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A
ORNL-3494 L.
UC-4 — Chemistry '\
TID-4500 (23rd ed.)
AN EXPERIMENTAL STUDY OF SORPTION OF
URANIUM HEXAFLUORIDE BY SODIUM
FLUORIDE PELLETS AND A MATHEMATICAL
ANALYSIS OF DIFFUSION WITH
SIMULTANEOQOUS REACTION
L. E. McNeese
OAK RIDGE NATIONAL LABORATORY
operated by
UNION CARBIDE CORPORATION
for the
U.5. ATOMIC ENERGY COMMISSION
——
e —— e
LEGAL NOTICE
This report was prepared os on cccount of Government sponsored work. Meither the United States,
ner the Commission, nor ony person acting on behalf of the Commission:
A. Mockes any warranty or ropresentation, expressed or implied, with respect to the sccwrocy,
completeness, or usefulness of the information contained in this report, or thot the use of
any informotion, opparatus, method, or process disclosed in this repert may not iniringe
privately owned rights; ar :
B. Assumes any lichilities with respect to the use of, or for damages resulting from the use of
any information, apparatus, method, or process disclosed in this report.
As used in the obove, "“‘person acting on behalf of the Commission"™ includes any employee or
controctor of the Commission, or employee of such centractor, to the extant that such employee
or contractor of the Commission, or employee of such controctor prepores, disseminotes, or
provides occess to, any information pursuont to his employment or contract with the Commissian,
or his employment with such contraetor.
y ¥
ORNL-349
Contract No. W-TLO5-eng-26
CHEMICAL TECHNOLOGY DIVISION
Unit Operations Section
AN EXPERIMENTAL STUDY OF SORPTION OF URANIUM HEXAFLUORIDE
BY SODIUM FLUORIDE PELLETS AND A MATHEMATICAL ANALYSIS
OF DIFFUSION WITH SIMULTANEOUS REACTION
L. E. McNeese
This report was prepared as a thesis and submitted to the Faculty of ,
the Graduate School of The University of Tennessee in partial fulfillment
of the degree of Master of Science in the Department of Chemical Engineering.
Date Issued
NOV 14 1363
OAK RIDGE NATIONAL LABORATORY
Oak Ridge, Tennessee
operated by
UNION CARBIDE CORPORATION
for the
U. S. Atomic Energy Commission
-t
ii
ACKNOWLEDGEMENT
The writer wishes to acknowledge the numerous helpful suggestions
of Dr. S. H. Jury of the Chemical Engineering Department of the
University of Tennessee and Dr. M. E. Whatley of the Chemical Technology
Division of the Oak Ridge National Laboratory.
Analyses of the sodium fluoride peilets and of the uranium .
hexafluoride-sodium fluoride complex were performed by members of the
Analytical Chemistry Division of Oak Ridge National Laboratory. The
porosimetry work on sodium fluoride pellets was done by P. G. Dake and
co-workers of the Special Analytical Service Group of the Oak Ridge
Gaseous Diffusion Plant. The measurements of the uranium concentration
profile for partially reacted pellets were done by H. W. Dunn of the
Analytical Chemistry Division of Oak Ridge National Laboratory. The
co-operation and care of these individuals is greatly appreciated.
The close attention to experimental detail and Fhe fine work of
J. Beams of the Chemical Technology Division of Oak Ridge National
Laboratory during the experimental phase of this study is appreciated.
This work was performed in conjunction with the Fluoride
Volatil?ty Process of the Chemical Technology Division, Oak Ridge
National Laboratory. The writer is grateful for the interest of
F. L. Culler, Jr., Division Director, M. E. Whatley, Section Chief, and
R. W. Horton, Group Leader, whose support made this work possible.
‘-
4
iid
ABSTRACT
The rembval of uranium hexafluofide frdm a gas stream containing
uranium hexafluoride and nitrogen by a single layer of sodium fluoride
pellets was investigated. Experimental data on the rate and extent of
sorption were obtained in the temperature range 29 to 100 degrees cen-
tigrade and uranium hexafluoride concentration range 0.57 to 10.9 mole
per cent uranium hexafluoride.
