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Thermodynamic properties,low-temperature heat-capacity anomalies,and single-crystal X-ray refinement of hydronium jarosite, (H3O)Fe3(SO4)2(OH)6
Authors:J.?Majzlan  author-information"  >  author-information__contact u-icon-before"  >  mailto:jmajzlan@princeton.edu"   title="  jmajzlan@princeton.edu"   itemprop="  email"   data-track="  click"   data-track-action="  Email author"   data-track-label="  "  >Email author,R.?Stevens,J.?Boerio-Goates,B. F.?Woodfield,A.?Navrotsky,P. C.?Burns,M. K.?Crawford,T. G.?Amos
Affiliation:(1) Thermochemistry Facility and Department of Geology, University of California at Davis, Davis, CA 95616, USA;(2) Department of Chemistry and Biochemistry, Brigham Young University, Provo, UT 84602, USA;(3) Department of Civil Engineering and Geological Science, University of Notre Dame, Notre Dame, IN 46556, USA;(4) Dupont Experimental Station E356/209, Wilmington, DE 19880, USA;(5) Present address: Department of Geosciences, Princeton University, Princeton, NJ 08544, USA
Abstract:Crystals of hydronium jarosite were synthesized by hydrothermal treatment of Fe(III)–SO4 solutions. Single-crystal XRD refinement with R1=0.0232 for the unique observed reflections (|Fo| > 4sgrF) and wR2=0.0451 for all data gave a=7.3559(8) Å, c=17.019(3) Å, Vo=160.11(4) cm3, and fractional positions for all atoms except the H in the H3O groups. The chemical composition of this sample is described by the formula (H3O)0.91Fe2.91(SO4)2[(OH)5.64(H2O)0.18]. The enthalpy of formation (DeltaHof) is –3694.5 ± 4.6 kJ mol–1, calculated from acid (5.0 N HCl) solution calorimetry data for hydronium jarosite, gamma-FeOOH, MgO, H2O, and agr-MgSO4. The entropy at standard temperature and pressure (So) is 438.9±0.7 J mol–1 K–1, calculated from adiabatic and semi-adiabatic calorimetry data. The heat capacity (Cp) data between 273 and 400 K were fitted to a Maier-Kelley polynomial Cp(T in K)=280.6 + 0.6149T–3199700T–2. The Gibbs free energy of formation is –3162.2 ± 4.6 kJ mol–1. Speciation and activity calculations for Fe(III)–SO4 solutions show that these new thermodynamic data reproduce the results of solubility experiments with hydronium jarosite. A spin-glass freezing transition was manifested as a broad anomaly in the Cp data, and as a broad maximum in the zero-field-cooled magnetic susceptibility data at 16.5 K. Another anomaly in Cp, below 0.7 K, has been tentatively attributed to spin cluster tunneling. A set of thermodynamic values for an ideal composition end member (H3O)Fe3(SO4)2(OH)6 was estimated: DeltaGof= –3226.4 ± 4.6 kJ mol–1, DeltaHof=–3770.2 ± 4.6 kJ mol–1, So=448.2 ± 0.7 J mol–1 K–1, Cp (T in K)=287.2 + 0.6281T–3286000T–2 (between 273 and 400 K).
Keywords:Hydronium jarosite  Formation enthalpy  Entropy  Spin glass  Crystal structure
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