Hayles Geoscience Surveys Ltd.

511 Robinson Avenue,
Selkirk, Manitoba,
Canada R1A 1E5
phone/fax: (204) 482 5249
toll free: (888) 297 0614
email: jgh@haylesgeoscience.ca

Home

Surface Surveys

Borehole Surveys

Surface to
Borehole Seismic

Airborne Geophysics

Grid Design and Data Plotting Services

Guidelines







Surface Surveys P- & S-wave Refraction Seismic Near-Surface Seismic Sources



Near-Surface Seismic Sources

Hammers directed vertically on the earth surface are the most common energy sources.  Normally the hammer striking a steel plate that has been firmly connected to the earth is used.  The photographs below show various sources.


Figure 1. Photographs of a hammer seismic source.  The instant of impact is sensed by a sensitive switch.

Figure 1.   Photographs of a hammer seismic source.  The instant of impact is sensed by a sensitive switch.


Figure 2. Two photographs are shown above of an accelerated weight drop source mounted on the back of a truck.  This system accelerates a 45 kg mass against a base plate that has been firmly connected to the earth.  Repetition rates of 5 strikes per minute permit signal averaging and rapid coverage.

Figure 2.   Two photographs are shown above of an accelerated weight drop source mounted on the back of a truck.  This system accelerates a 45 kg mass against a base plate that has been firmly connected to the earth.  Repetition rates of 5 strikes per minute permit signal averaging and rapid coverage.


Figure 3.  A 'Buffalo Gun' permits the use of shotgun shells as an energy source.  Two photographs of this source are shown above. This is a particularly good energy source for near-surface surveys, but needs careful procedures for safe use.

Figure 3.   A 'Buffalo Gun' permits the use of shotgun shells as an energy source.  Two photographs of this source are shown above. This is a particularly good energy source for near-surface surveys, but needs careful procedures for safe use.


Figure 4.  Shear-wave sources are very useful for near-surface reflection and engineering studies.  Estimates of the dynamic moduli (Poisson's Ratio, Shear, Young's and Bulk) can be obtained from the ratio of s-wave to p-wave velocity and a knowledge of the bulk density of the materials.

Figure 4.   Shear-wave sources are very useful for near-surface reflection and engineering studies.  Estimates of the dynamic moduli (Poisson's Ratio, Shear, Young's and Bulk) can be obtained from the ratio of s-wave to p-wave velocity and a knowledge of the bulk density of the materials.