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ORNL-CF-72-1-1.txt
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| 1972 2 sy u
onre tssoep;_FEB 4 ‘ | g
""uo- f’*‘ T e »
fd:{fi?m :(: . ? B e, v
TR ‘l”r'!;’“(‘\‘ i Ty r"’[ AR -
OAK RIDGE NATIONAL LABORATORY For Internal Use
CPERATED BY
UNION CARBIDE CORPORATION
NUCLISION 0 R N L fi( s
CENTRAL FILES NUMBER
OAK RIDGE, TENNESSEE 37831
Only
72-1-~1
DATE: January 28, 1972 COPY NO.
supJecT: Consideration of Possible Methods of Disposal of MSRE Salts
TO: Distribution
FROM: P. N. Haubenreich and R. B. Lindauer
Abstract
Since the MSRE was shut down in 1969, the fuel and flush salts,
containing the fissile material and fission products, have been stored
in the reactor drain tanks. Portions of the facility that would be used
in recovery of the uranium as UFs and removal of the salt to some longer-
term storage site are preserved. The present cost of recovery and storage
of the 36 kg of uranium (85% 2®°U) in the fuel salt is estimated to be
$82,000, Because of the high ??U content (220 ppm) remote handling is
necessary, and conversion to Uz0s would cost an additional $240,000. 1In
the future (probably 5 to 10 years hence) the salts, with or without the
uranium, could be stored in cans in the National Radioactive Waste Re-
pository or could be injected into deep shale beds at ORNL, Estimated
costs of disposing of both the fuel and flush salts are about $85,000 for
disposal in the NRWR and about $220,000 for shale injection. It appears
that disposal in the NRWR will be best, but it is not clear if and when
the uranium should be recovered. It is recommended, therefore, that the
salts be held at the MSRE until the NRWR is ready, that meanwhile the capa-
bility for fluorination be preserved, and that final decisions on uranium
recovery and salt disposal be deferred until requirements are more firmly
established.
This document has been approved for release
to the public by:
Dot € N ,fl(fiffi/‘?é
Té&chnical Information Officer
QRNL. Site
NOTICE
i This dacument contains information of a preliminary nature and was prepared
primarily for internal use at the Oak Ridge National Laboratory. |t is subject
to revision or correction and therefore does not represent a final report. The
information is not to be abstracted, reprinted or otherwise given public dis-
semination without the approval of the ORNL patent branch, Legal and Infor-
mation Control Department.
4
-.“"fl’.r‘ .
iii
Contents
Status of MSRE Facilities . . . . o
Description of MSRE Fuel and Flush Salt
Fuel Salt + ¢« ¢« ¢« ¢ ¢ o « s &
Flush Salt . . + « + o « & o &
Fissile Material Inventories .
Activities of Heavy Nuclides .
Fission Products . « « « « .« &
Fluorine Evolution Potential .
Options for Disposal . . « « . & &
Operations Involved in Disposal . .
Storage at MSRE Site . . . o &
Recovery of Uranium . . . . .
&
Storage in National Radioactive Waste Repository
Injection into X-10 Shale . .
Cost Estimates .« ¢« « o« o « o o« o o
o
@
a2
Discussion and Recommendations .. . « « & o o a s o o
References . o« o + o o« s s s a o &
&
cowownmbN MNP o
NN RN R
BN R 00N N e
o
Status of MSRE Facilities
The MSRE is located in building 7503, which is within a separately
fenced area in Melton Valley, about 0.6 mile southeast of the main ORNL
plant area (X-10). The reactor operated at a maximum power of 7.4 MW for
the equivalent of 13,172 full-power hours from 1965 to 1969. Nuclear
operation was concluded in December, 1969 and the facility was placed in
a standby condition.! The on-site salt processing system had previously
been placed in standby after successful operation® during the 1968 change-
238
over from 23®*y to 2°3°
U in the fuel salt. Between November, 1970 and Feb-
ruary, 1971 a limited program of post-operation examinations® was carried
out which incapacitated the reactor for further operation. There is cur-
rently no activity at the reactor site other than routine surveillance.”
