geomechanics and permeability changes
play

Geomechanics and Permeability Changes Ian Palmer Higgs - PowerPoint PPT Presentation

Geomechanics and Permeability Changes Ian Palmer Higgs Technologies, Houston 28 October 2004 Matrix shrinkage/swelling: can think of as due to temperature change Matrix Shrinkage/Swelling e b Co bP Co e = -------------- (1 + bP) P


  1. Geomechanics and Permeability Changes Ian Palmer Higgs Technologies, Houston 28 October 2004

  2. Matrix shrinkage/swelling: can think of as due to temperature change

  3. Matrix Shrinkage/Swelling e b Co bP Co e = -------------- (1 + bP) P where e = matrix shrinkage strain (fraction), Co = strain at infinite pressure 1/b = pressure at strain of 0.5Co (psi), P = current reservoir pressure

  4. Palmer-Mansoori Equation Based on rock mechanics f = 1 + Cm (P-Po) + Co (K/M-1) bP bPo (1) f o f o f o 1+ bP 1+ bPo Stress-dependent Matrix shrinkage term perm term � perm increases � perm decreases with depletion with depletion (2) k/ko= (f /f o) 3 Cm = 1/M - ß (K/M + f – 1) Co, b = parameters of volumetric strain change due to desorption (depletion) Co = strain at infinite pressure 1/b = pressure at strain of 0.5Co (psi)

  5. Other Models • Shi and Durucan: – based on rock mechanics – same equation – only difference is in (K/M -1) term in shrinkage • ARI: – based on empirical shrinkage depletion coefficient, instead of rock mechanics – same equation

  6. Contents • Production modeling and dilemmas (interpretation was clean 8 years ago, now messy) • Injection modeling and results (interpretation appears to be clean) • Way forward

  7. Production Dilemmas • Perm increases in San Juan basin are very large (by 10-100x) • Can be matched by Palmer-Mansoori model, but…… • Have to remove stress-dependent perm effect (a dilemma!) • Also, initial porosities are VERY small (=0.1%), and at lower limit of acceptable range (another dilemma?) • If can’t explain these dilemmas, may have to consider alternate models for perm increases due to depletion

  8. Summary of San Juan Fairway Data All are absolute k/ko versus Pb perms Mavor & Vaughan 100.00 datapoints are Mavor & Vaughan (1997) from 3 separate (PTA tests) wells 10.00 Zahner (1997) (PTA tests, Well B) k/ko 1.00 This line should 0 500 1000 1500 2000 be elevated Clarkson (2003) Zahner (1997) (history match) (PTA tests, Well A) 0.10 Pb (psi)

  9. ….contd • No perm decrease is evident in data • Even though P-M theory generally predicts such a decrease at early times, due to stress- dependent permeability • Possible explanations: – early time data missed – perm rebound point > Po (this is case for M&V data, but not rest of data) – perm decrease predicted by stress-dependent perm is inhibited by asperities (ie, roughness) in cleats, preventing cleats from closing as reservoir pressure is decreased

  10. One Match to Zahner/Clarkson Data: blue dashes The exponential curve is telling us something k/ko versus Pb important c/b=8 f =.0008 all parameters v=0.3 100.00 b=.0013 in range no stress- 10.00 perm 1.00 0 500 1000 1500 2000 k/ko 0.10 0.01 match if stress-dependent perm included We don’t see 0.00 this curve at all! 0.00 Pb (psi)

  11. Best matches to Clarkson/Zahner Data match quality: Zahner/Clarkson data (standard model) 30 Region of 25 acceptable 20 Co/b (psi) parameters good match 15 very poor match 10 okay match 5 0 0 0.1 0.2 0.3 0.4 0.5 phio (%) Acceptable matches Dilemma? have f o = 0.1% (lower limit of range)

  12. Dilemmas • Majority of data are consistent with exponential increase of permeability with depletion. No perm decreases are evident • Cannot match exponential perm increase data of Zahner/Clarkson using the full P-M equation (including the stress-perm effect), because prediction is too concave upwards, and abnormally strong matrix shrinkage would be required to “straighten out” the curve • Can match the data by omitting the stress-perm effect: this could be due to cleats unable to close during depletion, because of asperities (ie, roughness between cleat surfaces). • Other dilemmas: initial porosities are small (=0.1%), and at lower limit of acceptable range of 0.05 – 0.5%. Also, matrix shrinkage values are on low side of the acceptable range: b =0.0017 /psi compared with range of 0.0013 - 0.0033 /psi, and Co is low in proportion to b.

