MR013
Thermal, Chemical and Elastic Properties of Minerals and Metal Alloys with Applications to the Dynamo of Terrestrial-Type Bodies
Session ID#: 161432
Session Description:
Understanding the formation, internal structure, dynamics, and evolution of terrestrial-type bodies requires knowledge of relevant materials at high pressures and high temperatures, including their structural states and their elastic properties. In addition, constraining the thermal properties and heat flow in the interior structure is critical for elucidating the nature of dynamo action in terrestrial-type cores. The aim of this session is to bring together experimentalists and theoreticians whose research constrains core and mantle composition, thermal and chemical evolution, and phase relations of minerals and metal alloys of terrestrial-type bodies for applications to the origin of their magnetic field through dynamo action.
Index Terms:
3914 Electrical properties [MINERAL PHYSICS]
3919 Equations of state [MINERAL PHYSICS]
3924 High-pressure behavior [MINERAL PHYSICS]
3939 Physical thermodynamics [MINERAL PHYSICS]
Primary Convener: Meryem Berrada, University of Western Ontario, Earth Sciences, London, ON, Canada
Convener: Melissa Sims, Johns Hopkins University, Baltimore, MD, United States
Student/Early Career Convener: Claire H Blaske, Arizona State University, School of Earth and Space Exploration, Tempe, AZ, United States
Outer Core Heat Flux in Small Terrestrial Bodies from Electrical Resistivity Measurements of Liquid Fe-8wt%S-4.5wt%Si at High Pressure (1045881)
Eric Lenhart, London, Ontario, CANADA, Wenjun Yong, University of Western Ontario, London, ON, Canada and Richard Secco, Univ Western Ontario, London, ON, Canada
The Increasingly Curious Case of the Lunar Dynamo (Invited) (1051373)
Alexander J Evans, Brown University, Providence, RI, United States, Sonia Tikoo, Stanford University, Department of Geophysics, Stanford, CA, United States and Fiona Nichols-Fleming, Brown University, DEEPS, Providence, United States
Stratification in the Core of Mars by Liquid Immiscibility in Fe-S-H (Invited) (1079973)
Shunpei Yokoo1, Kei Hirose2, Shoh Tagawa1, Guillaume Morard3 and Yasuo Ohishi4, (1)The University of Tokyo, Department of Earth and Planetary Science, Tokyo, Japan, (2)The University of Tokyo, Department of Earth and Planetary Science, Bunkyo, Japan, (3)ISTerre Institute of Earth Sciences, Saint Martin d'Hères, France, (4)Japan Synchrotron Radiation Research Institute, Hyogo, Japan
Sound Velocities of Stishovite at Simultaneous High Pressure and High Temperature: Implication for the X-Discontinuity in the Upper Mantle (1091220)
Sibo Chen1, Siheng Wang1, Xintong Qi2, Man Xu3, Tony Yu4, Yanbin Wang4 and Baosheng Li2, (1)Stony Brook University, Stony Brook, NY, United States, (2)Stony Brook University, Stony Brook, United States, (3)The University of Chicago, Center for Advanced Radiation Sources, Chicago, IL, United States, (4)The University of Chicago, Center for Advanced Radiation Sources, Chicago, United States
Pressure enhances sodium solubility in magnesiowüstite (1093014)
Susannah Dorfman1, Han Hsu2, Farhang Nabiei3, Marco Cantoni3, James Badro4 and Vitali B Prakapenka5, (1)Michigan State University, Department of Earth and Environmental Sciences, East Lansing, MI, United States, (2)NCU National Central University of Taiwan, Jhongli, Taiwan, (3)EPFL Swiss Federal Institute of Technology Lausanne, Lausanne, Switzerland, (4)Institut de Physique du Globe de Paris, Paris, France, (5)The University of Chicago, Center for Advanced Radiation Sources, Chicago, United States
Effects of Hydrogen on Fe-S Alloy System and their Implications for the Martian Core (1098019)
Xuehui Wei, Arizona State University, Tempe, AZ, United States, Stella Chariton, University of Chicago, Center for Advanced Radiation Sources, Chicago, United States, Vitali B Prakapenka, The University of Chicago, Center for Advanced Radiation Sources, Chicago, United States and Sang-Heon Shim, Arizona State University, School of Earth and Space Exploration, Tempe, United States
Measuring the Thermal Conductivity of Iron at Extreme Conditions Using Laser-Driven Ramp Compression (1175660)
Tyler Perez1, Ray Smith2, Patrick LaChappelle3, Dayne E Fratanduono2, Jon Eggert2, Connor Krill4, Yuan Ping2 and June K Wicks5, (1)Johns Hopkins University, Earth & Planetary Sciences, Baltimore, United States, (2)Lawrence Livermore National Laboratory, Livermore, CA, United States, (3)Johns Hopkins University, Earth & Planetary Sciences, Balitmore, United States, (4)Johns Hopkins University, Balitmore, United States, (5)Johns Hopkins University, Earth & Planetary Sciences, Baltimore, MD, United States
Compressional and shear wave velocities of hcp-Fe at simultaneous high P-T conditions: Implications for the Earth’s inner core (1195028)
Siheng Wang1, Sibo Chen1, Xintong Qi2, Man Xu3, Tony Yu3, Yanbin Wang3 and Baosheng Li4, (1)Stony Brook University, Stony Brook, NY, United States, (2)Stony Brook University, Stony Brook, United States, (3)The University of Chicago, Center for Advanced Radiation Sources, Chicago, United States, (4)Mineral Physics Institute, Stony Brook, NY, United States
High-pressure, high-temperature phases of Canyon Diablo iron meteorite: A natural analog for terrestrial planetary cores (1196032)
Mercedes Vasquez1, Sarah M Arveson1, Thomas James Smart2, Yue Meng3, Minta C Akin4, Kanani K M Lee4,5 and Raymond Jeanloz1, (1)University of California Berkeley, Earth and Planetary Science, Berkeley, CA, United States, (2)University of California Berkeley, Physics, Berkeley, United States, (3)HPCAT, X-Ray Science Division, Argonne National Laboratory, Argonne, United States, (4)Lawrence Livermore National Laboratory, Livermore, CA, United States, (5)University of California Berkeley, Earth and Planetary Science, Berkeley, United States
