Electrical Resistivity Tomography (ERT) and Induced Polarization (IP)

Main Areas of Application

· Mineral and coal exploration

· Geotechnical investigations

· Hydrogeology

· Environmental studies

· Engineering & infrastructure

· Archaeology

Understand Subsurface Conditions with Confidence

Electrical Resistivity Tomography (ERT) and Induced Polarization (IP) are proven geophysical survey methods used to image subsurface conditions non-invasively. These techniques are widely applied in geotechnical investigation, groundwater exploration, and engineering risk assessment.

At GeophysicsPro, we deliver high-resolution resistivity imaging integrated with geological and geotechnical interpretation, helping you reduce uncertainty and make reliable project decisions.

👉 Request a consultation to discuss your project requirements

Why Use ERT & IP for Subsurface Investigation?

  • Non-invasive and cost-effective alternative to extensive drilling

  • Provides continuous 2D/3D subsurface imaging

  • Detects weak zones, fractures, and groundwater pathways

  • Reduces uncertainty in engineering design and site investigation

  • Effective in complex geological and tropical weathering environments

These advantages make ERT & IP surveys essential tools for modern subsurface investigation workflows.

Key Applications of Resistivity & IP Surveys

Geotechnical Investigation

  • Foundation assessment and bedrock mapping

  • Identification of weak zones and weathered materials

  • Fracture and fault zone detection

  • Subsurface variability analysis

Groundwater Exploration

  • Aquifer delineation and depth estimation

  • Mapping groundwater flow pathways

  • Seawater intrusion detection

  • Hydrogeological characterization

Infrastructure & Construction

  • Subsurface investigation for roads and buildings

  • Void and cavity detection

  • Utility corridor assessment

  • Pre-construction risk evaluation

Environmental Studies

  • Contamination and leachate detection

  • Landfill and waste site investigation

  • Monitoring subsurface fluid movement

  • Road Landslide

How Electrical Resistivity & IP Surveys Work

Electrical Resistivity Tomography (ERT)

ERT measures the electrical resistivity of subsurface materials by injecting current into the ground.

  • High resistivity → competent rock, dry materials

  • Low resistivity → clay-rich or water-saturated zones

This allows accurate imaging of:

  • Lithological boundaries

  • Bedrock depth

  • Groundwater zones

Induced Polarization (IP)

IP measures chargeability, indicating the ability of subsurface materials to store electrical charge.

  • High chargeability → clay-rich or conductive materials

  • Low chargeability → clean sands or massive rock

IP improves interpretation by distinguishing:

  • Clay vs water saturation

  • Material composition in complex environments

  • Resistivity vs Chargeability

Integrated Interpretation for Reliable Results

Combining ERT and IP provides a multi-parameter subsurface model, reducing ambiguity:

  • Resistivity defines structure and fluid distribution

  • Chargeability refines material characterization

This integrated approach is particularly effective for:

  • Fractured rock environments

  • Tropical weathering profiles

  • Urban subsurface complexity

Our Workflow for ERT & IP Surveys

1. Survey Design

  • Objective-based planning

  • Selection of optimal electrode arrays

  • Depth and resolution optimization

2. Data Acquisition

  • Multi-electrode resistivity and IP systems

  • High-density data collection

  • Field quality control and noise reduction

Equipment & Technology

We utilize advanced multi-channel resistivity meters with automated electrode switching to ensure:

  • High-resolution data acquisition

  • Reliable signal quality in challenging environments

  • Efficient field operations

3. Data Processing & Inversion

  • Industry-standard inversion (RES2DINV / RES3DINV)

  • Noise filtering and data validation

  • Generation of true resistivity and chargeability models

4. Interpretation

  • Integration with geological and geotechnical data

  • Identification of layers, anomalies, and structures

  • Engineering-focused interpretation

5. Deliverables

You receive clear, decision-ready outputs:

  • 2D and 3D resistivity & chargeability sections

  • Interpreted subsurface profiles

  • Identification of risk zones (voids, weak zones, fractures)

  • Technical report with actionable recommendations

Applications in Real Projects

  • Mapping subsurface fractures causing structural damage

  • Identifying slip surfaces in landslide-prone areas

  • Detecting voids beneath infrastructure

  • Delineating groundwater systems

Combine with Other Geophysical Methods

For improved results, ERT & IP surveys can be integrated with:

  • MASW for soil stiffness and shear wave velocity

  • GPR for shallow high-resolution imaging

This multi-method approach provides a comprehensive subsurface investigation solution.

Value to Your Project

Our resistivity and IP survey services help you:

  • Reduce uncertainty in subsurface conditions

  • Optimize drilling and investigation costs

  • Improve engineering design decisions

  • Detect geohazards early

  • Increase project safety and reliability

Why Choose GeophysicsPro

  • Integration of geophysics with geotechnical interpretation

  • Experience in complex geological and tropical environments

  • Use of advanced inversion and modeling techniques

  • Focus on decision-ready results, not just data

  • Flexible full-service and modular solutions

Frequently Asked Questions (FAQ)

What is a resistivity survey used for?

Resistivity surveys are used to image subsurface conditions, identify groundwater, detect weak zones, and support geotechnical investigations.

How deep can ERT investigate?

Depth depends on electrode spacing, but typically ranges from a few meters to over 100 meters.

Is ERT better than drilling?

ERT does not replace drilling but significantly reduces uncertainty by providing continuous subsurface imaging between boreholes.

When should IP be used with ERT?

IP is recommended when distinguishing between clay-rich materials and water saturation is critical.

Start Your Subsurface Investigation with Confidence

Whether you are planning infrastructure, assessing geohazards, or exploring groundwater resources, our ERT & IP survey services provide reliable, high-resolution subsurface insights.

👉 Contact us today to discuss your project and get a tailored survey solution

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