Interpex Ix1d V350 File

You can manually enter data or import from .RES, .DAT, or .SND files. The graphical editor plots the apparent resistivity curve (log-log scale). Anomalous points can be flagged and removed using the "Data Smoothing" tool, which applies a moving average filter.

Even before inversion, you can build hypothetical layered models and generate synthetic sounding curves. This is invaluable for survey design and teaching.

For EM inversion, IX1D remains one of the few widely available 1‑D EM inversion software packages. While 2‑D and 3‑D EM inversion tools are rare, studies have successfully replaced them by using IX1D on dense profile data to build quasi‑2‑D sections.

Forward Modeling: [Hypothetical Subsurface Layering] ---> Computes Expected Field Readings Inverse Modeling: [Actual Field Data Readings] --------> Calculates True Layer Thickness & Resistivity interpex ix1d v350

While modern geophysics often leans toward 2D and 3D imaging, 1D sounding remains essential for rapid reconnaissance, deep structural mapping, and vertical profiling where lateral changes are relatively gradual. Key Capabilities of v3.50

What you are trying to map (aquifers, bedrock, plumes)?

Choose your specific exploration method (e.g., DC Resistivity Sounding). Select your electrode array geometry. You can manually enter data or import from

and reduce them to simplified layered models for comparison with surface data. User Experience Insights Compatibility:

Determining overburden thickness and bedrock depth.

IX1D v350 supports most common DC resistivity arrays, including: Schlumberger Dipole-dipole Pole-dipole Pole-pole 2. Diverse Data Handling (Resistivity & IP) Even before inversion, you can build hypothetical layered

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If you want to tailor this modeling process to your specific fieldwork, tell me: