A finite difference algorithm for solving the forward modelling problem of geo-electromagnetic
induction in two-dimensional (2D) structures has been developed
in this thesis. The governing equations have been modified to solve for the anomalous
field by separating out the 'host' field which is assumed to be the field generated
by the one-dimensional (1D) conductivity distribution on the left hand side
of the model. This was done to prevent the small anomalous fields being masked
by the much larger host field due to the finite length of the computer word. One
of the most important features of this program is an automatic gridding subroutine
which greatly reduces the amount of time required to design a suitable grid
for a model and removes the human element from such grid design. Up to 20
periods can be submitted to the model at one time and specific locations (e.g.
the locations at which field data are available) can be added to the automatically
generated grid. Integral boundary conditions at the surface and bottom (z = d) of
the model eliminate the need to extend the grid above the earth's surface or down
into the half-space underlying the model.
The program has been used to perform a 2D inversion of magnetoteliuric data
from a NS profile in Sardinia. The magnetoteliuric responses from two sites along
this profile indicated that the structure underneath them could not be considered
to be solely 2D. To examine the conductivity anomalies perpendicular to the profile indicated
that are affecting the results at these two sites, 2D inversions were performed on
the data to obtain their EW conductivity models. The apparent resistivity curves
from the models fit the data fairly well at both sites especially at short periods.
Many features of the models were in agreement with the 2D model along the profile
obtained by Peruzza et al. (1990) and they also provided insight into the geological
structure of the area.
A study was made of the behaviour of 2D induction arrows over a buried conductivity
contrast. Although the general trend of in-phase arrows is to point towards
the regions of high electrical conductivity, some investigators have found small amplitude
in-phase arrows that point away from these same regions. Reversals such
as these, which do not behave according to the general trend, can cause confusion
and erroneous interpretation of the in-phase induction arrows. Using a model
with two semi-infinite conducting plates, one at the surface and one buried at a
depth d in a layered half space, it was found that the period at which a reversal
in the in-phase induction arrow direction occurs was a function of the apparent
resistivity of the layered host. Anomalous behaviour was found in the short period
in-phase arrows from which the coast effect had been removed. The problems in
interpretation of such arrows was discussed.
Finally a 2D inversion scheme was discussed in which a 2D forward modelling
program was incorporated with a minimization routine MTNDEF. First an investigation
was made into the relative merits of using the impedances ZTE, ZTM, Zave
and Zeff to calculate the ID inversions that are combined to form starting models
for the 2D inversions. A subsequent 2D inversion of the North American Central
Plains (NACP) anomaly results in a best fit model whose responses show good
agreement with the field data from 20 sites. Tests have been performed to ensure
that an oversimplification of the starting model is not responsible for the lack of
certain features found by other authors. It is concluded that the incorporation of
these features in the model is not required in order to obtain a good fit to the field
data. / Graduate
| Identifer | oai:union.ndltd.org:uvic.ca/oai:dspace.library.uvic.ca:1828/9674 |
| Date | 11 July 2018 |
| Creators | Poll, Helena Eva |
| Contributors | Weaver, J. T. |
| Source Sets | University of Victoria |
| Language | English, English |
| Detected Language | English |
| Type | Thesis |
| Format | application/pdf |
| Rights | Available to the World Wide Web |
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