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NAS-NS-3025.txt
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, " Wy R e Ty Wy
. !
e doa k.
it
i
National
Academy
of
Sciences | -.__
‘ -;lational Research Council
NUCLEAR SCIENCE SERIES
The Radiochemistry
of the Rare Gases
_— - '
o ——
— ——
T
Atomic
il
iifl
IR RY
Commission
I
L
COMMITTEE ON NUCLEAR SCIENCE
L. F. CURTIBSS, Chairman
National Bureau of Standards
ROBLEY D. EVANB, Vice Chairman
Massachusetts Institute of Technology
Jd. A. DaJUREN, Secrelary
Wenstinghouse Eleotric Corporation
C. J. BORKOWBKI
Oak Ridge Natonal Laboratory
ROBERT G. COCHRAN
Texas Agricultural and Mechanical
College
SAMUEL EPSTEIN
California Institute of Technology
U. FANO
Natonal Bureau of Standards
HERBERT GOLDSTEIN
Nuolear Development Corporation of
Amerioca
J. W, IRVINE, JR.
Magsachusetts Institute of Teohnology
E. D. KLEMA
Northwestern University
W. WAYNE MEINKE
University of Michigan
J. J. NICKBEON
Memorial Hospital, New York
ROBERT L. PLATZMAN .
Laboratoire de Chimie Physique
D. M. VAN PATTER
Bartol Research Foundation
LIAISON MEMBERS
PAUL C. AEBERSOLD
Atomic Energy Commission
J. HOWARD MoMITL1LEN
National Science Foundation
CHARLES K. REED
U. 8. Air Force
WILLIAM E. WRIGHT
Office of Naval Research
SUBCOMMITTEE ON RADIOCHEMISTRY
W. WAYNE MEINKE, Chairman
University of Michigan
GREGORY R. CHOPPIN
Florida State University
GEORQGE A. COWAN
Los Alamoa Bclentific Laboratory
ARTHUR W. FAIRHALL
University of Washington
JEROME HUDIS
Brookhaven National Laboratory
EARL HYDE
University of California (Berkeley)
HAROLD KIRBY
Mound Laboratory
GEORGE LEDDICOTTE
Osk Ridge National Laboratory
JULIAN NIELSEN
Hanford Laboratories
ELLIS P. STEINBERG
Argonne National Laboratory
PETER C. STEVENSON
University of California (Livermors)
LEO YAFFE
McGill University
CONSULTANTS
NATHAN BALLOU JAMES DeVOE
Centre d'Etude de 1"Energle Nucleaire University of Michigan
Mol-Donk, Belglum WILLIAM MARLOW
National Bureau of Standards
S
M133r
¢ .|
' The Radiochemistry of the Rare Gfises
By FLOYD F. MOMYER, JR.
Lasorence Radiation Laboratory
Universily of California
Livermore, California
October 1960
LOBS ALAMOS
SCIENTIFIC LABORATORY
APR - 6 1881
3 LIBRARIZS
— PROPERTY
=
=3
—
i=s
i
. Subcommittee on Radiochemistry
National Academy of Bciences —National Research Council
Printed in USA. Price $0.75. Available from the Office of Techmical
Ssrvices, Department of Commeroe, Washingtion 26, D. C.
FOREWORD
The Subcommittee on Radlochemlsgtry 1s one of a number of
subcommlttees workilng under the Committee on Nuclear Scilence
wlthin the Natlonal Academy of Sclences - Natlonal Research
Councll. 1Its members represent government, lndustrlial, and
unlverslty laboratorles 1n the areas of nuclear chemistry and
analytical chemistry :
The Subcommittee has concerned itself with those areas of
nuclear sclence whilch involve the chemlst, such as the collec-
tion and distributlon of radlochemlcal procedures, the estab-
lishment of specificatlons for radiochemlcally pure reagents,
avallabillity of cyclotron time for service irradlations, the
place of radiochemlstry in the undergraduate college program,
etc.
This serles of monographs has grown out of the need for
up-to-date compllations of radlochemlcal informetion and pro- -
cedures. The Subcommlttee has endeavored to present a serles
which will be of maximum use to the working sclentist and
which contalns the latest avallable Information. ‘Each mono-
graph collects 1n one volume the pertinent informatlon required
for radlochemical work with an individual element or a group of
closely related elemente.
