1887
image of Measurement of the normal/tangential fracture compliance ratio (ZN/ZT) during hydraulic fracture stimulation using S‐wave splitting data

Abstract

ABSTRACT

We develop a method to invert S‐wave splitting (SWS) observations, measured on microseismic event data, for the ratio of normal to tangential compliance (/) of sets of aligned fractures. We demonstrate this method by inverting for / using SWS measurements made during hydraulic fracture stimulation of the Cotton Valley tight gas reservoir, Texas. When the full SWS data set is inverted, we find that /= 0.74 ± 0.04. Windowing the data by time, we were able to observe variations in / as the fracture stimulation progresses. Most notably, we observe an increase in / contemporaneous with proppant injection. Rock physics models and laboratory observations have shown that / can be sensitive to (1) the stiffness of the fluid filling the fracture, (2) the extent to which this fluid can flow in and out of the fracture during the passage of a seismic wave and (3) the internal architecture of the fracture, including the roughness of the fracture surfaces, the number and size of any asperities and the presence of material filling the fracture. These factors have direct implications for modelling the fluid‐flow properties of fractures. Consequently, the ability to image / using SWS will provide useful information about fractured rocks and allow additional constraints to be placed on reservoir behaviour.

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/content/journals/10.1111/j.1365-2478.2012.01132.x
2013-02-28
2024-04-19
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References