The 2?3U fuel charge and the fission products have not yet been re-
moved from the MSRE, They are safely secured, for the present, in the
fuel and flush salts which are frozen in the sealed reactor drain tanks.,
Containment and monitoring systems remain in 0peration.“ Ultimate removal
was planned, and the parts of the facility that will be needed to melt and
transfer the salt into transport containers are preserved., The option of
recovering the uranium from the salt, if so desired, was retained by
placing the processing facility in standby condition and preserving the
information necessary to operate it again.®
The fuel salt is divided between the two fuel drain tanks, with
2480 kg in FD-1 and 2170 kg in FD-2. All of the flush salt (4290 kg) is
in the flush salt tank (FFT). All three of these tanks are in the fuel
drain cell. All salt lines which formerly connected these tanks to the
reactor vessel have been severed and plugged near the tanks. The line
connecting the tanks to the salt-processing tank (FST) in the adjacent
cell is intact, blocked with a plug of frozen salt. Cover-gas supply lines
to the tanks are capped outside the cell; vent lines are valved off out-
side the cell, Heaters on the drain tanks and flush tank are operable (but
not turned on except for a few days each year when the salt is heated to
recombine radiolytic fluorine). Pressure and temperature instrumentation
: . s 4
continue in operation.
~4
Description of MSRE Fuel and Flush Salts
Fuel Salt ) R
The MSRE fuel salt is a mixture having the composition: LiF-BeF.-
ZrF,-UF, (64.5-30.3-5.0-0.13 mole %).°® This mixture melts and thaws over
the range from 360°C to 440°C (solidus and liquidus temperatures). Unless
such salt is frozen extremely slowly, there is little or no segregation
during the freezing process and the frozen salt has a practically uniform
composition,
The density of the liquid at 440°C is 2.31 g/cm®. At 600°C (which
is about the temperature which the salt is usually transferred) the density
| is 2.22 g/em®, The change in density upon freezing has not been measured
directly, but is believed to be between +27 and -17%7 (corresponding to a
density of solid salt at 360°C between 2.36 and 2.29 g/cm®). (Ref. 7)
The measured density of solid salt at 26°C is 2.48 g/cm®. The increase
in density as the salt is cooled below the solidus is often accompanied, ¢ "
in large bodies of salt, by the formation of internal cracks. N
The volumes of fuel salt that must be dealt with in the disposal op- - i
erations can be calculated from the inventory (4650 kg) and the foregoing -
densities. At the temperature at which the salt would be transferred into
transport containers, there would be about 2.08 m® (73.8 ft®). The total
volume when it starts to freeze will be 2.01 m® (71.0 ft®). The volume of
frozen salt at room temperature will be about 1.88 m® (66.4 ft®). The
volumes would not be significantly less if the uranium were removed by
fluorination.
The thermal conductivity of the salt depends strongly on temperature.
Measurements by Cooke® show that the thermal conductivity of MSRE fuel salt
at 440°C is about 10 w/cm-°C, and is 13 w/cm~°C at 600°C. The conductivity
of the frozen salt (neglecting any effect of cracks) probably ranges from
about 16 w/cm-°C at 360°C to perhaps 30 w/cm-°C at 100°C. (The conduc~—
tivity of frozen MSRE salt was not measured; the foregoing values are esti=-
mated from measured values for frozen breeder fuel salt,?)
The vapor pressure of the salt is extremely low, even at temperatures
far above the liquidus. 1In the temperature ranges of interest for this
study it is quite negligible (on the order of 10™% torr or less).
o
The corrosiveness of the fuel salt depends strongly on whether or not
moisture or some other oxidant is present. Clean molten fuel salt corrodes
Hastelloy N at rates on the order of 0.1 mil/yr by leaching chromium from
the alloy. Nickel is less susceptible to corrosion; stainless steels, more.
For almost any material, corrosion by dry, frozen salt is not much of a
problem. (Ordinary steel drums are commonly used at ORNL to hold fluoride
salts that are removed from test loops to be discarded (buried). The fuel
salt is slightly hygroscopic, however, and if exposed to humid air will at~-
tract moisture and create quite corrosive conditions. (The water and salt
probably react to form HF which corrodes most common materials.)
When fuel salt is contacted with copious amounts of water, every con-
stituent element gradually appears in solution. Rates of dissolution, tem-
perature dependence, and effects of complexing among the constituents were
observed in experiments in which excess amounts of finely divided, simu-
lated MSRE fuel and coolant salts were stirred in warm water.?° This ex-
periment showed that at 25°C, equilibria were reached in 2 to 6 days.
