Papers - Seismic Methods - Seismic Refraction Methods as Applied to Shallow Overburdens (With Discussion)

The American Institute of Mining, Metallurgical, and Petroleum Engineers
F. L. Partlo Jerry H. Service
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
20
File Size:
856 KB
Publication Date:
Jan 1, 1934

Abstract

The following investigation was undertaken to develop a method for determining with reasonable accuracy the depth of overburdens of 100 ft. or less. Seismic methods seemed to offer good possibilities. The problem differed from that of the familiar salt-dome location in that the depth of overburden to be determined is much less than is encountered in oil prospecting. This means that a much shorter time interval must be measured with accuracy. Refraction methods seem at present to offer greater possibilities than reflection. The air sound persists for from 0.1 to 0.5 sec., because of echoes, and seismic reflections coming during this time are difficult to detect. A seismometer sensitive to vertical vibrations only offers possibilities and has been used here with some success. It is hoped that the application of this type of seismometer to reflection shooting in this region may be investigated still further. The apparatus used consisted of a carbon-button seismometer followed by a three-stage, transformer-coupled, vacuum-tube amplifier and a General Radio string oscillograph. Time marks are provided by a 1000-cycle, 600-r.p.m., synchronous motor provided with five spokes which intercept the light to the camera at 1/50 sec. intervals. This motor is driven by a two-stage vacuum-tube amplifier of 3 watt output, actuated by a tuning fork. The power supply for the seismometer amplifier is one 2-volt storage and one 45-volt B battery. The motor amplifier is powered by a 6-volt storage battery and 6 to 225-volt, 15-watt motor generator. The temperature-frequency characteristics of the tuning fork have been determined and for ordinary working temperatures the error in time that would be introduced is less than M millisecond for time intervals up to 100 milliseconds. The impact is produced by a sledge blow for surface distances less than 100 ft. and dynamite for greater distances. Two steel balls with wires attached form an electric circuit through a 1-ft. piece of railroad rail upon which they rest. When the rail is struck by the sledge the balls rebound, opening the circuit and indicating the time of impact by a break in the oscillograph record line as at A, Fig. 3. When dynamite
Citation

APA: F. L. Partlo Jerry H. Service  (1934)  Papers - Seismic Methods - Seismic Refraction Methods as Applied to Shallow Overburdens (With Discussion)

MLA: F. L. Partlo Jerry H. Service Papers - Seismic Methods - Seismic Refraction Methods as Applied to Shallow Overburdens (With Discussion). The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1934.

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