Giant orbital-magnon conversion driven perpendicular magnetization switching
Fanyu Meng, Ying Feng, Mingyang Sun, Baiyan Kang, Donglin Song + 5 more
TLDR
Researchers demonstrate giant orbital-magnon conversion, enabling efficient room-temperature perpendicular magnetization switching for advanced nano-devices.
Key contributions
- Demonstrated direct orbital-magnon (L-M) conversion in an orbital metal/antiferromagnetic insulator bilayer.
- Achieved L-M conversion efficiency over 10 times higher than traditional orbital systems at room temperature.
- Enabled efficient room-temperature perpendicular magnetization switching in CoFeB via this new mechanism.
Why it matters
This work establishes a direct link between orbitronics and magnonics, fields previously lacking efficient coupling. It provides a new, highly efficient mechanism for controlling magnetic states, crucial for next-generation, beyond-Moore information technologies.
Original Abstract
The pursuit of beyond-Moore information technologies has stimulated the exploration of novel information carriers, such as electron spin, orbital, and magnon, beyond electron charge. Efficient interconversion among these degrees of freedom and precise control over the information states are crucial for advancing nanoelectronic devices. However, a direct coupling between orbital angular momentum (L) and magnons (M) has remained elusive, and magnetization switching through orbital-to-magnon (L-M) conversion has not yet been achieved. Here, we report the experimental demonstration of L-M conversion in an orbital metal/antiferromagnetic insulator bilayer at room temperature, with an efficiency over an order of magnitude higher than that in traditional orbital systems lacking the L-M process. Consequently, we achieved efficient room-temperature perpendicular magnetization switching in a CoFeB ferromagnetic layer mediated by this new mechanism. Our findings establish a direct link between orbitronics and magnonics, providing a new platform for the development of advanced nano-devices based on orbital-driven magnonic phenomena.
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