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STEADY STATE HEAT CONDUCTION IN ONE DIMENSION
                        114
                                                              1  30  2
                                                            1    2      3





                                                                  x
                                                           x = 0

                                        Figure 4.9 Quadratic finite element discretization

                                                                       ◦
                           Incorporating the boundary condition, that is, T 3 = 40 C, results in the following set of
                        equations:
                                                                                
                                   
                                      1633.33 −1866.66 0.0 T 1
                                                                   1500 − 233.33(40) 
                                    −1866.66   3733.33 0.0      =   6000 + 1866.66(40)      (4.50)
                                                          T 2
                                         0.0      0.0  1.0             40.0      
                                                            T 3
                                                                     ◦
                                                                                      ◦
                           The solution to the above system gives T 1 = 46.43 C and T 2 = 44.82 C, which are
                        identical to the exact solution.
                        4.2.7 Plane wall with a heat source: solution by modified quadratic
                               equations (static condensation)

                        In many transient and nonlinear problems, it will be necessary to obtain the temperature
                        distribution several times. Hence, any possible reduction in the number of nodes, without
                        sacrificing accuracy, is important. For one- dimensional quadratic elements, it is possible to
                        transfer the central node contribution to the side nodes. Thus, there will be only two nodes
                        but the influence of the quadratic variation is inherently present. This process is referred
                        to as static condensation and the procedure will be demonstrated by considering a typical
                        quadratic element equation, namely,

                                                                  
                                                K 11 K 12 K 13 T 1
                                                                     f 1
                                               K 21 K 22 K 23   T 2  =  f 2               (4.51)
                                                                    
                                                K 31 K 32 K 33  T 3    f 3
                           In order to eliminate the middle node, that is, node 2, we transfer its contribution to
                        nodes 1 and 3. This is accomplished by expressing the temperature at node 2 in terms of
                        the temperatures at nodes 1 and 3, that is,

                                                    f 2    K 21 T 1  K 23 T 3
                                               T 2 =    −        +                          (4.52)
                                                    K 22    K 22    K 22
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