Marco Cantoni

1982-1988, Diploma course in Experimental Physics (certificate, 28.10.88)ETHZ Faculty IX MATHEMATICS and PHYSICS, Diploma Thesis: "Abweichungen von der ikosaedrischen Symmetrie in Al-Cu-Li Quasikristallen", Advisor: Prof. H.-U. Nissen 1989-1993, Ph.D. in Experimental Physics (certificate, 23.8.94) ETHZ Physics Department, Laboratory of Solid State Physics, Ph. D. Thesis No. 10421, Title: "Elektronenmikroskopische Untersuchung der Realkristallstruktur epitaktischer Schichten von Supraleitern des Typs SEBa2Cu3O7-x auf (100)-SrTiO3" Advisors: Prof. H.R. Ott, Prof. H. U. Nissen. 1994-1996,ETH Zürich,Material Science Department, Non-Metallic Materials, Prof. L. Gauckler: Microstructure characterisation of high-tech ceramic materials by means of SEM, TEM and atomic force microscopy: superconductor thick films (Bi-2212 on Ag) and solid oxide fuel cells (ZrO2, CeO2). 1996-1998, National Institute for Research in Inorganic Materials NIRIM, Japan Group for Special Research, Prof. S. Horiuchi: TEM of Bi-2223/Ag Tapes, Application of Imaging Plates (IP) in High Voltage TEM, Cryo-Lorentz-TEM of Superconducting Materials (Observation of Flux-Lines) 1998-2000, Ecole polytechnique fédéral de Lausanne, EPFL-CIME Centre interdépartemental de microscopie électronique CIME, Prof. P.A. Buffat: Projet 125, PPO II (programme prioritaire optique): Characterization of materials and devices for optic and optoelectronic applications by electron microscopy. 2001-2003, Ecole polytechnique fédéral de Lausanne, EPFL STI IMX LCCeramics Laboratory, Prof. Nava Setter Characterisation of ferroelectric materials, transmission electron microscopy of relaxor ferroelectric materials 2004, University of Geneva, Physics Department, Condensed matter Physics Group of Prof. R. Flükiger, TEM of Multifilament Nb3Sn superconducting wires, in collaboration with EPFL-CIME Since 1.11.04, EPFL-SB-CIME

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Electron microscope

An electron microscope is a microscope that uses a beam of electrons as a source of illumination. They use electron optics that are analogous to the glass lenses of an optical light microscope. As

Transmission electron microscopy

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Focused ion beam

Focused ion beam, also known as FIB, is a technique used particularly in the semiconductor industry, materials science and increasingly in the biological field for site-specific analysis, deposition,

MSE-352: Introduction to microscopy + Laboratory work

Ce cours d'introduction à la microscopie a pour but de donner un apperçu des différentes techniques d'analyse de la microstructure et de la composition des matériaux, en particulier celles liées aux microscopies électronique et optique. Le cours comprend des cours ainsi que des démonstrations.

MSE-636(a): Scanning electron microscopy techniques (a)

This intensive course is intended for researchers who envisage to use scanning electron microscopy techniques for their research or who want to understand how to interpret SEM images and analytical results presented in scientific publications.

MSE-636(b): Scanning electron microscopy techniques (b)

Composition and Pressure Effects on Partitioning of Ferrous Iron in Iron-Rich Lower Mantle Heterogeneities

James Badro, Charles-Edouard Boukaré, Marco Cantoni, Susannah McGregor Dorfman, Philippe Gillet, Farhang Nabiei

