Schlumberger

Technical Paper: Acoustic Characterization Of An Extremely Slow Formation In California

Society: SPWLA
Paper Number:
Presentation Date: 2005
 

Abstract

Slow formations are defined as those formations where the shear velocity is slower than the borehole fluid velocity. In order to measure shear velocities in such formations, sonic tools incorporating dipole transmitters were developed. Since their introduction more than a decade ago, dipole sonic logging tools have provided a wealth of information about the acoustic properties of slow formations, including the detection of anisotropy and inhomogeneity. The latter mechanism manifests itself as radial variations in compressional and shear slownesses, which is now possible to quantify.

The Cymric field is located in the San Joaquin valley near Bakersfield, California. One of the producing zones, the Opal A diatomite, is an extremely slow formation with compressional slownesses approaching 200 μs/ft and shear slownesses approaching 800 μs/ft. In this paper, we examine the results from a wideband crossed dipole sonic tool that was recorded in a well drilled in the Cymric field. The tool is specifically designed for 3D acoustic characterization of formations. This is achieved through a formation typing scheme that classifies formations into one of four categories: A) isotropic homogeneous, B) isotropic inhomogeneous, C) anisotropic homogeneous, and D) anisotropic inhomogeneous. Slowness frequency dispersion analysis is used in the classification scheme as each of these categories has a unique signature when dispersion analysis is employed.

When inhomogeneity is present, a new technique known as dipole radial profiling, can be applied to measure the radial variation of shear slowness away from the borehole. This can be used to determine the extent of possible formation damage, alteration, or filtrate invasion and to provide a measure of the far field shear slowness.

These techniques are applied to acoustically characterize the Opal A diatomite formation.

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