Scientific Research And Essays, cilt.6, sa.24, ss.5213-5223, 2011 (SCI-Expanded)
One
of the main problems in resistivity surveys is the terrain effect because of
which the true interpretation of the subsurface structure may be biased. There
are two approaches to deal with this problem: i) terrain-correction that uses
correction factors in a homogeneous earth or ii) inversion that incorporates
topography. Some terrain models such as hills and slopes are used to evaluate
the effect of the terrain on the 2D modelling and inversion where the finite
elements method is used for the forward modelling. The least-squares inversion
technique is used to estimate the resistivities within each block of the model
structure. The forward modelling results indicate that the terrain topography
significantly contaminates the subsurface response. The terrain-correction used
to eliminate the topography effect helps to isolate the response of the real
subsurface. The inversion incorporating topography also gives reliable results
if correct host rock resistivity is used in the process.