Page 75 - Basic physical chemistry for the atmospheric sciences
P. 75

Chemical kinetics

            dirty water will be left  in the tank, etc. Therefore, after 6 t 12  minutes
                                                                 1
            ( 1 / 2)  6  = ( l / 64)  of the  dirty  water will be left in the tank.  If we (arbi­
            trarily) decide that l/64 is a sufficiently small fraction that most of the
            dirty water can be considered to have been displaced,  for a chemical
            that is perfectly mixed in a reservoir for which the efflux is given by a
            first-order  reaction  [Eq.  (3. 1 3))  we  have  the  following  relationships
            between  the  renewal  time  ( T) ,   the  half-life  (t 12)  and  the  residence
                                                       1
            time ( T)
                                                                      ( 3 . 1 6 )
                                            1
                                       T=6t  2 =4T
                                           1
            In  practice,  of course,  natural  systems will fall  somewhere between
            the cases considered above of no mixing and perfect mixing.
              In  the  ocean,  elements  that  form  insoluble  hydroxides  have rela­
            tively short residence times (e.g. , Al and Fe have residence times  in
            the  ocean  of  1 00    and  200  years,  respectively).  Cation ,   such  as
                                                                 s
            Na+ (aq) and K  + (aq), and anions,  such as c1 - (aq) and B r - (aq), have
            longer  residence  times  in  the  ocean  (-7 x 1 0  6   to  1 0 8  years).  In  the
            atmosphere,  the  very  stable  gas  nitrogen  has  a  residence  time  of a
                                                               5
            million years or so, while oxygen has a residence time of  , 00  0- 1 0 , 000
            years.  Sulfur dioxide,  water, and carbon dioxide, on the other hand,
                                                                        y
            have residence times in  the atmosphere of only a few days, 1 0   da s ,
            and 4  years,  respectively. O f   course,  residence times may  e   deter­
                                                                  b
            mined  by  physical removal processes (e.g. ,  scavenging by precipita­
            tion) as well as chemical.



                                        Exercises
                                                              i
                                                                     o
            3 . 7 .    Answer,  interpret, or explain  the following  n   light  f   the
                      principles discussed in this chapter.
                      (a)  A piece of paper can remain in contact with air indefi­
                         nitely without any observable reaction,  but it reacts as
                         soon as it is touched with a flame.
                      (b)  A  match  is  stable until  its  head  is  rubbed  on  a  rough
                         surface.
                      (c)  Increasing pressure generally decreases the rates of re­
                         actions of solids or liquids.
                      (d)  Increasing pressure always increases the rates of reac­
                         tions of gases.
                      (e)  A catalyst is often in the form of a fine powder.
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