Inverse Isotope Effect on Kondo Temperature in Electron-Rattling System

Takashi Hotta

doi:10.1143/jpsj.78.073707

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arXiv · 0906.0815

Inverse Isotope Effect on Kondo Temperature in Electron-Rattling System

Takashi Hotta

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Abstract

In an electron system coupled with anharmonic phonons, i.e., {\it rattling}, inverse isotope effect on the Kondo temperature $T_{\rm K}$ is found to occur by the numerical evaluation of the Sommerfeld constant $γ$ of the Anderson-Holstein model. For the anharmonic potential of an oscillator with mass $M$ in which large $γ$ has been found to be almost independent of an applied magnetic field, $γ$ is significantly suppressed when $M$ is increased, i.e., $T_{\rm K}$ is enhanced due to the relation of $γ$$\sim$$T_{\rm K}^{-1}$ in the Kondo problem, leading to the inverse isotope effect on $T_{\rm K}$. Since this phenomenon does not occur for harmonic phonons, it can be a key experiment to prove the relevance of rattling to magnetically robust heavy electron state.

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Takashi Hotta. 2009-06-04. Inverse Isotope Effect on Kondo Temperature in Electron-Rattling System. https://doi.org/10.1143/jpsj.78.073707

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