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Published on: November 28, 2017
Enhanced Valley Zeeman Splitting in Fe-Doped Monolayer MoS2
Qi Li1, Xiaoxu Zhao2, Longjiang Deng1
1National Engineering Research Center of Electromagnetic Radiation Control Materials, School of Electronic Science and Engineering, University of Electronic Science and Technology of China, Chengdu, 611731, China.
Researchers achieved magnetic control of valley splitting in iron-doped molybdenum disulfide (MoS2) at room temperature. This breakthrough enhances the valley degree of freedom for potential spintronic applications.
Area of Science:
- Condensed Matter Physics
- Materials Science
- Spintronics
Background:
- The Zeeman effect enables magnetic manipulation of spin.
- Valley Zeeman splitting in 2D transition metal dichalcogenides (TMDs) was previously limited to low temperatures.
- Controlling valley pseudospins at room temperature is crucial for practical applications.
Purpose of the Study:
- To demonstrate magnetic manipulation of valley Zeeman splitting at room temperature in a 2D material.
- To investigate the effect of magnetic doping on valley Zeeman splitting.
- To explore the underlying mechanisms for enhanced valley splitting.
Main Methods:
- Chemical Vapor Deposition (CVD) growth of Fe-doped MoS2 monolayer.
- Experimental measurement of valley Zeeman splitting at 300 K and 10 K.
- Theoretical calculations to understand the magnetic interactions and orbital hybridization.
Main Results:
- Unambiguous magnetic manipulation of valley Zeeman splitting achieved at 300 K (g_eff = -6.4) and 10 K (g_eff = -11).
- Effective Landé g_eff factor tuned up to -20.7 with increasing Fe concentration, a ~5-fold enhancement over undoped MoS2.
- Enhanced splitting attributed to Heisenberg exchange interaction between Fe 3d electrons and MoS2 via d-orbital hybridization.
Conclusions:
- Fe-doped MoS2 enables magnetic control of valley Zeeman splitting at room temperature.
- Magnetic doping significantly enhances the effective Landé g_eff factor.
- The findings pave the way for spintronic devices utilizing valley pseudospins at ambient conditions.
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