TY - JOUR
T1 - Investigation of hydrogen sites of wadsleyite
T2 - A neutron diffraction study
AU - Sano-Furukawa, Asami
AU - Kuribayashi, Takahiro
AU - Komatsu, Kazuki
AU - Yagi, Takehiko
AU - Ohtani, Eiji
PY - 2011/11
Y1 - 2011/11
N2 - 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). å). 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 O4 atom, and the bond length is determined as 1.037(15). å for O1-D1, and 2.041(15). å for D1cṫO4. The O1-D1cṫO4 geometry is almost linear with angle of 171.7(5) ° The residual peak Q2 was found in the map at (0, 0.172, 0.268), suggesting the existence of a bent hydrogen bond between O1cṫO3 (3.035. å) of the M3 octahedral edge. The respective distances from the surrounding oxygen atoms are 0.97 and 2.13. å for O1-Q2 and Q2cṫO3. The O1-Q2cṫO3 configuration is nonlinear, with angle of 154.4 ° These results reveal that the dominant site of protonation in wadsleyite is the O1 site, which is consistent with the previous prediction.
AB - 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). å). 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 O4 atom, and the bond length is determined as 1.037(15). å for O1-D1, and 2.041(15). å for D1cṫO4. The O1-D1cṫO4 geometry is almost linear with angle of 171.7(5) ° The residual peak Q2 was found in the map at (0, 0.172, 0.268), suggesting the existence of a bent hydrogen bond between O1cṫO3 (3.035. å) of the M3 octahedral edge. The respective distances from the surrounding oxygen atoms are 0.97 and 2.13. å for O1-Q2 and Q2cṫO3. The O1-Q2cṫO3 configuration is nonlinear, with angle of 154.4 ° These results reveal that the dominant site of protonation in wadsleyite is the O1 site, which is consistent with the previous prediction.
KW - Mantle transition zone
KW - Neutron diffraction
KW - Wadsleyite
KW - Water
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U2 - 10.1016/j.pepi.2011.07.003
DO - 10.1016/j.pepi.2011.07.003
M3 - Article
AN - SCOPUS:80955163815
SN - 0031-9201
VL - 189
SP - 56
EP - 62
JO - Physics of the Earth and Planetary Interiors
JF - Physics of the Earth and Planetary Interiors
IS - 1-2
ER -