Single-Layer Fe-Cu Interphase in Ferritic Steels Stabilized by Magnetic Friedel Oscillations
Wen-Qiang Xie, Jin-Li Cao, and Wen-Tong Geng

TL;DR
This paper reveals that a single-layer magnetic Fe-Cu interphase, stabilized by Friedel oscillations, explains Fe content in Cu precipitates in steels, impacting steel design.
Contribution
It uncovers a novel single-layer Fe-Cu interphase stabilized by magnetic Friedel oscillations, challenging previous assumptions about interface sharpness and miscibility.
Findings
Fe-Cu interface is a single-layer mixed interphase.
Spin polarization and Friedel oscillations stabilize the interphase.
Fe content in Cu precipitates is significant due to this interphase.
Abstract
Copper precipitation is a technique extensively deployed in steel strengthening. Being as tiny as a few nanometers in diameter, the Cu precipitates present a real challenge to experimental techniques in determination of their composition. The late Professor Morris Fine called it a mystery when addressing the discrepancy between the fact of low solubility of Fe in bulk Cu and the remarkable content of Fe in Cu precipitates according to atom probe tomography measurement. With a thorough search using rigorous first-principles density functional theory calculations, we are surprised to find that the interface between Cu precipitate and Fe matrix is neither immiscibly sharp, nor commonly miscible over a range of atomic layers, but rather manifests itself as a single-layer mixed Fe-Cu interphase. Our detailed analysis reveals that spin polarization is a key factor in defining such an…
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Taxonomy
TopicsMagnetic Properties and Applications · Microstructure and Mechanical Properties of Steels · Metallurgy and Material Forming