An expert In the radlochemlstry of the particular element
has written the monograph, following a standard format developed
by the Subcommlttee. The Atomlc ‘Energy Commission has sponsored
the printing of the serles.
The Subcommittee 1ls confldent these publlcatlons willl be
useful not only to the radlochemist but also to the research
worker 1n other flelds such as physics, blochemlstry or mediclne
who wishes to use radlochemical technlques to solve a specifilc
problem.
W. Wayne Melnke, Chalrman
Subcommittee on Radlochemlstry
iii
INTRODUCTION
This report dealing with the radiochemistry of the rare gases was pre-
pared at the request of the Subcormmittee on Radiochemistry of the Committee
on Nuclear Science of the National Research Council a8 one of a series of
monographs on the radiochemistry of all the elements.
The early sections of this monograph are devoted to general reviews of
rare gas properties of interest to the radiochemist and to some general dis-
cussion of separation techniques for rare gases, The last three 6hapters are
respectively a discussion of the removal of rare gases from targets, a dis-
cuseion of techniques used for counting radioactive rare gases, and a collec-
tion of radiochemical prdcedures for rare gases.
The author would appreciate receiving from readers any additional in-
formation, published or unpublished, which should be included in such a report
on the radiochemistry of the rare gases. | _
The author takes this opportunity to acknowledge the able assiatance of
Mr. R. A. daRoza in the preparation of this monograph.
iv
CONTENTS
Foreword
Introduction
I. General References Pertinent to Rare Gas Radiochemistry
II. Table of Isotopes of He, Ne, A, Kr, Xe, and Rn )
III. Review of Features of Interest in Rare Gas Radiochemistry
IV. Sample Solution and Exchange with Carriers
VY. Counting Rare Gas Activities |
VI, Collection of Ra.di-ochemic'al Procedures for the Rare Gases
Procedure 1 — Removal of Kr and Xe from Air and
Their Subsequent Separation
Procedure 1 A — Removal and Separation of Kr and Xe
Fiassion Products from U235 Targets
Procedure 2 — The Extraction, Purification and
Industrial Uses of Krss
" Procedure 3 — Rapid Removal of Fiesion Product
Kr from U Foil
Procedure 4 — Recovery of Fission Product Xe
from U Metal .
Procedure 5 — Rapid Removal of Fission Product Xe
| | from UO, or UO,(NO,), - 6H,O Targets
Procedure 6 — Separation of Long-lived Fission Gases
Procedure 7 — Removal of Rn from Th Targets and its
Collection on the Cathode of a Discharge
Tube
Procedure 8§ — Determination of Active Gas Half-lives
by the Charged Wire Technique (II)
iii
iv
27 .
29
34
34
40
43
46
46
48
48
49
51
The Radiochemistry of the Rare Gases
FLOYD F. MOMYER, JR.
Lawrence Radiation Laboratory
University of California
Livermore, California
GENERAL REFERENCES PERTINENT TO RARE GAS RADIOCHEMISTRY
"H. Remy, Treatise on Inorganic Chemistry, Vol..I (translated by J. S.
Anderson), Elsevier Publishing Co., Few York (1956).
S. Dushman, Vacuum Technique, John Wiley and Sons, New York, 1949.
R. T. Sanderson, Vacuum Manipulation of Volatile Compounds, John
Wiley and Sons Inc., New York (1948).
R. E. Dodd and P. L. Robinson, Experimental Inorganic Chemistry
Chap. 2, Elsevier Publishing Co., New York (1954).
S. Brunauer, The Adsorption of Gases and Vapors, Vql. I, "Physical
Adsorption'", Princeton Universeity Press, Princeton, N.J. (1942),
A. I, M, Keulemans, Gas Chromatograzhx, Reinhold Publishing Co.,
New York, 1959, 2nd edition.
Lawrence A. Weller, '""The Adsorption of Krypton and Xenon on Activated
Charcoal -- A Bibliography," Mound Laboratory i'eport MLM-1092,
Miamisburg, Ohio, 1959.
A. Guthrie and R. K. 'Wakerling, editors, Vacuum Equipment a.fid Tech-
niques, National Nuclear Energy Series, Div. I, Vol. 1, McGraw-Hill
Book Co., Inc,, New York, 1949.
