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The upwind differencing scheme is a method used in numerical methods in computational fluid dynamics for convectiondiffusion problems. This scheme is specific for Peclet number greater than 2 or less than −2


Description

By taking into account the direction of the
flow Flow may refer to: Science and technology * Fluid flow, the motion of a gas or liquid * Flow (geomorphology), a type of mass wasting or slope movement in geomorphology * Flow (mathematics), a group action of the real numbers on a set * Flow (psych ...
, the upwind differencing scheme overcomes that inability of the central differencing scheme. This scheme is developed for strong convective flows with suppressed diffusion effects. Also known as ‘Donor Cell’ Differencing Scheme, the convected value of property \phi at the cell face is adopted from the upstream node. It can be described by Steady convection-diffusion partial Differential Equation: : \frac(\rho\phi)+\nabla \cdot (\rho \mathbf \phi)\,= \nabla \cdot (\Gamma\operatorname \phi)+S_
Continuity equation A continuity equation or transport equation is an equation that describes the transport of some quantity. It is particularly simple and powerful when applied to a conserved quantity, but it can be generalized to apply to any extensive quantity. S ...
: \left(\rho u A \right)_ - \left(\rho u A \right)_w = 0 \, where \rho is density, \Gamma is diffusion coefficient, \mathbf is the velocity vector, \phi is the property to be computed, S_\phi is the source term, and the subscripts e and w refer to the "east" and "west" faces of the cell (see Fig. 1 below). After
discretization In applied mathematics, discretization is the process of transferring continuous functions, models, variables, and equations into discrete counterparts. This process is usually carried out as a first step toward making them suitable for numerical ...
, applying continuity equation, and taking source term equals to zero we get Central difference discretized equation : F_ \phi_-F_ \phi_\,= D_(\phi_-\phi_)-D_(\phi_-\phi_) \;......(1) : F_-F_\,=0 \;.....(2) Lower case denotes the face and upper case denotes node; E, W, and P refer to the "East," "West," and "Central" cell. (again, see Fig. 1 below). Defining variable F as convection mass
flux Flux describes any effect that appears to pass or travel (whether it actually moves or not) through a surface or substance. Flux is a concept in applied mathematics and vector calculus which has many applications to physics. For transport ph ...
and variable D as diffusion conductance :F\,= \rho u A\; and \;D\,= \frac \; Peclet number (Pe) is a non-dimensional parameter determining the comparative strengths of convection and diffusion Peclet number: : Pe \,= \frac \,= \frac \; For a Peclet number of lower value (, Pe,  < 2), diffusion is dominant and for this the central difference scheme is used. For other values of the Peclet number, the upwind scheme is used for convection-dominated flows with Peclet number (, Pe,  > 2). For positive flow direction : u_ > 0 : u_ > 0 Corresponding upwind scheme equation: : F_ \phi_-F_ \phi_\,= D_(\phi_-\phi_)-D_(\phi_-\phi_).....(3) Due to strong convection and suppressed diffusion :\phi_ \,= \phi_ :\phi_ \,= \phi_ Rearranging equation (3) gives :
D_+F_)+ D_+ (F_-F_) D, or d, is the fourth letter in the Latin alphabet, used in the modern English alphabet, the alphabets of other western European languages and others worldwide. Its name in English is ''dee'' (pronounced ), plural ''dees''. History T ...
phi_\, =(D_+F_)\phi_+D_\phi_)\; Identifying coefficients, :a_\,=
D_ + F_) + D_ + (F_ - F_) D, or d, is the fourth letter in the Latin alphabet, used in the modern English alphabet, the alphabets of other western European languages and others worldwide. Its name in English is ''dee'' (pronounced ), plural ''dees''. History T ...
/math> \; :a_\,=(D_ + F_) :a_\,= D_ For negative flow direction :u_ < 0 :u_ < 0 Corresponding upwind scheme equation: : F_ \phi_-F_ \phi_\,= D_(\phi_-\phi_)-D_(\phi_-\phi_).....(4) :\phi_\,= \phi_ :\phi_\,= \phi_ Rearranging equation(4) gives : D_e - F_e ) + D_w + ( F_e - F_w )\phi_ = D_w \phi_ + ( D_e - F_e ) \phi_ Identifying coefficients, :a_\,= D_ :a_\,= D_ - F_ We can generalize coefficients as – :a_=D_ + \max(F_,0) :a_=D_ + \max(0,-F_)


Use

Solution in the central difference scheme fails to converge for Peclet number greater than 2 which can be overcome by using an upwind scheme to give a reasonable result. Therefore the upwind differencing scheme is applicable for Pe > 2 for positive flow and Pe < −2 for negative flow. For other values of Pe, this scheme doesn’t give effective solution.


Assessment

Conservativeness The upwind differencing scheme formulation is conservative. Boundedness As the coefficients of the discretised equation are always positive hence satisfying the requirements for boundedness and also the coefficient matrix is diagonally dominant therefore no irregularities occur in the solution. TransportivenessH. K. Versteeg & W. Malalasekera (1995). ''An Introduction to Computational Fluid Dynamics'', Chapter 5, page 118. (5.6.1.3) Transportiveness is built into the formulation as the scheme already accounts for the flow direction. Accuracy Based on the backward differencing formula, the accuracy is only first order on the basis of the Taylor series truncation error. It gives error when flow is not aligned with grid lines. Distribution of transported properties become marked giving diffusion-like appearance, called as the
false diffusion False diffusion is a type of error observed when the upwind scheme is used to approximate the convection term in convection–diffusion equations. The more accurate central difference scheme can be used for the convection term, but for grids wit ...
. Refinement of grid serves in overcoming the issue of false diffusion. With decrease in the grid size, false diffusion decrease thus increasing the accuracy.


References

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See also

* Central differencing scheme * Finite difference *
Upwind scheme In computational physics, the term upwind scheme (sometimes advection scheme) ''typically'' refers to a class of numerical discretization methods for solving hyperbolic partial differential equations, in which so-called upstream variables are used ...
Computational fluid dynamics Numerical differential equations