The present invention relates to a computerized simulation method suitable for fluid analysis for instance, more particularly to a method which can solve a nonuniform Poisson equation.
In a computerized simulation to analyze a fluid flowing in a given three-dimensional space, a mesh of the three-dimensional space is usually defined by utilizing a Cartesian grid, and at each grid point, the pressure, temperature and/or flow velocity of the fluid are calculated, wherein if the fluid can be considered as incompressible, the equation regarding the pressure is usually given as a Poisson equation. The Cartesian grid can be a rectangular Cartesian, cylindrical Cartesian and spherical Cartesian.
As a method to solve a Poisson equation, iterative methods such as Jacobi method, Gauss-Seidel method and SOR method have been known.
In a iterative method, usually, initial values are given firstly (step 1), and a computation is carried out (step 2), then a convergence test is carried out to determine whether or not the solution satisfies a judgment condition, and if the judgment condition is not satisfied, the step 2 is repeated until the solution satisfies the judgment condition (step 3).
In such a iterative method, when the size of the matrix to be calculated is increased, the solution becomes poorly-converged, and thereby a long computational time is required.
In recent years, therefore, an Algebraic Multigrid (AMG) Method is widely used. As well known in the art, the AMG method is a method extended so as to solve an unstructured grid in addition to an orthogonal grid, on the basis of the geometric multigrid method. Like the original multigrid method, the extended AMG method has a characteristic that the number of repetitions is independent of the mesh size.
Currently, it is considered as the most high-speed solver for a simultaneous linear equation.
Thus, the AMG method has been widely employed in the commercially offered general-purpose solvers (e.g. “FLUENT” of Ansys, Inc, “STAR-CD” of CD-Adapco).
As a solver for a large-scale matrix, the AMG method is excel in the convergence, but a large memory size is required for the computer.
on the other hand, a Block-cyclic Reduction Algorithm is known as a direct method in which a large-scale matrix can be solved without requiring a large memory size and the convergence is to machine precision.
However, the Block-Cyclic Reduction Algorithm is premised on that the constant “k” in a Poisson equation (for example, the “k” in the expression (1) in claim 1) is a fixed value. If the values of the “k” is not a fixed value and accordingly it is impossible to put the “k” outside the Poisson matrix as a common coefficient, then the Block-cyclic Reduction Algorithm can not be used to obtain the solution directly.
In order to use a Block-cyclic Reduction Algorithm properly, the values of the “k” used in a simulation must be a fixed value. In other words, it is necessary to use an explicit method (to satisfy the courant-Friedrichs-Lewy (CFL) condition) and to decrease the time intervals (steps) of the computing. Therefore, there is a disadvantage such that the computational cost increases.
The above-mentioned CFL condition is a necessary condition such that the velocity of propagation of data during computing in a simulation or numerical analysis must be faster than the velocity of propagation of wave or physical value in the real phenomenon to be simulated.
For instance, in the case that a wave motion in a discrete lattice system should be dealt with in the simulation, the values of the time intervals (at) used in solving of the motion equation for the numerical solution must be smaller than the time required for the real wave motion to progress between the adjacent grid units or cells.
If the value of Δt exceeds the upper limit determined by the CFL condition, then numerical divergence occurs, and it becomes impossible to obtain a sensible solution.
If the grid spacings are decreased in order to make a detailed simulation or analysis, the upper limit for the time step also decreases.
In the case of an advection equation, the CFL condition is given as
Δx/Δt>C
wherein
Δx is a grid spacing,
Δt is the computational time interval, and
C is the velocity of real wave (or characteristic velocity).
This CFL condition becomes a condition to be used when a temporal progress is made in an explicit method.
