SPE Reservoir Evaluation & Engineering
Volume 14, Number 1, February 2011, pp. 113-119

SPE-123930-PA

Identification and Characterization of High-Conductive Layers in Waterfloods

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DOI  More information 10.2118/123930-PA http://dx.doi.org/10.2118/123930-PA

Citation

  • Izgec, B. and Kabir, C.S. 2011. Identification and Characterization of High-Conductive Layers in Waterfloods. SPE Res Eval & Eng  14 (1): 113-119. SPE-123930-PA. doi: 10.2118/123930-PA.

Discipline Categories

  • 6.4.1 Waterflooding

Keywords

  • Modified-Hall Analysis, Waterflooding, High-Conductive Layers

Summary

This study expands upon the use of modified-Hall analysis (MHA) to discern the characteristics of a high-permeability channel. Briefly, the modified-Hall plot uses three curves involving improved Hall-integral (H-I) and the two derivatives, analytic and numeric. Ordinarily, the derivative curves overlay on the integral curve during matrix injection, but separates lower when fracturing occurs. This work presents a method to identify and characterize high-conductive layers or channels between injector and producer pairs with the MHA. The distance separating the integral and derivative curves provides the required information to quantify channel properties. A simple analytical solution is presented for transforming the separation distance into channel permeability-thickness product.

The analytic derivative is based on the radial-flow-pattern assumption and the numeric derivative is correlated to the pressure response. Therefore, a comparison of these two curves reveals clues about the maturity of a waterflood at a given time. Several simulated examples verified the channel-property-estimation algorithm and identified the distinctive derivative signatures for channeling and fracturing situations. This method is also useful for identification of wormhole propagation during sand production in unconsolidated formations.

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History

  • Original manuscript received: 25 August 2009
  • Meeting paper published: 4 October 2009
  • Revised manuscript received: 15 March 2010
  • Manuscript approved: 7 June 2010
  • Published online: 20 December 2010
  • Version of record: 21 February 2011