The study's goal is to provide parameter sensitivity maps for nonlinear and focused electrode arrays. To comprehend geoelectric arrays, you must first understand parameter sensitivity maps. These maps are displayed as anomalies caused by electric dipoles developing on opposing sides of an elementary cube beneath the subsurface at three distinct depths, and they indicate not only the dipole's entire influence, but also the effect of its components. In general, non-linear array parameter sensitivity maps feature (1) more equal sensitivity values in the x and y directions, (2) more opportunities for antisymmetry axis, and (3) a smoother lateral distribution of sensitivity values than linear array parameter sensitivity maps. We suggest employing parameter sensitivity maps in a systematic manner in geoelectric prospecting, both in terms of planning and analysing field findings.
S. Szalai,
Institute of Earth Physics and Space Science, H-9401 Sopron POB 5, Hungary.
L. Szarka,
Institute of Earth Physics and Space Science, H-9401 Sopron POB 5, Hungary.
M. K. Baracza,
Research Institute of Applied Earth Sciences, University of Miskolc, Hungary.
P. Szucs,
University of Miskolc, Institute of Environmental Management, Hungary and MTA-ME Geoengineering Research Group, Miskolc Hungary.
Please see the link here: https://stm.bookpi.org/CAGEES-4/article/view/7116
No comments:
Post a Comment