2007
DOI: 10.1107/s0108270107053462
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FeII2(PO4)(OH), a synthetic analogue of wolfeite

Abstract: This paper reports the hydrothermal synthesis and crystal structure refinement of diiron(II) phosphate hydroxide, Fe(II)2(PO4)(OH), obtained at 1063 K and 2.5 GPa. This phosphate is the synthetic analogue of the mineral wolfeite, and has a crystal structure topologically identical to those of minerals of the triplite-triploidite group. The complex framework contains edge- and corner-sharing FeO4(OH) and FeO4(OH)2 polyhedra, linked via corner-sharing to the PO4 tetrahedra (average P-O distances are between 1.53… Show more

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Cited by 5 publications
(4 citation statements)
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“…The structure of the (2b) type with the P2 1 /n space group is represented by three end-members: Mg 2 (PO 4 )F (this paper), Mg 2 (PO 4 )OH (Raade & Rømming, 1986) and Fe 2 (PO 4 )OH (Hatert, 2007) and minerals with intermediate composition, such as wagnerite (Mg, Fe) 2 (PO 4 )F (Coda et al, 1967), hydroxylwagnerite (Mg, Fe) 2 (PO 4 )OH (Brunet et al, 1998;Chopin et al, 2004), triploidite Mn 1.5 Fe 0.5 (PO 4 )OH (Waldrop, Table 1 Synthetic and natural end-members, with unit-cell dimensions in unified setting.…”
Section: Origin Of Modulation In Wagneritementioning
confidence: 99%
“…The structure of the (2b) type with the P2 1 /n space group is represented by three end-members: Mg 2 (PO 4 )F (this paper), Mg 2 (PO 4 )OH (Raade & Rømming, 1986) and Fe 2 (PO 4 )OH (Hatert, 2007) and minerals with intermediate composition, such as wagnerite (Mg, Fe) 2 (PO 4 )F (Coda et al, 1967), hydroxylwagnerite (Mg, Fe) 2 (PO 4 )OH (Brunet et al, 1998;Chopin et al, 2004), triploidite Mn 1.5 Fe 0.5 (PO 4 )OH (Waldrop, Table 1 Synthetic and natural end-members, with unit-cell dimensions in unified setting.…”
Section: Origin Of Modulation In Wagneritementioning
confidence: 99%
“…Spin-glass behavior was observed at low temperatures in γ-Co 2 (PO 4 )­(OH) . The other M 2 (PO 4 )­(OH) and M 2 (AsO 4 )­(OH) analogs reported in the structural literature appear to be confined to the orthorhombic and tetragonal polymorphs. The difficulty in isolating purely nickel-based analogs of these compounds has been documented elsewhere, so their synthesis as reasonably large-sized single crystals from high-temperature hydrothermal reactions is particularly fortuitous.…”
Section: Resultsmentioning
confidence: 98%
“…Iron hydroxyl phosphates (Fe x (PO 4 ) y (OH) z ·nH 2 O) [9,11], such as barbosalite Fe 3 (PO 4 ) 2 (OH) 2 [12,14], rockbridgeite Fe 5 (PO 4 ) 3 (OH) 5 [15,16], beraunite Fe 6 (PO 4 ) 4 (OH) 5 ·6H 2 O [17,18], and whitmoreite Fe 3 (PO 4 ) 2 (OH) 2 ·4H 2 O [19], are well-known minerals and important catalysts for oxidative dehydrogenation reactions [20,21]. They are significant in corrosion inhibition, passivation of metal surfaces [22], and also important in various considerations of the reactions of iron compounds contained in various soils with phosphate fertilizers [23].…”
Section: Introductionmentioning
confidence: 99%