Page 178 - Pressure Swing Adsorption
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 152   PRESSURE SWING ADSORPTION   EQUILIBRIUM THEORY                 153

 assumed local  eouilibnum and neglected pressure drop, and they solved  the   consideration  to  a  cycle  havmg  cornpiete  purge ..  To:  detemune  whether  a
 equat10ns  by  finite  differences.  A  subsequent moclei  that examined  pressur-  shock wave  may  form,  one must  simply examme whether the  characteristics
 ization  and  mcluded  effects  of  axial  dispersion,  but  not  of  mass  transfer   mtersect  (in  the  soace-!Jme  domam  bemg  considered).  The  oaths  of  the
 resistance  or pressure  ctrop,  was  developed  by  Rousar and  Ditl. 31   Another   characteristics  are  given  by  Eo.  4.33,  and  the  comno.sition  as  a  function  of
 local equilibrmm model was proposed by Kumar, 32   and it was one of very few   pressure can  be  determined from  EQ.  4.32.  When  the charactenstics do  not
 to mcorporate an energy balance. That model was used  to analyze adiabatic   intersect,  regardless  of  the  initial  and  boundary  conditions,  that  pair  of
 blowdown behav10r.  More detailed modeis are discussed later in  this section.   equations  1s  sufficient  to  predict  the  composition  nrOfile  durmg oressuriza~
 This section  first  examines  the  simoiest cases of pressurization  and blow-  , tion.  On  the  other  hand,  situations  that  result  m  the  fonnat10n  of shock
 down,.  and  suggests  that  the  key  features  predicted  by  more  sophist1catect   waves  reQUire  a  few  additional  steps  to  predict  the•  ultimate  composition
 models  can  be  obtained  analytically.  In  such  cases,  much  less  effort  1s   profile.  When  pressure vanes,  the  shock wave  traJectory can  be  determined
 required, and  reasonably accurate estimates of the exoected behavmr can  be   by  emoloymg Ea. A.7 from  Appendix A,  as  follows
 obtained.  That  upproach  neglects  axial  pre5surc  drop  and  mass  transfer   IJ.1JPyA
 resistance,  as  is  the  case  throughout  this  chapter.  Later  m  this  section,   lJsu  =  OA  t::i.PyA   (4.69)
 however,  the  impact  of  pressure  drop  on  pressurization  and  blowdown  1s
 considered.   The  interstitial  velocity  is  obtained  by  summmg  Eq.  4.4  for  components  A
 It  turns  out  that  the  coupling  of velocity,  composition,  and  pressure  1s   and  B.
 graspable  for  systems  governed  by  linear  isotherms!  but  when  nonlinear
 isotherms are invoived  the additional complexity makes the set of eouatlons   ( 4.70)
 unwieldy and to get detailed simulations via  the method of charactenstics is
         In this  equation,  the  axial  dependence  of pressure can  be  neglected, which,
 not practical. In addition, as noted in the previous section, the pressunzatmn
         given  the  dependence  of  pressure  on  time,  leaves  a  separable  ordinary
 and  blowctown  steps also  may  give  rise  to significant temperature shifts that
         differential eQuation,
 affect  the validity of predictions based on ·isothermal models.
 For  oressurizauon  a  number  of possibilities  exist,  and  the  two  simplest   d In  P   dv   dvy;
                    +
                      {3
 extremes  have  aiready  been  covered,  viz.,  pressurization  with  product  (see   ~  8 dz  + ({3A  - f3a)  dz  - O   (4.71)
 Secllon  4.4.1),  and  with  feed  (see  Sec!Jon  4.4.2).  These  were  assumed  to
         Integration reouires boundary conditions, and  a convenient  set 1s:  v  = u f  at
 begm  with  an  initial  condition  m which  the  bed  was  purged  with  the  oure
         z = L, and u = 0 at  z = 0. The result ts the expression that was simolv stated
 light component. When the bed  has not been completely purged, s1mu1atmg
         earlier m this chaoter:
 prc·ssurizatwn 1s slightly more complicated (see Sectton 4.4.3). All three cases
                                  -z        d  In  P
 represent  cyclic  steady-state  outcomes  of  operating  a  PSA  cycle  at  local   ( 4.6)
              v(P,y,z,t)  - f3a[I  + ({3- l)y]   dt
 equilibnum.  without  dispersive  effects.  A  slightly  more  comolex  s1tua!Jon
 occurs durmg startup, when  the gas used for purgmg (and possibly pressur-
         When Eqs. 4.6 and 4.69 are combined, the shock wave velocity may be found
 ization) 1s not pure. Other possible complications anse from mmor vanat10ns   from
 m operating procedures.  For example,  a oressure equalization step empioys
 the  gas  evolved  from  one  column {as  it  ctepressunzes)  for  pressurizing  a   -{3z   din!'   ( 4.72)
 parallel column. Such gas may have a slowly or suddenly varymg composition,   [1  + (/3  - l)y ](1 + (/3  - J)y ]   dt
                                1
                                               2
 due  to  uneven  rates  of  desorption,  poor  synchrontzat10n  of  the  valves,  or
            The dependence of  Y1  on  P,  and  that of  y on  z~  can  be  expressed  vm
                                                2
 contamination by  residual matenal in the connectmg fittmgs.
         Eqs. 4.7 and 4.8,  respectively.  By combining those with  Eq. 4.72,  the couoled
 Pressurization  at startup  or with  gas  having vanable composition  can  be   matenal balances can  be solved to get:
 regarded as fitting the following  possible scenanos: (1) Pressunzing with  gas
                       ay,
 that gradually becomes leaner m the heavy component, during which a shock   ( 4.73)
              Yz=  I  +(a~ l)y,
 wave cannot form,  or (2) pressunzmg with  gas that gradually becomes richer
 m  the  heavy  component,  dunng  which  a  shock  wave  may  form  if  the   where   a~ y (1  - Y )/lyw(l - y 211 )],  and  Yw  and  y  are  the  mitial
                            10
                      20
                                                          20
 composition  change is  suffic1entiy  large,  or (3)  oressunzmg  with  gas  that  is   compositions  at  the  leading  and  trailing  edges  of  the  shock  wave,  respec•
 significantly richer in  the heavy component than the mitial interstitial gas-,  for   tively.  Thus,  a  is  a  sort  of  select1v1ty,  analogous  to  relative  volatility  for
 which formation of a shocK wave 1s unavoidable. For s1mplic1ty, let us restnct   vapor-liouid equilibnum.
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