Resonant magnetic x-ray scattering and Summary • Resonant scattering – Why do it? – What is it? – How is it done? – Example(s) • The Real World …. CaFe2As2 Solving magnetic structures Determine the magnetic wavevector (what is the “magnetic unit cell”) Use the angular dependence of resonant and nonresonant scattering crosssections to determine magnetic moment directions. Scattering amplitudes → magnitude of the ordered magnetic moment. Long-range order Bragg peaks QBragg=2p/d t = 2p/2d I 1 t t 10-6 2d d 2p/d Q Why Bother? • Many of the technologically important RE compounds contain neutron opaque elements. • Superior reciprocal space (Q) resolution allows more detailed study … reinvestigation of “solved” structures. • Can be used for investigations of submillimeter-sized single crystals. • Resonant magnetic scattering occurs at well-defined energies specific to elements of interest -- probe local magnetism. • Studies of magnetic surfaces and interfaces. X-ray Resonant Magnetic Scattering (XRMS) •(L2, L3)-edge for rare-earths (6-10KeV) L3 - edge •Electric multipole transition (dipole : 2p – 5d, quadrupole 2p – 4f) EF •Dipole transition is dominant • 4f : magnetic properties 5d : exchange splitting by 4f outgoing photon P3/2 P1/2 Incoming photon f res el 4p ˆ L * M L * YLM kˆ YLM kˆ ˆ FLM TbNi2B2C k s p f M1 k M3 i analyzer s sample M2 Non-resonant: ds/dW S2sinQ2 outgoing s- pol.) 2sin2Q cosQ{(L1+S1) + S3sinQ}]2 (outgoing p- pol.) Resonant (E1): ds/dW 0 ^ ^ M1cosQ + M3sinQ2 outgoing s- pol.) (outgoing p- pol.) ^ 2 (k′· M) Resonant (E2): Much more complicated, but can probe M1, M2, M3 We can do this by plotting the q-dependence of integrated intensities (a la neutrons) Angular dependence of the scattering at (0 0 L ± t) of GdCo2Ge2 measured by resonant and nonresonant diffraction Gd L3 edge Alternatively… X-ray resonant magnetic scattering azimuth scans Q Gd5Ge4 θ θ f i k Gd5Ge4 (0 3 0) at T = 8 K I (M•k’)2 Integrated Intensity (arb. unit.) k' Intensity |k' • M|2 1.0 0.5 bc in scattering plane 0.0 0 30 ab in scattering plane 60 90 120 Azimuth (deg.) bc in scattering plane 150 180 GdNi2Ge2 – An Example Crystal structure Magnetization measurement Tt TN Gd Ni Ge S.L. Bud’ko, Z. Islam, T.A. Wiener, I.R. Fisher, A.H. Lancerda, P.C. Canfield Journal of Magnetic Materials 205, 53 (1999) 1st harmonic (magnetic) 2nd harmonic (charge) 3rd harmonic (magnetic) So, what do you learn from diffraction? • From peak positions – Lattice parameters and how they change with environmental conditions (e.g. temperature and pressure) • From peak widths – Crystal quality (e.g. mosaic) – Presence of strain (e.g. longitudinal widths) • From integrated intensities – Contents of the unit cell – Positions of atoms within the unit cell; magnetic ordering – Thermal parameters (thermal disorder) CaFe2As2…an example Peak positions: Temperature dependent studies Peak Positions: Pressure dependent studies Peak Widths – strain, crystallite size and mosaic 10000 103 (1 1 10) 206 200 FWHM = 0.017 deg 222 301 215 008 116 007 211 202 224 310 311 006 112 Rocking curve Counts / s 114 Sn traces 100 20 400 Si standard 004 1000 101 Intensity (counts) CaFe2As2 0 30 40 50 2 (deg) 60 Powder after grinding 70 80 Fig. X1 45.60 45.65 (deg) 45.70 Single crystal mosaic Integrated Intensities