S05 · Hydrogeology

Groundwater
Exploration.

Integrated airborne EM, magnetic, and gravity workflows to delineate aquifer boundaries, characterise hydrogeological structures, and identify optimal drilling targets across the Kingdom's arid terrain. Targeted reduction of dry-well risk.

Aquifer mappingDrill targetingTDEM / FDEMSalinity / TDS
Survey Snapshot
Methods
Airborne EM + Mag + Gravity
Depth of investigation
0–400 m
Resolution
1–5 Ω·m sensitivity
Coverage
~50 km²/day
Output
Drill-site recommendation report
Overview

Sub-surface water targeting at scale.

Saudi Arabia's hydrogeology is dominated by deep sandstone aquifers and structurally-controlled alluvial systems. Identifying productive zones at borehole scale requires more than satellite remote sensing or surface geology — it requires direct measurement of sub-surface conductivity.

Our airborne EM systems image conductivity to 400 m depth at survey speed, resolving the contrast between freshwater aquifers (high resistivity) and brackish/saline zones (high conductivity). Magnetic and gravity data add structural context — fault networks that control aquifer recharge and connectivity.

The deliverable is not a map — it is a ranked list of drill-site recommendations, each with its supporting geophysical evidence, predicted water quality, and confidence band on the productive horizon.

Sample Output · Processed Data Product
3D airborne EM conductivity-depth model resolving an aquifer
AEM · Conductivity Volume

3D conductivity model

Stitched conductivity curtains beneath flight lines, isolating a productive freshwater aquifer between resistive basement and conductive overburden.

Desert wadi where aquifer recharge concentrates
Wadi · Recharge zone

Structural recharge corridor

Processing Stack

1D laterally-constrained inversion → 3D blocky model build → fault-corrected interpretation → drill-target ranking → water-chemistry prediction (TDS proxy).

Methodology · 4 Phases

From conductivity map to productive borehole.

Phase 0101

Hydrogeological Briefing

Review existing wells, lithology, regional structure. Define target depth, expected water type, and drill-site constraints with client hydrogeologist.

Phase 0202

Airborne EM Acquisition

Time-domain or frequency-domain EM flown over target area with co-acquired magnetic and gravity gradient data.

Phase 0303

Inversion & Modelling

1D LCI followed by 3D blocky inversion. Conductivity model integrated with magnetic lineaments to identify fault-controlled aquifers.

Phase 0404

Drill-Site Report

Ranked drill targets with predicted depth-to-water, aquifer thickness, salinity proxy, and structural rationale. Delivered to client drilling team.

Deliverables

What you receive.

D01

3D conductivity model

Blocky 3D conductivity volume to depth-of-investigation. Voxel + GeoTIFF.

D02

Conductivity-depth sections

2D vertical sections along survey lines + interpreted cross-sections.

D03

Aquifer thickness map

Interpreted productive-horizon thickness with confidence bands.

D04

Salinity proxy map

Conductivity-derived TDS estimate with calibration against existing wells.

D05

Ranked drill targets

Priority-ranked sites with coordinates, predicted depth, and rationale.

D06

Hydrogeological report

PDF report tying geophysics to regional hydrogeology + chain of custody.

Target your aquifer.

Share your AOI, target depth, and existing well data. We respond with a survey design, drill-target framework, and timeline within 48 hours.