More lithium went into solution than would be possible in a simple so-
lution of LiF, presumably reflecting interactions with other constituents.
Solubilities increased with temperature over the range covered (25°C to
90°C)+ Using the results of this experiment, one can calculate that the
amount of water at 25°C required to dissolve a batch of fuel salt would
be about 0.08 kg H,0/g fuel. (If one uses accepted values for the solu-
bilities of the separate constituents and the amounts of each in the fuel
salt, the lower solubility of LiF results in a higher estimate of the re-
quired amount of water.)
Molten fuel salt is immune to radiation damage. Frozen fuel salt ir-
radiated at temperatures below about 100°C evolves radiolytic fluorine.
(This will be described in detail in a later section.)
The MSRE fuel salt is chemically toxic. The allowable ingestion of
the salt is limited now, however, by the radioactive nuclides included in
it. The maximum permissible concentration in air for occupational exposure
is limited to about 0.03 ug/m® by the plutonium and *?®Th, compared to a
limit of 4 ug/m® if beryllium were the only consideration. The limit '
that would be set by the fission products is intermediate, about 0.1 ug/m>. .:
(See later sections on inventories of radioactive nuclides.) 3‘2_
Flush Salt '
The flush salt is LiF-BeF, (66-34 mole %) with a small amount (about
47 by volume) of fuel salt mixed into it. Its physical properties will be
very close to those of the original 66-34 mole 7 mixture. Upon cooling,
this salt begins to form crystals of LiF at about 470°C and at about 455°C
solidifies into Li,BeF,. (Ref. 9).
The density of the liquid at 458°C is about 2.02 g/cm®; at 600°C it is
about 1.96 g/cm®. There is very little change in density (less than 27%) as
it freezes and thaws. The density of Li;BeF, crystals at room temperature
is about 2.17 g/cm®. (Ref. 10). The volume of the flush salt will be
2,18 m® (77.0 ft?) at 600°C, 2.12 m® (74.9 ft®) at the liquidus tempera-
ture and 1.98 m® (69.9 ft?®) at room temperature. .
With regard to vapor pressure, corrosion, water solubility, and chemi- ¢ :
cal toxicity, the flush salt is very similar to the fuel salt. .,
Fissile Material Inventories
The amounts of uranium and plutonium believed to be in the fuel and
flush salts are listed in Table 1. The totals are from a compilation by
R. E, Thoma.'' The amounts of uranium in the flush salt were obtained
directly from analyses of flush salt samples taken at the conclusion of the
MSRE operation. The amounts of plutonium in the flush salt were computed
from the observed fractions of the fuel salt inventory that mixed into the
flush salt during each operation and the computed plutonium inventory at
the time of each mixing. Thoma concluded,® from material balances and
the isotopic dilution that occurred when ?*°U was added, that in addition
to the quantities listed in Table 1 there is some 2.65 kg of uranium that
was removed from the fuel salt but did not show up as UF¢ on the absorbers
during the recovery of the original uranium charge in 1968. (This was a -
mixture of enriched and depleted uranium containing 33 wt % 23°U.) There
is no direct evidence on the location of this missing uranium but the most P
likely sites are in the processing systems. Location and recovery of this
uranium would be a separate operation from the removal and disposal of the
salts,
Table 1. Inventories of Uranium and Plutonium in MSRE Salts
Fuel Salt Flush Salt Total
Uranium (kg): 233y 30.82 0.19 31.01
234y 2.74 0.02 2.76
233y 0.85 0.09 0.94
236( 0.04 0.00 0.04
238y 2.01 0.19 2.20
Total U 36.46 0.49 36.95
Plutonium (g): 23%py, 657 13 670
240%py 69 2 71
Other Pu 2 _ 0 2
Total Pu 728 15 743
232
Activities of U and its Daughters
The 223U that was available for use in the MSRE was some that had an
12
unusually large amount (222 ppm) of 232) associated with it. There was
no conflicting demand for this material because of the inconveniently high
232y decay chain.
radiation source from the
Uranium=-232, which undergoes alpha decay with a half-life of 72 years,
is the first in a chain of 8 radionuclides that leads to stable *°°Pb. Six
alphas, two betas, and several hard gammas are emitted along the line. The
first daughter, 22®Th, has a half-life of 1.9 years. Subsequent nuclides
have very much shorter half-lives. Thus after uranium is separated from
its daughters, the total activity of the chain builds up, peaks at about
10 years, then decays with a 72-year half-life. In uranium containing
232
U
more than about 50 ppm , the activity will build up within a week or
two to levels that prohibit direct handling because of the gamma radiation.
