\documentstyle[preprint,tighten,prabib,prl,aps]{revtex} \def\tmi{T$_{mi}$} \def\tc{T$_{c}$} \def\tcm{T$_{c}^m$} \begin{document} \draft \title{ Direct Observation of Lattice Polaron Formation in the Local Structure of $\bf La_{1-x}Ca_xMnO_3$ } \author{S. J. L. Billinge,$^1$ R. G. DiFrancesco,$^1$ G. H. Kwei,$^2$ J. J. Neumeier$^3$ and J. D. Thompson$^3$} \address{ $^1$Department of Physics and Astronomy and Center for Fundamental Materials Research,\\ Michigan State University, East Lansing, MI 48824-1116.\\ $^2$Chemistry and Materials Sciences Department, Lawrence Livermore National Laboratory, Livermore, CA 94550.\\ $^3$Los Alamos National Laboratory, Los Alamos, NM 87545.} \date{\today} \maketitle \begin{abstract} The local atomic structure of $\rm La_{1-x}Ca_{x}MnO_3$ ($x= 0.12,$ 0.21 and 0.25) has been studied using pair-distribution-function analysis of neutron powder-diffraction data. A change is seen in the local structure which can be correlated with the metal-insulator transition in the $x=0.21$ and 0.25 samples. This local structural change is modeled as an isotropic collapse of oxygen towards Mn of magnitude $\delta = 0.12$~\AA\ occuring on one-in-four Mn sites. We argue that this is the direct observation of lattice polaron formation, associated with the metal-insulator transition in these materials. \end{abstract} \pacs{71.30+h,71.38.+i,61.12-q,72.80.Ga} \narrowtext The discovery in the 1950's of ferromagnetism coupled with a metal-insulator (MI) transition in the class of materials $\rm La_{1-x}A_xMnO_3$, where A is a divalent ion~\cite{jonke;p50}, led to a theoretical explanation which involved a new type of exchange interaction called double exchange (DE)~\cite{zener;pr51}. $\ldots$ The results are shown in Fig.~\ref{fig;str chg}. The upper set of curves, (i), in Fig.~\ref{fig;str chg}(a) show the appearance in the {\it data} of the structure change at T$^m_c$. The PDFs are from the $x=0.21$ sample at T=140~K (solid line) and 176~K (dotted line). $\ldots$ %\bibliography{/u24/billinge/tex/bib/hts,% % /u24/billinge/tex/bib/htsii,% % /u24/billinge/tex/bib/ndb,% % /u24/billinge/tex/bib/1995,% % /u24/billinge/tex/bib/1996} %\bibliographystyle{/u24/billinge/tex/1995/aip_simon} %\bibliographystyle{/u24/billinge/tex/bib/aip} \begin{thebibliography}{10} \bibitem{jonke;p50} G.~M. Jonker and J.~H. van Santen, \newblock Physica (Utrecht) {\bf 16}, 337 (1950); E.~O. Wollan and W.~F. Koehler, \newblock Phys. Rev. {\bf 100}, 545 (1955); C.~W. Searle and S.~T. Wang, \newblock Can. J. Phys. {\bf 47}, 2703 (1969); {\it ibid}, {\bf 48}, 2023 (1970). \bibitem{helmo;prl93} R.~von Helmolt et~al., \newblock Phys. Rev. Lett. {\bf 71}, 2331 (1993). \bibitem{magnote} The structure change correlates with the MI transition and not with the appearance of ferromagnetism. This is clear since the $x=0.12$ sample becomes ferromagnetic at a T$_c$ of $\approx 165$~K, with an ordered moment which is comparable to that observed in the other composition samples, although it remains insulating to the lowest temperatures. If the PDF were sensitive to the ferromagnetism rather than the structure change associated with the MI transition, it would be evident in the $x=0.12$ sample and it is not [Fig.~\protect\ref{fig;dat}]. \end{thebibliography} % \begin{figure} \caption{PDFs obtained from the $\rm La_{0.88}Ca_{0.12}MnO_3$ sample. $\ldots$ \protect\label{fig;dat}} \end{figure} % \end{document}