Abstract
Structural analysis, using neutron powder diffraction (NPD) data on small quantities (<300 mg) and in combination with single-crystal X-ray diffraction (SXD) data, has been employed to determine accurately the position of hydrogen and other light atoms in three rare beryllate minerals, namely bavenite, leifite/IMA 2007-017, and nabesite. For bavenite, leifite/IMA 2007-017, and nabesite, significant differences in the distribution of H, as compared to the literature using SXD analysis alone, have been found. The benefits of NPD data, even with small quantities of H-containing materials, and, more generally, in applying a combined SXD-NPD method to structure analysis of minerals are discussed, with reference to the quality of the crystallographic information obtained.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Fe site occupancy in magnetite-ulvöspinel solid solutions: A new approach using X-ray magnetic circular dichroism
- Discovery, mineral paragenesis, and origin of wadalite in a meteorite
- Cathodoluminescence microscopy and spectroscopy of synthetic ruby crystals grown by the optical floating zone technique
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- Recrystallization in fully metamict gadolinite from Ytterby (Sweden), annealed in air and studied by 57Fe Mössbauer spectroscopy
- Fantappièite, a new mineral of the cancrinite-sodalite group with a 33-layer stacking sequence: Occurrence and crystal structure
- Reinvestigation of the crystal structure of the zeolite gobbinsite: A single-crystal X-ray diffraction study
- Arsenic-rich fergusonite-beta-(Y) from Mount Cervandone (Western Alps, Italy): Crystal structure and genetic implications
- Crystal structure and low-temperature behavior of “disordered” thomsonite
- Cooling-induced crystallization of microlite crystals in two basaltic pumice clasts
- Crystal structure analyses of four tourmaline specimens from the Cleopatra’s Mines (Egypt) and Jabal Zalm (Saudi Arabia), and the role of Al in the tourmaline group
- Combined single-crystal X-ray and neutron powder diffraction structure analysis exemplified through full structure determinations of framework and layer beryllate minerals
- Olivine crystal size distributions in kimberlite
- Solubility of manganotantalite and manganocolumbite in pegmatitic melts
- The effect of silica on ferric/ferrous ratio in silicate melts: An experimental study using Mössbauer spectroscopy
- HRTEM investigation of trilling todorokite and nano-phase Mn-oxides in manganese dendrites
- Thermo-chemical and thermo-physical properties of the high-pressure phase anhydrous B (Mg14Si5O24): An ab-initio all-electron investigation
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- Sulfide oxidation observed using micro-Raman spectroscopy and micro-X-ray diffraction: The importance of water/rock ratios and pH conditions
- In situ measurements of plagioclase growth using SIMS depth profiles of 7Li/30Si: A means to acquire crystallization rates during short-duration decompression events
- Crystal chemistry of the MgAl2O4-MgMn2O4-MnMn2O4 system: Analysis of structural distortion in spinel- and hausmannite-type structures
- The effect of Al and water on the compressibility of diopside
- Geothermometric study of Mg-rich spinels from the Somma-Vesuvius volcanic complex (Naples, Italy)
- Serpentine minerals discrimination by thermal analysis
- A new type of cubic-stacked layer structure in anthoinite, AlWO3(OH)3
- Townendite, Na8ZrSi6O18, a new uranium-bearing lovozerite group mineral from the Ilímaussaq alkaline complex, Southern Greenland
- Letter. Pressure-induced transformations in kaolinite
- Letter. The crystal structure of gypsum-II determined by single-crystal synchrotron X-ray diffraction data