Home Trona at extreme conditions: A pollutant-sequestering material at high pressures and low temperatures
Article
Licensed
Unlicensed Requires Authentication

Trona at extreme conditions: A pollutant-sequestering material at high pressures and low temperatures

  • Earl O’Bannon III. EMAIL logo , Christine M. Beavers and Quentin Williams
Published/Copyright: October 14, 2014
Become an author with De Gruyter Brill

Abstract

Single-crystal X‑ray diffraction of trona, Na3CO3HCO3·2H2O, was measured between 100 and 340 K at ambient pressures, and the infrared and Raman spectra of this material characterized to ∼25 GPa. The thermal expansion of trona is greatest in the b direction, which is due to a particularly large expansion of the long Na2-O1 and the short Na2-O4 bonds within the sodium septahedron in the trona structure. This crystallographic direction is associated with the distance between neighboring carbonate groups and neighboring water molecules within the structure. The dimensions of the carbonate group undergo no systematic changes over this temperature range, and the disordered hydrogen atom within the structure does not order at temperatures down to 100 K. Thus, detailed changes in the geometry of the sodium polyhedra primarily modulate the response of trona to decreases in temperature. The infrared and Raman spectra undergo discontinuous and reversible changes at ∼7 and ∼14.5 GPa: the former of these phase transitions is likely associated with a shift primarily in the sodium-oxygen polyhedra, while the latter also involves shifts in bonding of the carbonate groups. New assignments are suggested for portions of the vibrational spectrum based on the high-pressure results. Resonance effects between different vibrational modes are observed, including the observation of a transmission maximum associated with a resonant interaction between the carbonate symmetric stretching vibration and a broad mode at similar frequencies. The behavior of trona under extreme conditions is useful for understanding CO2-vapor-saturated alkali-rich systems, and late-stage peralkaline magmatic processes and, in its usage as both a sorbent and scrubber of SO2 and CO2 in flue gasses and lignite coals.

Received: 2014-2-3
Accepted: 2014-4-29
Published Online: 2014-10-14
Published in Print: 2014-10-1

© 2014 by Walter de Gruyter Berlin/Boston

Articles in the same Issue

  1. Highlights and Breakthroughs. Pauling’s rules, in a world of non-spherical atoms
  2. Highlights and Breakthroughs. Theoretical and applied implications of the structural order of irradiated vermiculite
  3. Highlights and Breakthroughs. An examination of the Ti-in-quartz thermobarometer in rocks that contain dynamically recrystallized quartz: Re-equilibration of [Ti] during recrystallization
  4. The Second Conference on the Lunar Highlands Crust and New Directions. Visible-infrared spectral properties of iron-bearing aluminate spinel under lunar-like redox conditions
  5. The Second Conference on the Lunar Highlands Crust and New Directions. VNIR spectral variability of the igneous stratified Stillwater Complex: A tool to map lunar highlands
  6. The Second Conference on the Lunar Highlands Crust and New Directions. Spinel-rich lithologies in the lunar highland crust: Linking lunar samples with crystallization experiments and remote sensing
  7. The Second Conference on the Lunar Highlands Crust and New Directions. Phosphate-halogen metasomatism of lunar granulite 79215: Impact-induced fractionation of volatiles and incompatible elements
  8. The Second Conference on the Lunar Highlands Crust and New Directions. Reflectance spectroscopy of plagioclase-dominated mineral mixtures: Implications for characterizing lunar anorthosites remotely
  9. The Second Conference on the Lunar Highlands Crust and New Directions. The distribution of Mg-spinel across the Moon and constraints on crustal origin
  10. The occurrence and composition of chevkinite-(Ce) and perrierite-(Ce) in tholeiitic intrusive rocks and lunar mare basalt
  11. Garnet as a major carrier of the Y and REE in the granitic rocks: An example from the layered anorogenic granite in the Brno Batholith, Czech Republic
  12. Mid-infrared optical constants of clinopyroxene and orthoclase derived from oriented single-crystal reflectance spectra
  13. Time-resolved synchrotron X-ray diffraction study of the dehydration behavior of chalcophanite
  14. Ab initio investigations of dioctahedral interlayer-deficient mica: Modeling particles of illite found within gas shale
  15. Trona at extreme conditions: A pollutant-sequestering material at high pressures and low temperatures
  16. In-situ U-Th/Pb geochronology of (urano)thorite
  17. Temperature-induced amorphization of Na-zeolite A: A view from multi-nuclear high-resolution solid-state NMR
  18. “Silicified” pyrochlore from nepheline syenite (mariupolite) of the Mariupol Massif, SE Ukraine: A new insight into the role of silicon in the pyrochlore structure
  19. Physio-chemical properties of gamma-irradiated vermiculite and their significance for radiation protection and thermoluminescence
  20. Ti resetting in quartz during dynamic recrystallization: Mechanisms and significance
  21. Thermodynamic study of monoclinic pyrrhotite in equilibrium with pyrite in the Ag-Fe-S system by solid-state electrochemical cell technique
  22. Phase diagram and P-V-T equation of state of Al-bearing seifertite at lowermost mantle conditions
  23. Crystal structure of Guinier-Preston zones in orthopyroxene: Z-contrast imaging and ab inito study
  24. Crystal chemistry and surface configurations of two polylithionite-1M crystals
  25. Crystal chemistry of synthetic Ti-Mg-bearing hibonites: A single-crystal X-ray study
  26. Mineralogy and crystal chemistry of Mn, Fe, Co, Ni, and Cu in a deep-sea Pacific polymetallic nodule
  27. Agakhanovite-(Y), ideally (YCa)⃞2KBe3Si12O30, a new milarite-group mineral from the Heftetjern pegmatite, Tørdal, Southern Norway: Description and crystal structure
  28. Actinides in Geology, Energy, and the Environment. Ichnusaite, Th(MoO4)2·3H2O, the first natural thorium molybdate: Occurrence, description, and crystal structure
  29. Actinides in Geology, Energy, and the Environment. Quantification of α-particle radiation damage in zircon
  30. What Lurks in the Martian Rocks and Soil? Investigations of Sulfates, Phosphates, and Perchlorates. Spectral properties of Ca-sulfates: Gypsum, bassanite, and anhydrite
  31. What Lurks in the Martian Rocks and Soil? Investigations of Sulfates, Phosphates, and Perchlorates. Flower-like apatite recording microbial processes through deep geological time and its implication to the search for mineral records of life on Mars
  32. What Lurks in the martian Rocks and Soil? Investigations of Sulfates, Phosphates, and Perchlorates. Gypsum in modern Kamchatka volcanic hot springs and the Lower Cambrian black shale: Applied to the microbial-mediated precipitation of sulfates on Mars
  33. Letter. Identification of hydrogen defects linked to boron substitution in synthetic forsterite and natural olivine
  34. Letter. Densified glasses as structural proxies for high-pressure melts: Configurational compressibility of silicate melts retained in quenched and decompressed glasses
  35. Letter. Geobarometry from host-inclusion systems: The role of elastic relaxation
  36. New Mineral Names
  37. Book Review
Downloaded on 9.9.2025 from https://www.degruyterbrill.com/document/doi/10.2138/am-2014-4919/html
Scroll to top button