Page 177 - Physical chemistry understanding our chemical world
P. 177

144    REACTION SPONTANEITY AND THE DIRECTION OF THERMODYNAMIC CHANGE

                      SAQ 4.4 1 mol of oxygen is warmed from 300 K to 350 K. Calculate the
                      associated rise in entropy  S if C p(O 2 ) /JK −1  mol −1  = 25.8 + 1.2 × 10 −2 T/K.

              4.3     Introducing the Gibbs function


                       Why is burning hydrogen gas in air (to form liquid
                       water) a spontaneous reaction?

                      Reaction spontaneity in a system

                                      Equation (4.19) describes the reaction occurring when hydrogen
              The ‘twin’ subscript    gas is burnt in air:
              of ‘l and g’ arises
              because the reaction
                                                     O 2(g) + 2H 2(g) −−→ 2H 2 O (l and g)  (4.19)
              in Equation (4.19) is so
              exothermic that most
                                      We notice straightaway how the number of moles decreases from
              of the water product    three to two during the reaction, so a consideration of the system
              will be steam.
                                      alone suggests a non-spontaneous reaction. There may also be a
                                      concurrent phase change from gas to liquid during the reaction,
                      which confirms our original diagnosis: we expect  S to be negative, and so we
                      predict a non-spontaneous reaction.
                        But after a moment’s reflection, we remember that one of the simplest tests for
                      hydrogen gas generation in a test tube is to place a lighted splint nearby, and hear the
                      ‘pop’ sound of an explosion, i.e. the reaction in Equation (4.19) occurs spontaneously.
                        The ‘system’ in this example comprises the volume within which chemicals com-
                      bine. The ‘surroundings’ are the volume of air around the reaction vessel or flame;
                      because of the explosive nature of reaction, we expect this volume to be huge. The
                      surrounding air absorbs the energy liberated during the reaction; in this example, the
                      energy is manifested as heat and sound. For example, the entropy of the air increases
                      as it warms up. In fact,  S (surroundings) is sufficiently large and positive that the value
                      of  S (total) is positive despite the value of  S (system) being negative. So we can now
                      explain why reactions such as that in Equation (4.19) are spontaneous, although at
                      first sight we might predict otherwise.
                        But, as chemists, we usually want to make quantitative predictions, which
                      are clearly impossible here unless we can precisely determine the magnitude of
                       S (surroundings) , i.e. quantify the influence of the surroundings on the reaction, which
                      is usually not a trivial problem.


                       How does a reflux condenser work?

                      Quantifying the changes in a system: the Gibbs function

                      All preparative chemists are familiar with the familiar Liebig condenser, which we
                      position on top of a refluxing flask to prevent the flask boiling dry. The evaporating
   172   173   174   175   176   177   178   179   180   181   182