2009 MAGNETIC SYSTEMSMagnetic properties of ErCo x Mn 1−x O 3 perovskitesA spin reversal ph<strong>en</strong>om<strong>en</strong>on in perovskite manganitesABO 3 may appear wh<strong>en</strong> the rare-earth elem<strong>en</strong>t, having alarge magnetic mom<strong>en</strong>t (e.g. Gd, Er), interacts with theMn 3+ -Mn 4+ sublattice. This has be<strong>en</strong> found in manganitespartially substituted at the A-site by alkaline earth elem<strong>en</strong>ts.B-site substitutions also drastically modify the physicochemicalproperties of these materials, since for each dival<strong>en</strong>ttransition metal introduced in the lattice, a Mn 3+ ionwill transform into Mn 4+ . If the substitute is Co, the solidsolution may ext<strong>en</strong>d over a large range of conc<strong>en</strong>trationssince cobalt may adopt a 2+ and a 3+ oxidation states, dep<strong>en</strong>dingon the synthesis conditions. In these materials, thetotal magnetization changes its sign wh<strong>en</strong> field-cooled dueto a negative polarization of the rare-earth mom<strong>en</strong>t in thepres<strong>en</strong>ce of the internal field created by the ordered manganesesublattice [Peña et al., J. Magn. Magn. Mater. 310,159 (2007)].The isothermal magnetization shows two interesting features:(i) an intersection of the decreasing and increasingbranches of the magnetization loop at low fields, related tothe spin reversal <strong>des</strong>cribed above; (ii) a step-like increase athigh fields wh<strong>en</strong> the applied magnetic field increases [Peñaet al., J. Magn. Magn. Mater. 312, 78 (2007)]. Thesetwo anomalies have be<strong>en</strong> observed only in the Er-Co-basedsystem, for materials close to the ErCo 0.50 Mn 0.50 O 3 composition(figure 134).Figure 135: High field magnetization for ErCo x Mn 1−x O 3 samplesnormalized for the value at 15 T.Important results were obtained: (a) the high field transitionshifts towards higher applied fields wh<strong>en</strong> temperaturedecreases; (b) the high field transition shifts towards higherapplied fields wh<strong>en</strong> the Co/Mn conc<strong>en</strong>tration changes fromthe particular 50/50 ratio; (c) the magnetization does notsaturate at the highest applied field, but the ferromagneticloop <strong>en</strong>ds up at about 10 T; (d) no abrupt jumps are observedfor temperatures above 3 K; (e) magnetic relaxationis observed just before the transition occurs (figure 136).Magnetization loop for the ErCo 0.50 Mn 0.50 O 3 com-Figure 134:position.Figure 136: Magnetization as a function of time forErCo 0.50 Mn 0.50 O 3 . Insert: fit to a logarithmic behaviour.Furthermore, the high-field transition is of a dynamical naturesince both its amplitude and position dep<strong>en</strong>d on thesweep-rate of the applied-field. To get a deeper insight ofthis anomaly, high-field magnetization measurem<strong>en</strong>ts wereperformed at 4 K. (figure 135).Based on these results, several sc<strong>en</strong>arios are possible, suchas, dynamical movem<strong>en</strong>ts of domain walls, magnetic relaxationof ferromagnetic clusters, metamagnetic-like interactionsbetwe<strong>en</strong> Er 3+ and Co 2+ -Mn 4+ mom<strong>en</strong>ts.A. B. AntunesO. Peña (Sci<strong>en</strong>ces Chimiques de R<strong>en</strong>nes, Université de R<strong>en</strong>nes 1, R<strong>en</strong>nes, France), C. Moure (Electrocerámicas, Institutode Cerámica y Vidrio, CSIC, Madrid, Spain), S. de Brion (Institut Néel, Gr<strong>en</strong>oble, France)93
MAGNETIC SYSTEMS 2009Ferromagnetic domains in nanosized erbium perovskitesCooperative ph<strong>en</strong>om<strong>en</strong>a constitute an important researcharea because of many applications at the frontiers of chemistry,physics and electronics. Perovskites manganiteshave received growing att<strong>en</strong>tion because of mixed-val<strong>en</strong>ceMn 4+ /Mn 3+ and resulting magnetoresistance effect. Wepreviously reported interesting results in Er(Co,Mn)O 3 dueto an antiferromagnetic interaction betwe<strong>en</strong> Er and |Co,Mn|sublattices, producing a reversal of the magnetic mom<strong>en</strong>tand formation of ferromagnetic domains. An avalanchemechanism occurs under moderate magnetic fields (∼35 kOe), leading to the rotation of the domains in one ormore steps, dep<strong>en</strong>ding on the rate of variation of the appliedfield and on the grains formation [Peña et al., J. Magn.Magn. Mater. 312, 78 (2007)].In order to investigate the influ<strong>en</strong>ce of the micro-structurewe have elaborated nanosized materials and correlated themagnetic response to the grains size and to boundaries percolation.ErCo 0.50 Mn 0.50 O 3 compound was prepared at700 ◦ C by a citrate method and further calcined at increasingtemperatures. Samples were characterized by X-raydiffraction both before and after the sintering conditions,confirming the pres<strong>en</strong>ce of a pure perovskite orthorhombicPbnm structure and phase purity was checked by <strong>en</strong>ergydispersive analysis. The micro-structure, characterizedby scanning electron microscopy, consists of homog<strong>en</strong>eousspherical grains of 20 − 30 nm diameter for as-preparedsample synthesized at 700 ◦ C, which progressively growwith increasing sintering temperature, attaining 100 − 200nm and a very good percolation at 950 ◦ C, that is, wh<strong>en</strong>grains