When the uranium is intimately associated with certain light elements, as
in the MSRE fuel, neutrons produced by a-n reactions are also significant.
The uranium used for the MSRE had been purified in 1964 and by the
228
time the fuel concentrate was prepared in 1968 the Th daughter ac-
tivity was quite high. (Cans containing 450 g 233
U as oxide produced a
gamma dose rate of 25 r/hr at 1 ft.) The preparation of the MSRE fuel
concentrate was carried out in a shielded facility, however, and no ef-
228
ort was made to separate
Th from the uranium either before or during
this operation.'? If in the future the uranium is removed from the MSRE
salt by fluorination, the 22?°Th will be left behind., In that case the
228Th and daughter activities in the salt would begin to decay with a
1.9-year half-life, while the activities with the uranium would begin
to build up anew. If the MSRE salt is not fluorinated, the 2?°Th and
daughter activities will correspond to a buildup and decay transient
starting in 1964.
The radioactivityrof the MSRE fuel, including both the heavy nuclides
and the fission products, was calculated by M. J. Bell after the end of
nuclear operation, taking into account the history of power operation, the
1968 fluorination, and additions of uranium and plutonium to the reactor.®®
He used values for the 233
U and plutonium inventories that differ slightly
from those listed in Table 1. The radiocactivities of the heavy nuclides
in the MSRE listed in Table 2 were obtained by adjusting Bell's figures
to agree with the inventories at the end of nuclear operation (December
1969) as given in Table 1. It may be noted that the flush salt contains
2.0% of the plutonium in the MSRE but only 0.6% of the 2?3y, 222y, and
232y daughters. This difference reflects the fact that the uranium in
the flush salt is only that which mixed in during the two flushing opera-
tions subsequent to the loading of 223
U in 1968, but the plutonium (which
is not removed by the fluorination process) accumulated in the flush salt
over the entire period from 1966 through 1969,
Ty Table 2. Calculated Radiocactivity of Heavy Nuclides
. in MSRE Salts
» 4
¢ Half-life Inventories (curies)
Nuclide (vears) Fuel Salt Flush Salt
20811 b 58 0.4
21%po b 102 0.6
2i2py b 160 1.0
212pp b 160 1.0
21®po b 160 1.0
22%Rn b 160 1.0
22%Ra b 160 1.0
228Th b 160 1.0
232y 72 156 1.0
. 293y 1.62 x 10° 370 2.3
o 234y 2.47 x 10° 19 0.1
?' 233y 7.13 x 10° 0 0.0
v 23y 2.39 x 107 0 0.0
o 23%y 4,51 x 10° 0 0.0
| 238py 86.4 5 0.1
23%py 24,390 45 0.9
240%py 6,580 18 0.5
241py 13.2 227 4.5
241 Am 458 3 0.1
Total 1960 16
pctivities as of January 1977.
Activities are in secular equilibrium, decreasing with
the 72-y half-life of 232y,
Fission Products "
The calculated radioactivities of the fission products that are still
present to any significant extent are listed in Table 3. The calculations
took into account the effects of stripping the gaseous fission products
during operation and removing certain fission~-product elements during the
salt processing in 1968 (Ref. 13). No account was taken of the deposition
of noble-metal fission products on surfaces, however, so the figures for
Nb, Ru, Rh, Sb, and Te are upper limits which are probably several times
the actual inventories. For the long-lived fission products (those still
significant in 1977) that stay in the salt, 98.1% is in the fuel and 1.9%
is in the flush salt. In January, 1977 the fuel salt will contain about
47,000 Ci (0.10 Ci/g) of fission products. The flush salt will contain
900 Ci (0.20 mCi/g) of fission products.
Fluorine Evolution Potential®
Irradiation of frozen fluorides by gamma rays or charged particles
results in displacement of fluorine atoms. These atoms may either re-
combine (which they are almost certain to do at temperatures above about
4
>
£
'
. - - -
80°C) or they may migrate to a surface where they form gaseous fluorine.
