase diagram (Figure a in ref. []) reveals that the liquidus temperature is about 1400 °C, and due to the increase of the stability range with temperature, Fe 2 O 3 is favored to crystalize. CuFeO 2 melts incongruently, but the growth window is larger than in the case of CuAlO 2 (Figure in ref.…”
Section: Resultsmentioning
confidence: 99%
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“…If stoichiometric source material would be used, the peritectic Cu 2 O–Fe 2 O 3 phase diagram (Figure a in ref. []) reveals that the liquidus temperature is about 1400 °C, and due to the increase of the stability range with temperature, Fe 2 O 3 is favored to crystalize. CuFeO 2 melts incongruently, but the growth window is larger than in the case of CuAlO 2 (Figure in ref.…”
Section: Resultsmentioning
confidence: 99%
“…Fe 2 O 3 addition acts as a sintering agent and improves the conductivity for x < 0.2 by increasing the grain size . The only paper known to us with the aim to grow bulk ternary delafossites was the systematic study on OFZ growth of CuFe 1–x Ga x O 2 in Ar flow under normal pressure and with a pulling rate of 0.5 mm h −1 published by Song et al . The feed and seed rods were rotated at a rate of 15 rpm in opposite directions to homogenize the molten zone.…”
Section: Introductionmentioning
confidence: 99%
“…Typically the melting behavior is described to be peritectic, which means that upon heating in addition to melt with different composition some higher melting solid phase is formed. For CuAlO 2 , α-Al 2 O 3 is the higher melting phase, and in some recent publications Fe 2 O 3 is claimed to play this role for CuFeO 2 [25,26]. This assumption is, however, incorrect because Fe 2 O 3 decomposes to Fe 3 O 4 and cannot be treated as a stable component of the system.…”
Section: Discussionmentioning
confidence: 99%
“…The melting points of iron oxides (Fe 2 O 3 decomposes to Fe 3 O 4 , which melts at 1597 • C) are significantly lower than for Al 2 O 3 (T f = 2054 • C [24]), and consequently a larger growth window for CuFeO 2 (R 3m, a = 3.0351 Å, c = 17.166 Å) can be expected. (Some CuO-Fe 2 O 3 phase diagrams [25,26] in the literature neglect the decomposition of Fe 2 O 3 and show the congruent melting point of Fe 3 O 4 instead.) CuFeO 2 is the only delafossite compound, that has already be grown with reasonable quality in diameters up to 5-8 mm by the optical floating zone (OFZ) technique [25,27,28].…”
Section: While Examining the Mineralogical Collection Of The éCole Na...mentioning
confidence: 99%
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