In order to avoid the use of such condition, an implicit method is often employed.
one such popular method is SIMPLE (Semi Implicit Method for Pressure Linked Equations) method which is offered by commercial softwares like FLUENT of Ansys Inc. or by StarCCM+ of CD-Adapco. This method requires sub-iterations and all the Navier Stokes variables like velocity field and pressure field are corrected and updated to latest values for current time level. Since the gradients of velocity field required to update solution to next level are no longer the values of previous time level, the solution is essentially an implicit type method. For this reason, solution is numerically stable even for very large values of time step sizes.
It is therefore, an object of the present invention to provide a simulation method utilizing a Cartesian grid in which, even if the Cartesian grid is nonuniform and Poisson equation is nonuniform (K is not a fixed vale), by the use of a Block-Cyclic Reduction Algorithm, the Poisson equation can be solved rapidly even by a computer with a small memory size.
According to the present invention, a simulation method utilizing a Cartesian grid comprises
a process in which a Cartesian grid model of a two-dimensional or three-dimensional space discretized with a Cartesian grid is defined,
a process in which a Poisson equation
∇[k∇φ]=src expression (1)
(k: a constant defined for each cell individually,
φ: a variable to be calculated, and src: a source term)
is defined based on a physical value and condition associated with the Cartesian grid model, and
a calculating process in which the above-mentioned physical value is calculated based on the Poisson equation, wherein, the calculating process comprises
an error calculating step of calculating an error which is defined as
(
i: the number of iteration,
φ′i+1: a correction parameter added to the current value φi to produce φi+1 to be used in the next iteration computation (namely, φi+1=φi+φ′i+1)
by using a Block-cyclic Reduction Algorithm,
a testing step of testing whether the calculated error is within a predetermined acceptable range or not, and
an error correcting step of correcting the variable φ by the use of an correction parameter if the calculated error is outside the predetermined acceptable range, and
the above-mentioned calculating process repeats the error calculating step, testing step and error correcting step until the error becomes within the predetermined acceptable range, whereby the Poisson equation is solved approximately.
The Block-cyclic Reduction Algorithm is a direct method in which the solution having almost no error can be obtained by one time computation under ordinary circumstances.
However, a Poisson equation whose constant “k” is not a fixed value and which does not satisfy the conditions of application of the Block-cyclic Reduction Algorithm, can not be solved by the Block-cyclic Reduction Algorithm.
In the present invention, therefore, the concept of error is adopted, and in order to decrease the error, a computation of the error using a Block-cyclic Reduction Algorithm, and a correction of the error are repeated.
In other words, by utilizing the Block-cyclic Reduction Algorithm, it makes is possible to solve the Poisson equation with few time iterative computation.
As a result, it becomes possible to solve a Poisson equation with a computer with a small memory size.
Further, since an implicit method can be applied, it becomes possible to make an unsteady computation at relatively long computational time intervals. Therefore, an analysis of airflow involving a complicated disturbed flow is possible at high spacial resolution and high temporal resolution.
Thus, the simulation method according to the present invention is very useful for reducing the computational cost, and development of products, for example the improvement of the dimples of a golf ball.
Furthermore, the Block-cyclic Reduction Algorithm is used, the number of iteration becomes small, therefore, the accumulation of computational errors on the computational result due to the cancellation of significant digits and the like becomes small. As a result, the computational accuracy can be improved.
The patent or application file contains at least one color drawing. Copies of this patent or patent application publication with color drawing will be provided by the USPTO upon request and payment of the necessary fee.
a) is a perspective view for explaining a uniform Cartesian grid.
b) is a perspective view for explaining a nonuniform Cartesian grid.
a) is a perspective view of one cell of a three-dimensional Cartesian grid.
b) is a front view thereof.
a) is an example of a two-dimensional Cartesian grid for explaining the present invention.
b) is an example of the uniform Cartesian grid.
c) is an example of the nonuniform Cartesian grid.
a) and
a) and 30(b) are maps of the solutions of Poisson equations at the 2nd, 3rd, 4th 100th, 800th and 2000th iterative computation.
Embodiments of the present invention will now be described in detail in conjunction with accompanying drawings.
