United States
                     Environmental Protection
                     Agency
Office of
Radiation Programs
Washington DC 20460
EPA 520/8-81-007
    1981
                     Radiation
vvEPA
                     Short- and Long-Term Leach Rates of
                     Solidified Waste from a
                     Cylindrical Container

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                                     EPA 520/8-81-007
Short- and Long-Term Leach Rates of Solidified
      Waste from a Cylindrical  Container
               Kerry A. Landman
                  June  1981
 Division of  Statistics and Applied Mathematics
         Office  of  Radiation Programs
      U.S. Environmental Protection Agency
            Washington, D.C.   20460

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                               ABSTRACT
     The shor£- and long-term leach rates of radionuclides for the
three-dimensional diffusive flow and for purely axial diffusive flow
from a finite cylinder of solidified waste are determined here.
These analytical results are compared with the ones obtained
numerically by Hung (Hu80) for purely axial flow.
                                   11

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                               CONTENTS




                                                           Page



1.  Purely axial flow
             «•
             *

     1.1  Introduction                                      1


     1.2  Solution to the model equation                    1


     1.3  Short-term leach rates                            3


     1.4  Long-term leach rates                             6


     1.5  Conclusions                                       6


     Appendix A                                             7




2.  Three-dimensional flow                               -   9


     2.1  Introduction                                      9



     2.2  Determination of the  leach rate                   9


     2.3  Short-term  leach rates                           13



     2.4  Long-term  leach rates                            15


     Appendix B                                           17




References                                                 23

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1.  PURELY AXIAL FLOW
              i
i.l  Introduction

     A common method for the disposal of radioactive waste is to
embed the radionuclides into a solid container.  However, these
particles can still escape from the container and thus be a hazard
to the environment.
              *

     The short- and long-term leach rates of radionuclides for the
oiffusive flow from a finite cylinder of solidified waste are
discussed here.  Their transport is governed by diffusion,
desorption, and radioactive decay, and is assumed to be  in one
direction only.  (For example, the system presented here models a
cylindrical container of length L, where all the faces, except for
one end, are  insulated).

     This same system was discussed by Hung  (HuSO).  The solution to
the basic differential equation with prescribed boundary conditions
was obtained  by numerical analysis.  However, the equation has a
fairly simple solution, which will be discussed below.  Comparisions
of these results will be made with those of  Hung, and also to the
solution for  a semi-infinite cylinder with  insulated sides.

1.2  Solution to the Model Equation

     The basic equation for the transport of radionuclides through
the porous medium  of the container  (which has been  immersed  in an
aqueous solution), where diffusion, desorption, and radioactive
decay are  present, is given by Hung  (Hu80)  as


                                 -  xdc  ,  0 <_  x < L ,                (1.1)


where c  is the  concentration  of radionuclides  (Ci/cm3)  in  the
aqueous  solution which  is saturating the waste solid, De is  the
effective  diffusivity  through the  solidified waste  (cti^/year),
e  is the  porosity, R  is the retardation factor defined  in  (HuSO),
and A(J  is  the decay  constant  for  the radionucl ide.

     The  initial and boundary conditions on  the container  are

     c(x,0)  = CQ              0 <  x  < L,                              (1.2)

     c(0,t)  =0               t  >  0,                                  (1.3)

                              t>0.                                 (1'4)

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Therefore, it is assumed that the equilibrium state of desorption
has been reached at time t=0, there is no accumulation of
radionuclides at the end x=0 and that the other end, x=L, is
insulated.

     Tne equation (1.1) with conditions (1.2)-(1.4) can be solved by
the standard techniques of separation of variables and the super-
position of normal modes (Hi76).  This gives

c(x,t)=   p_        ^       1   sin (2n+l),rx e                  ,  (1.5)
         »         n=0     2n+T        2L

where    K » De/eR.

