Construction methods · Site investigation and testing

Geophysical surveys

Non-intrusive surveys that fill the gaps between boreholes: rock head profile, buried channels, cavities and soft pockets. They do not replace boreholes but they say where to put them.

Also called: seismic refraction, electrical resistivity, MASW, marine sub-bottom profiling

How it is done

  1. On land, run seismic refraction or MASW lines along the alignment to map rock head and stiffness; electrical resistivity tomography for cavities and moisture.
  2. On water, tow a sub-bottom profiler and side-scan sonar to map sediment thickness, buried channels and debris.
  3. Calibrate the sections against boreholes, then extend the ground model between them.

Where it fits

  • Long alignments, karst, buried channels, marine sites before the drilling campaign.
  • Sites where access for rigs is limited.

Where it does not

  • Using geophysics as the only evidence for a foundation level.

Plant, pace and money

PlantGeophones and a seismic source, resistivity cables, survey boat with profiler.
ProductivityKilometres per day on land; several line-kilometres per day at sea.
CostLow per metre; a few percent of the investigation budget.

Risks and controls

What goes wrong

  • Ambiguous inversions; a thin hard layer over soft can hide the soft.

Quality assurance

Calibration boreholes at line intersections; interpretation reported with confidence levels.

Examples

Sub-bottom profiling is routine before marine bridge investigations in the Gulf and Southeast Asia.

Related methods

Further reading

ASTM D5777 (seismic refraction) · ASTM D6431 (resistivity)