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Seismic Refraction

Seismic refraction maps contrasts in seismic velocity – the speed at which seismic energy travels through soil and rock. This parameter typically correlates well with rock hardness and density, which in turn tend to correlate with changes in lithology, degree of fracturing, water content, and weathering.

There are two basic approaches to seismic refraction data analysis: layer-cake and tomographic inversion. The former is the more traditional approach, although tomography has become more popular as faster computers have made it much more feasible than in the past.

Especially in the near-surface, it is not always the case that seismic velocities are divided into high-contrast, discrete layers. Nor is it the case that velocities are constant horizontally. Conventional layer-cake inversion techniques, such as the delay-time method, assume both, and require the geophysicist to provide layer assignments before the data inversion can be completed.

Tomography is less constrained in this sense; it does not “think” in terms of layers, and it better accommodates horizontal velocity variations. If discrete layering is not apparent in the raw data, the tomographic approach is generally more appropriate. As such, Geometrics’ SeisImager Refraction Analysis software offers both options.

Common applications

  • Estimating rippability prior to excavation
  • Mapping depth to bedrock/bedrock topography
  • Mapping depth to ground water
  • Calculation of elastic moduli/assessment of rock quality
  • Mapping thickness of landslides
  • Identification and mapping of faults

Considerations

  • The depth of penetration in a seismic refraction survey is approximately 1/5th of the
    length of the geophone spread, including offset shots. So if you need to see 10m deep,
    you will need room to lay out a (minimum) 50m seismic spread, as measured from
    offset shot to offset shot.
  • For most engineering refraction work, the best possible source is a 14 or 16lb
    sledgehammer. A downhole seisgun is not a good refraction source in general, except
    in cases where the surface is too soft to use a hammer effectively. An accelerated
    weight drop can be a good source, but is not portable and requires vehicle access to the
    shot points. Small explosives, such as Kinepak, are ideal when portability is required and
    the depth of interest is greater than what can be reached with a hammer.
  • Any Geometrics seismograph can be used for seismic refraction. For 24 channels or
    less, the SmartSeis ST is ideal. If using a laptop in the field works for you, the ES-3000 is a good alternative to the SmartSeis. For larger surveys, the Geode is recommended. For
    simple rippability, 12 channels will often suffice. For mapping bedrock topography, at
    least 24 channels are recommended. In general, the more detail required, the more
    channels you need.
  • A hammer-and-plate refraction survey is easily accomplished with two people. Longer
    lines and/or the use of explosives (which requires digging shot holes) generally require
    3-4 people.

Benefits/Limitations

  • Seismic refraction requires that velocities increase with depth. A lower velocity layer
    beneath a higher velocity layer will not be detected by seismic refraction, and will lead to
    errors in depth calculations. Fortunately, this is a fairly uncommon occurrence in the
    shallow subsurface.
  • The seismic source employed must match the desired depth of penetration. For hammer
    and plate work, the maximum depth you can expect to explore to is about 15-20m;
    however, this can vary significantly depending on geology, surface conditions, cultural noise,
    and the person swinging the hammer.
  • Refraction is a relatively broad-brush technique – it looks at gross velocity differences, and
    you should not expect to be able to map more than 3-4 individual velocity layers.
  • Cultural noise can be a problem – it is more difficult to conduct a seismic survey in an urban
    environment than in a rural one. Surveying along busy roadways should be avoided when
    possible. Shooting at night is sometimes necessary in order to achieve acceptable signal-to-noise ratio in busy areas.

Deliverables

  • The final product of a refraction survey is a velocity model, such as the layer-cake inversion shown below,
Layer-Cake Inversion Velocity Mode

Layer-Cake Inversion

or a tomographic inversion:

Tomographic Inversion

Tomographic Inversion

Best Tool

SmartSeis

Best Practices

  • Click here for a series of videos showing how to conduct a seismic refraction survey.

Further Reading

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