     Now that the radionuclide concentration in the aqueous
solution, which saturates the solidified waste, is known, the rate
of  leaching l(t) can be obtained from

         l(tj=DeAr  _ac_  (0,t)         (Ci/year),                (1.6)



where Ar is the cross-sectional area of the solid (cm2).  It
is  often useful to determine the rate of leaching as a fraction of
the total  initial activity A0.  Here

     A0=eRC0ArL  ;                                                (1.7)

then from  (1.5)-(1.7), the rate of radionuclide leaching as  a
fraction of the initial activity per year is
            e  d
            e                                                        (1.8)
                    n=0
 Here  a  new  parameter,  the  leaching  number,  Lc, has  been
 defined:

                       C       e  R  L2

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     In order,to conform to Hung's notation, we introduce a
dimensionless time variable t', a dimensionless leaching parameter
1* and a leaching number Ln:
         f. =''°e    t   =   Lt  ,
                 A            C
                eRL2 1 =   I       ,                                (1.10)

               Ao De     Ao Lc
and       Ln = xd/Lc



     Substitution of (1.10) into (1.8) gives
                 i t-
                -Lnt
                          00                  2
                                             <-  «• i
              2e                e      '             .                (1.11)
In tne  following two sections we consider  approximations  to  1' for
t1 small and  for t1 sufficiently large  (near one or  greater).

1.3  Short-Time Leach Rates

     An estimate of the  dimensionless  leach rate 1',  given by  (1.11)
is now  required.  This involves making  an  asymptotic  approximation
to the  summation S,
                    00      _ On+i ^ 2 £i

                        e       '                                     (1.12)
                    n=0
 for  0 <  t'  «  1.   To  do  this,  compare  the summation  with  the

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                   area under the graph- of   e             for   0 <_ n £00 ; this is
                   illustrated in Figure 1.   Since
/
                                                    2
                                     oo      -  -nir-     t
                                           e              dn .  --  ,                (1.13)
                              .   -  u
                   we have, from consideration of Figure 1,  the two unequal ities
                       s < 4-  [ 1    +  e          ]  <   i   [_L  + i ]  ,            d-14)
                                \£~F'                     "  \£T'

                    and

                           S  >-L_   [ 1       -  1] ,                               d.15)


                    for all values of t' > 0.  Therefore for  0 <  t'  « 1


                           S~      *   .                                             (1.16)
                    Combining  the  result with equation (1.11), and assuming  that
                    Lnt'  «  1,  as  well as t1 « 1,
                                                                                       (1.17)
                         Hence,  we  conclude that the short-time (dimensionless)  leach
                    rate for the finite-dimensional geometry is the same as that for the
                    semi-infinite geometry (as shown in Appendix A).  This confirms the
                    results of Hung (in  his Figures 2 and 3).

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        01234567
Figure 1.  Graphs of e~(rbr/2^ t§   versus n  for t1 > 0

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1.4  Long-Time Leach Rates

     For sufficiently large values of (dimensionless)  time,  the
value of 1' can be approximated by the first term in  the  series:
             .  - [Ln +-L-?'
      I1 -. 2*e •       4       .                                     (1.18)
For intermediate values of time, then the first few terms of the
series expansion (1.11) will be sufficient to give a good
approximation to 1 ' .

     The values given by (1.18), for t1 near one, match well with
the values illustrated in Figure 3 by Hung, which were obtained by
numerically solving the set of difference equations associated with
equation (1.1).

1.5  Conclusions

     The leach rates for the finite-dimensional model system can be
well approximated by the simple formulas:


        1'  -    1        for t' « 1 ,                              (1.19)
and
              2 e                    for t1 sufficiently            (1.20)
                                            large,
 for  the  dimensionless variables  1' and t'.  These results match well
 with  those  of Hung, which were carried out more expensively by using
 the  computer to  solve the basic  equation.

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                                  7

                             APPENDIX  A
     Tne analagous problem to  the  one  discussed  in  Section 2, but
for   0 < x <» is
         ac   =   a c   - x CH  ,
         	      —7        °
         at  '    ax
              c(x,0) = CQ       x > 0 ,                 .             (A.I)

              c(0,t) =0        t > 0 ,


where     * = De/eR.  This has an exact  solution

                  -A t
    c(x,t) =CQ e        erf(   x           ,                        (A.2)
where erf(y) is the well-known error function
                        2
erf(y) =  2         e~      du   .                       (A. 3)
                             f
                             /     ~ u
     Then the leach rate from the face x=0 is just
                                          -x t
            r.  _3C (0,t>    =  OeArCQ    e      .                   (A.4)

                ax

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                                  8
Using the notation of Section 1.2,  this gives





      I1  =  1      =     e    n     .              '                 (A. 5)
For small t1 ^nd Lnt', this may be approximated as





     I1  =        .                                                 (A. 6)

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2.  THREE-DIMENSIONAL FLOW

2.1  Introduction

     Numerous studies have been made to determine the leach rates of
radionuclides from solid waste.  However, the results obtained so
far are of limited use in practical applications because the basic
assumptions are often not physically acceptable.

