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Investigation On The Magnetic Property Under Pressure And Magnetoresistance Effect Of La1-xCaxMnO3(x=0.1,0.3,0.5)

Posted on:2022-01-23Degree:MasterType:Thesis
Country:ChinaCandidate:R RaoFull Text:PDF
GTID:2481306542960749Subject:Materials Science and Engineering
Abstract/Summary:PDF Full Text Request
The perovskite manganite possess lots of unique phyical properties,such as the colossal magnetoresistance(CMR),metal-insulator transition(MIT),Jahn-Teller(J-T)distortion,charge ordering and phase separation,etc.,enabling them to be used in fields of magneto-electric coupling,magnetic storage and the tunneling junction,etc.The manganite with the formula R1-xAxMnO3 is an important member of the perovskite manganites,where R represents trivalent rare earth metal ions(such as La3+,Nd3+),A denotes the divalent alkali earth metal ions(such as Ca2+,Sr2+and Ba2+),and Mn ions exhibits the mixture valences of Mn3+and Mn4+.Due to the interaction of charge-lattice-spin-orbit freedom degrees,R1-xAxMnO3 exhibits the rich physics,such as the Mn3+-O-Mn4+double-exchange(DE)ferromagnetism,the Mn3+-O-Mn3+or Mn4+-O-Mn4+super-exchange antiferromagnetism and the J-T distortion due to the interaction between eg electrons of Mn3+and the crystal lattice.The physical properties of R1-xAxMnO3 intensively depend on the doping level.The ground state of LaMnO3 is an A-type antiferromagnetic and insulating state.The substitution of Ca2+at Lasites produces the Mn with the+4 valence,resulting in the significant changes of physical properties of R1-xAxMnO3.For examples,La0.9Ca0.1MnO3 with x=0.1 exhibits the phase separation with the coexistence of ferromagnetic metallic,ferromagnetic insulatiing and(canted)antiferromagnetic insulating states in the temperature region below Tc.When the doping amount is 30%,La0.7Ca0.3MnO3 is a ferromagnetic metal state below Tc.For La0.7Ca0.3MnO3 with x=0.3,it exhibits the ferromagnetic metallic state below Tc;with increasing the temperature,the competition between Mn3+-O-Mn4+and the J-T distortion induces the MIT.For La0.5Ca0.5MnO3with x=0.5,it locates the phase boundary between the charge-ordered antiferromagnetic and ferromagnetic metallic states.Moreover,as a result of the approximate interaction energy among charge,lattice,spin and orbit,a tiny external stimulation such as the magnetic field/electric field/pressure can significantly change physical properties,such as the CMR effect and the MIT induced by the magnetic field,the electro-resistance effect induced by the electric field and the reduction of resistivity and MIT induced by the pressure.With respect to the pressure(P),just like the temperature and magnetic field,acting as clean and effective means,on one hand,it can manipulate the electric/magnetic properties of La1-xCaxMnO3;on the other hand,theoretically,it can manipulate the J-T distortion,as a result,it can be used to find novel phenomena and to reveal the physical mechanism.There are many reports on Raman,electrical transport properties and neutron diffraction under the pressure,but there are relatively few studies on magnetic properties under the pressure.In this thesis,we use the pressure as a means to study the influence of pressure on the magnetic properties of La1-xCaxMnO3.This thesis is divided into six chapters,and the content of each chapter is as follows:Chapter 1:We firstly introduce the crystal structure and basic physical properties of La1-xCaxMnO3.Then,the pressure effect and magnetoresistance effect were reviewed.Finally,the research purpose and significance of this thesis are pointed out.Chapter 2:We mainly introduce the methods of preparation and characterization of La1-xCaxMnO3 samples.Chapter 3:We investigated the magnetic properties under the pressure and the electrical transport under the magnetic field for the bulk La0.9Ca0.1MnO3 polycrystalline.At the ambient pressure,La0.9Ca0.1MnO3 exhibits a paramagnetic(PM)-ferromagnetic(FM)transiton at the Curie temperature(Tc)of 191 K and a canted-antiferromagnetic(C-AFM)transiton at 68 K.The sample exhibits the PM insulating state above Tc,but the phase separated FM insulating,FM metallic and the C-AFM states.The pressure enhances the antiferromagnetic coupling of ferromagnetic clusters with the concomitant variation of anisotropy in the PM region.Around Tc,the pressure suppresses the large J-T distortion,linearly increasing Tc