THERMODYNAMICS OF FE OXIDES: PART I. ENTROPY AT STANDARD TEMPERATURE AND PRESSURE AND HEAT CAPACITY OF GOETHITE (α-FEOOH), LEPIDOCROCITE (γ-FEOOH), AND MAGHEMITE (γ-FE2O3)

Show simple item record

dc.contributor.author Majzlan J.
dc.contributor.author Navrotsky A.
dc.contributor.author Lang B.E.
dc.contributor.author Stevens R.
dc.contributor.author Woodfield B.F.
dc.contributor.author Boerio-Goates J.
dc.date.accessioned 2021-12-02T03:58:05Z
dc.date.available 2021-12-02T03:58:05Z
dc.date.issued 2003
dc.identifier https://www.elibrary.ru/item.asp?id=14406582
dc.identifier.citation American Mineralogist, 2003, 88, 5, 846-854
dc.identifier.issn 0003-004X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/32616
dc.description.abstract The heat capacities (Cp) of goethite (goe, α-FeOOH), lepidocrocite (lep, γ-FeOOH), and maghemite (mag, γ-Fe2O3) were measured from below liquid helium temperature up to their decomposition temperatures by a combination of adiabatic, semi-adiabatic, and differential scanning calorimetry. All three phases were synthetic, with < 160 ppm of Al. Chlorine content in goe (32 ppm) and lep (202 ppm) is too low to affect the calorimetric results of this study. Phase purity was verified by Rietveld refinement of the powder X-ray diffraction (XRD) patterns; we determined lattice parameters, atomic positions, crystallite size, and microstrain for all three samples. The Brunauer-Emmet-Teller (BET) surface area is 21 (goe), 23 (lep), and 18 (mag) m2/g. No amorphous impurity was found in the goethite sample by extraction of the oxalate soluble fraction. The excess water, determined from weight loss after firing at 1200 K overnight. is 0.083 ± 0.010 (goe), 0.087 ± 0.005 (lep), 0.042 ± 0.003 (mag) moles of water per mole of FeOOH or Fe2O3. The entropy at standard temperature and pressure (STP) was calculated from subambient Cp data and corrected for the excess water content using a Debye-Einstein representation of the Cp of hexagonal ice. The entropy at STP is 59.7 ± 0.2 (goe), 65.1 ± 0.2 (lep), and 93.0 ± 0.2 (mag) J/(K·mol). Tfhe XRD pattern of maghemite lacks superstructure peaks, and complete disorder of the vacancies leads to configurational entropy S conf = 2.0 J/K·mol. Because very weak superstructure peaks can be overlooked, or the vacancies may be short-range ordered, this calculated Sconf represents only an upper limit. The heat capacity above 273 K was fitted to a Maier-Kelley polynomial Cp [J/(K·mol). T in K] = a + bT + cT2. The Cp polynomial coefficients are a = 1.246, b = 0.2332, c = 313900 (goe, valid in temperature range 273-375 K), a = 59.76, b = 0.06052, c = -772900 (lep, 273-390 K), and a = 106.8, b = 0.06509, c = -1886000 (mag, 273-760 K).
dc.subject Goethite
dc.subject Lepidocrocite
dc.subject Maghemite
dc.title THERMODYNAMICS OF FE OXIDES: PART I. ENTROPY AT STANDARD TEMPERATURE AND PRESSURE AND HEAT CAPACITY OF GOETHITE (α-FEOOH), LEPIDOCROCITE (γ-FEOOH), AND MAGHEMITE (γ-FE2O3)
dc.type Статья


Files in this item

Files Size Format View

There are no files associated with this item.

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record