     For modelling purposes, it is usually assumed that the flow out
of the solidified waste is in one direction only.  Both the
semi-infinite (Go74) and finite-dimensional (Hu80) models, with
uni-directional flow, have been studied.  However, these geometries
are too simplistic to give reliable results..  A real canister is
usually cylindrical and it cannot be assumed that all of its
exterior surfaces, except for one end face, are insulated.  In fact,
there will be a flux out of all the three faces of the cylinder,
giving rise to a three-dimensional flow.

     This paper addresses the problem of short- and  long-time leach
rates out of a cylinder, where the radionuclides can escape out of
all the sides.  Some of the results will be compared with Hung's
(Hu80).  He used a "sealing-effect" relationship, without adequate
justification, to approximate the three-dimensional  flow from a
cylinder with the one-dimensional flow.  However, we will show that
his results are not necessarily accurate.

     The other assumptions often made are that  the chemical and
physical characteristics of the solidified waste stay the same over
long time periods.  This may also be simplistic.

2.2  Determination of the Leach Rate

     The basic equation for the transport of radionuclides  through
the porous medium of  the container  (which has been immersed in an
aqueous solution), where diffusion, desorption, and  radioactive
decay are present,  is given by Hung (Hu80).  For a cylindrical
geometry, with axial  symmetry, this is  most conveniently  given  in
cylindrical co-ordinates:
    3C.      Un      A    O     _  0V.     j.    O   t        ,  _                (?  \\
    __     __

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                                  10

where r and z are the radial and axial co-ordvicites, respectively.
Here c is the concentration of radionuclides in the aqueous solution
which saturates the solid waste, De is the effective diffusivity,
c is the porosity, R is the retardation factor defined in (Hu80),
and xa is the decay constant for the radionuclide.

     The initial and boundary conditions for the container are:
             r
             •
     c = CQ     't = 0, 0 £ r < a, 0 < z < L,                       (2.2)


     c » 0       z = 0, z = L, 0 < r < a, t > 0,                    (2.3)


     c = 0       r = a, 0 < z < L, t  > 0.                           (2.4).
     Therefore, it  is assumed that the equilibrium state of
desorption has been reached at time t = 0 and that there is no
accumulation of radionucl ides on the exterior surfaces of the
container.

     The equation  (2.1) with boundary conditions  (2.3) - (2.4) can
be solved by the standard techniques of separation of variables and
the superposition  of normal modes as


                   00    00                              •   •
c(r.z.t)  . e        ^    -  BmnJ0  (umr)sin  n*z e  -~r           ,  (2.5)
                  m=l  n= 1                  L


where  K= De/eR.  The  yma are  the set of positive  zeros of  J0(x)
and  the  Bmn  are  constants which are  determined by  the  initial
condition (2.2)  as
  .
   mn   ^
 r a               r  l
 I      i"J,,(u r) dr I     sin nnz dz
•b                 4         T"

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                                  11

LHere the orthogonality relations for the J0(ymr) and
sin nitz functions are used (Hi76)].  Evaluation of the integrals gives
     L
                                                                    (2.7)
   Bmn
            •  0                 n even

Substitution of (2.7) into (2.5) then gives the solution as
                          00
 c(r,z,t) =^o_e  u    /_^i    VV '   sin n,z e    u   "'        (2.8)
            wa          m,n=l  np J-, (y a)      L
                        n odd

     Now  that the radionuclide concentration is known, the rate of
leaching  l(t) can be obtained.  Since the flux of radionuelides,, ^3  ,
is given  by                                                      "*

      0   = - Dg grad c » -Oe( ac r + ^c z)    ,                     (2.9)
      ^                       3 P      U 7
                              0 I       O fc

the concentration of radionuclides which passes out of the cylinder per
unit time is

     l(t) = -//  J . n  dS            ,                            (2.10)
where n  is  the unit normal  of  the surface  in  the outward direction
ana  the  integral  is taken  over the whole surface.  Therefore,  the
integral  in (2.10) has  three parts - one corresponding to  the  end

