Hydroxide in olivine: A quantitative determination of the absolute amount and calibration of the IR spectrum

By D. Bell, G. Rossman, J. Maldener, D. Endisch, F. Rauch. 2003

479 citations recorded by the source corpus.

Subfields: Geophysics, Mechanics of Materials

View Paper: https://www.semanticscholar.org/paper/dbdec31bf7541a64c8be8a8141f7e5592991f7e1

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In Mechanics of Materials

Citations in the corpus

A new analysis of experimental data on olivine rheology (2008, methodology): “[2004] is based on the new FTIR calibration by Bell et al. [2003], we also adopt this calibration and multiply a factor of 3.”
The effect of water on the electrical conductivity of olivine aggregates and its implications for the electrical structure of the upper mantle (2009, unknown): “5 (Bell et al., 2003; Hirschmann et al., 2005).”
Hydrogen incorporation in olivine from 2–12 GPa (2006, methodology): “First, Bell et al. (2003) presented a new calibration for H measurement in olivine using Fourier-transform infrared (FTIR) spectroscopy.”
Quantitative absorbance spectroscopy with unpolarized light: Part II. Experimental evaluation and development of a protocol for quantitative analysis of mineral IR spectra (2008, methodology): “We then develop a protocol for obtaining such quantitative analyses of OH in olivine with unpolarized radiation, using the calibrations made with polarized radiation that are available in the literature (i.e., Bell et al. 2003, 2004).”
Effect of water and stress on the lattice-preferred orientation of olivine (2006, methodology): “If a new calibration by Bell et al. (2003) is used, the results should be multiplied by a factor of ∼ 3.”
Lateral variation in upper mantle viscosity: role of water (2004, unknown): “These values may be low by up to a factor of 3 [50].”
Implications of grain size evolution on the seismic structure of the oceanic upper mantle (2008, background): “2 Behn et al.: Grain-size evolution in the oceanic upper mantle, revised for EPSL March 2008 of 3 relative to the values in Hirth & Kohlstedt (2003) based on the calibration for water content 119 in olivine (Bell et al., 2003).”
Water distribution across the mantle transition zone and its implications for global material circulation (2011, unknown): “Throughout this paper, I use the water content determined by using the SIMS calibration (Aubaud et al., 2007; Bell et al., 2003).”
Electrical conductivity anisotropy of dry and hydrous olivine at 8 GPa (2010, methodology): “However, recent studies that 168 utilized polarized FTIR spectroscopy have shown that H2O solubility in olivine is 169 higher by as much or more than a factor of two compared to previous studies that used 170 non-polarized FTIR spectroscopy (Bell et al., 2003; Mosenfelder et al., 2006).”
Solubility of hydrogen in olivine: dependence on temperature and iron content (2004, background): “5 based on the work of Bell et al. (2003) T (K) 1,273 1,323 1,373 1,423 1,473 1,523 1,573 fH2O(MPa) 278 286 293 299 303 307 311”
Anisotropy Versus Heterogeneity in Continental Solid Earth Electromagnetic Studies: Fundamental Response Characteristics and Implications for Physicochemical State (2005, methodology): “(1995), but using newer estimates of solubility and anisotropic defect diffusivities (Kohlstedt and Mackwell, 1998; Simpson, 2002; Bell et al., 2003; Zhao et al., 2004; Simpson and Tommasi, 2005).”
Geodynamic Significance of Seismic Anisotropy of the Upper Mantle: New Insights from Laboratory Studies (2008, background): “The values of water content will need to be modified if different calibrations are used [if the calibration from Bell et al. (2003) is used, the values of water content will be a factor of ∼3 higher than shown in this diagram].”