DocumentCode :
2688404
Title :
Hydraulic fracture induced changes in borehole modal dispersions
Author :
Ting Lei ; Sinha, Bikash K.
Author_Institution :
Schlumberger-Doll Res. Center, Cambridge, MA, USA
fYear :
2012
fDate :
7-10 Oct. 2012
Firstpage :
174
Lastpage :
177
Abstract :
Three dimensional finite-difference codes with a perfectly matched layer (PML) at the computational boundary enable us to study the influence of planar fractures on refracted headwaves as well as dispersive borehole modes. This paper describes borehole dispersions in the presence of different fracture geometries intersecting a fluid-filled borehole. Sonic signatures consist of compressional, fast-shear, and slow-shear slownesses obtained from the processing of an array of waveforms by the slowness-time coherence (STC) algorithm together with the axisymmetric Stoneley and dipole flexural dispersions obtained from the processing of monopole and dipole waveforms recorded at an array of hydrophone receivers placed in a fluid-filled borehole. Characteristic differences in the dispersion signatures and evidence of dipole shear-slowness anisotropy are indicators of the orientation and radial extent of fractures introduced by the hydraulic fracturing treatment. Long axial fractures of width 5 mm exhibits slower dispersisons in the intermediate frequency band with the flexural polarization parallel to the fracture plane and slower dispersions at low frequencies with the flexural polarization perpendicular to the fracture plane. Cross-dipole shear-slowness differences are signatures associated with axial fractures. In contrast, fractures parallel to the borehole cross-sectional plane produce a characteristic drop in the Stoneley slowness dispersion and an increase in the dipole flexural dispersion at low frequencies. Reflections from cross-sectional fractures are observed on both the Stoneley and flexural waveforms. Interestingly, higher order Stoneley and flexural modes are not observed in the presence of such reflections. In conclusion, we have identified clear differences between the Stoneley and dipole flexural dispersions before and after the fracturing operation. These characteristic differences can help in identifying the presence of open fractures that contribute to - he flow of hydrocarbons into the producing well.
Keywords :
acoustic dispersion; acoustic signal processing; finite difference methods; hydrophones; mechanical engineering computing; modal analysis; natural gas technology; oil technology; surface acoustic waves; waveform analysis; STC algorithm; Stoneley modes; Stoneley slowness dispersion; Stoneley waveforms; axial fractures; axisymmetric Stoneley dispersion; borehole cross-sectional plane; borehole modal dispersion; compressional slowness; computational boundary; cross-dipole shear-slowness; cross-sectional fractures; dipole flexural dispersion; dipole shear-slowness anisotropy; dipole waveforms; dispersion signatures; fast-shear slowness; flexural modes; flexural polarization; flexural waveforms; fluid-filled borehole; fracture geometries; fracture plane; hydraulic fracture induced changes; hydraulic fracturing treatment; hydrophone receiver array; monopole waveforms; perfectly matched layer; size 5 mm; slow-shear slowness; slowness-time coherence algorithm; sonic signatures; three dimensional finite difference code; waveform array processing; Acoustics; Anisotropic magnetoresistance; Arrays; Geophysics; Receivers; Solids; Stress; Borehole sonic technology; borehole dispersions; borehole waves; elastic wave propagation; fracture-induced anisotropy; fracture-induced nearwellbore alteration;
fLanguage :
English
Publisher :
ieee
Conference_Titel :
Ultrasonics Symposium (IUS), 2012 IEEE International
Conference_Location :
Dresden
ISSN :
1948-5719
Print_ISBN :
978-1-4673-4561-3
Type :
conf
DOI :
10.1109/ULTSYM.2012.0043
Filename :
6562049
Link To Document :
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