Home Physical Sciences (H3O)Fe(SO4)2 formed by dehydrating rhomboclase and its potential existence on Mars
Article
Licensed
Unlicensed Requires Authentication

(H3O)Fe(SO4)2 formed by dehydrating rhomboclase and its potential existence on Mars

  • Wenqian Xu EMAIL logo , John B. Parise and Jonathan Hanson
Published/Copyright: April 2, 2015
Become an author with De Gruyter Brill

Abstract

Rhomboclase, (H5O2)Fe(SO4)2·2H2O, transforms to a solid crystalline phase, (H3O)Fe(SO4)2, upon dehydration. The structure of (H3O)Fe(SO4)2 is found to be the same as a recently reported structure determined from single-crystal diffraction by Peterson et al. (2009), who synthesized the same compound using a hydrothermal method. The phase boundary between rhomboclase and (H3O)Fe(SO4)2 as a function of temperature (T) and relative humidity (RH) was determined by environment-controlled in situ X-ray diffraction (XRD) method. The stability of (H3O)Fe(SO4)2 against rhomboclase was further evaluated under a simulated martian condition (constant 50% RH, -20 °C, 6 mbar CO2). Both phases remained after 14 days with no observable transition. This result suggests that hydrate ferric sulfate minerals might not respond to diurnal RH fluctuation under the extremely slowed kinetics expected on the martian surface.

Received: 2009-12-4
Accepted: 2010-6-3
Published Online: 2015-4-2
Published in Print: 2010-10-1

© 2015 by Walter de Gruyter Berlin/Boston

Articles in the same Issue

  1. Ti-Al zoning of experimentally grown titanite in the system CaO-Al2O3-TiO2-SiO2-NaCl-H2O-(F): Evidence for small-scale fluid heterogeneity
  2. A new method for quantitative petrography based on image processing of chemical element maps: Part I. Mineral mapping applied to compacted bentonites
  3. A new method for quantitative petrography based on image processing of chemical element maps: Part II. Semi-quantitative porosity maps superimposed on mineral maps
  4. Enhancement of solid-state reaction rates by non-hydrostatic stress effects on polycrystalline diffusion kinetics
  5. (H3O)Fe(SO4)2 formed by dehydrating rhomboclase and its potential existence on Mars
  6. Crystal chemistry and low-temperature behavior of datolite: A single-crystal X-ray diffraction study
  7. Density and seismic velocities of chromitite body in oceanic mantle peridotite
  8. Packing schemes of cavities in selected clathrasils and zeolites and the analogous packings of atoms in crystal structures
  9. Temperature dependence of IR absorption of OH species in clinopyroxene
  10. Thermal behavior of vibrational phonons and hydroxyls of muscovite in dehydroxylation: In situ high-temperature infrared spectroscopic investigations
  11. Kinetics of Fe-oxidation/deprotonation process in Fe-rich phlogopite under isothermal conditions
  12. On the crystal chemistry of londonite [(Cs,K,Rb)Al4Be5B11O28]: A single-crystal neutron diffraction study at 300 and 20 K
  13. High-pressure melting of wüstite
  14. Primary Nb-Ta minerals in the Szklary pegmatite, Poland: New insights into controls of crystal chemistry and crystallization sequences
  15. Evolution of the interlayer space of hydrated montmorillonite as a function of temperature
  16. Morphology of pyrite in particulate matter from shallow submarine hydrothermal vents
  17. Influence of the fluid composition on diamond dissolution forms in carbonate melts
  18. Far infrared spectroscopy of carbonate minerals
  19. Assessment of the diamond-trap method for studying high-pressure fluids and melts and an improved freezing stage design for laser ablation ICP-MS analysis
  20. Françoisite-(Ce), a new mineral species from La Creusaz uranium deposit (Valais, Switzerland) and from Radium Ridge (Flinders Ranges, South Australia): Description and genesis
  21. Crystal chemistry and origin of grandidierite, ominelite, boralsilite, and werdingite from the Bory Granulite Massif, Czech Republic
  22. Lead-tellurium oxysalts from Otto Mountain near Baker, California: III. Thorneite, Pb6(Te26+O10)(CO3)Cl2(H2O), the first mineral with edge-sharing octahedral tellurate dimers
  23. Lead-tellurium oxysalts from Otto Mountain near Baker, California: IV. Markcooperite, Pb(UO2)Te6+O6, the first natural uranyl tellurate
  24. Lead-tellurium oxysalts from Otto Mountain near Baker, California: V. Timroseite, Pb2Cu52+(Te6+O6)2(OH)2, and paratimroseite, Pb2Cu42+(Te6+O6)2(H2O)2, two new tellurates with Te-Cu polyhedral sheets
  25. Lead-tellurium oxysalts from Otto Mountain near Baker, California: VI. Telluroperite, Pb3Te4+O4Cl2, the Te analog of perite and nadorite
  26. The determination of sulfate and sulfide species in hydrous silicate glasses using Raman spectroscopy
  27. The structure of crystals, glasses, and melts along the CaO-Al2O3 join: Results from Raman, Al L- and K-edge X-ray absorption, and 27Al NMR spectroscopy
  28. Ordering of iron vacancies in monoclinic jarosites
Downloaded on 10.2.2026 from https://www.degruyterbrill.com/document/doi/10.2138/am.2010.3470/html
Scroll to top button