C. D. Coryell and N. Sugarmé.n, editors, Radiochemical Studies: The
Fission Products, National Nuclear Energy Series, Div. IV, Vol, 9,
Booke 2 and 3, McGraw-Hill Book Co., Inc., New York, 1951, Papers
64-70, 139, 141, 145-50, 154, and 311-17,
II. TABLE OF ISOTOPES OF HELIUM, NEON, ARGON
KRYPTON, XENON AND RADON. "
Isotope Half-life Type of Decay Method of Preparation
He3 Stable (abundance 1,3 X 10_4% atmos.) Natural
(abundance 1.7 X10™°% wells)
He4 Stable (abundance ~1007) Natural
He® ~0. 8 sec B Beg(n,a)
Ne 18 1.6 sec fl+ F_lg(P. 2n)
Nelg ~18 sec fi+ Flg(p,n)
Nezo Stable (abundance 90.92%) Natural
Nez'1 Stable (abundance 0.257%) Natural
Nez'z Stable {abundance 8. 82%) Natural
23 - 22 . 22
Ne ~40 sec B Ne "{n,y); Ne"" (4, p);
23 26
Na""(n,p); Mg~ (n,a)
Ne24 3.38 min g Nezz(t, p)
A35 ~1.8 sec fi+ S3z(u.,n); C135(p,n)
a3 Stable {abundance 0. 337%) Natural
37 . 34 37, ..
A -_35 day EC S™ "(a,n); C1™ (d, 2n};
c*’(p, n); X* (4, a);
Ca40(n. a)
A38 Stable (abundance 0. 063%) Natural
39 - 38 39
A ~265 yr B A7 (n,vy); K™ (n, p)
A0 Stable (abundance 99. 600%) Natural
41 . - 40 40
A ~110 min B A7(d,p); A" (n,¥)s
41
. K" (n,p)
A42 >3.5yr B A41(n,y); parent K42
Kr 0 9.7 hr EC - v8%(p, apall)
77 ; + T4
Kr ~1.2 hr EC~20%, B ~80% Se'“(a,n)
Kr'?8 Stable {(abundance 0, 3549%}) Natural
79 ' + 76 79
Kr 34,5 hr EC 95%, B 5% Se “(a,n); Br (4, 2n);
Br' ’(p,n); Kr ' (d,p);
Kr?B(n.v)
KrBO
Stable {abundance 2,27%)
Natural
x
Listed are thoee nuclides having an "A'" or "B'" classification in '"Table of
Isotopes'', D. Strominger, J. M., Hollander and G. T. Seaborg: Revs. Mod.
Phys. 30, No. 2, Part II, April 1958,
the original literature may be found in said article,
Further information and references to
TABLE OF ISOTOPES OF He, Ne, A, Kr, Xe,
and Rn,. {Cont'd)
‘Half-life
Isotope Type of Decay Method of Preparation
Kr81 ~10 sec IT Brsl(p,n); daughter Rbs-l
Krsl 2, l><105 yr EC Kreo(n,y)
K82 Stable (abundance 11.569%) Natural |
K™ 114 min IT 5e%%a,n); Kr®%(a,p);
Kraz(n.y)§ X-rays on
. Kr83-; fission U, daughter
Br®3; daughter RBS>
Kr83 Stable (abundance 11, 55%) Natural; fission U
Kr84 Stable (abundancé 56. 90%) Natural; fiseion U
Kr3®™ 4 36 hr p 78%, IT 22% se®?(a, n); Kr®4(4, p);
Kr84(n,y); Rb85(n,p);'
Sr88(n, a); fission U,
daughter Br35
I:(r85 10.3 yr B K:r84(n,y); fission U
Kr86 Stable (2bundance 17.37%) Natural; fission U
®Kr®7 78 min | 'y Kr28(a,v); kKe384, p);
Rb87(n, p): fission U
K98 ‘2.8 hr B Fission U, Th
Kr? 3 min 8 Fission U, Pu
Kz’ 33 gec - g Fission U, Pu
Krg1 9.8 sec B Fission U, Pu
Kr % 3.0 sec p Fission U, Pu, Th
K> 2.0 sec B Fiassion U, Pu
K:94 1.4 sec B Fission U
Kr?! l sec B Fission U, Pu
XelZI 40 min [3+ 112.7(p, n)
xel?2 20 hr EC 1127(p, 6n)
Xe123 2 hr EC, 'fi+ 1127(p,5n) .
