1972 - Fellow of American Geophysical Union (AGU)
1967 - Fellow of American Physical Society (APS)
His primary scientific interests are in Thermodynamics, Bulk modulus, Mineralogy, Elastic modulus and Anharmonicity. The Thermodynamics study combines topics in areas such as Elasticity, Inner core and Core. His work deals with themes such as Volume, Geophysics, Crystal structure, Spinel and Shear modulus, which intersect with Bulk modulus.
His Mineralogy research focuses on Porosity and how it connects with Sound and Fracture. His biological study spans a wide range of topics, including Grüneisen parameter, Debye model and Atmospheric temperature range. His Debye model research includes elements of Absolute zero and Equation of state.
Orson L. Anderson spends much of his time researching Thermodynamics, Mineralogy, Bulk modulus, Thermal and Anharmonicity. His research in Thermal expansion, Debye model, Grüneisen parameter, Volume and Equation of state are components of Thermodynamics. His studies deal with areas such as Single crystal and Heat capacity as well as Debye model.
His Mineralogy research incorporates elements of Elasticity, Crystallite, Sound, Elastic modulus and Isotropy. His research investigates the connection between Bulk modulus and topics such as Adiabatic process that intersect with issues in Analytical chemistry. Orson L. Anderson works mostly in the field of Thermal, limiting it down to topics relating to Mantle and, in certain cases, Plate tectonics.
Orson L. Anderson mainly investigates Thermodynamics, Geophysics, Mineralogy, Inner core and Thermal. His work on Equation of state and Bulk modulus as part of general Thermodynamics research is frequently linked to Piston cylinder, thereby connecting diverse disciplines of science. His studies in Bulk modulus integrate themes in fields like Cube root, Crystal structure and Wurtzite crystal structure.
His study in the field of Core–mantle boundary also crosses realms of Earth. His Inner core study integrates concerns from other disciplines, such as Alloy, Core and Analytical chemistry. In his study, Forsterite, Peridot and Heat capacity is strongly linked to Volume, which falls under the umbrella field of Thermal.
His primary areas of study are Thermodynamics, Inner core, Alloy, Outer core and Impurity. His research in the fields of Isothermal process, Thermal and Triple point overlaps with other disciplines such as Melting curve analysis. His Inner core study incorporates themes from Amplitude, Crystallography, Debye model and Analytical chemistry.
Orson L. Anderson combines subjects such as Mean squared displacement, X-ray crystallography, Diffraction and Debye with his study of Analytical chemistry. His Alloy research is multidisciplinary, relying on both Core and Silicon. His Outer core study often links to related topics such as Thermal conductivity.
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A simplified method for calculating the debye temperature from elastic constants
Orson L. Anderson.
Journal of Physics and Chemistry of Solids (1963)
Elastic constants and their measurement
Edward Schreiber;Orson L. Anderson;Naohiro Soga;James F. Bell.
Elastic moduli, pressure derivatives, and temperature derivatives of single‐crystal olivine and single‐crystal forsterite
Mineo Kumazawa;Orson L. Anderson.
Journal of Geophysical Research (1969)
Some elastic constant data on minerals relevant to geophysics
Orson L. Anderson;Edward Schreiber;Robert C. Liebermann;Naohiro Soga.
Reviews of Geophysics (1968)
Anharmonicity and the equation of state for gold
Orson L. Anderson;Donald G. Isaak;Shigeru Yamamoto.
Journal of Applied Physics (1989)
Stress corrosion theory of crack propagation with applications to geophysics
Orson L. Anderson;Priscilla C. Grew.
Reviews of Geophysics (1977)
The bulk modulus-volume relationship for oxide compounds and related geophysical problems
Orson L. Anderson;John E. Nafe.
Journal of Geophysical Research (1965)
High‐temperature elastic constant data on minerals relevant to geophysics
Orson L. Anderson;Donald Isaak;Hitoshi Oda.
Reviews of Geophysics (1992)
Brief report: The bulk modulus‐volume relationship for oxides
Don L. Anderson;Orson L. Anderson.
Journal of Geophysical Research (1970)
Elasticity of single‐crystal forsterite measured to 1700 K
Donald G. Isaak;Orson L. Anderson;Takayasu Goto;Isao Suzuki.
Journal of Geophysical Research (1989)
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