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                                  12

face z = 0, a similar one for z = L, and one for the surface r
writing this out more fully we must evaluate

       0   D
                                r dr de
                         z=0
             .2*  /.a
                        0  3£
                           3Z
                                    r dr de
                                z=L
(2.11)
              .2w
                          0   ac
                           e  3?
                                    a dz de
                                 r=a
     From equation  (2.8),  it  is  easily verified  that

                           00
l(t)  =32
        L
                                             i       r/*\   .    -I  .

                                             —e   T     m
                         m,n=l
                         n odd
It  is often  useful  to  determine  the  rate  of leaching as a fraction
of  tne  total  initial activity  A0.  Here

 •A0 = cRCQira2  L   ,
                                                                   (2.13)
so  that
                         00
  ill)
  A_
                                                      ,2 A  2
                     m,n=l    /nit \
                     n odd    ( l'
                                                               .    (2.14)
      In  the  following two sections  we consider approximations to
 l(t)/A0  for  small  and long periods  of time and compare our results
 to Hurig's  for  a  particular example  he discusses.

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                                  13

2.3  Short-Time Leach Rates

     An estimate of the rate of radionuclide  leaching  as  a  fraction
of the initial activity, given by equation  (2.14)  is now  required.
This involves making an asymptotic approximation to the double
summation

             00
    S  .   .                  *         e-T            •           (2.15)
           •n.n-1       (n.)    '  „.
           n oda       v LJ

for t sufficiently  small.   With  some  manipulation  this may be rewritten as

                    2
        oo       nir,  rt   oo             2   ..
       n=l  x
       n odd
                           00
         00
        —,                 .
        111=1                n odd
 It  is  convenient  to  define two dimensionless time scales
   T = ict     and     T = Kt                .                           (2.17)
      7                7
      In Appendix B, the asymptotic forms of each of the series in
 equation  (2.16)  is determined for small values of T and T.  The results
 there  give
                                      L2  ,  T, T«l
                                     •^^M

                                      8                              (2.18)
S


- 1 .
4V7T
- _1 	 r
leViT
a2.
4
£
Vf
+ 1
2v
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                                  14

     Therefore, for small values of Kt/1.2,  Kt/a2 and x^t, the
rate of leaching as a fraction of the initial activity is
     This asymptotic form shows that the rate of leaching for the
three-dimensional flow from a cylinder is made up of two
contributions — one that would occur from the purely radial flow and
tne other from the purely axial flow.

     Indeed, since the radius a of a canister used for disposal
purposes is usually smaller than the length L, choosing a time t
such tnat ict/a2 « l shows us that the dominant contribution to
the leach rate is from the radial flow.

     This shows that the one-dimensional axial flow from a cylinder
will not accurately determine the short time leach rates from a
cylinder, since the radial flow will usually contribute a larger
amount .

     If  T and T are small, but the decay constant is large enough so
that xdt is no longer small, then the fractional leach rate  is
               "Xd
   lill -   2  e           r   1    +  1 1                              (2.20)
    AQ         •    >»t    L   a       L J

 and the above  remarks remain valid.  In  fact, the  example  presented
 by Hung (Hu80) for  the  predicted leach rate at  time t =  100 years  is
 really  a problem of determining the short-term  leach rate  for  the
 three-dimensional  flow  described here.   The parameters are as
 follows:  the  number <  ,  which measures  the physical and chemical
 properties  of  the radionuclides in the solidified  waste  medium,  can

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                                  15

oe determined from the leaching constant for the 5-cm long test
piece, so that

     K = 3.74 x 10-6 x (5)2 = 9.35 x 10~5 cm2/day.                  (2.21)

Also
          xd = 6.33 x 10~b/day

          a  '• s 30 cm

          L .   = 90 cm                                              (2.22)

          t    =3.65 x 104 day.


