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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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Specific Heat of SrRuO 3<br />

taken in 0 T after application of an 8 T field (circles) shows that the zero-field<br />

data are not hysteretic. On this plot of ∆c/T, the 8 T data (diamonds) show<br />

that the only observed change in the specific heat is a decrease in the linear-T<br />

term.<br />

To further understand the field dependence of γ, specific heat points<br />

between 4 K and 5 K at several intermediate fields were also taken. These<br />

data are shown in Figure B- 3 (open circles) as γ(H) = (c(T,H) - βT 3 )/T using the<br />

value of β measured at 0 T and 8 T. On the same plot, the open squares<br />

indicate the fitted value of γ from the three data sets in Figure B- 1.<br />

Figure B- 3 shows that the coefficient of the linear-T term in the specific heat<br />

decreases approximately linearly with applied magnetic field, H.<br />

To summarize, the specific heat between 3 and 13 K can be described by<br />

c(T,H) = (γ - γ ´H)T+βT 3 .<br />

Although the magnetization of polycrystalline SrRuO 3 is irreversible, the<br />

measured heat capacity is not. Therefore, the heat capacity originates from<br />

processes reversible with respect to a magnetic field, showing that the entropy<br />

associated with random domains is negligible. In this sense, the heat capacity<br />

is a better thermodynamic measure of the low-lying excitations. The<br />

magnetic field dependence of the heat capacity and the magnetization are<br />

related by the following Maxwell relation:<br />

⎛ ∂CH ⎞<br />

⎝ ∂H ⎠ T<br />

= T ∂ 2 M<br />

∂T 2<br />

⎛ ⎞<br />

⎜ ⎟<br />

⎝ ⎠ H<br />

(1)<br />

According to equation 1, the first derivative of the heat capacity with<br />

respect to field gives information about the second derivative of the<br />

magnetization with respect to temperature. This relation is generally valid<br />

for an isotropic system as long as there are no irreversible processes involved<br />

and no PV work is done. Equation 1 is actually three equations since H and M<br />

177

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