In conjunction with Baker Atlas Inc. Michigan Technological University devised a system capable of recording the earth motion and pressure due to downhole and surface seismic sources. The essential elements of the system are 1) a borehole test site that will remain constant and is available all the time and for any length of time, 2) a downhole sonde that will itself remain constant and, because of its downhole digitization feature, does not require the wireline or surface recording components to remain constant, and 3) a set of procedures that ensures that the amplitude and frequency parameters of a wide range of sources can be compared with confidence.This system was used to record four seismic sources, three downhole sources and one surface source. A single activation of each of the downhole sources was not seen on time traces above the ambient noise, however, one sweep of the surface source, a small vertical vibrator, was easily seen in a time trace. One of the downhole sources was seen by means of a spike in its spectrum and a second downhole source was clearly seen after correlation and stacking. The surface vibrator produced a peak to peak particle motion signal of approximately 4.5 X 10 -5 cm/sec and a peak to peak pressure of approx. 2.5 X 10 -7 microPascals at a depth of 1,485 ft.
Calibration and Testing of Sonic Stimulation Technologies Final Report DE-FC26-01BC15165 March 2005 Michigan Technological University 3
Calibration and Testing of Sonic Stimulation TechnologiesFinal Report:
Executive SummaryThe track record of the sonic stimulation of oil reservoirs is, at best, irregular and uncertain. Theoretical work, some of it performed on this contract, gives us a glimpse of why that performance is so variable, namely it will work well only under a very narrow range of conditions, which rarely occur, although it will work weakly under a range of conditions, given a strong enough source.One of the many parameters needed in any performance analysis is the strength and frequency band of the seismic source being used to do the stimulation. Under this contract, we have begun a catalog of such sources by organizing the elements needed for rigorous testing and conducting four tests under identical conditions.In conjunction with Baker Atlas Inc. Michigan Technological University devised a system capable of recording the earth motion and pressure due to downhole and surface seismic sources. The essential elements of the system are 1) a borehole test site that will remain constant and is available all the time and for any length of time, 2) a downhole sonde that will itself remain constant and, because of its downhole digitization feature, does not require the wireline or surface recording components to remain constant, and 3) a set of procedures that ensures that the amplitude and frequency parameters of a wide range of sources can be compared with confidence.Because sonic stimulation is the underlying interest in this study, we focused on the signal strength of a single activation of sources, recording...