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Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet

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only adequate smoothing of the observed anomal.ous surface field.<br />

Then a certain well defined depth dep'endence of the anomalous<br />

current density is adopted as discussed below and the anomalous<br />

current distribution can be derived in a straightforward manner.<br />

Suppose an observed anomaly 51, at a given frequcncy has been ex-<br />

plained in this way by a distribu-tion of anomalous internal.<br />

currents. Its connection to the internal conductivity is esta-<br />

blished by the normal and anomalous electric field vector accor-<br />

ding to<br />

Assuming the normal conductivity distribution un(z) to be known,<br />

E as a function of depth 'is readily calculated. There is no<br />

-I1<br />

simple way, however, to derive the anomalous electric field of<br />

the TE mode except by numerical models as discussed below. There<br />

is in particular no justification to regard it as small. i.n com-<br />

parison to the normal electric field and thus to drop the second<br />

term in the above relation. Instead the following argumentati.on<br />

has to be used:<br />

The anomalous electric field in the TE mode can be thought to<br />

contain two distinct components. The first component may be re-<br />

garded as the result of local self-induction due to EaII. I -.<br />

can be neglected a-t suffici.ently low frequencies, when the ;-lzlf-<br />

width of the anomaly is small in comparison to the minimum skin-<br />

depth value within the anomalous zone.<br />

The second component arises from electric charges at boundari-es<br />

and in zones of gradually changing conductivi-by. These charges<br />

produce a quasi-static electric field norroal to bounclarics and<br />

paral7.el -to in-ternal conduc-tivity gradients which ensures the<br />

continuity of the current across boundaries and internal gradient<br />

zones. Hence, this second component of the anomalous electric<br />

field does not disappear, when the frequency becomes small.<br />

It vanishes, however, if anomalous internal currents do not cross<br />

boundaries of gradient zones, i.e. when the normal field is in<br />

E-polarisa-tion with respect to the -tl>end of elongated s'iructures.

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