Structure and elasticity of single‐crystal (Mg,Fe)O and a new method of generating shear waves for gigahertz ultrasonic interferometry

By S. Jacobsen, H. Reichmann, H. Spetzler, S. Mackwell, J. Smyth, R. Angel, C. McCammon. 2002

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Very low sound velocities in iron‐rich (Mg,Fe)O: Implications for the core‐mantle boundary region (2010, methodology): “84)O from an ultrasonic study [Jacobsen et al., 2002].”
Lower mantle composition and temperature from mineral physics and thermodynamic modelling (2005, background): “However, a recent study by Jacobsen et al. (2002) shows that the bulk modulus of (Mg1−x ,Fex )O remains relatively constant (within experimental uncertainties) up to at least x = 0.3.”
Deformation of polycrystalline MgO at pressures of the lower mantle (2002, background): “Ambient conditions measurements of elastic moduli show that A is essentially constant from pure periclase end-member to compositions with $25% FeO, but then decreases sharply with the FeO end-member being nearly isotropic [Jacobsen et al., 2002].”
Solids, liquids, and gases under high pressure (2018, methodology): “Utilizing single-crystal XRD and gigahertz ultrasonic interferometry to generate high-frequency shear waves, Jacobsen et al. (2002) studied the effects of nonstoichiometry on the elastic moduli of (Mg,Fe)O.”