fuse together and grain barriers almost disappear.Magnetic measurem<strong>en</strong>ts were performed on the startingmaterial and sintered pellets.temperatures of 950 ◦ C and above, that is, wh<strong>en</strong> grain barrierst<strong>en</strong>d to disappear. We correlate this sudd<strong>en</strong> jump withthe reori<strong>en</strong>tation of ferromagnetic domains. At the sametime, the critical field H c decreases with increasing annealingtemperature suggesting that ferromagnetic domains rotatemore easily inside a large homog<strong>en</strong>eous grain since nobarriers are pres<strong>en</strong>t.To confirm the reori<strong>en</strong>tation ph<strong>en</strong>om<strong>en</strong>on, we have performedsubsequ<strong>en</strong>t runs at 2 K, measuring the full M(H)loop. The starting bulk corresponds to a piece of the pelletsintered at 950 ◦ C. This piece was th<strong>en</strong> crushed into finepowder (sieved at 80 µm) and let free to rotate under theaction of the applied field. In a third run, this same powderwas homog<strong>en</strong>eously dispersed inside a drop of liquefiedvacuum grease, th<strong>en</strong> froz<strong>en</strong> at 2 K in order to blockany rotation of the fine particles, and performed a M(H)loop. Finally, the gel-type solution was heated at 350 K insidethe cryostat, and a 50 kOe field was applied. The gelwas th<strong>en</strong> cooled under the same static field down to 2 K,with all domains ori<strong>en</strong>ted parallel to the applied field. Figure138 shows the full M(H) loop under these 4 differ<strong>en</strong>texperim<strong>en</strong>tal set-ups.Figure 138: M(H)-loops measured under 4 differ<strong>en</strong>t conditionsfor ErCo 0.50 Mn 0.50 O 3 sample calcined at 950 ◦ C.Figure 137: Positive part of magnetization loops at T = 2 K forgiv<strong>en</strong> calcination temperatures (in ◦ C).Figure 137 pres<strong>en</strong>ts part of the M(H)-loops for selectedpellets. Below an annealing temperature of about 950 ◦ C,the magnetization increases smoothly with increasing field,until an inflexion point occurs at about 40 kOe. This inflexionpoint transforms into a sudd<strong>en</strong> jump at H c , for sinteringIt can immediately be noticed that the most significantchange in the magnetization loop concerns the height of thejump, which increases by about 60% in the ori<strong>en</strong>ted powderwith respect to the bulk ceramics. It is also evid<strong>en</strong>t that,wh<strong>en</strong> the particles are homog<strong>en</strong>eously dispersed and not allowedto rotate (run 3), the magnetization jump is smoothedout and becomes just an inflexion point. In conclusion, wehave unambiguously shown that grains size and percolationare the most important mechanisms in the rotation of magneticdomains in this material.A. B. AntunesC. M. Campos, O. Peña (Sci<strong>en</strong>ces Chimiques de R<strong>en</strong>nes,Université de R<strong>en</strong>nes 1, R<strong>en</strong>nes, France), G. Pecchi (Facultadde Ci<strong>en</strong>cias Químicas, Universidad de Concepción, Concepción, Chile)94
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LABORATOIRE NATIONAL DES CHAMPS MAG
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TABLE OF CONTENTSPreface 1Carbon Al
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Coexistence of closed orbit and qua
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2009PrefaceDear Reader,You have bef
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2009 CARBON ALLOTROPESInvestigation
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2009 CARBON ALLOTROPESPropagative L
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2009 CARBON ALLOTROPESEdge fingerpr
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2009 CARBON ALLOTROPESObservation o
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2009 CARBON ALLOTROPESImproving gra
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2009 CARBON ALLOTROPESTuning the el
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2009 CARBON ALLOTROPESElectric fiel
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2009 CARBON ALLOTROPESMagnetotransp
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2009 CARBON ALLOTROPESGraphite from
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2009Two-Dimensional Electron Gas25
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TWO-DIMENSIONAL ELECTRON GAS 2009Di
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TWO-DIMENSIONAL ELECTRON GAS 2009Sp
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TWO-DIMENSIONAL ELECTRON GAS 2009Cr
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TWO-DIMENSIONAL ELECTRON GAS 2009Re
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TWO-DIMENSIONAL ELECTRON GAS 2009In
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TWO-DIMENSIONAL ELECTRON GAS 2009Ho
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TWO-DIMENSIONAL ELECTRON GAS 2009Te
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2009 PUBLICATIONS[21] O. Drachenko,
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2009 PUBLICATIONS[75] S. Nowak, T.
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Contributors of the LNCMI to the Pr
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Institut Jean Lamour, Nancy : 68Ins
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Lawrence Berkeley National Laborato