Page 65 - Modern physical chemistry
P. 65

54                        Gases and Collective Properties

             number of ith particles per unit area in thickness dz then gives the net pressure due to
             the change in potential. w:;:eC,N A ( _ a:,: ) dz ~ --c,N A d.,.        [3.781



                Combining equations (3.77) and (3.78) leads to

                                                                                     [3.79]
             or
                                               dCi  = _ d1>i                         [3.80]
                                               Ci     kT
             where k is the Boltzmann constantRIN A • Integrating equation (3.80) from potential energy
             o to potential energy ei yields
                                                                                     [3.81 ]
                Since c i  and ciQ are proportional to the number of molecules of the ith species at levels
             ei and eiQ, Ni and NiO  respectively, equation (3.81) implies that

                                            N · - N·  e-CilkT  .                     [3.82]
                                              t  -
                                                   to
             From the way it has been derived, we see that equation (3.82) gives us the equilibrium
             distribution of molecules in a potential field. In the next section, we will derive an equiv-
             alent form for the distribution over kinetic energy.
                The form encompassing both potential and kinetic energies is known as the Boltz-
             mann distribution law.




             Example 3.9
                A gold sol containing particles averaging 4.5 x  10- 7  cm in radius reached equilibrium
             at 25° C. With an ultramicroscope, 89 particles were observed in 32 successive counts at
             a certain level. How many particles should be observed in 32 successive counts in a layer
             0.200 cm higher?
                For the volume of a typical particle, we have


                                     3
                              v = ~ nr = ~ n( 4.5 x 10- cm t = 3.82 x 10- 19   cm •
                                                   7
                                                                        3
             Since the water buoys up the particle, its effective density equals its density in air minus the
             density of water:
                                                                       3
                                                            3
                               p'= Pgold  - Pwater = 19.3 -1.0 g cm- = 18.3 g cm- •
             So the gravitational force acting on the particle is

                                    3
                        F  = 18.3 g cm- (3.82 x 10- 19  cm 3 X9.807 N kg-I) = 6.85 x 10- 20  N.
                            1000 g kg- 1
             On moving 0.200 cm up, its potential energy increases by

                                                        2
                              1> = (6.85 x 10- 20   N X 0.200 x 10- m) = 1.37 x 10- 22   J.
   60   61   62   63   64   65   66   67   68   69   70