Shaker tests on downhole seismic tools
Shaking a downhole seismic tool in situ is a powerful test procedure able to detect abnormal acoustical behavior. It consists of feeding a swept voltage to a special geophone located inside the tool, close to the triaxial measurement geophones. The special geophone creates a swept force, which excites the tool‐formation system. The resulting motion of the tool is recorded through the triaxial geophones. In this paper, a simple model of the tool‐formation system excited by the shaker is given. Predictions from this model compare nicely with results from a field experiment conducted with a very compact seismic tool. Another field experiment, conducted with a longer tool, shows that tool intrinsic modes are clearly visible in the shaker data. Their frequencies and amplitudes depend upon the geometry of the contact between the tool and the formation. A comparison between shaker data and impulsive shot data shows that moderate modal vibrations do not significantly deteriorate the quality of VSP data, but that large modal vibrations, when present, are visible on the shot data and also correspond to an increased sensitivity to tube waves. Recording one shaker trace at each depth allows routine well‐site quality control of VSP data. Such quality control is especially important for the horizontal axes of a tool and in an open hole, where coupling conditions are not easily controlled.