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Hydrologic Characterization of Fractured Rocks for DFN Models

Hydrologic Characterization of Fractured Rocks for DFN Models. Useful Definitions and Concepts. Transmissivity -- Properties of a conductor (aquifer, reservoir, single fracture, fracture zone) ( L 2 /T ) Permeability, Hydraulic Conductivity -- Property of material inside conductor ( L/T ).

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Hydrologic Characterization of Fractured Rocks for DFN Models

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  1. Hydrologic Characterization of Fractured Rocks for DFN Models

  2. Useful Definitions and Concepts • Transmissivity -- Properties of a conductor (aquifer, reservoir, single fracture, fracture zone) (L2/T) • Permeability, Hydraulic Conductivity -- Property of material inside conductor (L/T)

  3. Definitions, continued • Storativity -- Storage of a conductor or conducting feature (dimensionless) • Specific Storage -- Property of material in a conductor (1/L) • Hydraulic Diffusivity -- Ratio of T/S (L2/T) • Controls speed of propagation of pressure effect of a disturbance • Very (!!!) important for scaling results

  4. Overview • Useful Concepts • Steady Flow Methods • Packer Tests • Flow Logs • Transient Flow Methods • Boundary effects • Dimension effects

  5. Steady Flow Methods • Packer Testing • Falling Head Test • Constant Pressure/Lugeon Test • Flow Logging • Heat pulse • Spinner • Hydrophysical

  6. Steady Radial Flow rw • Pressure and flow constant • Only exists with constant pressure boundary • Generally under-estimates due to skin R

  7. Packer Test (Fixed Interval Length) • Used in Civil Engineering • Testing at fixed interval lengths • Some zones have no fractures; some zones have multiple fractures • Efficient testing has some no flows but not too many

  8. Pn - # of no flows/# of tests L - length of test zone

  9. Oxfilet (Osnes Extraction of Fixed Interval Length Evaluation of Transmissivity) • Guess T and P10 of Fractures • Oxfiet generated fracture along hole • Oxfilet calculates packer test transmissivities • Oxfilet compares measured and simulated pacer test transmissivities

  10. Oxfilet Interface Fracture Network Stats Data and Simulated PDF’s Packer Test Stats Data and Simulated CDF’s

  11. Oxfilet Challenges • Results non-unique but constrained (range of combinations of distributions of T and frequency that will fit a test • Flow logging preferred method

  12. Flow Log Types • Spinner • Heat pulse • Hydrophysical • Induced electromagnetic

  13. Hydrophysical Log (1) Replace fluid with deionized water (2) Log fluid resistivity while pumping Spinner

  14. UCM (Electromagnetic Log) Fluid Resistivity Flow Temp

  15. Posiva (Finland) Heat Pulse Flow Log (Äspö) Heat Pulse Log

  16. Thoughts on Flow Logging • Cumulative logging methods fast and easy • Discrete interval logging methods provide better detail and wide range of distribution • Complementary temperature and fluid resistivity can be useful

  17. Image Logging Borehole TV (BIPS) FMI (micro-resistivity)

  18. Hydro-Testing Work Flow • Steady tests (flow log) to identify conductors • Image log or core analysis to geo-logically characterize conductors • Transient tests to characterize network away from hole

  19. Transient Well Tests

  20. Overview of Transient Tests • Important source (most important?) of geometric information on fracture plumbing system • Cylindrical flow and beyond • Dimensions, boundaries, and reading derivative curves

  21. Radial Diffusion Equation(Radial Cylindrical Flow)

  22. Exponential Integral:

  23. Semilog Approximation of the Exponential Integral (MKS units)

  24. Exponential Integral Function Semilog Log-Log

  25. Derivative Methods • Plots P/log(t) • Intent to make semi-line unambiguous • Effect is a very powerful tool to interpret geometry from tests • Derivative is a map of transmissivity versus distance from the well • Shape of derivative constrains network geometry

  26. Exponential Integral and Derivative

  27. Calculating Pressure Derivative in Spreadsheets Formula in Cell C8: t   p/  t, or approximately =a8*(b9-b7)/(a9-a7) If the derivative is noisy, calculate derivative over a larger spread, for example, at C7 calculate using rows 10 and 4 Note: Averaging deteriorates at beginning and end of data especially if a larger is used

  28. Dimensionless Variables(Radial Cylindrical Flow)

  29. Useful Definitions

  30. Generalized Radial Flow

  31. Dimension Information from Well Tests

  32. Integer Flow Dimensions

  33. Spherical (3-D) x-section area r2 Linear (1-D), x-section area r0 Generalized Flow, x-section area  rn-1 Cylindrical (2-D) x-section area r1

  34. Log Slope and Dimension For Log Plots of Pressure or Inverse Flow Verus Time For Log Plots of Pressure or Inverse Flow Derivative

  35. Boundary and Dimension Effects 2-D 1-D 3-D Reservoir geometry Network/Flow geometry

  36. Fracture Intensity (Fracture Area/Rock Mass Volume) Can Influence Dimension Boundary Effect

  37. Geometric Information From Well Tests

  38. Composite Dimension 1.00E+03 1.00E+02 Composite Boundary 1.00E+01 Dimensionless Pressure Linear Flow 1.00E+00 Spherical Flow 1.00E-01 1.00E-02 1.00E+00 1.00E+01 1.00E+02 1.00E+03 1.00E+04 1.00E+05 1.00E+06 1.00E+07 1.00E+08 Dimensionless Time

  39. Comments on Interference Tests • Radius of Investigation (very handy !!!) • Estimate diffusivity from response time • Independent of dimension

  40. Important Notes on Tests • Transmissivity can be determined only from pumping wells in fractured or heterogeneous rock without assuming uniform flow over region of influence • Storativity (diffusivity) can only be obtained from observation responses • Observation wells give geometric information for areas farther from pumping source than themselves

  41. Composite Dimension • Dimesional Variation Reflect Local Scale versus Larger Scale Effects • May Reflect Borehole Geometry as Well as Conductive Geometry

  42. Parts of Composite Dimension Curves • Early Time Effects (Wellbore Storage, Finite Borehole) • Inner Shell (n1) • Transition (changes in area, property) • Outer Shell (n2) • Boundary Effects

  43. Composite Interference Response • Response depends on relative distances of transition radius and observation well radius • Inner zone not observed for observation points near or beyond the transition radius

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