The simulation method is executed by a computer and in this embodiment comprises
a process (S1) in which a model of a two-dimensional or three-dimensional space (in
the above-mentioned Cartesian grid can be
a uniform Cartesian grid composed of uniform cells or
a nonuniform Cartesian grid composed of nonuniform cells,
a process (s2) in which a Poisson equation is defined by a characteristic formula based on a physical value and condition associated with the Cartesian grid model,
a process (s3) in which the Poisson equation is solved in order to calculate the above-mentioned physical value.
For the above-mentioned two-dimensional or three-dimensional space, an Cartesian coordinate system, cylindrical coordinate system or polar coordinate system can be employed, for instance.
In the coordinate system employed in the two-dimensional or three-dimensional space, the Cartesian grid model is defined as Euler mesh, for instance.
Those data are stored in the computer (not shown).
The model has cells or spaces divided by the grid, and boundary conditions, variables and the like are assigned thereto.
In the case of a fluid simulation, the model represents a flow field of the fluid.
From such Cartesian grid model, desired physical values at each grid point, e.g. pressure, flow velocity and the like are calculated.
In this specification and claims, as shown in
For example, in the case of Cartesian coordinates,
the grid spacings in the x-axis direction are constant,
the grid spacings in the Y-axis direction are constant, and
the grid spacings in the z-axis direction are constant.
Thus, all of the cells (a1) are provided with the same shape and the same volume.
On the other hand, the “nonuniform Cartesian grid” means such a Cartesian grid in which
the grid spacings taken in the direction of the axis of at least one of the dimensions are not constant as shown in
In the case of the nonuniform Cartesian grid, it is possible that a specific space A1 for which minute analysis is desired is modeled by relatively-small cells a2, and a specific space A2 for which minute analysis is not necessary is modeled by relatively-large cells a3.
Therefore, the computational cost can be reduced while maintaining the necessary computational accuracy.
As explained, the present invention can be applied to both of the uniform Cartesian grid (“k” is a fixed value) and the nonuniform Cartesian grid (“k” is not a fixed value).
In the process s2, the Poisson equation
∇[k∇φ]=src Expression (1)
is defined by the computer based on necessary parameters, boundary conditions and specifications of the Cartesian grid model entered by an operator.
The “φ” in the expression (1) is a variable to be calculated. In the fluid simulation, the “φ” may be the pressure P, three-components (u, v, w) of the velocity and the like. Anyway these variables are collectively expressed by the single symbol “φ” here.
The “src” in the expression (1) is an abbreviation of “source term”. In the fluid simulation, the “src” becomes the term of the mass flux which usually becomes a function f(φ) of the above-mentioned variable “φ”.
The “k” in the expression (1) is a constant given to each cell individually. In the case of the implicit method which needs not satisfy the CFL condition, the “k” can be nonconstant values.
The “k” can be expressed as
k=vol/Ap
wherein
“vol” is the volume of the cell concerned,
“Ap” is diagonal elements of the momentum equation.
The “Ap” is a function of the mass flux.
In the case of a fluid simulation, the “Ap” can be expressed as
Ap=−(AE+AW)+ρ/Δt
wherein
AE=(ρu/2Δx)−(Γ/Δx2)
AW=−(ρu/2Δx)−(Γ/Δx2)
“ρ” is the density of the fluid (constant under sonic speed),
“u” is the velocity of the fluid,
“Γ” is the viscosity of the fluid.
(cf. “Computational Methods for Fluid Dynamics 3rd Edition” written by J. H. Ferziger, M. Peric, for instance)
The “Ap” is a function of the velocity (u) of the fluid. In the space, the velocity (u) has a nonuniform distribution as long as the flow is not a smooth flow. Accordingly, the “k” becomes not a fixed value.
On the other hand, in the explicit method,
k=ρ/Ap,
and
Ap=ρ/At.
Accordingly,
k=Δt.
Usually, the time intervals Δt are kept constant at all times, therefore, the “k” becomes a fixed value.