Xe124 Stable {abundance 0, 096%) ‘Natural
Xe 2™ 55 gec IT (7) 1127(a, 6n)Cs?>; daugh-
ter Cs]'25
xe!?3 18,0 hr EC Tel?2(q, n) Xe 24 (n, v)
Xe126 Stable (abundance 0, 090%) Natural '
xel?7T 75 sec IT 1127(a, 4n)Cs '%7; daugh-
ter CSIZT '
(Table Continues on page 4)
TABLE OF ISOTOPES OF He, Ne, A, Kr, Xe, and Rn, (Cont'd)
Isotope Half-life Type of Decay Method of Preparation
xel?T 36.41 day EC Te'?%(a,n); 1'%7(q, 2n)
127(P.m); Xe 2 (r, y)
xe 128 ~ Stable {abundance 1.919%) Natural '
Xel?9™M g 0day IT xe'%8(n, y)
Xe129 Stable (abundance 26, 44%) Natural
Xe130 Stable (abundance 4. 08%) ' Natura.ll
xe!3!™ 12 0 day IT Xe'3l(n,n'); fission U
Xe131 Stable (abundance 21. 18%) Natural; fission U
Xe132 Stable (abundance 26. 89%) Natural; fission U
xe!33m 5 2 day IT , Xel3?(a,v); fission U
xe'3® 5,270 day B Xe132(n,v); Xe 1324, p);
.. xe 340, 20): Te 3%, n);
cs133 (. p); Be136(n a):
fission U
xe 134 Stable (abundance 10.44%) ‘Natural; fission U
Xe 113%™ 15 min IT - %e138(n, 2n); Xe!34m,v);
_ Ba138(n, a); figgsion U
xe!®® 9,13 hr 8 xe 3% n, v); xe 3¥(4, p);
36(n, 2n); Ba138(n, a);
fission U
Xe136 Stable {abundance B, 87%) Naturél' fission U
Xe137 3.9 min p 136(n v); fission U
Xe 138 17 min B Fission U
xe !9 41 sec B Fission U, Th
xe!? -10 sec 8 Fission U, Th
xe 41 ~2 sec g Fission U
xe 143 1.0 sec B ' Fission U
xe 44 ~1 sec B Fission U
Rn?%® <6 min ' a 65%, EC 35% At (%, sn)
Rn?%7 <10 min EC 96%, a 4% Aat T4, an)
Rn?%® 22 min . EC~809%, a-20% Spall Th; Pb(Clz, apall)
Rn?%? 30 min EC 83%, a17% Spall Th; Pb(C'%, spall)
’a?'% 2.7h: ' a-96%, EC~4% Spall Th; Pb(C %, spall)
RnZ!! 16 hr EC 74%, a26% Spall Th; Ph(C'%, spall)
Rn?!'? 23 min a Spall Th; Pb(C ', epall)
Rn% 1> ~10705ec {est.) a U??7chain from Th?32
(2, 9n)
TABLE OF ISOTOPES OF He, Ne, A, Kr, Xe, 'and Rn, (Cont'd)
Isotope Half-life Type of Decay Method of Preparation
Rn’ 16 ~10"%sec (est. ) a ~ u?28 hain from Th232
| (a.8n)
Rn? 17 1072 sec a - U%%%nain from Th?3?
. (a,7n)
Rn218 0.019 sec a U230chain from Th232
| (a, 6n)
' R.nz'19 3.92 sec a Member U2'35.deca.y
| chain
anzo 51.5 sec a Member Th232' decay
| chain
Rn?%! 25 min B ~80%, a~20% Th%>%(p, spall)
anzz 3.8229 day a | Member Uz'38 decay
"chain
III. REVIEW OF FEATURES OF INTEREST
IN RARE GAS RADIOCHEMISTRY
The rare gases, Group O of the periodic table, are helium, neon, argon,
—'kry-pton, xenon, and radon. Helium and neonl possess no radioactive isotopes
of half-life long enough to permit radiochemical studies in the ordinary sense.
One can conceive situations in which the separation of the remaining four rare
gases from contaminants and from one another might be necessary. However,
the most common problem by far is the separation of krypton and xenon re-
sulting from fission of heavy elements from other fission producte and from
each other. The literature on rare gas radiochemistry is \largely concerned
with this problem, and most detailed discussion in this monograph will like-
wige center around krypton and xenon. As rare gas separations generally
depend on some property which varies greatly and in a regular manner as one
proceeds through the group from helium to radon, the further applicati'on of
the procedure to include other rare gasea will often be simple if required.
