83rd Annual Meeting of the APS Southeastern Section
Volume 61, Number 19
Thursday–Saturday, November 10–12, 2016;
Charlottesville, Virginia
Session C3: New Developments in Superconductivity
1:30 PM–3:30 PM,
Thursday, November 10, 2016
Room: Monroe Room
Chair: Utpal Chatterjee, University of Virginia
Abstract ID: BAPS.2016.SES.C3.1
Abstract: C3.00001 : Spatial inhomogeneities in the Fe chalcogenide superconductors
1:30 PM–2:00 PM
Preview Abstract
Abstract
Author:
Despina Louca
(University of Virginia)
Much remains unknown of the microscopic origin of superconductivity when it
materializes in atomically disordered systems as in amorphous alloys or in
crystals riddled with defects. A manifestation of this conundrum is
envisaged in the highly defective iron chalcogenide superconductors. How can
superconductivity survive under such crude conditions that call for strong
electron localization and scattering? With vacancies present both at the K
and Fe sites in the K$_{\mathrm{x}}$Fe$_{\mathrm{2-y}}$Se$_{\mathrm{2}}$
superconductor, superconductivity is bordering a semi-metallic region below
x \textasciitilde 0.7 and an insulating and antiferromagnetic region above x
\textasciitilde 0.85. In this talk, I will discuss our recent results on the
bulk local atomic structure and single crystal work that show striking
differences between superconducting and non-superconducting compositions
regarding the ordering of the Fe and K sublattices. In a related system, the
intercalation of LiFeO$_{\mathrm{2}}$ in the tetragonal lattice of
Fe$_{\mathrm{1-y}}$Se leads to a great enhancement of the superconducting
transition temperature, T$_{\mathrm{C}}$ \textasciitilde 43 K and possibly
to an antiferromagnetic transition at 8.5 K. While the LiFeO$_{\mathrm{2}}$
layer acts as a charge reservoir, its Fe$^{\mathrm{3+}}$ ion
(3d$^{\mathrm{5}})$ is magnetic that may create a magnetic buffer layer.
Most recently, we developed a new synthesis method to control the Fe
concentration in the intercalating layer as well as the filling ratio of the
Li$_{\mathrm{1-x}}$Fe$_{\mathrm{x}}$O$_{\mathrm{2}}$ : FeSe layers. Neutron
scattering measurements were carried out on powder samples of
(Li$_{\mathrm{1-x}}$Fe$_{\mathrm{x}}$O2)$_{\mathrm{y}}$FeSe. With the
intercalation, no crystal structural transition from the P4/nmm symmetry
occurs but the c-axis lattice constant expands substantially, evidence of
the intercalation. Our results indicate that the amount of Fe in the
LiFeO$_{\mathrm{2}}$ layer has a direct correlation to the transition
temperature.
To cite this abstract, use the following reference: http://meetings.aps.org/link/BAPS.2016.SES.C3.1