SPE Journal
Volume 10, Number 4, December 2005, pp. 449-457

SPE-84548-PA

Estimation of Flow Functions During Drainage Using Genetic Algorithm

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DOI  More information 10.2118/84548-PA http://dx.doi.org/10.2118/84548-PA

Citation

  • Sun, X. and Mohanty, K.K. 2005. Estimation of Flow Functions During Drainage Using Genetic Algorithm. SPE  J.10 (4): 449-457. SPE-84548-PA.

Discipline Categories

  • 6.6.2 Core Analysis
  • 6.3.2 Multi-phase Flow
  • 6.3.1 Flow in Porous Media

Summary

Unsteady-state relative permeability experiments followed by automatic history matching have been used in the past for estimating relative permeability and capillary pressure simultaneously. The performance of the automatic history matching largely depends on the simulator, the functional form of the flow functions, and the optimization tool. The Newton method is commonly used as the optimization tool for the automatic history matching; we have used a genetic algorithm (GA) as the optimization tool in this work. One of the advantages of GA is that it requires only function evaluations for the solution searching and not Jacobian or gradient calculations as required by the Newton method. The Corey model and piece-wise spline interpolation were used to represent the relative permeability. A new coding method in GA was developed for piece-wise spline interpolation. In-situ saturation data were collected during an unsteady-state primary drainage experiment by CT scanning. Simulation and experimental data were used to test the performance of the algorithm. Test results showed a good match between the simulation data and experimental data for low-injection-rate primary drainage. At higher rates, GA did not converge to the global optimum.

Introduction

Relative permeability and capillary pressure are two important functions for describing multiphase flow through porous media. They depend on saturation, saturation history, wettability, porous medium microstructure, capillary number, and Bond number, in general. Pore network models are being developed to estimate these functions, but most researchers rely on experimental measurements of these functions. 

Capillary pressure and relative permeability have been measured separately in previous works. Capillary pressure can be measured by the porous-plate method, the centrifuge method, or by mercury porosimetry. Relative permeability can be measured by steady-state or unsteady-state coreflooding experiments. The drawback of determining capillary pressure and relative permeability separately is that the capillary pressure measured in this manner gives a static capillary pressure curve, while it is the dynamic capillary pressure that influences the flow. As pointed out by Bentsen and Manai and then in Bentsen, the capillary pressure in a dynamic system may be different from that in a static case, because the dynamic capillary pressure is affected by many factors including flow rate, possible variations of the wetting property, and microheterogeneity. Therefore, simultaneously estimating the capillary pressure and the relative permeability for a given flow system is preferable. In the present work, we use unsteady-state experiments followed by the history-matching method to estimate relative permeability and capillary pressure.

History-matching techniques have been developed to estimate relative permeability and capillary pressure simultaneously. Functional forms with a set of parameters are presumed for relative permeability of each phase and capillary pressure. A series of forward simulations is run with the parameters taking a certain set of values. The parameters are automatically tuned by an optimization tool to match the simulation data (generally the pressure drop and the production) with the experimental data.

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History

  • Original manuscript received: 28 January 2004
  • Revised manuscript received: 18 March 2005
  • Manuscript approved: 3 April 2005
  • Version of record: 15 December 2005