The Operator Compact Implicit Method for Reservoir Simulation

1980 ◽  
Vol 20 (03) ◽  
pp. 120-128 ◽  
Author(s):  
Stephen H. Leventhal

Abstract This paper describes the application of the fourth-order operator compact implicit (OCI) method to multiphase flow through porous media. A conservative form of the method is developed and used to solve a one-dimensional, two-phase, immiscible waterflood problem.The results of numerical experiments demonstrate the ability to track sharp fronts with relatively few mesh points. Comparisons with conventional finite-difference methods and variational methods are given. Introduction In recent years, new work in the numerical solution of boundary-value problems for differential equations has been in the direction of high-order methods - that is, methods whose order of accuracy is higher than the first- and second-order methods generally in use. These high-order methods have been developed for both finite-difference, finite-element, and collocation techniques.High-order finite-difference techniques are formed by expanding the computational molecule of the problem. For example, while a second problem. For example, while a second order-accurate formula for a second derivative involves three points, a fourth-order-accurate formula involves five points. This growth in the number of points in the approximation leads to an increase in points in the approximation leads to an increase in the bandwidth of matrices and the need to impose special difference formulas near the boundary.Variational methods achieve higher-order accuracy by using a higher-degree piecewise polynomial subspace for its approximation. The problem of special treatment near the boundary does not exist, but the increase in the degree of the polynomial also leads to an increase in the work for a given number of mesh points. However, this increase is offset by the need for fewer mesh points to achieve a given accuracy. Thus, on model test problems it has been shown that the total work is less for high-order methods.An alternative to the approach of increasing bandwidth to increase order of accuracy is the operator compact implicit (OCI) method. In this method, an approximation to the spatial part of the differential operator is sought using not only the value of the function at adjacent points but also the value of the operator at these points. By this technique, an implicit relationship is defined between the differential operator and the function on the most compact set of points possible. For example, an implicit fourth-order relationship for a second derivative may be derived using only three points.The OCI method has been applied successfully to two-point boundary-value problems, first- and second-order wave equations, diffusion-convection equations, and viscous flow problems. In this paper, a form of the OCI method problems. In this paper, a form of the OCI method applicable to equations in conservation form is presented and the method is applied to the equations presented and the method is applied to the equations of flow through porous media.The specific example considered is a one-dimensional, two-phase waterflood problem studied by Spivak et al. After presenting the form of the two-phase flow equations to be used, the OCI method is developed. In the implementation of the method it is necessary to define transmissibilities at half mesh points. Therefore, we next examine the problem of interpolation. Finally, numerical results problem of interpolation. Finally, numerical results are presented on the performance of the method for the one-dimensional waterflood problem. Development of the Differential Equations The physical problem that the OCI method is applied to in this study is a one-dimensional, compressible, two-phase, immiscible waterflood problem. SPEJ P. 120

2021 ◽  
Vol 89 (2) ◽  
Author(s):  
Sofia Eriksson

AbstractThe scalar, one-dimensional advection equation and heat equation are considered. These equations are discretized in space, using a finite difference method satisfying summation-by-parts (SBP) properties. To impose the boundary conditions, we use a penalty method called simultaneous approximation term (SAT). Together, this gives rise to two semi-discrete schemes where the discretization matrices approximate the first and the second derivative operators, respectively. The discretization matrices depend on free parameters from the SAT treatment. We derive the inverses of the discretization matrices, interpreting them as discrete Green’s functions. In this direct way, we also find out precisely which choices of SAT parameters that make the discretization matrices singular. In the second derivative case, it is shown that if the penalty parameters are chosen such that the semi-discrete scheme is dual consistent, the discretization matrix can become singular even when the scheme is energy stable. The inverse formulas hold for SBP-SAT operators of arbitrary order of accuracy. For second and fourth order accurate operators, the inverses are provided explicitly.


Geophysics ◽  
2011 ◽  
Vol 76 (2) ◽  
pp. T37-T42 ◽  
Author(s):  
Jing-Bo Chen

Based on the formula for stability of finite-difference methods with second-order in time and general-order in space for the scalar wave equation, I obtain a stability formula for Lax-Wendroff methods with fourth-order in time and general-order in space. Unlike the formula for methods with second-order in time, this formula depends on two parameters: one parameter is related to the weights for approximations of second spatial derivatives; the other parameter is related to the weights for approximations of fourth spatial derivatives. When discretizing the mixed derivatives properly, the formula can be generalized to the case where the spacings in different directions are different. This formula can be useful in high-accuracy seismic modeling using the scalar wave equation on rectangular grids, which involves both high-order spatial discretizations and high-order temporal approximations. I also prove the instability of methods obtained by applying high-order finite-difference approximations directly to the second temporal derivative, and this result solves the “Bording’s conjecture.”


1989 ◽  
Vol 79 (4) ◽  
pp. 1210-1230
Author(s):  
C. R. Daudt ◽  
L. W. Braile ◽  
R. L. Nowack ◽  
C. S. Chiang

Abstract The Fourier method, the second-order finite-difference method, and a fourth-order implicit finite-difference method have been tested using analytical phase and group velocity calculations, homogeneous velocity model calculations for disperson analysis, two-dimensional layered-interface calculations, comparisons with the Cagniard-de Hoop method, and calculations for a laterally heterogeneous model. Group velocity rather than phase velocity dispersion calculations are shown to be a more useful aid in predicting the frequency-dependent travel-time errors resulting from grid dispersion, and in establishing criteria for estimating equivalent accuracy between discrete grid methods. Comparison of the Fourier method with the Cagniard-de Hoop method showed that the Fourier method produced accurate seismic traces for a planar interface model even when a relatively coarse grid calculation was used. Computations using an IBM 3083 showed that Fourier method calculations using fourth-order time derivatives can be performed using as little as one-fourth the CPU time of an equivalent second-order finite-difference calculation. The Fourier method required a factor of 20 less computer storage than the equivalent second-order finite-difference calculation. The fourth-order finite-difference method required two-thirds the CPU time and a factor of 4 less computer storage than the second-order calculation. For comparison purposes, equivalent runs were determined by allowing a group velocity error tolerance of 2.5 per cent numerical dispersion for the maximum seismic frequency in each calculation. The Fourier method was also applied to a laterally heterogeneous model consisting of random velocity variations in the lower half-space. Seismograms for the random velocity model resulted in anticipated variations in amplitude with distance, particularly for refracted phases.


2019 ◽  
Vol 2019 ◽  
pp. 1-9 ◽  
Author(s):  
Lei Ren ◽  
Lei Liu

In this paper, a high-order compact finite difference method is proposed for a class of temporal fractional subdiffusion equation. A numerical scheme for the equation has been derived to obtain 2-α in time and fourth-order in space. We improve the results by constructing a compact scheme of second-order in time while keeping fourth-order in space. Based on the L2-1σ approximation formula and a fourth-order compact finite difference approximation, the stability of the constructed scheme and its convergence of second-order in time and fourth-order in space are rigorously proved using a discrete energy analysis method. Applications using two model problems demonstrate the theoretical results.


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