The results of this study indicate that the rate controlling
mechanisms are: transfer of uranium hexafluoride across a stagnant gas
film surrounding the pellet, diffusion of gaseous uranium hexafluoride
in the pores of the pellet, and diffusion of uranium hexafluoride
through a layer of uranium hexafluoride-sodium fluoride complex covering
the unreacted sodium fluoride in the interior of the pellet. The
crystalline density of the complex, UF6-2NaF, was determined to be
4,13 grams per cubic centimeter which indicates that incomplete reaction
of the sodium fluoride will occur for pellets in which the initial
volume void fraction is less than 0.807.
A useful model was devised to represent the sorption of uranium
hexafluoride by a single pellet of sodium fluoride, and differential
equations based on the model were written. A general method of solution
of the partial differential equation describing simultaneous diffusion
and irreversible reaction with variable diffusivity and reaction rate
constant was derived for systems in which a steady-state type of
solution is valid. The experimental data were correlated on the basis
of the model with a root-mean-square error of 9.5 per cent for all
'
iv
points. The resulting computer code and associated data may be used
for design of sorber systems such as fixed and moving beds.
&
v
TABLE OF CONTENTS
CHAPTER \ PAGE
I. INTRODUCTION. « ¢ ¢ ¢ & o o 4 o o o o o o o o o o s o s o & 1
IT. REVIEW OF THE LITERATURE. . . ¢ « « o « + v ¢ & « + e o o 3
Uranium Hexafluoride-Sodium Fluoride System . . . . . . . 3
Uptake of Gases by Solids « « ¢« + ¢« v ¢ v 4 ¢ 4 ¢ o =« » « 6
Diffusion of Gases Through Porous Solids. . . . . . . . . 10
? Simultaneous Diffusion and Irreversible Reaction. . . . . 12
Mass Transfer to the External Surface of the Pellet . . . 15
IIT. MATHEMATICAL MODEL«. + + &« ¢ &« & & « o o o o o o o « + + » + 19
IV. METHOD OF SOLUTION OF SIMULTANEOUS DIFFUSION AND REACTION
EQUATION + ¢ ¢ = o « « & o « o o o o o o o o o o o o « « o 32
V. MATERIALS AND EQUIPMENT + «. « « o s ¢ ¢ o s s s o o o« « » o« ho
MAteridals « « o v o« v s o o o o o o o o o s s e o o o+ . ko
EQUIPmMENnt « « v o o 4 o ¢ 4 4 4 o 4 4 v s e e e e e e .. ke
VI. EXPERTMENTAL PROCEDURE. « « « + « v « v o v v v v v v v .. L5
‘ Differentiai-Bed Studies. + + + &+ 4 4 4 4 4 s s s . . . . b5
: Determination of Density of Complex . . . . . . . . . . . LT
VII. EXPERIMENTAL RESULTS. . « + « &« ¢ o ¢« o « 4 o + & +» « « « . ko
Differential-Bed Studies. . . « +« ¢« « v & & « + o + « « . U9
Examination of Partially Reacted Pellets. . . . . . . . . 56
Density of Complex. . . . . . . . « . « . « . . . . . . . 59
VIII. ANALYSIS AND DISCUSSION OF RESULTS. + « « v + o « o « o « . 65
Diffefential-Bed Data + « + + o o 4 e 4 v s e 4 s e 4 e . B5
Application of Data to Sorber Design. . « . « . « + « « . T8
CHAPTER
Vi
Discussion of EXror . ¢ ¢ ¢ ¢ ¢ o o o o o o o o s o s
IX. CONCLUSIONS AND RECOMMENDATIONS . -« « « « « & & « o« « o &
Conclusions .« + « ¢ ¢ ¢ ¢ 4 ¢ v & 4 o s o ¢ & o o o o o
Recommendations . « « &+ « ¢« ¢ ¢ ¢ ¢ o & o « o o o o+
LIST OF REFERENCES. . . « ¢ & ¢ ¢« ¢« & o & o s o o o o o &
APPENDICES
A. Temperature of Pellet During Sorption . . . . . . .
B. Viscosity of Uranium Hexafluoride-Nitrogen Mixtures
C. Bulk Diffusivity of Uranium Hexafluoride. . . . . .
D. Mean Free Path of Uranium Hexafluoride in Mixtures
of Uranium Hexafluoride and Nitrogen. . . . . . .
