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Pressure driven magnetic order in Sr[Formula: see text] Ca[Formula: see text] Co[Formula: see text] P[Formula: see text]

The magnetic phase diagram of Sr[Formula: see text] Ca[Formula: see text] Co[Formula: see text] P[Formula: see text] as a function of hydrostatic pressure and temperature is investigated by means of high pressure muon spin rotation, relaxation and resonance ([Formula: see text] SR). The weak pressur...

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Detalles Bibliográficos
Autores principales: Forslund, Ola Kenji, Andreica, Daniel, Sassa, Yasmine, Imai, Masaki, Michioka, Chishiro, Yoshimura, Kazuyoshi, Guguchia, Zurab, Shermadini, Zurab, Khasanov, Rustem, Sugiyama, Jun, Månsson, Martin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9585139/
https://www.ncbi.nlm.nih.gov/pubmed/36266305
http://dx.doi.org/10.1038/s41598-022-21699-y
Descripción
Sumario:The magnetic phase diagram of Sr[Formula: see text] Ca[Formula: see text] Co[Formula: see text] P[Formula: see text] as a function of hydrostatic pressure and temperature is investigated by means of high pressure muon spin rotation, relaxation and resonance ([Formula: see text] SR). The weak pressure dependence for the [Formula: see text] compounds suggests that the rich phase diagram of Sr[Formula: see text] Ca[Formula: see text] Co[Formula: see text] P[Formula: see text] as a function of x at ambient pressure may not solely be attributed to chemical pressure effects. The [Formula: see text] compound on the other hand reveals a high pressure dependence, where the long range magnetic order is fully suppressed at [Formula: see text]  kbar, which seem to be a first order transition. In addition, an intermediate phase consisting of magnetic domains is formed above [Formula: see text]  kbar where they co-exist with a magnetically disordered state. These domains are likely to be ferromagnetic islands (FMI) and consist of an high- (FMI-[Formula: see text] ) and low-temperature (FMI-[Formula: see text] ) region, respectively, separated by a phase boundary at [Formula: see text]  K. This kind of co-existence is unusual and is originating from a coupling between lattice and magnetic degrees of freedoms.