Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet
Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet
Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
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.