  1. AngusD.A., VerdonJ.P., FisherQ.J. and KendallJ.‐M.2009. Exploring trends in microcrack properties of sedimentary rocks: An audit of dry core velocity‐stress measurements. Geophysics 74, E193–E203.
    [Google Scholar]
  2. BackusG.E.1962. Long‐wave elastic anisotropy produced by horizontal layering. Journal of Geophysical Research 67, 4427–4440.
    [Google Scholar]
  3. BartonN.2007. Rock quality, seismic velocity, attenuation and anisotropy . Taylor and Francis.
    [Google Scholar]
  4. BatzleM.L., SimmonsG. and SiegfriedR.W.1980. Microcrack closure in rocks under stress: Direct observation. Journal of Geophysical Research 85, 7072–7090.
    [Google Scholar]
  5. ChapmanM.2003. Frequency‐dependent anisotropy due to meso‐scale fractures in the presence of equant porosity. Geophysical Prospecting 51, 369–379.
    [Google Scholar]
  6. CrampinS., VoltiT. and StefánssonR.1999. A successfully stress‐forecast earthquake. Geophysical Journal International 138, F1–F5.
    [Google Scholar]
  7. EisnerL., Williams‐StroudS., HillA., DuncanP. and ThorntonM.2010. Beyond the dots in the box: Microseismicity‐constrained fracture models for reservoir simulation. The Leading Edge 29, 326–333.
    [Google Scholar]
  8. HallS.A. and KendallJ.‐M.2000. Constraining the interpretation of AVOA for fracture characterisation. in Anisotropy 2000: Fractures, Converted Waves, and Case Studies. Society of Exploration Geophysics 107–144.
    [Google Scholar]
  9. HallS.A., KendallJ.‐M., MaddockJ. and FisherQ.2008. Crack density tensor inversion for analysis of changes in rock frame architecture. Geophysical Journal International 173, 577–592.
    [Google Scholar]
  10. HanD.‐H., NurA. and MorganD.1986. Effects of porosity and clay content on wave velocities in sandstones. Geophysics 51, 2093–2107.
    [Google Scholar]
  11. HerwangerJ.V., WorthingtonM.H., LubbeR., BinleyA. and KhazanehdariJ.2004. A comparison of crosshole electrical and seismic data in fractured rock. Geophysical Prospecting 52, 109–121.
    [Google Scholar]
  12. HobdayC. and WorthingtonM.H.2012. Field measurements of normal and shear fracture compliance. Geophysical Prospecting 60, 488–499.
    [Google Scholar]
  13. HornbyB.E.1994. The elastic properties of shales . PhD thesis. Cambridge University.
  14. HsuC.‐J. and SchoenbergM.1993. Elastic waves through a simulated fractured medium. Geophysics 58, 964–977.
    [Google Scholar]
  15. HudsonJ.A.1981. Wave speeds and attenuation of elastic waves in material containing cracks. Geophysical Journal of the Royal Astronomical Society 64, 133–150.
    [Google Scholar]
  16. HudsonJ.A., LiuE. and CrampinS.1996a. The mechanical properties of materials with interconnected cracks and pores. Geophysical Journal International 124, 105–112.
    [Google Scholar]
  17. HudsonJ.A., LiuE. and CrampinS.1996b. Transmission properties of a fault plane. Geophysical Journal International 125, 559–566.
    [Google Scholar]
  18. HudsonJ.A., LiuE.andCrampinS.1997. The mean transmission properties of a fault with imperfect facial contact. Geophysical Journal International 129, 720–726.
    [Google Scholar]
  19. HudsonJ.A., PointerT. and LiuE.2001. Effective medium theories for fluid saturated materials with aligned cracks. Geophysical Prospecting 49, 509–522.
    [Google Scholar]
  20. JacobyH.D., O’SullivanF.M. and PaltsevS.2012. The influence of shale gas on U.S. energy and environmental policy. Economics of Energy and Environmental Policy 1, 37–51.
    [Google Scholar]
  21. JohnstonJ.E. and ChristensenN.I.1993. Compressional to shear velocity ratios in sedimentary rocks. International Journal of Rock Mechanics and Mining Science 30, 751–754.
    [Google Scholar]
  22. LaubachS.E.1988. Subsurface fractures and their relationship to stress history in East Texas basin sandstone. Tectonophysics 156, 37–49.
    [Google Scholar]
  23. LaubachS.E. and MonsonE.R.1988. Coring‐induced fractures: Indicators of hydraulic fracture propagation in a naturally fractured reservoir. (SPE 18164).
  24. LubbeR., SothcottJ., WorthingtonM.H. and McCannC.2008. Laboratory estimates of normal and shear fracture compliance. Geophysical Prospecting 56, 239–247.
    [Google Scholar]
  25. MacBethC. and SchuettH.2007. The stress dependent elastic properties of thermally induced microfractures in aeolian Rotliegend Sandstone. Geophysical Prospecting 55, 323–332.
    [Google Scholar]
  26. MaxwellS.C.2010. Microseismic: Growth born from success. The Leading Edge 29, 338–343.
    [Google Scholar]
  27. Nolen‐HoeksemaR.C. and RuffL.J.2001. Moment tensor inversion of microseisms from the B‐sand propped hydrofracture, M‐site, Colorado. Tectonophysics 336, 163–181.
    [Google Scholar]
  28. PointerT., LiuE. and HudsonJ.A.2000. Seismic wave propagation in cracked porous media. Geophysical Journal International 142, 199–231.
    [Google Scholar]
  29. Pyrak‐NolteL.J., MyerL.R. and CookN.G.W.1990. Transmission of seismic waves across single natural fractures. Journal of Geophysical Research 95, 8617–8638.
    [Google Scholar]
  30. RathoreJ.S., FjaerE., HoltR.M. and RenlieL.1994. P‐ and S‐wave anisotropy of a synthetic sandstone with controlled crack geometry. Geophysical Prospecting 43, 711–728.
    [Google Scholar]
  31. RutledgeJ.T. and PhillipsW.S.2003. Hydraulic stimulation of natural fractures as revealed by induced microearthquakes, Carthage Cotton Valley gas field, East Texas. Geophysics 68, 441–452.
    [Google Scholar]
