4.4 Article

Investigation of hydrogen sites of wadsleyite: A neutron diffraction study

Journal

PHYSICS OF THE EARTH AND PLANETARY INTERIORS
Volume 189, Issue 1-2, Pages 56-62

Publisher

ELSEVIER
DOI: 10.1016/j.pepi.2011.07.003

Keywords

Wadsleyite; Neutron diffraction; Water; Mantle transition zone

Funding

  1. Japan Society for the Promotion of Science
  2. Photon Factory in KEK, Japan [2008G518, 2010G015]
  3. Grants-in-Aid for Scientific Research [22000002, 20103002] Funding Source: KAKEN

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A neutron powder diffraction experiment was conducted to refine the hydrogen position of Mg-endmember deuterated wadsleyite. Preliminary refinement using the dry-structure determined by single crystal X-ray diffraction reveals a maximum peak Q1 of nuclear density in the difference Fourier map at the M3 octahedral edge, between the O1 and O4 atoms (3.071(3)angstrom). Full Rietveld refinement was conducted assuming that the maximum peak corresponds to deuterium atom. The deuterium position was determined as (0.096, 0.289, 0.315) with occupancy of 8.2%. The O1-D1 vector lies along M3 octahedral edge pointing 04 atom, and the bond length is determined as 1.037(15)angstrom for O1-D1, and 2.041(15)angstrom for D1 center dot center dot center dot O4. The O1-D1 center dot center dot center dot O4 geometry is almost linear with angle of 171.7(5)degrees. The residual peak Q2 was found in the map at (0, 0.172, 0.268), suggesting the existence of a bent hydrogen bond between O1 center dot center dot center dot O3 (3.035 angstrom) of the M3 octahedral edge. The respective distances from the surrounding oxygen atoms are 0.97 and 2.13 angstrom for O1-Q2 and Q2 center dot center dot center dot O3. The O1-Q2 center dot center dot center dot O3 configuration is nonlinear, with angle of 154.4 degrees. These results reveal that the dominant site of protonation in wadsleyite is the 01 site, which is consistent with the previous prediction. (C) 2011 Elsevier B.V. All rights reserved.

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