In the case that a fluid simulation in a three-dimensional space to which a Cartesian grid is applied is to be solved by the implicit method, the “Ap” can be obtained as follows.
Each cell has six adjacent cells, namely, North (N), South (S), west (W), East (E), Front (F) and Back (B) cells as shown in
The distance from the concerned cell to each of the six adjacent cells measured between the centers (black dots) of the cells is expressed as
The six surfaces of the concerned cell facing in the N, S, W, E, F and B directions each have a surface area and a fluid velocity at the centroid of the surface area, wherein the surface area is expressed as
“Area_” and an initial letter (N,S,W,E,F,B), and the fluid velocity is expressed as
“Velocity_” and an initial letter (N,S,W,E,F,B).
The mass flow rate at each of the six surfaces is expressed as
“Flux_” and an initial letter (N,S,W,E,F,B).
So, the mass flow rates are
Flux—N=ρ×Area—N×Velocity—N
Flux—S=ρ×Area—S×Velocity—S
Flux—W=ρ×Area—W×Velocity—W
Flux—E=ρ×Area—E×Velocity—E
Flux—F=ρ×Area—F×Velocity—F
Flux—B=ρ×Area—B×Velocity—B.
If the flow velocities do not have identical values, then the mass flow rates also do not have identical values. The off diagonal elements A_*(*: N,S,W,E,F,B) are
A—N=−Γ×(Area—N/Dist—N)+Min(Flux—N,0)
A—S=−Γ×(Area—S/Dist—S)+Min(Flux—S,0)
A—W=−Γ×(Area—W/Dist—W)+Min(Flux—W,0)
A—E=−Γ×(Area—E/Dist—E)+Min(Flux—E,0)
A—F=−Γ×(Area—F/Dist—F)+Min(Flux—F,0)
A—B=−Γ×(Area—B/Dist—B)+Min(Flux—B,0)
wherein
“Γ” is the viscosity of the fluid, and
“Min(arg.)” is a function which returns the argument if it is negative or 0 (zero) if the argument is positive.
Using the above-mentioned variables, in the case that the Cartesian grid is three-dimensional, the “Ap” may be expressed as
Ap=−1×(A—N+A—S+A—W+A—E+A—F+A—B).
When all of the surfaces do not have identical mass flux, all of the cells do not have identical Ap, therefore, the “k” becomes not a fixed value.
In the case of the explicit method,
k=ρ/Ap,
Ap=ρ/Δt,
and
k=Δt=constant,
therefore, it is possible to put the “k” outside the Poisson equation. In this case, accordingly, the Poisson equation can be expressed in a form not containing the “k” as follows
In the case of the implicit method,
k=vol/Ap,
and
Ap=−(AE+AW)+ρ/Δt,
therefore, the “Ap” becomes a function of the flow velocity (u). Since the velocity is usually varied according to the positions, the “k” is not a fixed value. Accordingly, the “k” can not be placed outside the Poisson equation.
In the new method according to the present invention, an approximate calculation of a Poisson equation such as the expression (1) is possible at short times. In particular, in order to approximately solve the Poisson equation, the Block-cyclic Reduction Algorithm is used in a manner analogous to the iterative method (calculating process S3).
As explained, the Block-cyclic Reduction Algorithm is a direct method in which a solution containing almost no error can be obtained by one time computation. But, the Poisson equation in which the “k” is not a fixed value can not be solved by the Block-cyclic Reduction Algorithm in a straightforward manner.
Therefore, in this invention, the concept of error is adopted. And the error is calculated iteratively by the use of the Block-cyclic Reduction Algorithm, and gradually decreased by correction. In other words, by utilizing the cyclic reduction method, the Poisson equation in which the “k” is not a fixed value can be solved by few time iterative computation.
Hereinafter, a concrete example will be explained together with the reason why the Block-cyclic Reduction Algorithm can not be applied to the implicit method in a straightforward manner.
a) shows an example of a two-dimensional space which is divided into fifteen cells as a 3-by-5 Cartesian grid. As shown, index numbers are assigned to the respective cells. The domain of this two-dimensional space is one-meters square.
