24.02.2013 Views

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

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

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 />

11

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!