Read Back Signals in Magnetic Recording - Research Group Fidler
Read Back Signals in Magnetic Recording - Research Group Fidler
Read Back Signals in Magnetic Recording - Research Group Fidler
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2 BasicsEquation<br />
Section (Next)<br />
2.1 Ohm’s Law<br />
Basics<br />
Georg Simon Ohm (1789-1854) found that the current I through most materials is<br />
proportional to the applied voltage V.<br />
V = R⋅ I<br />
(2.1)<br />
The proportional coefficient is called resistance R. The more general form of this equation is<br />
shown below.<br />
σ⋅ E = j (2.2)<br />
E [V/m] denotes the electric field, and j [A/m 2 ] the current density. σ [A/Vm] is a property<br />
of matter named conductivity. Generally the conductivity is a tensor, but here all conductors<br />
will be assumed to be isotropic.<br />
2.2 Maxwell’s Equations<br />
James Clerk Maxwell (1831-1879) was the first who jo<strong>in</strong>ed the theories of electricity and<br />
magnetism. He proposed follow<strong>in</strong>g four equations to describe both theories (<strong>in</strong> SI).<br />
� ∫ DdA= ∫ρdV<br />
(2.3)<br />
∂V<br />
V<br />
� ∫ BdA= 0<br />
(2.4)<br />
∂V<br />
∂<br />
� ∫Eds=− d<br />
∂t<br />
∫B<br />
A<br />
(2.5)<br />
∂A<br />
A<br />
∂<br />
� ∫ Hds= ∫jdA+ d<br />
∂t<br />
∫D<br />
A<br />
(2.6)<br />
∂A<br />
A A<br />
These four <strong>in</strong>tegral equations can also be written as equivalent differential equations.<br />
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