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GRAVITATION                                                                                191

                             ( )
                           F h     GM                               Thus the force on the point mass is
                     g h        =     E  2  .           (8.14)
                      ( ) =
                            m    (R + h )                             F (d)  =   G  M  m  /  (R – d )  2  (8.17)
                                    E                                              s       E
                   This is clearly less than the value of g on the    Substituting for  M  from above , we get
                                                                                        s
                                    GM E                                                             3
                surface of earth :  g =  2  .   For h <<  R  ,we can  F (d)   =  G  M  m ( R  – d ) /  R E   (8.18)
                                                                                   E
                                                                                          E
                                     R               E
                                       E                            and hence the acceleration due to gravity at
                expand the RHS of Eq. (8.14) :
                                                                 a depth d,
                               GM  E                  − 2
                                                                               d
                     g ( ) =             =  g  (1 h R+  /  E  )              F ( )
                       h
                                   /
                           R E 2  (1 h R  E  ) 2                       g(d) =     is
                               +
                                                                              m
                          h
                     For    << 1  , using binomial expression,               F d
                                                                              ( ) GM
                         R                                                            E
                                                                        d
                           E                                          g ( ) =    =   3   (R −  d )
                                                                                           E
                                2 h                                         m     R  E
                     g h ( ) ≅  g 1  −   .             (8.15)
                             
                                R                                       R −  d
                                   E
                                                                           E
                   Equation (8.15) thus tells us that for small       =  g  R   =  g (1 d R−  /  E  )    (8.19)
                heights h above the value of g decreases by a                E
                                                                    Thus, as we go down below earth’s surface,
                factor (1 2 /h R−  ).
                               E                                 the acceleration due gravity decreases by a factor
                   Now, consider a point mass m at a depth d
                                                                 (1 d R   ). The remarkable thing about
                                                                   −
                                                                      /
                below the surface of the earth (Fig. 8.8(b)), so         E
                that its distance from the centre of the earth is  acceleration due to earth’s gravity is that it is
                                                                 maximum on its surface decreasing whether you
                (R −  d )  as shown in the figure.   The earth can
                  E                                              go up or down.
                be thought of as being composed of a smaller
                sphere of radius  (R  – d )  and a spherical shell
                                   E                             8.7  GRAVITATIONAL POTENTIAL ENERGY
                of thickness d.  The force on m due to the outer
                shell of thickness  d is zero because the result  We had discussed earlier the notion of potential
                quoted in the previous section. As far as the    energy as being the energy stored in the body at
                smaller  sphere of radius  ( R  – d  ) is concerned,  its given position.  If the position of the particle
                                          E
                the point mass is outside it and hence according  changes on account of forces acting on it, then
                to the result quoted earlier, the force due to this  the change in its potential energy is just the
                smaller sphere is just as if the entire mass of  amount of work done on the body by the force.
                the smaller sphere is concentrated at the centre.  As we had discussed earlier, forces for which
                If M is the mass of the smaller sphere, then,    the work done is independent of the path are
                   s
                                    3
                     M /M = ( R – d)  / R  3           ( 8.16)   the conservative forces.
                      s   E      E      E
                   Since  mass of a sphere is proportional to be    The force of gravity is a conservative force
                cube of its radius.                              and we can calculate the potential energy of a
                                                                 body arising out of this force, called the
                                                                 gravitational potential energy. Consider points
                                                                 close to the surface of earth, at distances from
                                                                 the surface much smaller than the radius of the
                                                                 earth.  In such cases, the force of gravity is
                                                                 practically a constant equal to mg, directed
                              M
                                s                M
                                                  E              towards the centre of the earth.  If we consider
                                                                 a point at a height h  from the surface of the
                                                                                      1
                                                                 earth and another point vertically above it at a
                                                                 height h  from the surface, the work done in
                                                                         2
                                                                 lifting the particle of mass m from the first to
                                                                 the second position is denoted by W
                Fig. 8.8 (b) g at a depth d. In this case only the                                  12
                                                                      W   = Force × displacement
                           smaller sphere of radius (R –d)              12
                                                          E
                           contributes to g.                                = mg (h  – h )               (8.20)
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                                                                                 2
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