E. Properties of the Sodium Fluoride Pellets . . .
F. Confiergence Characteristics of Numerical Method . .
G. Heat Transfer-Characteristics of Differential-Bed
and Gas Preheater . . « « « « ¢ ¢ v ¢ ¢« s o o o
H. Computer Code . . + . + « « - v v v v v v v 0 o b
I. Original Data . . . . . . e c e e s e e e
LIST OF SYMBOLS « + ¢ ¢ ¢ ¢ « o o &+ 4 o s o o o & s o s
- PAGE
80
81
81
82
8k
91
95
101
104
108
11k
116
121
122
.
v
n)
o
=of
TABLE
IT.
III.
IvV.
VI.
VII.
VIII.
IX.
Experimental Results
with 2.62 Mole Per
Experimental Results
with 2.35 Mole Per
Experimental Results
with 0.57 Mole Per
Experimental Results
with 2.45 Mole Per
Experimental Results
with 8.51 Mole Per
Experimental Results
vii
LIST OF TABLES
from
Cent
from
Cent
from
Cent
from
Cent
from
Cent
from
Differential-Bed Runs
Uranium Hexafluoride.
Differential-Bed Runs
Uranium Hexafluoride.
Differential-Bed Runs
Uranium Hexafluoride.
Differential-Bed Runs
Uranium Hexafluoride.
Differential-Bed Runs
Uranium Hexafluoride.
Differential-Bed Runs
PAGE
at 29°C
c e e e .. 50
at 50°C
at 100°C
e e e 4« . 53
at 100°C
c o« s« e 54
Showing
Variation of Effective Capacity for Uranium Hexafluoride
with Temperature.
&« e s« .« 55
Weight Gain and Exposure Data for Preparation of Uranium
Hexafluoride-Sodium Fluoride Complex at 100°C . . . . . . 62
Uranium Content of Samples of the Complex Before and After
Exposure to Toluene . .
e e e oos Bh
Viscosity of Uranium Hexafluoride-Nitrogen Mixtures in the
Temperature ‘Range 29 to 100°C and Uranium Hexafluoride
Concentration Range 0.57 to 8.5 Mole Per Cent at One
Atmosphere. . . .
- X
TABLE
x.
XI.
. XII.
viii
Diffusivity of Uranium Hexafluoride in Mixtures of Uranium
Hexafluoride and Nitrogen at Atmospheric Pressure in the
Temperature Range 29 to 100°C .. « . . . . .
PAGE
. 100
Mean Free Path of Uranium Hexafluoride in Uranium Hexafluoride-
Nitrogen Mixtures in the Temperature Range 29 to 100°C
and Composition Range 0.5 to 8.5 Mole Per Cent Uranium
Hexafluoride at Atmospheric Pressure.
Composition of Sodium Fluoride Pellets Before and After
Fluorination at 400°C for One Hour.
. 103
. 105
&
FIGURE
a)
10.
ix
LIST OF FIGURES
PAGE
Spherical Shell Used in Derivation of Diffusion Equation
for Variable Reaction Rate, Diffuéivity, and Volume
Void Fraction. . . . ; =
Crystalline and Broken Layers»of Complex vaering
Unreacted Sodium FIUOTide. « « o o o « o v o o o 0 v o 28
Typical One-eighth-inch Right Circular Cylindrical Sodium
Fluoride Pellets « « v ¢ & ¢ ¢ o v o o o o o« o o & + « « k41
Flow Diagram for Equipment Used in the Study of Sorption
of Uranium Hexafluoride by Sodium Fluoride . . . . . . . L3
Sorption Vessel Used in Differential-Bed Studies. . . . . . L6
Axially-Sectioned Sodium Fluoride Pellets Containing
Uranium Hexafluoride Sorbed at 50°C. « . « + « « « + « .+ 57
Axially-Sectioned Sodium Fluoride Pellets Containing
‘ Uranium Hexafluoride Sorbed at 100°C . . . . . . . . . . 58
Typical Solid-Phase Uranium Hexafluoriae Concentration
Profile for Pellets Reacted at 100°C . . . . . . . . . . 60
Comparison of Experimental and Model-Predicted Data Showing
| Variation of Pellet Loading with Time at 100°C and 0.57
.Mble Per Cent Uranium Hexafluoride . . . . . . . . . . . 70O
Comparison of Experimental and Model-Predicted Data Showing
>Variation of Pellet Loading With Tifie at 100°C and 2.45
Mole Per Cent Uranium Hexafluoride . « . ¢« . . . + . « « T1
FIGURE PAGE
11. Comparison of Experimental and Model-Predicted Data Showing
Variation of Pellet Loading wifh Tifie at 100°C and 8.51
Mole Per Cent Uranium Hexafluoride. . . . . . . . . . . . 72
12. Comparison of Experimental and Model-Predicted Data Showing
Variation of Pellet Loading with Time at 50°C and 2.35
Mole Per Cent Uranium Hexafluoride . . . . . . . . . . . 73
