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Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet

Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet

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All field quanti-ties are functions of position _r and time t. Al.so tl:c<br />

(isotropic) conductivi.-t)~ u is a func.tion of position. -e I 3,s the<br />

current density of the external cilrrent sources being different from<br />

0 only at source points. The displacement current c 0- E is generally<br />

neglected in induction studies. This is justified as follows: within<br />

the conductor -- .the conduc-tion current UC - exceeds the displ.acement<br />

current even in the case of ].owest periods (0.001 sec) and highest<br />

5 2<br />

resis1:ivities (10 Rm) still 10 times. In the vacuum where .the<br />

conduction current is absent the inclusion of the, displacsment<br />

current merely introduces a slight phase shift of the external field<br />

at different points. for in this case the solution of (1.2) and (1.3<br />

(including at the RFIS of (1.2) ) are electromagnetic waves, e. g.<br />

the plane wave e i(k*r - - - u ~ ) where , w is the angular frequency and<br />

.- k the wave vector along the direction of propagation. The phase<br />

difference<br />

4<br />

between P and P2 is<br />

1<br />

,/ case<br />

- .<br />

PI Ax P2<br />

MAX<br />

l,j&t = -- coscl<br />

C<br />

.Z in the very pessimistic<br />

of Ax = 1000 km and T = lse<br />

- H ar~d - .I can he eliminated fPonl (1.. 2 - (1.4). It results<br />

L Induction equation<br />

----- - I<br />

6!t using C1.2) and (1.4) the elec-trical charge density p(1') - is<br />

given by<br />

p = E div - E = - c E - grad I.oga, (1.7)<br />

0 0 -<br />

i.e. there is charge accumulated if an electrical field compunclnt :<br />

parallel to the gradj.en.t. of the conductivi-ky. Physically 'this is<br />

cl.ear,, since the normal. componen-t of .the current density is conti-<br />

nuous whereas the charges accoun-i: for tl-~e corresponding discon-ti-<br />

nuity of the normal electri.cal. field.

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