Analysis of various experiments indicates that radiolysis of the MSRE
salts due to included radioactivity will probably be equivalent to about
0.04 atoms F/100 eV of absorbed energy (or evolution of 0.02 molecules
F,/100 eV if there were no recombination). Rates of recombination in
salt in intimate contact with gas containing F. were found to depend
strongly on temperature and practically not at all on F, partial pressure.
The recombination data over a wide range of conditions were fitted to *50%
by the empirical relation
-(9710/T)
cc (STP)F, ) = 1.15 x 10° e
recombination rate (g;:EBEE"EZTt
where T is the temperature of the salt in degrees Kelvin. When salt that
was initially free of unrecombined fluorine is irradiated at low tempera-
tures (where recombination is insignificant) there is typically an "in-
duction period" before any gaseous F,; is evolved. The energy absorbed
Table 3. Calculated Fission Product Activities in MSRE Salts?
Activity (curies)
Nuclide Half-life (y) Jan, 1972 Jan, 1977
®%sr 0.14 30 0
°%sr 28.1 12,800 11,300
2%y 0.0 12,800 11,300
?ly 0.16 54 0
*37r 0.18 136 0
®*Nb 0.10 178 0
19€Ru 1.0 1,820 58
196Rh 0.0 1,820 58
123gp 2.7 396 110
125Mre 0.16 185 52
127Mre 0.30 36 0
127Te 0.0 36 0
137Cs 30 10,700 9,500
137, 0.0 9,970 8,880
t44Ce 0.78 20,400 240
1ebpr 0.0 20,400 240
147pm 2.6 22,500 6,010
*318m 20 145 140
15%80 16 32 26
133Eu 1.8 162 24
Total 115,000 48,000
aTotal in fuel and flush salts.
distributed 98.17% in the fuel and 1.97 in the flush salt.
Long-lived fission products are
10
during such induction periods was about 60 watt-h/mole salt for simulated L.
MSRE fuel salt irradiated with ®°Co gamma rays. These observations can
be used in conjunction with the energy disposition rates due to the radio- ’ g
activity in the fuel and flush salts to predict the radiolytic fluorine .
behavior.
The radiolytic production of 0.04 atoms F/100 eV is equivalent to
0.17 ce (STP)F,/watt-hr; that is, if there were no internal recombination
F, gas would eventually (after the induction period) be evolved at this
rate. By January 1977, the radioactive energy source in the fuel salt
will be down to about 181 watts., This is enough, if all were absorbed,
to produce F, at a rate of 31 cc(STP)/hr. The flush salt, containing only
3.4 watts of radioactivity could evolve only 0.6 cc(STP) F,/hr.
The energy sources are distributed throughout 1.06 x 10° moles of
fuel salt and 1.30 x 10® moles of flush salt. The specific heat sources
as of January 1977 are 1.71 x 107% watts/mole fuel salt and 2.6 x 10-%
watt/mole flush salt. The times corresponding to an induction period of
60 watt-h/mole at these rates are 3.5 x 10° h (4.0 years) for the fuel
salt and 2.3 x 10° h (264 y) for the flush salt. (It is questionable if o
quantitative extrapolations of the observations on fluorine evolution to
the extremely low levels of self-radiation in the flush salt are meaningful.)
In summary, if the salts were chilled in January 1977, immediately
after having been hot enough to recombine the fluorine, it would be at
least -4 years before any F, evolution would be expected from the fuel salt
and then the rate would be about 30 cc(STP)/hr or less. Alternatively, if
the fuel salt were kept at 62°C or above, recombination would be expected
to prevent any F, evolution. Little or no F2 evolution would be expected
from the flush salt.
11
Options for Disposal
No decision as to the ultimate disposal of the MSRE fissile and
radioactive materials had been made at the time the reactor was shut
down. Instead the materials were left in the MSRE, with the equipment
for stripping the uranium and removing the salts kept intact, until the
needs for the uranium and the requirements for long-term storage could be
better defined.'® Whether or not the uranium is actually recovered should
be decided on the basis of: (a) the value placed on the uranium, either
for some specific application or in anticipation of future use, (b) the
estimated costs of recovering and handling the uranium, and (c) the ex-
tent to which removal of the uranium can be expected to simplify the dis-
posal of the salt.
