2015
DOI: 10.2109/jcersj2.123.983
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Assessment of carbon contamination in MgAl<sub>2</sub>O<sub>4</sub> spinel during spark-plasma-sintering (SPS) processing

Abstract: Carbon contamination caused during spark-plasma-sintering (SPS) processing was investigated in the MgAl 2 O 4 spinel by Raman spectroscopy. Although the carbon contamination became remarkable around the sample surfaces directly contacting the carbon paper, it sensitively changes with the SPS conditions, particularly for the heating rate. For the slow heating rate of 10°C/min, the carbon contamination can be detected around the surface regions rather than inside. For the high heating rate, however, a large amou… Show more

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Cited by 39 publications
(9 citation statements)
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“…The spectra are consistent with the signature of two main contributions, a sextet (major) and a doublet (minor) with an average isomer shift < δ > of 0.40 mm.s −1 and an average hyperfine field (<B hyp > of 49.0 T) (see Figure SI-4 in the supporting information section). The sextet is quite consistent with ferric cations involved in the ferrimagnetic spinel structure but some of them with a partial electron delocalization (explaining the inner wing of the left outer line), while the quadrupolar doublet must be assigned to paramagnetic ferrous species: they result probably from a small contamination by a paramagnetic phase non detected by XRD, such as siderite FeCO 3 (that would be compatible with the observation of traces of carbon as often reported on SPS sintered ceramics 44,45 ) and/or the replacement of the CoO phase by its solid solution Co 1-x Fe x O (x close to zero) (that would be compatible with the diffusion of iron cation from spinel to adjacent rock-salt grains because an interatomic diffusion in SPS sintered nanocomposites was also reported 34 ).…”
Section: Resultssupporting
confidence: 81%
“…The spectra are consistent with the signature of two main contributions, a sextet (major) and a doublet (minor) with an average isomer shift < δ > of 0.40 mm.s −1 and an average hyperfine field (<B hyp > of 49.0 T) (see Figure SI-4 in the supporting information section). The sextet is quite consistent with ferric cations involved in the ferrimagnetic spinel structure but some of them with a partial electron delocalization (explaining the inner wing of the left outer line), while the quadrupolar doublet must be assigned to paramagnetic ferrous species: they result probably from a small contamination by a paramagnetic phase non detected by XRD, such as siderite FeCO 3 (that would be compatible with the observation of traces of carbon as often reported on SPS sintered ceramics 44,45 ) and/or the replacement of the CoO phase by its solid solution Co 1-x Fe x O (x close to zero) (that would be compatible with the diffusion of iron cation from spinel to adjacent rock-salt grains because an interatomic diffusion in SPS sintered nanocomposites was also reported 34 ).…”
Section: Resultssupporting
confidence: 81%
“…[42][43][44] Morita et al found that during the annealing, the carbon phases generate CO/CO 2 gases by reacting with oxygen and form many pores due to the inner pressure of the generated gases. 45,46 Such pores dramatically degrade the optical and laser properties. 41 | 699 et al reported that preheating the starting powder in air can improve transmittance without increasing its grain size.…”
Section: Microstructure and Crystal Structurementioning
confidence: 99%
“…However, those methods involve pressure and specific atmospheric conditions during sintering (argon pressure or vacuum with graphite contact, for respectively HIP and SPS). For SPS, graphite pollution has been widely reported to be a limiting transparency phenomenon [11,12]. Dopants were also studied for the sintering of spinel, notably LiF [13][14][15].…”
Section: Introductionmentioning
confidence: 99%