Andrea Regina Biedermann

University of Bern

Switzerland

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Articles (12)

Year:

2025

Year:

2023

Year:

2023

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2022

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2022

Year:

2022

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2021

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2021

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2020

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2020

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2020

Year:

2020

Collaborators (4)

Matthias Arenz

Professor

University of Bern

SWITZERLAND

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Thomas Weber

Head of X-ray Platform

ETH Zurich

SWITZERLAND

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Donna Whitney

University of Minnesota

UNITED STATES

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Pierre Lanari

Assistant Professor

University of Bern

SWITZERLAND

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Andrea Regina Biedermann

Research Interests

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Articles (12)

Magnetic and Crystallographic Fabric Analyses of Amphibolite: A Proposed Methodology Applied to a Migmatite Dome

Toward Better Understanding of the Ferrofluid Impregnation Process and Potential Artefacts—A Prerequisite for Reliable Interpretation of Magnetic Pore Fabrics

Physical and Chemical Stability of Nanoparticles in Ferrofluid Before and After Impregnation: Implications for Magnetic Pore Fabric Studies

Quantitative Comparison of 3D Pore Space Properties With Magnetic Pore Fabrics—Testing the Ability of Magnetic Methods to Predict Pore Fabrics in Rocks

Magnetic Properties of Ferrofluid Change Over Time: Implications for Magnetic Pore Fabric Studies

Ferrofluid Impregnation Efficiency and Its Spatial Variability in Natural and Synthetic Porous Media: Implications for Magnetic Pore Fabric Studies

Tough metal-ceramic composites with multifunctional nacre-like architecture

Explaining the large variability in empirical relationships between magnetic pore fabrics and pore space properties

FinIrrSDA: A 3‐D Model for Magnetic Shape and Distribution Anisotropy of Finite Irregular Arrangements of Particles With Different Sizes, Geometries, and Orientations

Beyond the second-order magnetic anisotropy tensor: higher-order components due to oriented magnetite exsolutions in pyroxenes, and implications for palaeomagnetic and structural interpretations

Crystallographic preferred orientation, magnetic and seismic anisotropy in rocks from the Finero peridotite, Ivrea-Verbano Zone, Northern Italy – Interplay of anisotropy contributions from different minerals

Anisotropy of Full and Partial Anhysteretic Remanence Across Different Rock Types: 1—Are Partial Anhysteretic Remanence Anisotropy Tensors Additive?

Collaborators (4)

Matthias Arenz

Thomas Weber

Donna Whitney

Pierre Lanari

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