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inclusion of a thermodynamic system in order that energy be conserved. Of course, the
                        detailed workings of the thermodynamic system are often ignored, indicating that any
                        thermodynamic “feedback” mechanism is weak. In the waveguide example, for instance,
                        the heating of the metallic walls does not alter their electromagnetic properties enough
                        to couple back into an effect on the fields in the walls or in the guide. If such effects were
                        important, they would have to be included in the conservation theorem via the bound-
                        ary fields; it is therefore reasonable to associate with these fields a “flow” of energy or
                        momentum into V . Thus, we wish to develop conservation laws that include not only the
                        Lorentz force effects within V , but a flow of external effects into V through its boundary
                        surface.
                          To understand how external influences may effect the electromagnetic subsystem, we
                        look to the behavior of the mechanical subsystem as an analogue. In the electromagnetic
                        system, effects are felt both internally to a region (because of the Lorentz force effect) and
                        through the system boundary (by the dependence of the internal fields on the boundary
                        fields). In the mechanical and thermodynamic systems, a region of mass is affected both
                        internally (through transfer of heat and gravitational forces) and through interactions
                        occurring across its surface (through transfers of energy and momentum, by pressure
                        and stress). One beauty of electromagnetic theory is that we can find a mathematical
                        symmetry between electromagnetic and mechanical effects which parallels the above con-
                        ceptual symmetry. This makes applying conservation of energy and momentum to the
                        total system (electromagnetic, thermodynamic, and mechanical) very convenient.


                        Conservation of momentum and energyin mechanical systems.        We begin by
                        reviewing the interactions of material bodies in a mechanical system. For simplicity we
                        concentrate on fluids (analogous to charge in space); the extension of these concepts to
                        solid bodies is straightforward.
                          Consider a fluid with mass density ρ m . The momentum of a small subvolume of the
                        fluid is given by ρ m v dV , where v is the velocity of the subvolume. So the momentum
                        density is ρ m v. Newton’s second law states that a force acting throughout the subvolume
                        results in a change in its momentum given by
                                                      D
                                                        (ρ m v dV ) = f dV,                   (2.272)
                                                      Dt
                        where f is the volume force density and the D/Dt notation shows that we are interested
                        in the rate of change of the momentum as observed by the moving fluid element (see
                        § A.2). Here f could be the weight force, for instance. Addition of the results for all
                        elements of the fluid body gives
                                                    D
                                                         ρ m v dV =  f dV                     (2.273)
                                                    Dt  V          V
                        as the change in momentum for the entire body. If on the other hand the force exerted
                        on the body is through contact with its surface, the change in momentum is
                                                     D
                                                          ρ m v dV =  t dS                    (2.274)
                                                    Dt  V           S
                        where t is the “surface traction.”
                          We can write the time-rate of change of momentum in a more useful form by applying
                        the Reynolds transport theorem (A.66):
                                          D                ∂
                                               ρ m v dV =    (ρ m v) dV +  (ρ m v)v · dS.     (2.275)
                                          Dt  V          V ∂t           S



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