13. Comparison of Experimental and Model-Predicted Data Showing
Variation of Pellet Loading with Time at 29°C and 2.62
Mole Per Cent Uranium Hexafluoride. + + « « ¢ ¢« « « « « « Th
1k. Comparison of Experimentally Determined and Model-Predicted
Results on Variation of Effective Pellet Capacity with
Temperature o« + + « o o o s o o o « s o s 2 o« o« o o « « « 5
15. Calculated Values of Effective Pellet Capacity for Pellets
having an Initial Void Fraction of 0.45 Showing Effect
of Pellet Surface Area. . . . « . « . . . + ¢« + . o« . TT
16. Calculated Values of Effective Pellgt Capacity for Pellets
having an Initial Void Fraction of 0.45 and a Surface
Area of 0.86 Square Meter per Gram. . + « « o« & RN
17. Time Variation of Temperature Difference Between Pellet
Surface and Gas Stream. .« « « « + + =« + 4+ ¢« s « o + « « . Oh
18. Porogram of Sodium Fluoride Pellets Treated with Fluorine
for One Hour at 4O0°C +« ¢ ¢« + & o ¢ &+ « « o o« o« « « « « 2107
19. Variation of Convergence Ratio with Number of Shells and
Dimensionless Parameter © « « « « « « « + « + + + o« » .« 113
1
CHAPTER I
INTRODUCTION
The study reported here concerns the determination of the rate
controlling mechanisms for the removal of uranium hexafluoride from
flowing streams of uranium hexafluoride in nitrogen by cylindrical
pellets (one-eighth-inch right circular) of sodium fluoride.
Uranium hexafluoride reacts reversibly with sodium fluoride to
form a solid complex. The reversible character of the reaction makes
it attractive as a means for separating uranium hexafluoride from other
gases and/or as an alternative to low-temperature cold trapping for
collecting uranium hexafluoride.
An important application of the uranium hexafluoride-sodium
fluoride system is in the Oak Ridge National Laboratory's Fluoride
Volatility Process for recovery of uranium from irradiated nuclear
fuels.lLE During the final step of the process, a molten fluoride salt
containing dissolved uranium tetrafluoride and fluorides of fission
products and corrosion products is contacted with gaseéus elemental
fluorine at 500 to 600°C (degrees centigrade). The gas stream leaving
the fluorinator consists of a mixture of uranium hexaflfioride, unreacted
fluorine; fission product fluorides, and corrosion product fluorides.
Differences in the decomposition pressures of the fluorides that form
sodium fluoride complexes are exploited during alternate sorption and
desorption of the uranium hexafluoride in fixed beds of sodium fluoride
to produce a uranium hexafluoride product of high purity.
2
Information on the effects of various system parameters on the
rate of.sorption is needed so that sodium fluoride sorbers may be
designed for a wide range of operating conditions..
In this study, a determination was made of the rate-controlling
steps in the sorption of uranium hexafluoride from a stream of uranium
hexafluoride and nitrogen by sodium fluoride in the form of one-eighth-
inch right circular cylindrical pellets at atmospheric pressure. The
temperature range covered was 29 to 100°C; the uranium hexafluoride
concentration range was 0.57 to 10.9 mole per cent.
5
CHAPTER II
REVIEW OF THE LITERATURE
The removal of uranium hexafluoride from a flowing stream of
uranium hexafluoride in nitrogen by sodium fluoride pellets is believed
to involve some or all of the following processes.
w)
1.
- 5.
Transfer of uranium hexafluoride from the gas stream to the
external surface of the pellet.
Transfer of uranium hexafluoride from the external surface of
the pellet to the interior of the pellet by diffusion of
gaseous uranium hexafluoride in the pores of the pellet.
Adsorption of uranium hexafluoride on the internal surface
of the pellet.
