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Pressure‐induced enhancement of proton conduction in brucite
Author(s) -
Guo Xinzhuan,
Yoshino Takashi
Publication year - 2014
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2013gl058627
Subject(s) - brucite , conductivity , proton , materials science , thermal conduction , electrical resistivity and conductivity , crystal (programming language) , perpendicular , hydrogen , crystal structure , nuclear magnetic resonance , dielectric spectroscopy , analytical chemistry (journal) , chemistry , magnesium , crystallography , composite material , physics , geometry , mathematics , organic chemistry , quantum mechanics , electrochemistry , electrode , chromatography , computer science , metallurgy , programming language
The electrical conductivity of single‐crystal brucite was measured as a function of pressure and temperature (P‐T) using impedance spectroscopy (IS). IS measurements demonstrated that electrical conductivity perpendicular to the c axis is nearly half order of magnitude higher than that parallel to the c axis under the same P‐T conditions. Electrical conductivity increased by 2 orders of magnitude during compression from 3.7 to 11 GPa, irrespective of crystallographic direction. However, the conductivity increase with pressure became less significant upon further compression from 11 to 13 GPa. The pressure effect is closely related to the interactions between neighboring hydroxyls. The ratio of free protons to total hydrogen increases from 2% to 33% when pressure increases from 3.7 to 13 GPa at 950 K. This indicates that most of the protons are bound within the crystal structure at low pressures, whereas more protons become free and mobile at higher pressures.