  32. RutledgeJ.T., PhillipsW.S. and MayerhoferM.J.2004. Faulting induced by forced fluid injection and fluid flow forced by faulting: An interpretation of hydraulic fracture microseismicity, Carthage Cotton Valley Gas Field, Texas. Bulletin of the Seismological Society of America 94, 1817–1830.
    [Google Scholar]
  33. SambridgeM.1999a. Geophysical inversion with a neighbourhood algorithm I. Searching a parameter space. Geophysical Journal International 138, 479–494.
    [Google Scholar]
  34. SambridgeM.1999b. Geophysical inversion with a neighbourhood algorithm II. Appraising the ensemble. Geophysical Journal International 138, 727–746.
    [Google Scholar]
  35. SayersC.M.1999. Stress‐dependent seismic anisotropy of shales. Geophysics 64, 93–98.
    [Google Scholar]
  36. SayersC.M. and den BoerL.D.2012. Characterizing production‐induced anisotropy of fractured reservoirs having multiple fracture sets. Geophysical Prospecting ??, ??–??
    [Google Scholar]
  37. SayersC.M. and HanD.‐H.2002. The effect of pore fluid on the stress‐dependent elastic wave velocities in sandstones. SEG Expanded Abstracts 21, 1842–1845.
    [Google Scholar]
  38. SayersC.M. and KachanovM.1995. Microcrack induced elastic wave anisotropy of brittle rocks. Journal of Geophysical Research 100, 4149–4156.
    [Google Scholar]
  39. SayersC.M., TaleghaniA.D. and AdachiJ.2009. The effect of mineralization on the ratio of normal to tangential compliance of fractures. Geophysical Prospecting 57, 439–446.
    [Google Scholar]
  40. SchoenbergM. and SayersC.M.1995. Seismic anisotropy of fractured rock. Geophysics 60, 204–211.
    [Google Scholar]
  41. TeanbyN.A., KendallJ.‐M. and van der BaanM.2004. Automation of shear‐wave splitting measurements using cluster analysis. Bulletin of the Seismological Society of America 94, 453–463.
    [Google Scholar]
  42. ThomsenL.1986. Weak elastic anisotropy. Geophysics 51, 1954–1966.
    [Google Scholar]
  43. UrbancicT.I. and RutledgeJ.2000. Using microseismicity to map Cotton Valley hydraulic fractures. SEG Expanded Abstracts 19, 1444–1448.
    [Google Scholar]
  44. ValckeS.L.A., CaseyM., LloydG.E., KendallJ.‐M. and FisherQ. J.2006. Lattice preferred orientation and seismic anisotropy in sedimentary rocks. Geophysical Journal International 166, 652–666.
    [Google Scholar]
  45. VerdonJ.P., AngusD.A., KendallJ.‐M. and HallS.A.2008. The effects of microstructure and nonlinear stress on anisotropic seismic velocities. Geophysics 73, D41–D51.
    [Google Scholar]
  46. VerdonJ.P. and KendallJ.‐M.2011. Detection of multiple fracture sets using observations of shear‐wave splitting in microseismic data. Geophysical Prospecting 59, 593–608.
    [Google Scholar]
  47. VerdonJ.P., KendallJ.‐M. and WüstefeldA.2009. Imaging fractures and sedimentary fabrics using shear wave splitting measurements made on passive seismic data. Geophysical Journal International 179, 1245–1254.
    [Google Scholar]
  48. VernikL.1993. Microcrack‐induced versus intrinsic elastic anisotropy in mature HC‐source rocks. Geophysics 58, 1703–1706.
    [Google Scholar]
  49. VlastosS., LiuE., MainI.G., SchoenbergM., NarteauC., LiX.‐Y. and MaillotB.2006. Dual simulations of fluid flow and seismic wave propagation in a fractured network: Effects of pore pressure on seismic signature. Geophysical Journal International 166, 825–838.
    [Google Scholar]
  50. WalkerR.N.1997. Cotton Valley hydraulic fracture imaging project. (SPE 38577).
  51. WesselsS.A., De LaPeña A., KratzM., Williams‐StroudS. and JbeiliT.2011. Identifying faults and fractures in unconventional reservoirs through microseismic monitoring. First Break 29, 99–104.
    [Google Scholar]
  52. WookeyJ.2012. Direct probabilistic inversion of shear‐wave data for anisotropy. Geophysical Journal International 189, 1025–1037.
    [Google Scholar]
  53. WorthingtonM.2007. The compliance of macrofractures. The Leading Edge 26, 1118–1122.
    [Google Scholar]
  54. WorthingtonM.H. and LubbeR.2007. The scaling of fracture compliance, in Fractured Reservoirs. Geological Society of London Special Publication 73–82.
    [Google Scholar]
  55. WüstefeldA., Al HarrasiO., VerdonJ.P., WookeyJ. and KendallJ.‐M.2010. A strategy for automated analysis of passive microseismic data to image seismic anisotropy and fracture characteristics. Geophysical Prospecting 58, 755–773.
    [Google Scholar]
  56. WüstefeldA., KendallJ.‐M., VerdonJ.P. and van AsA.2011a. In‐situ monitoring of rock fracturing using shear‐wave splitting analysis: An example for a mining setting. Geophysical Journal International 187, 848–860.
    [Google Scholar]
  57. WüstefeldA., VerdonJ., KendallJ.‐M., RutledgeJ., ClarkeH. and WookeyJ.2011b. Inferring rock fracture evolution during reservoir stimulation from seismic anisotropy. Geophysics 76, WC157–WC166.
    [Google Scholar]
  58. YoshiokaN. and ScholzC.H.1989a. Elastic properties of contacting surfaces under normal and shear loads: 1. Theory. Journal of Geophysical Research 94, 17681–17690.
    [Google Scholar]
  59. YoshiokaN. and ScholzC.H.1989b. Elastic properties of contacting surfaces under normal and shear loads: 2. Comparison of theory with experiment. Journal of Geophysical Research 94, 17691–17700.
    [Google Scholar]
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  • Article Type: Research Article
Keywords: S‐wave splitting ; Microseismic ; Fracture
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