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 />
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