1887

Abstract

Summary

During the exploration and development of shale gas, one of the most important factors that affect hydraulic fracture propagation is the brittleness of shale. Shale brittleness is affected by many factors, including water content,mineralogy compositions,temperature and so on. In this study, Ultrasonic measurements were performed to investigate the effect of water saturation on brittleness of a set of synthetic shale samples. In order to reduce the number of unknown factors caused by multiple minerals, we made 6 samples each with a different diagenetic pressure: 25MPa, 50MPa, 75MPa, 100MPa, 125MPa, 150MPa, named A1–A6. The results show that synthetic shale with larger diagenetic pressure shows higher Young’s modulus, lower Poisson’s ratio and higher brittleness. In the water saturation case, Young’s modulus decreases slightly compared to that of dry samples, but Poisson’s ration increases significantly. Poisson’s ratio is more sensitive to water compared with Young’s modulus. Water saturation leads to brittleness of samples significant reduction. The effect of water saturation on elastic properties of synthetic shale varies with directions, and the difference is related to the diagenetic pressure.

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/content/papers/10.3997/2214-4609.201601137
2016-05-30
2024-04-18
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References

  1. Banik, N.
    [2012] Effects of VTI anisotropy on shale reservoir characterization. Middle East Unconventional Gas Conference and Exhibition, Society of Petroleum Engineers, SPE 150269.
    [Google Scholar]
  2. Cheadle, S.P., Brown, R.J. and Lawton, D.C.
    [1991] Orthorhombic anisotropy — A physical seismic modeling study. Geophysics, 56, 1603–1613.
    [Google Scholar]
  3. Guo, Z.
    [2013] A shale rock physics model for analysis of brittleness index, mineralogy and porosity in the Barnett Shale. Journal of Geophysics and Engineering, 10(2), 025006.
    [Google Scholar]
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