1887
Volume 28, Issue 1-2
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

In order to evaluate naturally fractured reservoirs, it is critical to assess whether natural fracture sets believed to exist at depth (eg, from surface mapping and/or seismic data) are likely to be open and productive or closed and nonproductive. The semi-log relation between stress and the closure of natural fractures is combined with the effective normal stress acting on fractures to yield:

which relates fracture closure (8), the constants in the semilog fracture closure/stress relation (k and s), and maximum effective horizontal stress (o) magnitude with the effective horizontal stress ratio (n), and the angle between the normal to the fracture and the direction (0).

This relation shows that: (i) for a given fracture, the sensitivity of fracture closure to the anisotropy of the in situ stress field can be constrained by the effective horizontal stress ratio (n); (ii) natural fracture closure is sensitive to fracture orientation with respect to the in situ stress field where n is high; (iii) the sensitivity of natural fracture closure to its orientation with respect to the in situ stress field decreases markedly as n drops; and (iv) the rate of change of closure with changing orientation is relatively low at very low and very high misalignment angles, and much greater at intermediate angles.

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1997-03-01
2026-01-22
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References

  1. Bandis, S.C., Lumsden, A.C. and Barton, N R., 1983, Fundamentals of rock joint deformation: International Journal of Rock Mechanics and Mining Science and Geomechanical Abstracts 20, 249-268.
  2. Barton, N. Bandis, S. and Bakhtar, K., 1985, Strength, deformation and conductivity coupling of rock joints: International Journal of Rock Mechanics and Mining Science and Geomechanical Abstracts 22, 121-140.
  3. Brown, S.R. and Scholz, C.H., 1986, Closure of rock joints: Journal of Geophysical Research 91, 4939-4948.
  4. Bush, I. and Crampin, S., 1991, Paris Basin VSPs: case history establishing combinations of fine-layer (or lithologic) anisotropy and crack anisotropy from modelling shear wavefields near point singularities: Geophysical Journal International 107, 433-447.
  5. Cook, N.G.W., 1992, Natural joints in rock: mechanical, hydraulic and seismic behaviour and properties under normal stress: International Journal of Rock Mechanics and Mining Science and Geomechanical Abstracts 29, 198-223.
  6. Corbett, K., Friedman, M. and Spang, J., 1987, Fracture development and mechanical stratigraphy of Austin Chalk, Texas: American Association of Petroleum Geologists, Bulletin 71, 17-28.
  7. Comet, F.H. and Jones, R., 1994, Field evidences on the orientation of forced water flow with respect to the regional principal stress directions. In: Nelson and Laubach, eds, Rock mechanics, North American Rock Mechanics Symposium. Balkema, 61-69.
  8. Dyke, C.G., 1992, Stress insensitive natural fracture permeability within hydrocarbon reservoirs. In: Hudson, J.A., ed., Eurock ‘92, International Society of Rock Mechanics Symposium, London, 1992. Thomas Telford, London, 281-286.
  9. Hickman, S.H., Healy, J.H. and Zoback, M.D., 1985, In situ stress, natural fracture distribution, and borehole elongation in the Auburn geothermal well, Auburn, New York: Journal of Geophysical Research 90,5497-5512.
  10. Hillis, R R. and Williams, A.F., 1993, The contemporary stress field of the Barrow-Dampier Sub-Basin and its implications for horizontal drilling: Exploration Geophysics 24, 567-576.
  11. Horn, M.K., 1991, Play concepts for horizontal drilling. In: Fritz, R.D., Horn, M.K., and Joshi, S.D., eds, Geological aspects of horizontal drilling. American Association of Petroleum Geologists, Continuing Education Course Note Series 33, 189-323.
  12. Jaeger, J.C., 1969, Elasticity, fracture and flow with engineering and geological applications: Mefhuen and Company, London.
  13. Lefeuvre, F., Turpening, R., Caravana, C, Bom, A. and Nicoletis, L., 1993, Vertical open fractures and shear-wave velocities derived from VSPs, full waveform acoustic logs, and televiewer data: Geophysics 58, 818-834.
  14. Lorenz, J.C., Teufel, L.W. and Warpinski, N.R., 1991, Regional fractures I: a mechanism for the formation of regional fractures at depth in flat-lying reservoirs. American Association of Petroleum Geologists, Bulletin 75, 1714-1737.
  15. Martin, M.A. and Davis, T.L., 1987, Shear-wave birefringence: a new tool for evaluating fractured reservoirs: The Leading Edge 6, October, 22-28.
  16. McNaughton, D.A., 1991, Horizontal drilling vs. hydraulic fracturing: American Association of Petroleum Geologists, Explorer 12, January, 39.
  17. Queen, J.H. and Rizer, W.D., 1990, An integrated study of seismic anisotropy and the natural fracture system at the Conoco borehole test facility, Kay County, Oklahoma: Journal of Geophysical Research 95, 11255-11273.
  18. Swan, G., 1983, Determination of stiffness and other joint properties from roughness measurements: Rock Mechanics and Rock Engineering 16, 19-38.
  19. Teufel, L.W., 1991, Influence of lifhology and geologic structure on in situ stress: examples of stress heterogeneity in reservoirs. In: Lake, L.W., Carroll, H.B. and Wesson, T.C., eds. Reservoir charaterization II. Academic Press, San Diego, California, 565-578.
  20. Timoshenko, S.P. and Goodier, J.N., 1951, Theory of elasticity, 2nd Edition: McGraw-Hill, New York.
  21. Winterstein, D.F. and Meadows, M.A., 1991, Shear-wave polarizations and subsurface stress directions at Lost Hills field: Geophysics 56, 1331-1348.
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  • Article Type: Research Article
Keyword(s): fracture stiffness; in situ stress; open natural fractures

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