Diffusion of adsorbed uranium hexafluoride or gaseous uranium
hexafluoride from the internal surface of the pellet through
a layer of uranium hexafluoride-sodium fluoride complex to
underlying sodium fluoride.
Reaction of ufanium hexafluoride with sodium fluoride.
A discussion of the pertinent information from the literature is given
below.
Uranium Hexafluoride-Sodium Fluoride System
The reaction of uranium hexafluoride with sodium fluoride was
noted first by Ruff and Heinzelman in 1911.
>0 Grosse in 19&126 reported
that hydrogen fluoride was necessary for the reaction, which resulted
4
in the formation of a ternary complex. Subsequent study of the complex
formed in the temperature range 30 to 100°C Ey Martin et al. in 195157
showed the composition UF6-5NaF and indicated decomposition of theA
complex at 450°C yielding uranium hexafluoride and fluorine. It was
also concluded that the presence of hydrogen fluoride is not necessary
for obtaining a reaction between uranium hexafluoride and sodium
fluoride.
Cathers et al. in 195712 studied the formation and decomposition
reactions of the complex and concluded that the reaction involved an
equilibrium between gaseous uranium hexafluoride, solid sodium fluoride,
and the solid complex which was given the formula UF6-3NaF although it
was noted that some preparations had a composition nearer to 2UF6'5NaF.
The decomposition pressure of the complex was measured in the tempera-
ture range 80 to 360°C and conformed to the equation
log10 p = 10.88 -~ 5.09 x 103/T ) (2)
where
p = decomposition pressure in millimeters mercury,
T = temperature in degrees Kelvin.
Use of the Clausius-Clapeyron relation with the decomposition pressure
relation yielded the heat of sorption for the complex: -23.2 kilocal-
ories per mole. A study was made of the rate of decomposition by two
alternative reactions reported by Martin et al., the first of which was
found to yield fluorine and a white complex in which uranium had the
valence of plus five, and a subsequent reaction which was found to yield
7
>
a green complex in which uranium had the valence of plus four, the
result of the liberation of additional fluorine. Based on the rate
constant for the first decomposition reaction, these reactions can be
neglected in the present study in which the temperature range is below
100°C.
Worthington 'in 195763 studied the rate of reaction between pure
gaseous uranium hexafluoride (at a pressure of fifty-six millimeters of
mercury ) and finely divided sodium fluoride in the temperature range
80 to 150°C. No estimates of particle size or surface area were given.
At a given temperature, the reaction followed the logarithmic rate law.
The final composition contained slightly fiore uranium than would corre-
spond to the fofmula UF6-3NaF. The average rate increased with tempera-
ture up to 130°C, after which a marked decrease was observed. In view
of the e#perimental method used (admission of uranium hexafluoride to
an evacuated chamber contéining a thin layer of sodium fluoride), the
temperature control of the sample was undoubtedly poor in the early
stages of sorption; it is believed that this is the origin of the
decrease in average reaction rate above 130°C.
The rate of reaction between pure uranium hexafluoride at ninety
millimeters mercury pressure and sodium fluoride in the form of powder,
crushed pellets, and pellets was investigated by Massoth et al. in
195859 in the temperature range 24 to 68°C. The reaction with powder
having a surface area of 0.33 square meters per gram followed the para-
bolic law after a loading of 0.6 grams of uranium hexafluoride per gram
of sodium fluoride had been established. Insufficient data were
6
available to establish the rate law at lower loadings.
The reaction with crushed pellets followed the logarithmic law
until the loading reached 1.9 grams of uranium hexafluoride per gram of
sodium fluoride, after which reaction in accord with the parabolic law
was observed. It was concluded that the thickness of the film of com-
plex at the onset of the parabolic law was the same in both cases, based
on measurement of the particle size of the materials. An increase in
reaction rate was observed as the sorption temperature was raised for
both powdered sodium fluoride and crushed pellets. The data on the
sorption rate with whole pellets (one-eighth-inch right circular
cylinders) scattered badly and few conclusions can be drawn. A rapid
initial reaction was observed, after which sorption stopped at a loading
of about one gram of uranium hexafluoride per gram of sodium fluoride.
An inverse effect of temperature on the maximum loading was noted.