In the following two cases, Poisson equation is defined: the first case is a model of a uniform Cartesian grid as shown in
Here, an intent is to show that this example problem can not be solved by using the Block-cyclic Reduction Algorithm if the “k” is not a fixed value.
This example problem used is such that for the rightmost boundary w of the Cartesian grid, a condition of a fixed value (=10.0) is defined, and to the remaining three boundaries, zero gradient is given.
Further, as the source term, −100 is defined for cell #1, and 0 (zero) is defined for other cells #2-#15.
Incidentally, this example problem is merely for a matrix calculation, not a reproduction of an actual physical phenomenon.
Further, the “k” is defined as follows.
In the first case (uniform Cartesian grid), the “k” is a fixed value, and 1 (one) is defined for each cell as shown in
In the second case (nonuniform Cartesian grid), the “k” is not constant, and as shown in
In
In the matrix shown in
The matrix shown in
The matrix of
In order to solve the equation of
In the finite difference method, as shown in
In the finite difference method, there is used a general expression shown in
In this example problem, as the domain of the two-dimensional, 3-by-5 Cartesian grid model is one-meters square,
Δx=1 m/3≈0.333333 m,
and
Δy=1 m/5=0.2 m.
Using these values and the above-mentioned boundary conditions, in the first case (k=1) shown in
In the second case shown in
As shown, in the first case, diagonal blocks (corresponding to the blocks A2-A5 in
Ai=ai×I
wherein, ai is a scalar, and I is a unit matrix.
In the second case (
Ai=ai×I.
In order that the (block) cyclic reduction method can be applied to the equation, it is necessary for the equation to meet the following three conditions 1-3. In particular, the blocks A-C need to be in the following forms.
Ai=ai×I conditions 1:
Bi=B+bi×I conditions 2:
Ci=ci×I conditions 3:
wherein, ai, bi and ci are scalars, and I is a unit matrix.
(In this regard, see “A Direct Method for the Discrete Solution of Separable Elliptic Equations” written by Paul N Swarztrauber, for instance.)
Next, it is discussed whether the first case and second case satisfy the above-mentioned three conditions or not.
In the first case, the three conditions 1-3 are all satisfied, therefore, the Poisson equation for the uniform Cartesian grid (k is a fixed value of 1) can be solved by applying the cyclic reduction method thereto as a direct method.
However, in the second case (k is not a fixed value), the blocks A-C can not be transformed into the format of “scalar×unit matrix”, and can not satisfy the three conditions 1-3. Therefore, the (block) cyclic reduction method as a direct method can not be applied to the nonuniform Cartesian grid.
In the present invention, therefore, the cyclic reduction method is utilized in a manner analogous to the iterative method and thereby nonuniform Poisson equation for such nonuniform Cartesian grid can be calculated rapidly.
An example of the computational procedure therefor is shown in
As shown, firstly, the error (r) is calculated (step s31). Since the error (r) should become zero finally, the error (r) is defined as follows
error(r)=src−A·φ expression (4)
wherein
“src” is the above-mentioned source term,
“φ” is the variable,
“A” is the matrix of the Poisson equation (k is not a fixed value) shown in
As to the “φ”, 0 (zero) is given to the “φ” in the first time computation. But, in the second time computation and the rest, the “φ” is given by
φ=φold+φ′corr expression (5).
(This expression (5) corresponds to φi+1=φi+φ′i+1 in claim 1) Here, the “φold” is the previous calculated value of the “φ”. The “φ′corr” is a correction parameter (in claim 1 expressed as φ′i+1) indicating a correcting quantity to reduce the above-mentioned error and defined as
φ′corr=Auni−1·[r/k_bar] expression (6).