Reviews of the '""chemical properties' of the rare gases will be found
in most texts on inorganic chemistry. . In a practical sense, the rare gases
are chemically inert. They will remain chemically unaltered in any reactions
chosen to quantitatively remove impurities other than rare gases from them. .
However, rare gas atoms do interact with other atoms,. molecules, or ions in
their neighborhood. Whether these interactions are properly considered
chemical or "van der Waal's' in nature is of no concern here,
The existence in discharges of species such as HeH" and He2+ has been
established. Hydrates for the four heavier members of the group are known
to exist, and solubilities of rare ga.ae.s in a number of solvents are relatively
high, Solubility in a given solvent generally increases with atomic number of
the rare gas._ A number of studies of rare gas solubility dependence on sol-
vent, temperature, and partial pressure of the rare gas (Henry's law is ap-
plicable over wide ré.nges) have appeared in the literature. One of the more
comprehensive studies also outlines a proposed system for recovering krypton
and xenon from gas streams by their absorption in a counter-current stream
of organic liquid (kerosene). 2
In handling rare gases, especially tracer amounts, one does well to
remember that co_nta.?:t with liquids or solids (including system walls) or
condensation from the gas phase of other liquids or solids may result in re-
moval of rare gases from the gas phase through solution, adaorption or phys-
ical occlusion. Thus in quantitative work rare gas carriers are usually added
for essentiallylthe same reasons that carriers are added for species to be
separated from solutions, . .
A series of substances known as clathrates has received considerable
3,4 Clathrates of argon, krypton and xenon have been prepared by
study.
crystallizing quinol under an atmosphere of the rare gas at high preasure.
Rare gas atoms are contained in "cages' within the reéulting crysfal, the
number of these cages setting an upper limit on the amount of rare gas in the
crystal (one rare gas atom for every three quinol molecules). The actual
concentration of rare gas in the crystal depends markedly on the conditions of
crystallization and is usually considerably less than the theoretical limit. '
Clathrates of fission-product krypton have recently been prepared for use as
sources of Kr85 activity. > The preparation described in the reference re-
sults in krypton concentrations equal to 25% of the theoretical limit, This
correEPOnds to the concentration in the gas phase at about 25 atmosphéres
pressure and results in 3 curies of Kr85' per gram of clathrate (using fission
product krypton. which is about 5% Kr85). The material may be ground to a
powder with no appreciable loss of activity and the loss on standing is only a
few parts per million. per day if the material is protected from water and
other subsfancea which dissolve quinol. '
The chemical operations involved in separating and purifying rare gases
are performed on elements or compounds other than rare gases. The Bepara-
tion of the rare gases from one another must be accomplished on the basis of
differences in some physical property (usually vapor pressure or extent of
6
adsorption). It may often happen that this physical separation will also sepa-
rate some or all of the impurities other than rare gases from a particular
rare gas. Thus it ie often neither necessary nor most convenient to purify
the rare gases chemically as a group as the first step or steps in a radiochem-
ical procedure. Depending upon the conta.ml:.nati.ng species and their amounts
it may be possible that no chernical operations whatever will be necessary.
Substances which may contaminate rare gases are limited to those which
may exist in appreciable concentratione in the gae phase at the temperature of
the experiment. At said temperature thie will include: 1) gases, the term
being used here to denote appreciable amounte of substances above their
critical temperature or having vapor pressures greater than 1 atmosphere;
2) unsaturated vapors, substances whose vapor presa-urés are less than one
atmosphere but which are present in amounts appreciable but small enough -
that their partial pressures are less than their vapor pressures; and 3) satu-
rated vapors in equilibrium with solids or liquids having appreciable vapor
pressures. The word "appreciable in the foregoing must of course be de-
fined in the context of the experiment. Although the above is a large category,
the number of contaminants usuélly encountered is quite small. The rare
gas'es must often be purified from the constituents of air, from volatile species
involved in target dissolution such as hydrogen, hydrogen halides and oxides
of nitrogen, and occasionally from small amounts of hydrocarbons and trace
amounts of elemental halogens. Methods of removal are listed below for each
of these. The list is by no means complete as regards methods which have
been or could be used, but it is hoped that it is representative enough to be
useful.
