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Ph.D. THESIS Multipolar ordering in f-electron systems

Ph.D. THESIS Multipolar ordering in f-electron systems

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Chapter 2 Overview of the Theoretical Background 31<br />

Figure 2.5: Experimentally <strong>in</strong>vestigated temperature-magnetic field phase diagram of<br />

PrFe 4 P 12 skutterudite [37].<br />

moments. Pr 3+ ions have the 4f 2 configuration and the n<strong>in</strong>efold degenerate<br />

J = 4 Hund’s rule ground state multiplet. The ma<strong>in</strong> component of the crystal<br />

field is cubic, but there is also a tetrahedral component [38]. While recent<br />

<strong>in</strong>vestigations <strong>in</strong>dicate that the <strong>in</strong>clusion of the tetrahedral component gives<br />

rise to <strong>in</strong>terest<strong>in</strong>g features, it is a good approximation to take a cubic crystal<br />

field which splits J = 4 multiplet accord<strong>in</strong>g to<br />

Γ J=4 = Γ 1 ⊕ Γ 3 ⊕ Γ 4 ⊕ Γ 5 . (2.33)<br />

The correspond<strong>in</strong>g eigenstates are listed <strong>in</strong> Appendix A.<br />

The order of the crystal field levels is difficult to derive from experiments.<br />

Analyz<strong>in</strong>g the anisotropy of the magnetization curves above the ordered<br />

phase where s<strong>in</strong>gle-ion results are valid, it was concluded that the<br />

likely possibilities are: a Γ 1 ground state and a low-ly<strong>in</strong>g exited state Γ 4<br />

(the Γ 1 –Γ 4 scheme); or the Γ 1 –Γ 5 scheme; or the Γ 3 –Γ 4 scheme [37]. At the<br />

first sight, the assumption of a Γ 3 ground state looks plausible. We have<br />

shown <strong>in</strong> (2.19) that the Γ 3 doublet carries the Γ 3g quadrupolar moments, so<br />

antiferro-quadrupolar <strong>order<strong>in</strong>g</strong> can give a unique ground state. The assumption<br />

of the Γ 3 ground state (see the left part of Fig.2.6) is also compatible<br />

with the symmetry analysis of the structural distortion accompany<strong>in</strong>g the<br />

antiferro-quadrupolar <strong>order<strong>in</strong>g</strong> [39]. However, the field dependence of the<br />

transition and other magnetic properties rema<strong>in</strong> unexpla<strong>in</strong>ed.<br />

As mentioned before, magnetization data also allow that the ground state<br />

be the Γ 1 s<strong>in</strong>glet. Of course, a s<strong>in</strong>glet carries no moment (either quadrupolar<br />

or anyth<strong>in</strong>g else), so it cannot be taken alone. We analyzed the two allowed<br />

possibilities for the two lowest levels: Γ 1 –Γ 4 and Γ 1 –Γ 5 , and concluded that

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