Chemistry:Iron(II) oxalate
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IUPAC name
Iron(II) oxalate
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Other names
Iron oxalate
Ferrous oxalate | |
Identifiers | |
3D model (JSmol)
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EC Number |
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PubChem CID
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UNII |
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Properties | |
FeC2O4 (anhydrous) FeC2O4 • 2H2O (dihydrate) | |
Molar mass | 143.86 g/mol (anhydrous) 179.89 g/mol (dihydrate) |
Appearance | yellow powder |
Odor | odorless |
Density | 2.28 g/cm3 |
Melting point | dihydrate: 150–160 °C (302–320 °F; 423–433 K) (decomposes) |
dihydrate: 0.097 g/100ml (25 °C)[1] | |
Hazards | |
GHS pictograms | [2] |
GHS Signal word | Warning |
H302, H312[2] | |
P280[2] | |
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa). | |
verify (what is ?) | |
Infobox references | |
Ferrous oxalate (iron(II) oxalate) are inorganic compound with the formula FeC2O4(H2O)x where x is 0 or 2. These are orange compounds, poorly soluble in water. Thyy
Structure and reactions
Like other iron oxalates, ferrous oxalates feature octahedral Fe centers. The dihydrate FeC2O4(H2O)x is a coordination polymer, consisting of chains of oxalate-bridged ferrous centers, each with two aquo ligands.[3]
When heated to 120 °C, the dihydrate dehydrates, and the anhydrous ferrous oxalate decomposes near 190 °C.[4] The products of thermal decomposition is a mixture of iron oxides and pyrophoric iron metal, as well as released carbon dioxide, carbon monoxide, and water.[5]
Ferrous oxalates are precursors to iron phosphates, which are of value in batteries.[6]
Natural occurrence
Anhydrous iron(II) oxalate is unknown among minerals as of 2020. However, the dihydrate is known as humboldtine.[7][8] A related, though much more complex mineral is stepanovite,
Na[Mg(H2O)6] [Fe3+(C2O4)3]·3H2O - an example of trioxalatoferrate(III).[9][8]
See also
- Iron(III) oxalate
- Potassium ferrioxalate
- Sodium ferrioxalate
References
- ↑ "Iron(II) oxalate dihydrate". http://chemister.ru/Database/properties-en.php?dbid=1&id=2084.
- ↑ 2.0 2.1 2.2 Sigma-Aldrich Co., Iron(II) oxalate dihydrate. Retrieved on 2014-05-03.
- ↑ Echigo, Takuya; Kimata, Mitsuyoshi (2008). "Single-crystal X-ray diffraction and spectroscopic studies on humboldtine and lindbergite: weak Jahn–Teller effect of Fe2+ ion". Physics and Chemistry of Minerals 35 (8): 467–475. doi:10.1007/s00269-008-0241-7. Bibcode: 2008PCM....35..467E.
- ↑ Mu, Jacob; Perlmutter, D.D. (1981). "Thermal decomposition of carbonates, carboxylates, oxalates, acetates, formates, and hydroxides". Thermochimica Acta 49 (2–3): 207–218. doi:10.1016/0040-6031(81)80175-x.
- ↑ Hermanek, Martin; Zboril, Radek; Mashlan, Miroslav; Machala, Libor; Schneeweiss, Oldrich (2006). "Thermal Behaviour of Iron(II) Oxalate Dihydrate in the Atmosphere of Its Conversion Gases". J. Mater. Chem. 16 (13): 1273–1280. doi:10.1039/b514565a.
- ↑ Ellis, B. L.; Makahnouk, W. R. M.; Makimura, Y.; Toghill, K.; Nazar, L. F. (2007). "A multifunctional 3.5 V iron-based phosphate cathode for rechargeable batteries". Nature Materials 6 (10): 749–753. doi:10.1038/nmat2007. PMID 17828278. Bibcode: 2007NatMa...6..749E.
- ↑ "Humboldtine". https://www.mindat.org/min-1946.html.
- ↑ 8.0 8.1 "List of Minerals". 21 March 2011. https://www.ima-mineralogy.org/Minlist.htm.
- ↑ "Stepanovite". https://www.mindat.org/min-3763.html.
Original source: https://en.wikipedia.org/wiki/Iron(II) oxalate.
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