(In the format used in claim 1, this correction parameter is defined as
wherein
i: the number of iteration,
φ′i+1: a correction parameter added to the current value φi to produce φi+1 to be used in the next iteration computation, namely, φi+1=φi+φ′i+1).
In the expression (6), the “k_bar” is the average value of the “k” across all of the cells.
The “Auni−1” is the inverse matrix of the matrix A of the uniform Cartesian grid in the first case shown in
In this computational expression (6) of the “φ′corr”, since the above-mentioned matrix A satisfies all the conditions 1-3 of application of the cyclic reduction method, the matrix Auni−1 as the inverse matrix thereof also satisfies all the conditions 1-3 of application.
Therefore, in the computation of the above-mentioned correction parameter “φ′corr”, the cyclic reduction method as a direct method can be applied, therefore, an accurate solution of the correction parameter can be obtained by one time computation.
As shown in the equations shown in
In the next step in this embodiment, it is checked whether the summation Σ|ri| of the error (r) is within a predetermined acceptable range or not. (step s32)
If within the acceptable range (if “Y” in step s32), the computational procedure is ended.
If the summation Σ|ri| of the error (r) is outside the acceptable range (if ‘N′’ in step s32), according to the above-mentioned expression, the “φ′corr” and new φ are calculated, and then returning to the step s31, the error (r) is again calculated. Such equation is shown in
The computational results of the variable φ is shown in
Until the summation of the error (r) becomes within the acceptable range, the above-explained steps are repeated.
As shown, by making only three time computations, it is possible to greatly reduce the summation of the error (r).
At the time when the summation of the error (r) becomes within the predetermined acceptable range, the value of the variable φ (in claim 1, φi+1 of the expression (2)) becomes the solution to be sought.
Incidentally, the acceptable range can be arbitrarily defined according to the purpose, usage and the like of the simulation.
As described above, if we try to solve Poisson equation by the use of the implicit method, since the “k” is not a fixed value, it can not be solved by the cyclic reduction method as it is. However, in this invention, the concept of error is adopted, and in order to compute the error, the inverse matrix of the matrix of the uniform Cartesian grid model (k=constant) having the same boundary conditions as those of the nonuniform Cartesian grid model (k=not constant) is used, and thereby it makes it possible to apply the cyclic reduction method thereto. Further, the error is gradually decreased by correction. As a result, it makes it possible to compute the Poisson equation of which k is not constant by utilizing the cyclic reduction method. Accordingly, in comparison with the AMG method solver, the computational time and computational cost can be remarkably reduced with less memory usage.
In the above-mentioned example, the Cartesian grid is two-dimensional. However, it is of course possible that the Cartesian grid is three-dimensional. In such case, in the above-mentioned calculating process, the equation in the above-mentioned expression (1) is Fourier transformed beforehand. Thereby, the dimension of the matrix of the expression (1) is reduced to two-dimension. Thereafter, the computational procedure explained as above can be utilized as it is.
Concretely speaking, the above-mentioned expression (7) can be transformed into expression (8) in the form of a determinant.
Here, each element Ti of the expression (8) means the matrix A in
The “φi” (i=1 to n) means a matrix as an aggregation of (I).
The “Si” (i=1 to n) means a source term corresponding to [ri/k_bar].
The 4-by-4 matrix shown in the expression (8) corresponds to the “Auni−1”.
The matrix of the expression (8) can be transformed into the matrix of the expression (9) by Fourier transformation.
Each matrix element of the expression (9) as shown as
{tilde over (T)}l{tilde over (Φ)}l={tilde over (s)}l expression (10)
(l:1 to n) can be calculated by utilizing the Block-cyclic Reduction Algorithm according to the above-explained computational procedure.
In the expressions (9) and (10), the addition of the tilde ˜ means that the item goes to Fourier space.
[Comparison Test]
using the method according to the present invention and the above-mentioned AMG method, the same problem was solved, and the results were compared with each other.
The computer used was as follows.
Hardware: HP xw9300 workstation
CPU: AMD Dual-core opteron 275 (2.2 GHz)
Memory: 32 GB
OS: x86 64 redhat linux
The software used was as follows.
