: Full configuration capabilities for Vertical Electrical Sounding (VES). It supports Wenner, Schlumberger, dipole-dipole, pole-dipole, and pole-pole arrays.
Geophysicists can manually input or dynamically manipulate stratigraphic models through an integrated spreadsheet grid. Models can be structured via absolute layer depth or explicit layer thickness. Boundary elevations automatically calibrate themselves dynamically whenever surface topography data is supplied. Parameter Isolation via Fix Flags
Synthetic curve line sheets, Zaborovsky plots, colored depth profiles IX1Dv3.exe Software Evolution Notes interpex ix1d v350
However, the IX1D V350 is not without limitations. Its primary constraint is its inherent 1D assumption: it presumes the subsurface is composed of horizontal, laterally infinite layers. In areas with steeply dipping beds, boulders, or significant 3D structures (like a narrow dike), the inversion can produce misleading or non-unique results. Furthermore, the interface, while functional and efficient, retains a distinctly late-1990s aesthetic, lacking the interactive 3D visualization common in modern software like Res2DInv or Voxler. For a generation of students raised on touchscreens, the dialog-box-driven workflow can feel initially archaic.
Handles Frequency Domain EM (like the Geonics EM31/34) and Time Domain EM (TEM/TDEM) sounding data. Models can be structured via absolute layer depth
Before running an automatic inversion, build a rough conceptual model:
If you require further technical details, licensing inquiries, or training schedules, contact Interpex Limited directly at or visit the official website: http://www.interpex.com. Its primary constraint is its inherent 1D assumption:
Interpex IX1D v3.50: Complete Guide to 1D Geophysical Inversion
This is called . IX1D v3 uses sophisticated algorithms (like the "Smooth Model" or "Layered Model" approaches) to mathematically calculate the depth and resistance of each layer. It essentially works backward from the data to build a cross-section of the earth.
The unified package integrates quantitative interpretation for several major sounding techniques:
is a specialized software application designed for the forward modeling and automatic inversion of 1D resistivity sounding data. Unlike full tomography software, IX1D v350 focuses on the vertical variation of resistivity beneath a single point—the "sounding" center.
