It is possible to determine the detailed resistivity structure of the ground.
"Resistivity tomography" is an exploration method that involves installing electrodes around the exploration area using the ground surface and boreholes. It measures the potential generated by the current flowing into the earth to estimate the underground structure (primarily resistivity structure). It is suitable for detailed cavity and resistivity surveys, as well as investigations of fault zones and altered zones, and is expected to improve analysis accuracy compared to 2D resistivity surveys. 【Features】 ■ Non-destructive survey considerate of the Earth ■ High-precision automatic measurement ■ Measurement and analysis possible in a shorter time than before ■ Capable of measuring in areas with vibration noise *For more details, please download the PDF or feel free to contact us.
Inquire About This Product
basic information
【Application Examples】 ■ Detailed cavity and detailed resistivity survey ■ Fault fracture zone and alteration zone survey ■ Measurement of ground improvement effects and groundwater level fluctuation survey *For more details, please download the PDF or feel free to contact us.
Price range
Delivery Time
Applications/Examples of results
For more details, please download the PDF or feel free to contact us.
catalog（1）
Download All Catalogs
Company information
Our company has been engaged primarily in geological structure surveys and ground property investigations through elastic wave exploration, electrical exploration, and logging using boreholes, with the motto of "safe, swift, and careful observation and measurement" and "high-precision and rapid analysis using advanced systems." Additionally, we conduct investigations such as buried pipe surveys using ground-penetrating radar, depth surveys for guardrail posts, dynamic seismic performance assessments of wooden houses using the Waseda method, simultaneous measurement of microtremors inside boreholes and at the surface, as well as investigations to understand the amplification characteristics of earthquakes (transfer functions) through standalone measurements at the surface. Please feel free to contact us if you have any requests.