In May, 1971 the USAEC requested ORNL to continue active considera-
tion of disposal in the National Radicactive Waste Repository and also
"to evaluate alternate disposal approaches and provide cost estimates for
these proposals. At least one of the alternates should be feasible within
present technology and should involve only storage and operating facilities
that are presently available and are considered acceptable for this use."®®
Storage of the frozen salt in the tanks at the MSRE is safe enough
under present conditions, but does require some attention and is not re-
garded as a permanent situation. Surveillance requirements could be re-
duced and the salts might be said to have been disposed of if the under-
ground cell around the salt tanks were filled with concrete. This would
be relatively inexpensive to do and is certainly feasible within present
technology. It is possible, however, that this approach will be incon-
sistent with future national policy on radioactive waste disposal, which
may require deep underground disposal of such quantities of radioactive
material as those in the MSRE. Recovery of the salts from the MSRE tanks
imbedded in concrete would be quite expensive.
For deep underground storage other than in the NRWR, we can consider
injection into the deep shale beds underlying the valley in which the MSRE
is located. The required technology exists and has been proved by similar
injections at a facility less than a half-mile from the MSRE.*’ Although
12
additional development and equipment would be required to put the MSRE
materials into aqueous solutions as required in this process, we believe
that shale-injection is the only clearly foreseeable alternative to stor-
age in the NRWR,
Possible methods of disposal of the fuel and decisions to be made are
outlined in Figure 1. Similar choices exist for the flush salt. Because
of the much lower fissile and radioactive content of the flush salt, it
is conceivable that its disposal might differ from that of the fuel.
Note that plutonium recovery does not appear in Fig. 1. Plutonium
is not removed from the salt by the fluorination that is used to take out
the uranium, and recovery of the small amount present by other processes
would be prohibitively expensive. Figure 1 considers, therefore, that the
plutonium will be left in the salt, without question.
Operations Involved in Disposal
Storage at MSRE Site
As described in detail in reference 4, the salts are presently frozen
in the sealed tanks, within secondary containment which is sealed except
for one line connected through filters to a stack. The stack fan and cer-
tain pressure, temperature, and radiation instrumentation are kept in op-
eration. Surveillance consists of remote monitoring of instrument signals
and daily visits by X-10 plant personnel, with periodic inspections and
equipment tests by MSRE personnel. Access to the reactor building is con-
trolled by a security fence,
Filling the drain tank cell with concrete would not be a major oper-
ation. Radiation from the tanks would be significant, probably requiring
that the lower courses be poured using the building crane, operated from
the remote maintenance control room. No forms, reinforcement, or com-
paction would be needed, however, so the placement would be relatively
simple and inexpensive., About 250 cu yd of concrete would fill the cell
to the bottom of the existing roof plugs.
ORNL DWG. 72-1639
Use 1in
MSRE operation.
Store at MSRE,
Separate U YES
from salt?
NO Permanent storage YES Fluorinate to
‘ at MSRE acceptable? get UFqs on NaF,.
NRWR X-10 shale Fill cell NO Permanent storage YES
or NRWR? with concrete. at MSRE acceptable?
{
./~ X-10 Shale \X-10 Fill cell
or NRWR? with concrete.
b
] !
Seal in cans.
}
Ship to
NRWR.
Store,
Salt with U
in NRWR.
Move to X~-10.
!
Dissolve.
|
Mix with
grout and
inject.
Salt with U
in grout in shale.
Fig. 1..
Seal 1n cans.
Move to X-10.
!
l
Ship to Dissolve.
NRWR.
!
Mix with
Store. grout and
inject.
Stripped salt
in NRWR.
-
Alternatives in Disposal
3
Stripped salt
grout in shal
of MSRE Fuel Salt
NO
Convert
tO U’Oa .
Y
Acceptable
as UF4?
i
UF‘ on NaF
€1
14
Recovery of Uranium i)
Recovery of the #2°U in the MSRE fuel salt would be done in the same ‘:
equipment and with procedures similar to those used during the *°°U re- Y
covery in 1968. (Ref. 2) Processing to recover the 2337 would differ .
from the *2°U processing in several respects, however.
1) Since the present uranium charge is only 1/6 as great as the
previous charge, processing could easily be done in 1 run instead of the
6 runs used before., This would reduce the overall time required for the
processing from 6 days to less than 1 day. It is estimated that the ac-
tual fluorine sparge time would be reduced from 46 to 11 hours. (About
2/3 of the time from the start to finish of the previous fluorination in-