Abstract
The effect of high pressure (0–8 GPa) on the magnetic structure of polycrystalline samples of manganites at 5 K is investigated using neutron-diffraction technique. Application of pressure is found to modify the previously reported magnetic structure, observed under ambient conditions, in these compounds [I. Dhiman et al., Phys. Rev. B 77, 094440 (2008)]. In composition, at 4.6(2) GPa and beyond, -type antiferromagnetic structure is found to coexist with charge-exchange (CE)-type antiferromagnetic phase, observed at ambient pressure, with . For sample, as a function of pressure the CE-type phase is fully suppressed at 2.3(1) GPa and -type antiferromagnetic phase is favored. Further Sr doping at , the -type antiferromagnetic phase is observed at ambient pressure and for . This phase is retained in the studied pressure range. However, the magnetic moment progressively reduces with increasing pressure, indicating the suppression of -type antiferromagnetic phase. The present study brings out the fragile nature of the CE-type antiferromagnetic state in half-doped manganites as a function of pressure and disorder . We observe that pressure required for destabilizing the CE-type antiferromagnetic state is reduced with increasing disorder . External pressure and changing -site ionic radii have analogous effect on the magnetic structure.
- Received 26 November 2009
DOI:https://doi.org/10.1103/PhysRevB.81.104424
©2010 American Physical Society