Abstract
Synthetic deuterated letovicite (ND4)3D(SO4)2 has been investigated using static 2H NMR spectroscopy acquired with a quadrupolar echo sequence. Subsequently, the experimental signals were fitted with theoretical quadrupolar lineshapes to extract the quadrupolar coupling parameters. Experiments were carried out in the temperature range of 102-425 K. Two different signals were distinguished due to ammonium and free acidic deuterons. The ammonium deuterons show only small quadrupolar interaction at room temperature, which can be described best by a fast anisotropic dynamic reorientation of the tetrahedra leading to residual quadrupolar interaction. The dynamically averaged “static” quadrupolar coupling constant is CQ = 2.4 kHz at room temperature. The development of CQ as a function of temperature clearly indicates three phase transitions at 160, 260, and 400 K (triclinic P1 → monoclinic P2/n or Pn → monoclinic C2/c → rhombohedral R3̄m). The asymmetry parameter η shows a similar behavior. It indicates strongest the monoclinic → monoclinic phase transition at 260 K. The lineshape corresponding to the free acidic protons is difficult to simulate because it is strongly superimposed by the dominant ammonium proton resonance. However, the decrease of the quadrupolar coupling constant of the signal from CQ = 108 kHz at 130 K to 31.5 kHz above 370 K can be assigned to a time-averaging of the quadrupolar interaction due to the increased motion of the sulfate tetrahedra about their threefold axis, so that CQ amounts to only 1/3 of the static quadrupolar coupling constant of the static spectrum at low temperatures.
© 2015 by Walter de Gruyter Berlin/Boston
Artikel in diesem Heft
- Evaluation of image classification routines for determining modal mineralogy of rocks from X-ray maps
- Atomic structure and formation mechanism of (301) rutile twins from Diamantina (Brazil)
- Significance of the depth-related transition montmorillonite-beidellite in the Bouillante geothermal field (Guadeloupe, Lesser Antilles)
- High-pressure infrared spectra of talc and lawsonite
- Proton dynamics in letovicite: Part I. Static 1H and 15N NMR MAS experiments and lineshape simulations
- Proton dynamics in letovicite: Part II. Static 2H NMR experiments and lineshape simulations
- Chemical and structural variations at augite (100) deformation twin boundaries
- Comparative compressibility and structural behavior of spinel MgAl2O4 at high pressures: The independency on the degree of cation order
- Multiple breakdown and chemical equilibrium of silicic clinopyroxene under extreme metamorphic conditions in the Kontum Massif, central Vietnam
- Direct EXAFS evidence for incorporation of As5+ in the tetrahedral site of natural andraditic garnet
- Deformation-controlled cation diffusion in tourmaline: A microanalytical study on trace elements and boron isotopes
- Scandium-45 NMR of pyrope-grossular garnets: Resolution of multiple scandium sites and comparison with X-ray diffraction and X-ray absorption spectroscopy
- Partitioning of trace elements among coexisting crystals, melt, and supercritical fluid during isobaric crystallization and melting
- Thermal diffusivity of aluminous spinels and magnetite at elevated temperature with implications for heat transport in Earth’s transition zone
- High-pressure structure and bonding in CaIrO3: The structure model of MgSiO3 post-perovskite investigated with time-of-flight neutron powder diffraction
- Application of major- and trace-element geochemistry to refine U-Pb zircon, and Sm/Nd or Lu/Hf sampling targets for geochronology of HP and UHP eclogites, Western Gneiss Region, Norway
- Measurement of U-Pb ages of uraninite and davidite by laser ablation-HR-ICP-MS
- A modeling approach to understanding the role of microstructure development on crystalsize distributions and on recovering crystal-size distributions from thin slices
- Neptunium substitution in synthetic uranophane and soddyite
- Coexistence of twisted and untwisted crystals: An impurity/structural order model with implications for agate patterns
- Intracrystalline boron isotope partitioning in illite-smectite: Testing the geothermometer
- Mineralogy of the hardpan formation processes in the interface between sulfide-rich sludge and fly ash: Applications for acid mine drainage mitigation
- Dissolution of radiation-damaged zircon in lateritic soils
- Hydrogen analysis in minerals by continuous-flow mass spectrometry
- Re-examination of berlinite (AlPO4) from the Cioclovina Cave, Romania
- Letter. Valence state partitioning of Cr between pyroxene-melt: Effects of pyroxene and melt composition and direct determination of Cr valence states by XANES. Application to Martian basalt QUE 94201 composition
Artikel in diesem Heft
- Evaluation of image classification routines for determining modal mineralogy of rocks from X-ray maps
- Atomic structure and formation mechanism of (301) rutile twins from Diamantina (Brazil)
- Significance of the depth-related transition montmorillonite-beidellite in the Bouillante geothermal field (Guadeloupe, Lesser Antilles)
- High-pressure infrared spectra of talc and lawsonite
- Proton dynamics in letovicite: Part I. Static 1H and 15N NMR MAS experiments and lineshape simulations
- Proton dynamics in letovicite: Part II. Static 2H NMR experiments and lineshape simulations
- Chemical and structural variations at augite (100) deformation twin boundaries
- Comparative compressibility and structural behavior of spinel MgAl2O4 at high pressures: The independency on the degree of cation order
- Multiple breakdown and chemical equilibrium of silicic clinopyroxene under extreme metamorphic conditions in the Kontum Massif, central Vietnam
- Direct EXAFS evidence for incorporation of As5+ in the tetrahedral site of natural andraditic garnet
- Deformation-controlled cation diffusion in tourmaline: A microanalytical study on trace elements and boron isotopes
- Scandium-45 NMR of pyrope-grossular garnets: Resolution of multiple scandium sites and comparison with X-ray diffraction and X-ray absorption spectroscopy
- Partitioning of trace elements among coexisting crystals, melt, and supercritical fluid during isobaric crystallization and melting
- Thermal diffusivity of aluminous spinels and magnetite at elevated temperature with implications for heat transport in Earth’s transition zone
- High-pressure structure and bonding in CaIrO3: The structure model of MgSiO3 post-perovskite investigated with time-of-flight neutron powder diffraction
- Application of major- and trace-element geochemistry to refine U-Pb zircon, and Sm/Nd or Lu/Hf sampling targets for geochronology of HP and UHP eclogites, Western Gneiss Region, Norway
- Measurement of U-Pb ages of uraninite and davidite by laser ablation-HR-ICP-MS
- A modeling approach to understanding the role of microstructure development on crystalsize distributions and on recovering crystal-size distributions from thin slices
- Neptunium substitution in synthetic uranophane and soddyite
- Coexistence of twisted and untwisted crystals: An impurity/structural order model with implications for agate patterns
- Intracrystalline boron isotope partitioning in illite-smectite: Testing the geothermometer
- Mineralogy of the hardpan formation processes in the interface between sulfide-rich sludge and fly ash: Applications for acid mine drainage mitigation
- Dissolution of radiation-damaged zircon in lateritic soils
- Hydrogen analysis in minerals by continuous-flow mass spectrometry
- Re-examination of berlinite (AlPO4) from the Cioclovina Cave, Romania
- Letter. Valence state partitioning of Cr between pyroxene-melt: Effects of pyroxene and melt composition and direct determination of Cr valence states by XANES. Application to Martian basalt QUE 94201 composition