Abstract
Understanding the complex glassy phenomena, which accompany polaron formation in optimally doped manganites (ODMs) is a cumbersome issue with many unexplained perspectives. Here, on the basis of and nuclear magnetic resonance (NMR) measurements, performed in the temperature range 80–900 K we show that glass freezing, observed in the paramagnetic (PM) phase of ODM , is not a random uncorrelated process but the signature of the formation of a genuine spin-glass state, which for consolidates with the ferromagnetic (FM) state into a single thermodynamic phase. Comparison with NMR measurements performed on systems for and ODM , demonstrates the key role played by the local lattice distortions, which control (i) the stability of the spin-glass phase component and (ii) the kind (first or second order) of the PM-FM phase transition. The experimental results are in agreement with the predictions of the compressible random bond-random field Ising model, where consideration of a strain field induced by lattice distortions is shown to invoke at a discontinuous first-orderlike change in both the FM and the “glassy” Edwards-Anderson order parameters.
3 More- Received 8 September 2009
DOI:https://doi.org/10.1103/PhysRevB.82.235102
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