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Experimental constraints on hydrogen solubility in pyrolytic melts
AGU 2024
study of earth's deep interior | 11 december 2024
Francesca Miozzi, Anat Shahar, James Badro, Jing Y...
The question about the interaction of H2 rich atmospheres with planetary interiors during formation and accretion is at the forefront in the field of ...
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Measurements of electrical conductivity of iron at Earth core conditions
AGU 2024
study of earth's deep interior | 09 december 2024
Zachary M. Geballe, Jing Yang, Vasilije V Dobrosa...
Earths core cooling rate is controlled by thermal conduction from the core into the mantle. One crucial piece of knowledge for modeling this process i...
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“INTREPID”: A New Open Source Python Code to Model the 1D Internal Structure and Thermal Evolution of Rocky Planets with Arbitrary Composition and Mass, With Applications to Solar System and Exo-Planets
AGU 2024
study of earth's deep interior | 09 december 2024
Peter E. Driscoll, Francesca Miozzi
The evolution of rocky planet surfaces and magnetic fields are fundamentally determined by the mass, composition, and dynamics of their interiors. Exi...
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In situ femtosecond diffraction in dynamically compressed TiO2: Extreme lowering of synthesis pressure of the Fe2P-type phase
ADVANCED EXPERIMENTAL, COMPUTATIONAL, AND ANALYTICAL APPROACHES IN EXPLORING DEEP PLANETARY INTERIORS IV ORAL
mineral and rock physics | 12 december 2023
Ian K. Ocampo, Donghoon Kim, Francesca Miozzi, Mar...
Rutile, TiO2, is a widely distributed accessory mineral in the Earths crust. As a result of its abundance as well as the presence of three naturally o...
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Iron Melting at 80 GPa Using Pulsed Joule Heating
ADVANCED EXPERIMENTAL, COMPUTATIONAL AND ANALYTICAL APPROACHES IN EXPLORING DEEP PLANETARY INTERIORS IV ORAL
mineral and rock physics | 15 december 2022
Zachary M. Geballe, Jing Yang, Francesca Miozzi, C...
Measurements of the melting curve of iron are important for understanding Earth's core, from its formation, to the way it crystallizes and loses heat....
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Dynamic probing of the high pressure and temperature phase transitions of iron on millisecond timescales
ADVANCED EXPERIMENTAL, COMPUTATIONAL AND ANALYTICAL APPROACHES IN EXPLORING DEEP PLANETARY INTERIORS II POSTER
mineral and rock physics | 15 december 2022
Silvia Pandolfi, Matthew Ricks, Francesca Miozzi, ...
We investigate the high pressure (HP) and high temperature (HT) phase transitions of iron using the fast-loading dynamic-diamond anvil cell (d-DAC) se...
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Structural and Electronic Transitions in Liquid FeO Under High Pressure
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
05 november 2022
Guillaume Morard, Daniele Antonangeli, Johann Bouc...
FeO represents an important end‐member for planetary interiors mineralogy. However, its properties in the liquid state under high pressure ar...
An experimental study on the solubility of diamond in aqueous fluids at 5 GPa and 950˚C.
HYDROGEN AND CARBON IN THE SOLID EARTH FROM CRUST TO CORE I ORAL
mineral and rock physics | 14 december 2021
Francesca Miozzi, Simone Tumiati, Patrizia Fumagal...
In recent years efforts have been made to investigate the solubility of graphitic carbon in aqueous fluids at high pressure, high temperature conditio...
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