ความต้านทานไฟฟ้าและโพลาไรซ์เหนี่ยวนำ

พื้นที่ใช้งานสำหรับวิธีต้านทานไฟฟ้า

WHY DO I NEED AN ELECTRICAL RESISTVITY SYSTEM?

An electrical resistivity system can be an efficient tool to map the subsurface conditions, such as bedrock or groundwater level, when you need a non-destructive investigation technique and/or want improved data coverage compared to traditional, point-by-point, intrusive methods (such as drilling or digging). The range of models and accessories in the ABEM Terrameter LS 2 product range makes it suitable for many applications and budgets. The ABEM Terrameter LS 2 can also be used to measure the IP (induced polarization) effect as well as the SP (self-potential). Measurements can be straightforward soundings (just measuring resistivity against depth), 2D profiles (so called ERT, Electrical Resistvitiy Tomography) or even 3D volumes. Data can be collected on land, in water, or within boreholes and can be single “point in time” measurements or repeated readings to fulfil a need for monitoring changes in the subsurface.

The most common applications for electrical resistivity methods include investigations of groundwater aquifers and to map waste (landfill areas) and groundwater contaminants (including saltwater intrusion). Geological investigations for mapping soil and bedrock types or soil and bedrock changes are also common applications. Electrical resistivity measurements are widely used for investigating the depth to bedrock, bedrock topography and fracture and fault zone identification.

The electrical resistivity method also works efficiently for cavity detection and mapping as well as investigation of ores and mineral deposit. Read more about utilizing resistivity in mining here:

Mineral Exploration

Mining Operations

Post-mining Operations