Therefore


   T = *t  . 3.79 x 10"3  > Kt                                       (2.23)
                           ""
hence both  the dimensionless time scales  r and T are small.  However,

          xdt . 2.31,                                                (2.24)

so  that  the short term  leach rate as given by equation (2.20) applies.  This
gives


          l(t)  = 2.51 x 10"7/day;                                    (2.25)

          o

so  that,  for  this particular choice of  the parameters, the  predicted
fractional  leach rate has  the  same order  of magnitude as  that
obtained by Hung  (his equation (32)), with the use of his scaling
effect  argument.  However,  this will not  always be true,  the
relative size of  the parameters  is  important.

2.4  Long-Term Leach Rates

      For sufficiently large values of the dimensionless  time
variable 
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                                  16
wnere £j  = 2.405 is the first positive zero of J0(x).  For
intermediate values of (dimensionless) time, the first few terms of the
series expansion (2.14) will be sufficient to give a good approximation
to 1/A0.                                    /

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                                  17

                              APPENDIX B
i.  Consider the purely axial flow from a cylinder, radius a  and
length L.  Suppose u(z,t) satisfies


   u  =   au             0<*< L  -,
             '•   .                                                    (B.I)
  u(*.0) = 'UQ             0 < * < L   ,

  u(0,t) = u(L,t)= 0         t > 0    .
The solution to this problem, when obtained  by  separation  of variables
and superposition of the  normal modes,  is

                  oo                   ,nn»2 0  ,
    •j            ~"~L                    1^
   rlo.^            K
   **                           ,                                     (B.4)

    u  =  0 ,  * = 0,L

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                                  18


The solution to (B.4) is



       U   r,    sinhqz + sinhq(L-fr)
 u  ~  —  *•     ~    sinhqL


 Then,



   1 uj   •   ~  -    1  u.

                     *o


           -  *  i  coshqL-1
             K q  *•  sinhqL
              L
              q
                                   -I
                                      QC

                                                                     (B.6)
           • JL ri + 2     ,             ,    .
             K q   L        n=l             J


Taking  the  inverse  transform  of  these  standard  Laplace  transform
functions (Ab72)  gives

                                                 n2!2
                                      oo       - n  L
 i|     =_i£l     -   °  [1 * 2
3*  -feO     a* I *=L  A i — r        n=l
                                     22
                         A i — r
                         VlT
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                                  19

     Similarly,  from (B.2)  we  can  evaluate  the  average concentration in
tne cylinder as  a function  of  time:
     -ij    U(*.t)d»  =  f!^_  2J  i
                                   _  e   u           .         (B.10)

                             n=l
                             n odd
But from (B.5) and then (B.6),


     -if    ~(-t  )  d* - Uo fl   — fcosncll—1\
   v = -j- /      *  '"'     ~ — "•    Lq *  sinhqL
         0                  P
                                             oo
                                                               .     (B.ll)
Taking the inverse transform gives


                                00

  v = u  - 4Ufl,<.t,1/2MT-1/2 + 2  Z(-Dn  ierfc   n	 -,       .        (B.12)
Again comparison of (B.10) with-the above  equation  gives,  for small values
of r ,

      oo               o ?
                   a-nSr     2        .                           (B.13)
E
         1    e"
         ri
n odd
2.  Consider the purely radial  flow from a cylinder  of  radius  a  and  length
L.  Suppose u(r,t) satisfies
  —  ~ K L  L- (r —1       0 < r < a  ,
  at      r  ar »  ar'
                                                                    (8.14)
  u(r,0) = UQ                0 <_ r < a- ,

  u(a,t) =0                 t > 0  .

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                                 20
The solution to this  problem, using the separation of variable technique,

is
                 00
                                    2 Kt
  u(r,t) = 2UQ   ]T

                m=l
                                                                   (B.15)
wnere J0(O=Q» O 0.   Then,
                 00
                           7
                                                                   (B.16)
                m=l
However, the series in (B.15)  and  (8.16) converge very slowly for

small values of Kt/a2.  The Laplace  transform method is better for

this case; then (B.14) becomes:
 2-
d u

               -      2-
           1   du  -  q u

           r   dr
                              U
    us  0,     r=a


The solution to (B.17) is
                                                                   (B.17)
                                                                   (B.18)
Therefore,