53
Studies in progress by Katz”” with sodium fluoride powder having
a surface area of 7.0 square meters per gram show that the composition
of the complex is UF6°2NaF. It is believed that the lower extent of
reaction noted in previous studies with low-surface-area powders was
due to the buildup of a thick film of complex on the outside of the
individual particles. This film was five to ten times as‘thick as the
film on the higher surface area material and caused a low rate of
sorption.
Uptake of Gases by Solids
The uptake of gases by solids may be divided into two types:
that of adsorption, where the gas is retained on the surface of the
T
solid, and that of sorption wherein the interior of a nonporous solid
is penetrated. Study of adsorpFion, both theoretically and experimen-
tally, has been widespread, while only rudimentary data are available on
the somewhat more complicated process of sorption. -
“Adsorption is further divided into physical (van der Waals)
adsorption and activated adsorption (chemisorption). In physical
adsorption the adsorbed gas is held at the solid surface by relatively
weak forces comparable to van der Waals forces in a gas. This type of
adsorption is similar to the condensation of a pure vapor in that in
both processes the rate is almost instantaneous. A second similarity
is that the quantity of heat released on adsorption is approximately
the latent heat of vaporization (five to ten Rilocalories per mole) of
the adsorbing material. Also, physical adsorption is observed only at
temperatures near or below the boiling point of the adsorbing material,
whereas chemisorption commonly occurs at temperatures far above the
boiling point of the material being adsorbed.
Chemisorption more closely resembles chemical reaction -than con-
densation. The bonding forces between the gas and the solid are
normally stronger than those in physical adsorption; this is reflected
in the heat of adsorption, which is usually greater than ten kilocal-
ories per mole but less than the heat of reaction for typical chemical
reactions, which is about one hundred kilocalories per mole. Chemi-
sorption normally proceeds at a rate which is lower than that of
physical adsorption, and in most cases, an activation energy is observed
as in most chemical reactions.
8
Adsorption normally results in the deposition of a monolayer or,
at most, a few molecular layers of the adsorbing gas whereas sorption
often results in complete reaction of the original solid. As pointed
out by Cabrera gg_gl:,B if the lattice constants of the reacting.solid
and the solid product differ by more than about ten per cent; cracking
and degradation of the product film may occur. M.cBainlLl discusses
numerous examples where an initially érystalline material is reduced to
a powder during sorption of a gas or liquid. Katz33 observed that the
sorption of approximately three moles of hydrogen fluoride per mole of
_sodium fluoride results in complete disintegration of the pellets with
a tenfold increase in surface area. It is believed that sorption of
hydrogen fluoride results in a decrease in the size of the initially
crystalline particles originally in the pellet.
‘Most of the data on the rate of sorption of gases by finely
divided solids can be represented by one of three common relations: the
linear law, the parabolié law, and the logarithmic law. The linear law,
which predicts a constant rate of reaction for slab geometry, .is
observed in cases where the sorption rate is controlled by the rate of
reaction betwéen the reacting solid and gas. The parabolic law predicts
that the rate of sorption is inversely proportional to the thickness of
reaction product through which the gas must diffuse. The parabolic rate
is thus independent of reaction rate and is the rate of diffusion of
reactant.
The logarithmic law, known also as the Elovich equation, is less
well understood. Since the sorption of uranium hexafluoride by sodium
9
fluoride was observed to follow this law, it will be considered in
greater detail. Numerous attempts have been made to provide a theoret-
ical basis for the law, which states that the sorption rate decreases
exponentially with the quantity sorbed. Evans in 19#322 derived the
logarithmic rate law in consideration of the rate of oxidation of zinc
where cracking of the oxide layer was believed to occur. This mechanism
is believed to be applicable to the sorption of uranium hexafluoride on
sodium fluoride and will be discussed in Chapter III. Taylor in 195255
derived the logarithmic law for chemisorption leading to a monolayer.
