• journal_title：American Mineralogist
• Contributor：Riham M. Morcos ; Benjamin G. Ellis ; Alexandra Navrotsky
• Publisher：Mineralogical Society of America
• Date：2007-
• Format：text/html
• Language：en
• Identifier：10.2138/am.2007.2451
• journal_abbrev：American Mineralogist
• issn：0003-004X
• volume：92
• issue：7
• firstpage：1064
• section：Articles

Iron-oxide-rich melts are encountered in iron-ore sintering, smelting, and other industrial processes, whereas melts containing iron oxides but richer in silica are the mainstay of igneous processes near the Earth’s surface and at depths down to the core-mantle boundary. High-temperature calorimetry has been used to evaluate the enthalpy of solution of Fe₂O₃ in a series of iron-oxide-based melts at 1353 °C. For a typical melt found in iron-ore sintering, the heat of solution of Fe₂O₃ is 54.4 ± 5.9 kJ/mol, with no dependence on the Fe₂O₃ concentration between 59 and 69 mol%. The heat content of a series of samples (59 to 64 mol% Fe₂O₃), measured by transposed-temperature drop calorimetry, is also independent of composition.