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Geoelectric / Resistivity Survey
Survei Geolistrik
Geoelectric survey is a geophysical method that measures the resistivity of rocks and soil beneath the surface. By injecting electrical current into the ground through electrodes and measuring the resulting potential difference, we can map the resistivity distribution both vertically and laterally.
Methods & Equipment
Wenner Array
Symmetric configuration for lateral mapping and apparent resistivity determination. Suitable for shallow to medium depth surveys.
Schlumberger Array
Vertical Electrical Sounding (VES) configuration for determining depth of rock layers and aquifers.
Dipole-Dipole
Configuration with high lateral resolution, ideal for detecting vertical structures such as faults and cavities.
Pole-Dipole
Asymmetric configuration with greater depth range, suitable for deep surveys.
Equipment Used
Applications & Use Cases
Standards & Regulations
What You Receive
- 1Survey point location map and electrode configuration
- 22D resistivity cross-section from inversion
- 3Resistivity distribution map per depth
- 4Subsurface geological and hydrogeological interpretation
- 5Technical recommendations for project planning
- 6Complete report per SNI standards
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