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Groundwater Mapping

Understanding groundwater mapping

Groundwater mapping is the process of using geophysical methods to locate and study underground water systems. This includes identifying:
  • Aquifers: Subsurface layers that store and transmit water.
  • Water-bearing formations: Rock or soil layers that hold groundwater.
  • Flow pathways: Routes that groundwater takes below the surface.
This process involves:
  • Measuring variations in ground properties like resistivity, which change with water presence and saturation.
  • Using advanced tools like tTEM to create high-resolution subsurface maps, enabling the identification of potential groundwater aquifers.
With tools like tTEM, groundwater mapping and MAR projects become more efficient and effective, ensuring sustainable water management.

TEM's role in groundwater maping

See how our instruments enhance precision and efficiency in exploring raw material deposits
Shallow Groundwater Exploration

tTEM is designed to detect shallow groundwater and aquifers, identifying water-saturated zones and distinguishing them from dry areas.

Non-Invasive & Fast

Unlike drilling, tTEM is non-invasive and covers large areas quickly, making it a cost-effective and efficient tool for initial groundwater mapping.

High Resolution Mapping

It creates detailed maps of groundwater features like fractures, porous zones, and aquifers, essential for exploration and management.

Adaptive to various Terrain

tTEM can be used across many terrains, from flat land to rugged areas, with minimal environmental impact.

Principle of Operation

sTEM uses time-domain electromagnetic (TEM) signals, sending out a current pulse and measuring how long it takes for the signal to return after interacting with subsurface materials. The resistivity varies based on water content—water-rich zones have lower resistivity, helping identify aquifers and water-bearing fractures.

Deep Penetration

sTEM provides deep subsurface penetration, ideal for investigating groundwater systems or aquifers located hundreds of meters below the surface.

Targeting Deep Aquifers & Water Zones

Stationary sTEM surveys allow for detailed analysis of specific groundwater layers and deep aquifers, where tTEM may be less effective.

Realtime Data Collection

Data is processed in real time, mapping the resistivity profile of the subsurface and identifying groundwater boundaries, flow characteristics, and water quality. This is useful for assessing resources, planning well installation, or detecting saltwater intrusion.

Precision and efficiency in exploring raw material deposits