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Read Back Signals in Magnetic Recording - Research Group Fidler

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FEM Simulations<br />

has a greater <strong>in</strong>fluence. The result is a more likely antiparallel state, which is equivalent to a<br />

higher total resistance.<br />

This proves that the shield also have an <strong>in</strong>fluence on the read head behavior and cannot be<br />

neglected <strong>in</strong> micromagnetic simulations.<br />

6.2.4 Relaxation<br />

The micromagnetic behavior of the GMR sensor depends on the Gilbert damp<strong>in</strong>g constant.<br />

Start<strong>in</strong>g from an equilibrium state with an external field of H ext = 0.03 T <strong>in</strong> positive z-<br />

direction, the relaxation to the new equilibrium state when suddenly switch<strong>in</strong>g off the field, is<br />

shown <strong>in</strong> Figure 6.8.<br />

Output Voltage [V]<br />

0.1060<br />

0.1055<br />

0.1050<br />

0.1045<br />

0.1040<br />

0.1035<br />

0.1030<br />

0.0 0.2 0.4 0.6 0.8<br />

Time [ns]<br />

α = 0.1<br />

α = 0.2<br />

α = 0.3<br />

α = 0.5<br />

α = 1<br />

Figure 6.8: The output signal over time for a relaxation from equilibrium state with<br />

Hext = 0.3 T to the equilibrium state without field for different Gilbert damp<strong>in</strong>g constants.<br />

For large Gilbert damp<strong>in</strong>g constants we have strong damp<strong>in</strong>g, result<strong>in</strong>g <strong>in</strong> a quite large<br />

relaxation time (larger than 0.4 ns). New read heads work with a read frequency up to 2 GHz.<br />

Therefore such large relaxation times would weaken the read back signal. Fortunately realistic<br />

damp<strong>in</strong>g constants are about α ∼ 0.1,<br />

which lead to an undercritical damp<strong>in</strong>g, result<strong>in</strong>g <strong>in</strong><br />

damped oscillations. Smallest relaxation times are achieved for critical damp<strong>in</strong>g with<br />

damp<strong>in</strong>g constants around 0.3.<br />

73

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