  13. Stress-Dependent Permeability in Lab: It does Exist!

  14. Stress-Dependent Permeability in Field: It does Exist! • In San Juan basin, a set of cavity surges was observed (delayed) at an observation well 242 ft away • Delay of buildup peaks was different from delay of blowdown troughs • Different delays imply different permeabilities • Buildup perms > blowdown perms • Agrees with stress-dependent perm (but stronger than lab measurements)

  15. Surges at Cavity Well and Observation Well

  16. Other Mechanisms to Explain Exponential Increase in Perm with Depletion • Matrix shrinkage leads to a horizontal fracture, which grows with time, and dominates gas production • Differential depletion: need to use average perm and average pressure (two or more seams) • A non-Langmuir shape governs the matrix shrinkage vs pressure • DOES NOT APPEAR to be due to rel perm changes • CANNOT be due to concentration of CO2 increasing over time in the produced gas stream • CANNOT be due to new coal failure induced by matrix shrinkage, as Mavor and Vaughan have suggested • CANNOT be resolved by replacing stress-perm term by exponential term, as seen in lab

  17. Mechanism 1 (maybe) • Matrix shrinkage tends to open up (widen) existing vertical cleats. • Bulk shrinkage also occurs in vertical direction, but there are no horizontal cleats • Vertical compaction occurs, creating an interface crack under a rigid shale (eg, caprock) • This acts like a horizontal fracture, and it will grow with depletion

  18. Interface Crack caused by Shrinkage & Compaction Shale (rigid) vertical shrinkage creates crack coal horizontal shrinkage enhances perm shale

  19. Mechanism 2 (less likely) • Differential depletion: two or more coals • Coal with higher perm will deplete faster. In the Clarkson data, perm increase comes from average perm calculated from total production • If two coals are contributing, this average perm should be tied to an average of the two depleted pressures, when creating the plot of k/ko vs P. In practice, lowest reservoir pressure was used • This will act to bend the true perm increase curve downwards at larger depletions. This may straighten a true perm increase curve that was concave • But the perm increase of Zahner is exponential, and derived from PTA tests (also may be “contaminated” by rel perm effects) • Need to evaluate this mechanism further

  20. Mechanism 3 (unlikely) • A non-Langmuir shape governs the matrix shrinkage vs pressure • Using b/2 in place of b in P-M model gives a better match to Zahner/Clarkson exponential data than any match with the standard model • We know of no physical justification for this

  21. Summary • Majority of data are consistent with exponential increase of permeability with depletion. No perm decreases are evident • Cannot match exponential perm increase data of Zahner/Clarkson using the full P-M equation (including the stress-perm effect), because prediction is too concave upwards, and abnormally strong matrix shrinkage would be required to “straighten out” the curve • Can match the data by omitting the stress-perm effect: this could be due to cleats unable to close during depletion, because of asperities (ie, roughness between cleat surfaces). • Other dilemmas: initial porosities are small (=0.1%), and at lower limit of acceptable range of 0.05 – 0.5%. Also, matrix shrinkage values are on low side of the acceptable range: b =0.0017 /psi compared with range of 0.0013 - 0.0033 /psi, and Co is low in proportion to b.

  22. Injection vs Production • Injection • Production • Reservoir pressure • Reservoir pressure rises falls • Perm increases due • Perm decreases due to stress-dependent to stress-dependent perm perm (or does it?) • Perm drops due to • Perm increases due matrix swelling to matrix shrinkage

  23. Application to Greenhouse Gas Sequestration • Same physics of stress-dependent permeability and matrix shrinkage should control reservoir performance during injection of gases such as CO2 • But during injection, we expect stress-perm effect to be fully active, while during production it appears to be suppressed • Parameters derived from our matches may be useful as starting points for injection modeling, prediction, and history matching in San Juan basin • Eg, initial porosities are small (=0.1%), and at lower limit of acceptable range of 0.05 – 0.5%.

  24. Mavor Formulation and Application to Canada Coals • Based on P-M equation • Adapted to injection • Generalized to multi-component gas compositions, often changing with time • Extended to rel perms • Modeled perm changes due to injection, soak, production • Calibrated model using injections/falloff tests of (1) water or WAG and (2) SAG • Forecast injection performance for gas sequestration

  25. Strains Induced during Gas Fillup Strain Stress-perm These are modeled Swelling Reservoir pressure �

  26. Perm Change during Gas Fillup Perm ratio This results from K/Ko previous slide Virgin perm Reservoir pressure �

  27. Porosity Change vs Pressure and Composition Porosity water ratio N2 These are modeled CH4 CO2 Reservoir pressure �

Download Presentation
Download Policy: The content available on the website is offered to you 'AS IS' for your personal information and use only. It cannot be commercialized, licensed, or distributed on other websites without prior consent from the author. To download a presentation, simply click this link. If you encounter any difficulties during the download process, it's possible that the publisher has removed the file from their server.

Recommend


More recommend