He assumed that a certain number of active sites are produced at the
onset of sorption, that the sorption rate is proportional to the number
of active sites, and that the number of active sites decays bimolecu-
5T
larly. Trapnell in 1955 showed that a logarithmic law would be
followed if the activation energy increased linearly with the degree
of surface coverage for a monolayer buildup if the coverage is not near
completion. The uranium hexafluoride loading due to a monolayer of
uranium hexafluoride on sodium fluoride of the type used in this study
is 0.004 gram of uranium hexafluoride per gram of sodium fluoride, which
is approximately one per cent of the loading which is observed. For
this reason, these derivations of the logarithmic law are not considered
pertinent to the present discussion. Freund in 195"{2LF examined data
for the sorption of hydrogen on various oxides and found good agreement
between values of constants in the logarithmic law determined experimen-
tally and values calculated from a relation obtained by Sutherland et al.
in 195552 for the case in which the rate of sorption was controlled by
10
55
Knudsen flow in a porous material. Landsberg in 1955 reviewed the
literature on the logarithmic rate law for chemisorption and the oxida-
tion of mgtals.and gave a derivation of the law. The assumption was
made that the rate of adsorption was proportional to the surface density
of adsorption sites which were initially present or were generated
during sorption by such processes as the diffusion of adsorbed material
away from the ;urface. Although the basic idea on which the derivation
is based is certainly plausible, its use is limited by its indefinite
nature.
Diffusion of Gases Through Porous Solids
Gases may be transported through porous solids by bulk diffusion,
Knudsen diffusion, or a combination of the two. Bulk diffusion occurs
in a pore when the mean free path of the diffusing gas molecules is
small compared to the radius of the pore, so that ifi most collisions
the gas molecule collides with another gas molecule. When the mean free
path of the diffusing gas molecule is the same as or larger than the
radius of a pore, the gas molecule will collide more often with the
pore wall than with other gas molecules, and Knudsen diffusion will
occur. As discussed in Chapter III, only bulk diffusion is believed
important in this study.
The effective diffusivity of a gas being transported within a
porous solid by a diffusive mechanism is less thah the normal diffu-
sivity of the gas. Numerous efforts have been made to relate the ratio
of effective diffusivity to normal diffusivity and characteristics of
11
the porous solid. Maxwell in 1873ho considered the solid to be composed
of uniform spheres and obtained the relation:
D
BE'= 3 ?ee ’ (2)
where
De = effective diffusivity,
D = normal diffusivity, .
€ = volume void fraction.
Bruggeman in 19356 extended the range of validity of Maxwell's expres-
sion to higher values of ¢ by the use of a continuum model which yielded
the result:
UlmU
.52 - - (3)
Buckingham in 190&,T on the basis of data on the rate of diffu-
sion of oxygen and carbon dioxide through soil, suggested the relation
D :
S (1)
Masamune in 1962,38 working with large pore silver cat&lyéts‘in.which
only bulk diffusion was present; found that the Buckingham relation
represented the data better than the Maxwell or the Bruggeman relations.
58
Wakao in 1962 derived an expression for the effective diffusivity in
a solid containing both macro- and micropores; it reduces to Equation
() for the case of bulk diffusion in macropores. Currie in 196016
measured the rate of diffusion of hydrogen through a number of materials
in which the void fraction € varied from 0.18 to 0.98 and recommended
the relation:
12
n
De=7€:7_<_1:n21: (5)
where ¥ and n are characteristic éf a given material.
Petersen in 1958LL6 considered the effect of periodic pore con-
strictions (such as in pelleted or extruded porous solids) on the effec-
tive diffusivity. The pore model assumed was a hyperbola of revolution
giving a pore constriction at the vertex of the hyperbola. The solution
to the steady-state diffusion equation for a pore of this shape was
found at different values of £, the ratio of the maximum to minimum
cross section of the pore. Comparison of the rate of diffusion in this
fype pore and in an equivalent cylindrical pore showed that the normal
diffusivity was reduced by a factor of three when B had a value of
twenty-five.
Simultaneous Diffusion and Irreversible Reaction
The process in which a substance diffuses into a rigid medium
with which it reacts irreversibly is encountered in many fields and has
consequently received considerable study. In the most general form of
the problem, the rate of sorption of the reacting substance depends on
both the rate of diffusion of the substance in the medium (or in the
p;oduct of reaction between the reacting substance and the medium) and
the rate of reaction between the diffusing substance and the medium.
