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102             Chapter 2  Mathematical  Models of  Systems

                                 I
                               0.95

                               0.9

                               0.85
                               0.8                 u
                                        /  T"   " " *         "  "'"  T" "  "  " i
                                       I   i       |        -;_      j
                            -  0.75
                                      I                     '
                               0.7
           FIGURE 2.40         0.65
           The tank water level
           time history ob-
           tained by integrat-  0.6   /                     !
           ing the nonlinear
           equations of motion   0.55   /          '        j  _    _ i
           in Equation (2.125)
           with H(0) =  0.5 m   0.5
           and Q 1{f)  =          0       50      100      150      200     250      300
           Q*  =  34.77 kg/s.                            Time (s)




                           With //(0)  =  0.5 m and Q\{t)  =  34.77 kg/s, we can numerically  integrate  the non-
                           linear model given by Equation  (2.125) to obtain the time history  of H(t)  and £^(0-
                           The  response  of the system  is shown  in Figure  2.40. As  expected  from  Equation
                                                                                                  3
                           (2.114), the  system  steady-state  water  level  is H* =  1 m when  Q* = 34.77 kg/m .
                               It  takes  about  250 seconds to reach  steady-state. Suppose that the system  is at
                           steady state and we want to evaluate the response to a step change in the input mass
                           flow rate. Consider
                                                        AQi(0  =  1  kg/s.

                           Then  we can  use the transfer  function  model to obtain the unit step response. The
                           step  response  is shown  in Figure  2.41  for both  the linear  and nonlinear  models.
                           Using  the  linear  model,  we  find  that  the  steady-state  change  in  water  level  is
                           AH   =  5.75 cm. Using the nonlinear  model, we find  that  the steady-state  change in
                           water  level is AH  = 5.84 cm. So we see a small  difference  in the results  obtained
                           from the linear model and the more accurate nonlinear model.
                               As the final  step, we consider the system response to a sinusoidal change in the
                           input  flow rate. Let

                                                       AQiO?) =  2 ^  2,
                                                                s  +  or
                           where  &>  =  0.05 rad/s and q a = 1. The total water input flow rate is
                                                      Q x(t)  = Q* +  AQ x(t),

                           where Q* =  34.77 kg/s. The output  flow rate  is shown in Figure 2.42.
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