Abstract

We report the pressure effect on the magnetic ground state of the heavy-fermion (HF) canted antiferromagnet YbRhSb (orthorhombic $\ensuremath{\varepsilon}$-TiNiSi-type) by means of magnetization and resistivity measurements using a single crystal. At ambient pressure, this compound undergoes a transition at ${T}_{M1}=2.7$ K into a canted antiferromagnetic (AF) state with a small spontaneous moment of $3\ifmmode\times\else\texttimes\fi{}10$${}^{\ensuremath{-}3}\phantom{\rule{0.28em}{0ex}}{\ensuremath{\mu}}_{B}/$Yb. With increasing pressure $P$ above 1 GPa, another magnetic transition occurs at ${T}_{M2}$ above ${T}_{M1}$, and ${T}_{M1}(P)$ has a deep minimum of 2.5 K at 1.7 GPa. For $P\ensuremath{\ge}2$ GPa, the canted AF structure changes to a ferromagnetic (FM) one, where a large moment 0.4 ${\ensuremath{\mu}}_{B}/$Yb lies in the orthorhombic $b\ensuremath{-}c$ plane and a metamagnetic transition occurs at $B$ $||\phantom{\rule{0.16em}{0ex}}a$ $=$ 1.5 T. This unusual FM state below ${T}_{M3}\ensuremath{\cong}4.3$ K is ascribed to the balance between the single-ion crystalline electric field (CEF) anisotropy with easy direction $||\phantom{\rule{0.16em}{0ex}}a$ and the intersite exchange interaction with easy $b\ensuremath{-}c$ plane. Furthermore, we have investigated the pressure dependence of ${T}_{M3}$ up to 20.4 GPa using electrical resistivity measurements. The structural stability under pressures up to 19 GPa was examined by x-ray diffraction. We find that ${T}_{M3}$ above 2.5 GPa steeply increases up to about 7 K, showing a broad maximum and then slightly decreases with increasing pressure above 8 GPa, while the structure remains unchanged. We attribute the enhancement of ${T}_{M3}$ above 2.5 GPa to an increase of the CEF anisotropy with respect to magnetic exchange anisotropy. Finally, we compare and discuss the volume dependence of magnetic phase diagram of YbRhSb with the isostructural HF ferromagnet YbNiSn.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.