Both seismic observations of dense low shear velocity regions and models of magma ocean crystallization and mantle dynamics support enrichment of iron in Earth’s lowermost mantle. Physical properties of iron-rich lower mantle heterogeneities in the modern Earth depend on distribution of iron between coexisting lower mantle phases (Mg,Fe)O magnesiowüstite, (Mg,Fe)SiO3 bridgmanite, and (Mg,Fe)SiO3 post-perovskite. The partitioning of iron between these phases was investigated in synthetic ferrous-iron-rich olivine compositions (Mg0.55Fe0.45)2SiO4 and (Mg0.28Fe0.72)2SiO4 at lower mantle conditions ranging from 33–128 GPa and 1900–3000 K in the laser-heated diamond anvil cell. The resulting phase assemblages were characterized by a combination of in situ X-ray diffraction and ex situ transmission electron microscopy. The exchange coefficient between bridgmanite and magnesiowüstite decreases with pressure and bulk Fe# and increases with temperature. Thermodynamic modeling determines that incorporation and partitioning of iron in bridgmanite are explained well by excess volume associated with Mg-Fe exchange. Partitioning results are used to model compositions and densities of mantle phase assemblages as a function of pressure, FeO-content and SiO2-content. Unlike average mantle compositions, iron-rich compositions in the mantle exhibit negative dependence of density on SiO2-content at all mantle depths, an important finding for interpretation of deep lower mantle structures.

2021

Investigating Magma Ocean Solidification on Earth Through Laser‐Heated Diamond Anvil Cell Experiments

James Badro, Charles-Edouard Boukaré, Marco Cantoni, Philippe Gillet, Cécile Hébert, Farhang Nabiei

We carried out a series of silicate fractional crystallization experiments at lower mantle pressures using the laser-heated diamond anvil cell. Phase relations and the compositional evolution of the cotectic melt and equilibrium solids along the liquid line of descent were determined and used to assemble the melting phase diagram. In a pyrolitic magma ocean, the first mineral to crystallize in the deep mantle is iron-depleted calcium-bearing bridgmanite. From the phase diagram, we estimate that the initial 33%–36% of the magma ocean will crystallize to form such a buoyant bridgmanite. Substantial calcium solubility in bridgmanite is observed up to 129 GPa, and significantly delays the crystallization of the calcium silicate perovskite phase during magma ocean solidification. Residual melts are strongly iron-enriched as crystallization proceeds, making them denser than any of the coexisting solids at deep mantle conditions, thus supporting the terrestrial basal magma ocean hypothesis (Labrosse et al., 2007).

2021

Evolution of the Morphology Near Triple-Phase Boundaries in Ni–Yttria Stabilized Zirconia Electrodes Upon Cathodic Polarization

Priscilla Caliandro, Marco Cantoni, Guillaume Jeanmonod, Arata Nakajo, Lucie Navratilova, Giorgio Rinaldi, Jan Van Herle

Microstructural changes in Ni–yttria stabilized zirconia (YSZ) near the YSZ electrolyte were examined by three-dimensional (3D) electron microscopy after electrolysis and fuel cell operation up to 10,700 h and 15,000 h, respectively. The depletion of Ni and three-phase boundaries (TPBs) close to the electrolyte was detected upon cathodic polarization. It corresponded to spatial variations of dihedral angles (θ) at TPBs and Ni surface curvature along the direction perpendicular to the electrolyte, which comport with electrowetting and Zener pinning theory on several aspects. θNi decreased by up to 6 deg next to the electrolyte after electrolysis but remained uniform after fuel cell operation. This is in line with predictions from electrowetting theory with capacitances measured by electrochemical impedance spectroscopy and distribution of relaxation times. The decrease in θNi was concurrent to transition toward concave Ni/pore interfacial shapes and lower genus of the Ni phase, which suggests the pinch-off of Ni ligaments following surface diffusion-controlled Rayleigh instability. The increase in absolute mean curvature near the electrolyte interface is a driving force for outward transport of Ni. The decrease in θYSZ further suggests that TPB lines relocate on YSZ surface features that provide higher Zener pinning force. In contrast, few localized contact losses between Ni and YSZ that can also occur under high cathodic polarization and trigger Ni depletion were detected. The results are expected to advance the understanding of the driving forces that cause Ni depletion near the electrolyte in electrolysis for the design of improved solid oxide cell electrode microstructures.

2020