MAGNETISM ELECTRON TRANSPORT MAGNETORESISTIVE LANTHANUM CALCIUM MANGANITE
MAGNETISM ELECTRON TRANSPORT MAGNETORESISTIVE LANTHANUM CALCIUM MANGANITE
MAGNETISM ELECTRON TRANSPORT MAGNETORESISTIVE LANTHANUM CALCIUM MANGANITE
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Critical Transport and Magnetization of La 0.67 Ca 0.33 MnO 3<br />
competition between ferromagnetic and antiferromagnetic interactions. As<br />
pointed out by DeGennes, there is competition between double exchange<br />
(ferromagnetic) and superexchange (antiferromagnetic) as will be discussed<br />
further in section 7.1.4. One of the early theories of double exchange<br />
presented by Anderson and Hasagawa [7] also predicts a downward curvature<br />
in 1/χ vs. T.<br />
It is not too surprising that two different values of γ (0.7 and 0.9) are<br />
obtained from the same data. The two methods weight the data differently<br />
and as discussed above, the true critical region where γ is a constant has<br />
probably not been reached.<br />
7. 1. 3 Positive nonlinear susceptibility<br />
A peculiarity of the T > T C isotherms of Figure 7-1, which likely affects the<br />
determination of γ, is their negative slope as they approach M 2 = 0. This slope<br />
is proportional to the nonlinear susceptibility. For M = χH + χ 3 H 3 , χ is the<br />
linear susceptibility and χ 3 is the third-order nonlinear magnetic<br />
susceptibility. The slope of a T > T C isotherm in an M 2 vs. H/M Arrott plot as<br />
M 2 approaches zero is given by -χ 4 /χ 3 . For a normal ferromagnet, χ > 0 while<br />
χ 3 < 0 giving a positive slope for all T > T C isotherms. However in<br />
La 0.67 Ca 0.33 MnO 3 a negative slope is found which implies that χ 3 > 0. This can<br />
also be seen in a plot of M vs. H, which is shown in Figure 7-1. A positive χ 3<br />
produces the faster than linear increase in M with H which leads to an<br />
inflection point in the M vs. H curve due to the saturation of M for large H.<br />
This effect is not likely due to the sample preparation since it is seen in both<br />
the polycrystal and float-zone crystal samples. Arrott plots of SrRuO 3<br />
(Appendix A) at similar temperatures do not show χ 3 > 0, which indicates that<br />
the effect is not due to the measurement system. A more pronounced<br />
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