1887
ASEG2007 - 19th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

An experimental device for measuring the transverse isotropic (TI) elastic properties of sediments under uniaxial strain conditions has been developed. The utilizes matched sets of Pand S-wave ultrasonic transducers located along the sides of the sample and an ultrasonic P-wave phased array source with pinducer receiver on the ends of the sample. The phased array provides plane P-waves that are used to measure phase velocities over a range of angles. From these measurements, the five elastic constants for TI media can be recovered as the sediment is compacted, without the need for sample unloading or reorienting. Descriptions of the apparatus and data processing and an application to an unconsolidated sand sample are provided in this paper. P-wave anisotropy of 20% has been observed in dry sand under an axial stress of 5 MPa.

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/content/journals/10.1071/ASEG2007ab130
2007-12-01
2026-01-24
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References

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  8. Vega, S., Mavko, G., Nur, A., and Prasad, M., 2006, Detection of stress-induced velocity anisotropy in unconsolidated sands: The Leading Edge, 25 (3),252-256.
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/content/journals/10.1071/ASEG2007ab130
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  • Article Type: Research Article
Keyword(s): Anisotropy; multicomponent seismic.; unconsolidated sand
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