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MAGNETISM ELECTRON TRANSPORT MAGNETORESISTIVE LANTHANUM CALCIUM MANGANITE

MAGNETISM ELECTRON TRANSPORT MAGNETORESISTIVE LANTHANUM CALCIUM MANGANITE

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108 Chapter 5<br />

of the nonlinear M 2 vs. H/M Arrott plot is given in Figure 5-4.<br />

5. 1. 5 Magnetism model<br />

To explain the magnetism, a mean field model was used assuming a<br />

ferrimagnetic ground state. Other possible explanations for the magnetism in<br />

Gd 0.67 Ca 0.33 MnO 3 are briefly discussed<br />

5 kOe<br />

Gd 0.67 Ca 0.33 MnO 3 Mean Field Calculation<br />

Remnant<br />

Gd<br />

Mn<br />

20 40 60 80 100 -5<br />

Temperature (K)<br />

3<br />

2<br />

1<br />

0<br />

-1<br />

-2<br />

-3<br />

-4<br />

Magnetization (µ B /mol)<br />

5 kOe<br />

0 50 100 150 200 250<br />

0<br />

300<br />

Temperature (K)<br />

Figure 5-5 Magnetization and inverse magnetic susceptibility<br />

calculated for Gd 0.67 Ca 0.33 MnO 3 using the simplified mean field<br />

theory described in the text and T C = 83 K, T Comp = 17 K. The<br />

contribution to the magnetization of each sublattice is shown<br />

in dashed lines.<br />

5. 1. 5. 1 Mean Field Model<br />

Due to the stronger 3d exchange interaction compared to that of the 4f, the<br />

Mn-Mn coupling is expected to be stronger than the Mn-Gd, and the Gd-Gd<br />

interaction to be negligible. Since the observed Curie temperature is about<br />

40<br />

35<br />

30<br />

25<br />

20<br />

15<br />

10<br />

5<br />

1/χ (mol G/emu)

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