            •   a  |i.
         r=a    p  y^

Using the expansion of  I  (x)  for  large values of x,
                                                                   (B.19)
  Iu(x) .  ex fl -  4v2-l
   »      r^ir L     1 I  U
                             (4v2-l)(4v2-32)
                                   ^7
                             2: (ax) *
                                                                (B.20)

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                                  21
equation (B.19) becomes
r=a
= q
p
[i
L1
o
~ ql -
+ 1 +
Sqa
I28q2a2 +
9 +
...j
...-,
Taking the inverse transform (Ab72), gives
   ar
      r=a
Hence,
                                     a
                                                                    (B.21)
                                                                     (8.22)
Compare this with (8.16); we see that for small values of ict/a2
following asymptotic approximation is valid:
     oo
              m
  (B.23)


T, the



  (B.24)
     Similarly,  from  (B.15) we  can evaluate  the  average  concentration  in  the
cylinder as a function of time:
                ru(r,t)dr  = 4 UQ ^  _1_

                                  m=l   *r
                                              -   —o
                                             e   m  a2
  (B.25)
But  from  (B.18) we  also  have

             a
v = 2
    7
                 rdr  =
                                  ai  I0(
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                                  22
Using equations (B.19) and (6.20), this has the expansion
                 2U°
                 apq
                           -     —
                           2qa  8q2fl2
Taking the .inverse transform, the average concentration is




   v  =  UQ-U

                "' ad vS"  \a'        a-


Compare this with (B.25); we see that for small values of
  m=l
            m
(B.27)
                                                                    (B.28)
                                                                     (B.29)

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                                  23
                              REFERENCES
Ab72  Abramowitz, M. and Stegun, I.A.,  Handbook  of Mathematical
  Functions wjth Formulas,  Graphs,  and  Mathematical  Tables,
  National .bureau of Standards, Applied Mathematics  Series 55, 1972.

Go74  Goodbee, H.W. and Joy D.C.,  Assessment of  the  loss  of  radio-
  active isotopes from waste solids to  the environment.   Part I:
  Background and theory.  Oak Ridge National Laboratory,  ORNL-TM-
  4333, 1974.

Hi76  Hildebrand, F.B.,  Advanced Calculus for Applications,
  Prentice Hall, Inc., 1976.

Hu80  Hung, C.Y., Prediction of long-term Teachability of a
  solidified radioactive waste from a short-term Teachability
  test by  a similitude  law for leaching systems.  U. S.  Environ-
  mental Protection Agency, Office ofRadiation Programs,  Washington,
  D.C. 20460, 1980.

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TECHNICAL REPORT DATA
(Please read Instructions on the reverse before completing)
1. REPORT NO. ' 2.
EPA 520/8-81-007
4. TITLE AND SUBTITLE
Short- and Long-Term Leach Rates of Solidified
Waste from a Cylindrical Container
7. AUTHOR(S)
Kerry Landman
9. PERFORMING ORGANIZATION NAME.ANO ADDRESS
Office of Radiation Programs
Environmental Protection Agency
Washington, D.C. 20460
12. SPONSORING AGENCY NAME AND ADDRESS
Same
3. RECIPIENT'S ACCESSION NO.
5. REPORT DATE
June 1981
6. PERFORMING ORGANIZATION CODE
8. PERFORMING ORGANIZATION REPORT NO
10, PROGRAM ELEMENT NO.
11. CONTRACT/GRANT NO.
13. TYPE OF REPORT AND PERIOD COVERED
14. SPONSORING AGENCY CODE
15. SUPPLEMENTARY NOTES
16. ABSTRACT
       The short- and long-term  leach rates of radionuclides for  the
  three-dimensional diffusive  flow and for purely axial diffusive flow
  from a finite cylinder of  solidified waste are determined here.
  These analytical results are compared with the ones obtained
  numerically by Hung for purely axial flow.
17. KEY WORDS AND DOCUMENT ANALYSIS
a. DESCRIPTORS
radionuc i ides
axial flow
three-dimensional flow
leach rates
18. DISTRIBUTION STATEMENT
b.lOENTIFIERS/OPEN ENDED TERMS

19. SECURITY CLASS I This Report/
Unclassified
20. SECURITY CLASS iTMs page/
Unclassified
c. COSATI Field/Group

21. NO. OF PAGES
26
22. PRICE
SPA form 2224—1 
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