AMG method: AMG method solver incorporated in Fluent ver.6.3.26
As shown in
k=√{square root over (x2+y2+z2)}
namely, as a function of the coordinates of the grid. Therefore, the Poisson equation to be calculated is
∇[(√{square root over (x2+y2+z2)})∇φ]=0 expression (11).
As to the scale of the grid, three types of models (the number of the cells=5,000,000, 10,000,000 and 15,000,000) were prepared.
Using these models, the number of iterations and the computational time required to reduce the error down to 1/1000 of the value obtained by the first time computation were obtained.
<Test Results>
As explained above, the error of each cell is src−A·φ. The summation of the error is Σ|ri|.
As shown in the test results, in the comparative example in which the Fluent's AMG method solver was used, at least four time iterative computation was needed in order to reduce the error down to 1/1000 (1.0E-3).
In contrast, in the practical example according to the invention, by making only three time iterative computation, the error became under 1/1000 in every model.
Further, with respect to the 10 million cell model, it is observed how the values of the error are changed by increasing the number of iterations of the computation.
In the case of the practical example, however, the error decreases almost linearly. This is a merit of the present invention.
In the case of the comparative example, the necessary memory arrays are 7×N×2=14N, wherein N is the number of the cells. In the case of the practical example, the necessary memory arrays are 9×N. Accordingly, the memory usage in the practical example is about 65% of that in the comparative example.
a) and 30(b) show maps of the solutions of the Poisson equations of the respective cells.
In theory, the correct solution is such that the values at all area (cells) are 100.
In the case of the practical example, by making only three time iterative computation, “100” as the convergent solution could be obtained.
In the case of the comparative example, however, even after 2,000 time iterative computation, the values at almost all area were under 100. Namely, the error could not be reduced.
Although the maps in the attached drawings are monochrome, in the original maps, different values are indicated in different colors.
In order to show the superiority of the method according to the present invention, with respect to a large-scale nonuniform Cartesian grid model shown in
As shown, in the practical example according to the invention, regardless of whether the matrix is very large scale, by making only five time iterative computation, the error could be reduced down to 1/100,000,000 (1.0E-8).
In such a large-scale model problem, to obtain the convergent solution at high speed like this will be impossible unless the method of the present invention is employed.
Further, in the method of the present invention, the error can be reduced down to under 1.0E-10 by making only 12 time iterative computation. In a large-scale model problem, a computational procedure for Poisson equation which can reduce the error down to such very small values maybe do not exist other than the method of the present invention.
Number | Date | Country | Kind |
---|---|---|---|
2010-229824 | Oct 2010 | JP | national |
Number | Name | Date | Kind |
---|---|---|---|
8100196 | Pastusek et al. | Jan 2012 | B2 |
20110242095 | Tsunoda | Oct 2011 | A1 |
20110313742 | Tamada et al. | Dec 2011 | A1 |
20120296616 | Tsunoda et al. | Nov 2012 | A1 |
Entry |
---|
Swarztrauber et al., “The Fourier and Cyclic Reduction Methods for Solving Poisson's Equation”, John Wiley & Sons, 1996, pp. 1-17. |
Bini et al., “The cyclic reduction algorithm: from Poisson equation to stochastic processes and beyond”, Springer Science + Business Media, Nov. 2008,pp. 23-60. |
Gallopoulos et al., “A parallel block cyclic reduction algorithm for the fast solution of elliptic equations”, Elsevier Science Publishers B.V., 1989, pp. 143-157. |
Gander et al. “Cyclic Reduction—History and Applications”, Workshop on Scientific Computing, 1997, pp. 1-15. |
Zhang et al.,“On cyclic Reduction and Finite Difference Schemes”, University of Kentucky, 1999, pp. 1-11. |
Number | Date | Country | |
---|---|---|---|
20120089380 A1 | Apr 2012 | US |