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Carnot cycles. You should convince yourself that traversing the individual
                                                        Carnot cycles in Fig. 2.12.1  in sequence
                                                        is  exactly  equivalent,  in  terms  of  heat
                                                        transferred and work done, to traversing

                                                        the  jagged  sequence  of  isotherms  and
                                                        adiabatic  lines  that  approximates  the
                                                        actual cycle. This is so because adjacent

                                                        Carnot cycles have a common isotherm,
                                                        and  the reversible cycle is superimposed
                                                        on  a  family  of  isotherms.  The  isotherms
                                                        are connected by adiabatic lines, forming

                                                        an  assembly  of  Carnot  cycles    where
                        Figure 2.12.1                   there are two arbitrary points on the cycle,
                                                        and  1  and  2  are  reversible  paths

            connecting them.
            two traversals, in opposite directions, cancel each other in the region of
            overlap as far as heat transfer and work done are concerned. By making

            the  temperature  interval  between  the  isotherms  in  Fig.2.12.1  are  small
            enough, we can approximate the actual cycle as closely as we wish by an
            alternating sequence of isotherms and adiabatic lines.

                       We can then write for the isothermal-adiabatic sequence of lines in
            Fig.2.12.1
                                                              Q
                                                                         0                                    (2.12.3)
                                                              T

            or, in the limit of infinitesimal temperature differences between the

            isotherms
                                                   dQ
                                                             0                                                (2.12.4)
                                                   T
            in which        indicates that the integral is evaluated for a complete traversal

            of the cycle, starting and ending at the same arbitrary point of the cycle. .
            We use dQ here to mean a small quantity of heat, not a true differential,

            dQ means the small quantity of heat that enters or leaves the system along
                                                         dQ
            a short element of the path. But                     must be a differential change in a
                                                          T
            state variable. We call this new variable the entropy S and the differential
            of the entropy is equal to






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