: Directly integrates low-induction number apparent conductivity datasets (expressed in milliSiemens/meter) sourced from legacy or modern instruments like the Geonics EM-31, EM-34, or EM-38.
For decades, geophysicists and hydrogeologists have relied on Vertical Electrical Sounding (VES) to map subsurface resistivity. The technique—rooted in the Schlumberger or Wenner arrays—produces raw data that is almost useless without robust inversion modeling. Enter , a name synonymous with reliable geophysical software, and their flagship product, IX1D . interpex ix1d v350
Alluvial basin in Rajasthan, India Goal: Locate a fresh water aquifer under 40 m of clayey sand Method: 10 VES soundings with AB/2 from 1.5 m to 300 m Enter , a name synonymous with reliable geophysical
IX1D v3.50 minimizes data preparation time. Users can import ASCII files, text sheets, and instrument-specific files directly from major hardware manufacturers like Iris Instruments, ABEM, and Phoenix Geophysics. 2. Smooth vs. Layered Inversion use File >
: Provides both forward and inverse modeling. It can generate "smooth" models (using many thin layers) or discrete "layered" models, which can be constrained by known geological data like layer thickness or depth.
After launching , use File > Import to load your field data. The software automatically recognizes common electrode spacings (AB/2 or a-spacing). You can edit bad points directly in the data grid.