Article ID Journal Published Year Pages File Type
1593461 Solid State Communications 2010 4 Pages PDF
Abstract

In order to clarify the nature of a possible magnetic phase transition at Tm=13 K for the misfit layered cobalt dioxide with a double rocksalt (RS-) type block, [Ca0.85OH]1.16RS[CoO2], we have measured the muon spin rotation and relaxation (μ+SR) spectra in the temperature (TT) range between 1.8 and 20 K. All μ+SR parameters, such as the dipolar interaction frequency (fμOH) due to the formation of μ+μ+–OH, its asymmetry (AμOH) and relaxation rate (σμOH), are found to be independent of TT both above and below Tm. This is a clear indication that the transition at Tm is not due to magnetic order but has a structural and/or electronic origin. In addition, we have been able to determine the muon stopping site for this misfit layered compound. It is found to be located within the CaOH blocking layers, where the muon and OH-group form a water-like Hμ+O unit as indicated by a very slow oscillation in the zero-field relaxation spectrum.

Related Topics
Physical Sciences and Engineering Materials Science Materials Science (General)
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