In order to extend the study and use of the elastic properties of geological bodies to include effects involving the amplitude and frequency of elastic radiation, a new source of energy is needed
A large moving-coil transducer is described which, when attached rigidly to the rock, radiates sinusoidal vibrations of controllable amplitude, frequency and duration. The operation of the vibrator is analysed in detail by the method of electromechanical analogy.
For experiments in a chalk-mine, energy at each of the frequencies 300, 600 and 1,000 c/s. was radiated in the form of a square-enveloped pulse, of 20 msec duration. Vibrations were detected in the rock by means of a piezoelectric microphone, amplifiers and an oscillograph, with an overall magnification of about 109. Oscillograms show the complex disturbances produced by the arrival of direct and reflected energy, at distances out to the limit of the mine at 450 ft. Measurements of amplitude at 130 ft. are used to examine the mechanism of the transfer of energy from the vibrator to the rock.
The power radiated was about 0.05 watt at 600 c/s., of which about one-sixth was in the compressional mode and five-sixths in the shear mode, but this power may readily be increased.