MR24A:
Elastic and Transport Properties of Core and Mantle Materials I
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MR24A:
Elastic and Transport Properties of Core and Mantle Materials I
Elastic and Transport Properties of Core and Mantle Materials I
Session ID#: 34570
Session Description:
Understanding the properties of mantle and core materials, such as sound velocity, thermal and
electrical conductivity, diffusivity and viscosity at extreme conditions is essential for modeling of the
internal structure of planets. In particular, knowledge of elastic and transport properties allows the
translation of variations in seismic velocities laterally and vertically to the composition, temperature
and dynamics of the deep Earth. In addition, constraints on the major element abundances,
oxidation state, deep volatile budget, light element content, temperature, and dynamics of planetary
mantles and cores require precise knowledge of the elastic and transport properties of planetary
materials at high-pressures and temperatures. In order to construct a self-consistent database for
the broader geophysics community, it is important to cross-validate the results of elastic and
transport properties from different experimental and computational techniques. This multi-disciplinary
session invites contributions from experimental, theoretical and observational studies that contribute
towards building models of the structure and dynamics of the interiors of Earth and other planetary
bodies.
electrical conductivity, diffusivity and viscosity at extreme conditions is essential for modeling of the
internal structure of planets. In particular, knowledge of elastic and transport properties allows the
translation of variations in seismic velocities laterally and vertically to the composition, temperature
and dynamics of the deep Earth. In addition, constraints on the major element abundances,
oxidation state, deep volatile budget, light element content, temperature, and dynamics of planetary
mantles and cores require precise knowledge of the elastic and transport properties of planetary
materials at high-pressures and temperatures. In order to construct a self-consistent database for
the broader geophysics community, it is important to cross-validate the results of elastic and
transport properties from different experimental and computational techniques. This multi-disciplinary
session invites contributions from experimental, theoretical and observational studies that contribute
towards building models of the structure and dynamics of the interiors of Earth and other planetary
bodies.
Primary Convener: Jiachao Liu, Michigan State University, Earth and Environmental Sciences, East Lansing, United States
Conveners: Hauke Marquardt, Bayerisches Geoinstitut, Universitaet Bayreuth, Bayreuth, Germany, Stephen Stackhouse, University of Leeds, School of Earth and Environment, Leeds, LS2, United Kingdom and Mainak Mookherjee, Florida State University, Earth, Ocean, and Atmospheric Science, Tallahassee, FL, United States
Chairs: Mainak Mookherjee, Florida State University, Earth, Ocean, and Atmospheric Science, Tallahassee, FL, United States and Jiachao Liu, Michigan State University, Earth and Environmental Sciences, East Lansing, United States
OSPA Liaison: Jiachao Liu, Michigan State University, Earth and Environmental Sciences, East Lansing, United States
Cross-Listed:
- DI - Study of the Earth's Deep Interior
- P - Planetary Sciences
- S - Seismology
- V - Volcanology, Geochemistry and Petrology
Index Terms:
3909 Elasticity and anelasticity [MINERAL PHYSICS]
3924 High-pressure behavior [MINERAL PHYSICS]
5120 Plasticity, diffusion, and creep [PHYSICAL PROPERTIES OF ROCKS]
Abstracts Submitted to this Session:
Diffusive Transport and Structural Properties of Liquid Iron Alloys at High Pressure (Invited) (212618)
Electron-Electron Scattering And Thermal Conductivity Of Iron At Inner Earth's Core Conditions (253825)
See more of: Mineral and Rock Physics