One may also have the added complication that the point values of
'diffusivity and the rate of reaction are dependent on the quantity of
the substance that has reacted at the point. To date, an analytical
solution yielding the rate of sorption and associated information has
13
not been found for the general problem. A number of solutions, both
analytical and numerical,.have been obtained for special cases of the
general problem and will be discussed'below. Most of these solutions
are of a steady-state nature; that is, the rate of sorption does not
include the time rate of change of the total quantity of unreacted
substance in the medium. These solutions result from solution of the
appropriate form of the general diffusion equation and can be grouped
according to reaction rate and diffusivity in the following manner:
1. Instantaneous reaction, constant diffusivity.
2. Instantaneous reaction, variable diffusivity.
5. Variable reaction rate, constant diffusivity.
In the first type of solution, distifiguished by an instantaneous
reaction rate and constant diffusivity, the rate of sorption of the
reacting substance is controlled solely by the rate of diffusion of
reactant through the reacted portion of the medium to the reaction
interface, which is of infinitesimal thickness and separates the region
in which complete reaction with the medium has occurred from the region
in which no reaétion has occurred. This type of solution was first
investigated by Hill in 192929 in the study of the diffusion of oxygen
and lactic acid in muscle tissue. Other investigations of this type
include the work of fiermans-inf19h728 on the diffusion of sulphide ions
into a gel containing heavy metal ions, and of the work of Booth in
19&85 who derived the condition for the existenge of a steady—gtate
type of solution for slab geometry. Crank in 195715 showed that the
agreement between the actual solution and the steady state approximation
1L
was dependent on the ratio S/C, where S is the capacity of the medium
for the reacting substance and C is the concentration of the reacting
substance in the fluid adjacent to the medium. For values of s/c
greater than ten, results calculated from the steady-state solution
agree to wichin one per cent of results from the actual solution for
plane, cylindrical, and spherical geometries. Kawasaki et al. in
1962,5u and Scott in 1962,51 encountered this type solution in the
reduction of pellets of ircn oxide and copper oxide, respectively, by
hydrogen and carbon monoxide. 1In these two studies, the diffusional
procesc was that of councerdiffusion of reactant and product gases;
however, this does not change the characteristics of the solution.
The second type of soiution, distinguished by instantaneous
feaction and variable diffusivity, was studied by Olofsson in 195645
and in 196OuuAin the study of uptake of periodate.ions by cellulose
fibers. The change of diffusivity with time was attributed to swelling -
of the fiber, and a sharp reaction interface was observed, as in the
first type of solution.
The third type of solution, distinguished by variable reaction
rate and constant diffusivity, is used widely in the field of hetero-~
geneous. catalysis for the pfediction of catalyst activity, selectivity
and other properties. In this type of solution, one or more reactants
and products penetrate the catalfst particle by diffusion through the
'pofe space in the particle to a depth dictated by the relative races of
diffusion and reaction. A constant value of the diffusivity of
reactants and products is observed since the gross structure of the
15
catalyst is unchanged by the occurrence of a reaction on the pore walls.
The vériability of reaction rate in the catalyst particle is caused by
the dependence of the rate upon the concentration of the reactants.
Hence, in the third type of solution, the reaction zone may be
restricted to a narrow region near the surface of the particle if the
reaction rate is high compared with the diffusion rate, or, the reaction
may occur throughout the entire particle if the reaction rate is low
compared with the diffuéion rate.
The third type of solution was inveétigated by Thiele in 1959.55
He obtained an analytical solution for slab geometry with first- and
second-order reactions, and for spherical geometry with first~order
reaction. Danckwerts in 195717 obtained the general solution for first-
order reaction in various simple geometries, of which the Thiele treat-
ment is a special case. The Thiele treatment has been used widely in
catalysis by Wheeler in 195160 and in 1955,61 by Bokhoven et al. in
195'+,L-L by Barnett et al. in 19615 and by numerous other investigators.
A similar type of solution was also obtained by Ausman et al. in 1962l
for the burning of carbon frém the internal surfaces of a porous cata-
lyst pellet where the burning rate was assumed to be first order with
respect to oxygen concentration. The Thiele.concept has been extended
to nonisothermal conditions by Tinkler et al. in 196156 and by Carberry
in 1961.10
Mass Transfer to the External Surface of the Pellet
The resistance to mass transfer of a component from a fluid
stream to the surface of a solid particle in a fixed bed is normally
16
considered to be the resist;nce to diffusion across a hypothesized
stagnant film of fluid surrounding the particle. The rate of transfer
per unit.area is assumed to be given by the product of a mass transfer
coefficient and the concentration difference across the film. Many
investigations have been made for determining the dependence of the mass
transfer coefficient on factors characterizing the fluid, the soiidJ and
the flow conditions.