Material Research in Atomic Scale by Mössbauer Spectroscopy 2003
DOI: 10.1007/978-94-010-0151-9_27
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Synthesis Of Iron Sulfides: A Mössbauer Study

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Cited by 5 publications
(16 citation statements)
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“…The previous synthetic studies [37][38][39][40][41][42][43][44][45][46] have been largely aimed at mimicking the mineral formation processes, including extra-terrestrial ones, and commonly used strict precautions against oxidation of the iron sulfide part of tochilinite, akin to mackinawite [57][58][59][60], to preserve low-spin Fe 2+ . The materials manufactured here through the simple method contain high-spin ferric and ferrous cations, which are paramagnetic both at 293 and 4.2 K. At the same time, the low-temperature Mössbauer spectra show several magnetic ordered states attributed to the abovementioned iron centers in the sulfide layers, and Fe 3+ coordinated to OHand minor O 2ligands in Mg-based hydroxide sheets.…”
Section: Discussionmentioning
confidence: 99%
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“…The previous synthetic studies [37][38][39][40][41][42][43][44][45][46] have been largely aimed at mimicking the mineral formation processes, including extra-terrestrial ones, and commonly used strict precautions against oxidation of the iron sulfide part of tochilinite, akin to mackinawite [57][58][59][60], to preserve low-spin Fe 2+ . The materials manufactured here through the simple method contain high-spin ferric and ferrous cations, which are paramagnetic both at 293 and 4.2 K. At the same time, the low-temperature Mössbauer spectra show several magnetic ordered states attributed to the abovementioned iron centers in the sulfide layers, and Fe 3+ coordinated to OHand minor O 2ligands in Mg-based hydroxide sheets.…”
Section: Discussionmentioning
confidence: 99%
“…3, Table 2). It is likely that, akin to valleriite [50], doublets with the chemical shift δ = 0.3-0.4 mm/s and quadrupole splitting ∆ of 0.4-0.6 mm/s are due to Fe 3+ -S centers, and the ones with δ ≥ 0.4 mm/s and ∆ of 1±0.2 mm/s originate from high-spin Fe 3+ cations in octahedral OHenvironment (Fe 3+ -6OH), whereas the quantities of Fe 2+ -OH centers (δ ∼ 1 mm/s, ∆ > 2 mm/s [40][41][42][56][57][58][59][60]) are minor. The electron densities and electric field gradients at Fe 2+ nuclei in tetrahedral coordination to S are close to those for Fe 3+ -6OH centers so their signals are difficult to resolve.…”
Section: Mössbauer Spectroscopy and Magnetization Study 57mentioning
confidence: 99%
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“…Valleriite (CuFeS2)(Mg,Al,Fe)(OH)2 [19][20][21][22][23][24][25][26][27] and tochilinite mFeSn(Mg,Fe)(OH)2 [30][31][32][33][34][35][36] are the most known and important of them; particularly, valleriite ores of Noril'sk ore provenance (Russia) are of commercial importance but not involved in the exploitation because of the lack of processing technologies. Synthetic valleriite and tochilinite have been prepared and characterized too [37][38][39][40][41][42][43][44][45][46][47][48][49][50]; however, the yields of the target substances were lower than 50%, and those were substantially contaminated by the reaction by-products. Another group of layered iron chalcogenide-hydroxide materials with the composition Fe(Se,S)(Li,Fe)OH and some their derivatives [51][52][53][54][55] synthesized in the recent years are attracting much attention because of the superconducting properties but little efforts have been made to study other characteristics and applications.…”
Section: Introductionmentioning
confidence: 99%