with the pressure coefficient of 15.9 K/GPa and simultaneously increasing the magentization.But the pressure reduces the magnetization below Tc,attributable to the suppression of pressure to the weakly distorted MnO6 octrhedron in the FM metallic phase,making the Mn ionic moment canted.The pressure suppresses the C-AFM state,gradually reducing the anisotropy related to the C-AFM transition,indicating that the pressure changes the FM and C-AFM phase-separated state below Tc to a more homogeous C-AFM state.Moreover,the magnetic field causes a negative magnetoresistance effect.Magnetoresistance exhibits peaks at 191 K and 127 K,attributable to the suppression of spin-related scattering by the magnetic field and the transition of the antiferromagnetic insulating phase to the ferromagnetic metal phase.Chapter 4:We investigated the magnetic properties under the pressure and the electrical transport under the magnetic field for the bulk La0.7Ca0.3MnO3 polycrystalline.The pressure induces the antiferromagnetic(AFM)coupling of the FM clusters in the PM region above Tc;suppresses the J-T distortion around Tc and enhances the DE interaction,hence increasing Tc;enhances the distortion of MnO6 octahedral in the ferromagnetic metallic region below Tc,resulting in the decrease of magnetization.MR appears a peak at 255 K,due to the enhanced DE interaction by the magnetic field and the increase in the kinetic energy of the eg electrons.The rise in the magnetic field decreases the activation energy of polarons in the para-magentic region.Chapter 5:Effects of pressure on magnetic properties of La0.5Ca0.5MnO3 were investigated.Results showed that the application of pressure reduced PM-ferromagnetic FM transition temperature Tcfrom 226 K to 223 K,as well as FM-AFM transition temperature TN from 180K to 175 K.Meanwhile,the applied pressure also increased charge/orbital ordering transition temperature TOO from 70 K to 74 K.Below TN,inhomogeneous AFM phases,including FM and AFM phases,coexisted in La0.5Ca0.5MnO3.The application of pressure led to changes in zero-cooling magnetization(?MZFC),with?MZFC?0 in the PM region above 285 K,?MZFC>0 at T+/-<T<285 K,and?MZFC<0 at T<T+/-(where T+/-corresponding to temperature at which?MZFC changed from the positive to negative value).Analysis of the data revealed that?MZFC>0 did not result from enhanced double-exchange coupling by the applied pressure but most-likely from pressure-induced AFM-to-FM transition.On the other hand,?MZFC<0 in the low temperature region below T+/-may be attributed to the pressure-induced FM-to-AFM transition,the variation in AFM type,and enhancement of J-T distortion.The difference of pressure-induced effects below and above T+/-was related to the formation and the evolution of charge/orbital ordering in the low temperature region.Chapter 6:The CoFe2O4/La0.7Ca0.3MnO3 polycrystalline bulk is chosen as the studying object.The pressure is applied during the magnetic measurements in order to tune the interparticle distance,and hence change the inter-grain exchange-coupling,dipolar interaction and the anisotropy,for the purpose to study their effects on the magnetic property of the composite.The main results are as follows.At the ambient pressure,the step-like spontaneous magnetizing is observed due to the difference of anisotropy of the particles.The magnetic transition temperature Tc of the La0.7Ca0.3MnO3 in the composite is lower than that of pure La0.7Ca0.3MnO3,due to the lattice mismatch and the Co(Fe)-O-Mn super-exchange,occurring at the interface between CoFe2O4 and La0.7Ca0.3MnO3.In the low temperature region,the pressure reduces the magnetization,due to the enhanced distortion of Mn3+O6 octahedral in La0.7Ca0.3MnO3,induced extra anisotropy and the enhanced dipolar interaction by the pressure.The coercivity Hc of the composite at 10 K monotonically increases with the pressure,due the induced anisotropy by the pressure,while the remanence ratio Mr/Ms decreases with the pressure,because of,on one hand,the reduced remanence magnetization Mr due to the enhanced distortion of Mn3+O6octahedral and induced anisotropy by the pressure,on the other hand,the larger saturation magnetization Ms of the composite than that of the pure CoFe2O4.Summary and outlook.
Keywords/Search Tags:Perovskite manganite, Pressure, Magnetic properties, Double-exchange, Jahn-Teller distortion
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