1) Nitrogen: Mole amounta may be qfia.ntitatively removed by reacting
with titanium sponge, 14-20 mesh at 1000-1100°C. Use of lower temperatures
" (ca. 850°C) has been reported. 6 Oxygen is also removed quantitatively,
Quartz or ceramic furnaces are necessary as these temperatures are above
the sbftening point of Pyrexl glasses,. The reaction is quite exothermic and
so the temperature must be monitored and flow rate of the gas controlled to
prevent destruction of the furnace. Calcium has often been used aa.tisfa.cltorily
to remove nitrogen (400-500°C). Calcium does, however, tend to become
passive through formation of surface filme, For small amounts of impurities
this problem is sometimes circumvented by conducting the reaction in the gas
phase with Ca vapor. 7 Clean uranium turnings at 800°C will aleo react with
nitrogen (and decompose hydrocarbOnsB).
2) Oxygen: Will be removed with nitrogen in the above reactions, Oxy-
gen also reacts rapidly with copper turnings above 350°C to give CuO.
3) Hydrogen, carbon monoxide, light paraffin hydrocarbons: Paesage
9
of the gas stream over CuO at 500°C will oxidize H, and CO to CO,
rapidly. Hydrocarbons will be oxidized in like manner to HZQ and COZ but a
to HZO
temperature of 900°C is necessary to achieve rapid reaction. Subsequent re-
moval of oxygen may be necessary (and is easily accomplished), if high enough
temperatures are used that the dissociation pressure of oxygen over CuQO becomes
appreciable. :
4) Water: In addition to condensation of water in cold traps (a method
often not specific enough), water may be removed by passage through any one
of a number of desiccants. PZOS' Mg(ClO4)Z,' and Ca.Clz are representative,
with equilibrium partial pressures of water over them at room temperature
-5
of 2 X 10
resent the extremes of efficiency in common desiccants. Magnesium per-
, 5%x10°%, and 0.2 mm Hg respectively. P,O; and CaCl, rep-
chlorate has achieved wide use as it is efficient enough for practically all pur-
poses and is easily regenerated by distilling the water off in vacuo at 220°C.
Where 'la.rge amounts of water are involved, gases are often driéd first with
C‘.=1C12 to remove most of the water and then with Mg(GlO4)2 to remove re-
maining traces of moisture,
5} Carbon dioxide: May be removed by passing the gas through a trap .
containing Ascarite, a granular commercial preparation which is esé_entia.lly
asbestos impregnated with sodium hydroxide. Sofnolite, or soda-lime, a
mixture of NaOH and Ca0 may also be used. Sweeping the gas through a
solution of alkali metal hydroxide is' also effective. Solutions are sometimes
less convenient in vacuum systems than solid materials, ‘however.
6) Hydrogen halides: May be removed in the same manner as carbon
dioxide. | |
7) Oxides of nitrogen: Dissolution of targets in nitric acid will result
in evolution of NZO' NO and NO2 ir varying proportions, NZO usually occurs
in relatively small amounts. Its removal may be accomplished by catalytic
reduction with hydrogen or by oxidation to NO by scrubbing the gas with.a
solution of strong oxidizing agént such as permanganate. NO and NO, may
be removed by sweeping the gas stream through a solution of sodium hydrox-
ide. Performing the solution under reflux will in fact wash a good portion of
the higher oxides back into the dissolver flask. If alternate methods of solu-
tion are available it is often most convenient to avoid the us e of nitric acid. |
8)- Halogens: Free halogens are all relatively volatile,. and active halo-
gens may often be present in trace amounts in tai-gets from which rare gases
are to be remdved. If the solution process leaves them partly or entirely in
the zero oxidation state, the gas stream will be contaminated.- Sweeping the
gas through a solution of sodium hydroxide will rapidly convert all the free
halogens to non-volatile species (halide and hypohalite). 10 The rapid ex-
change of the halogens with their corresponding halides in solution is another
8
useful means of decontamination from tracer halogens, 1,12
Iodine is quan-
titatively removed by contact with silver (silvered Raschig rings have been
used as a trap packing for this purpose).- Iodine is reduced to iodide in 1’\1’a.HSO3
solution. _
Where reaction rates are slow enough that purification may not be com-
pleted in one pass, it may be necessary to circulate fhe offgases from target
dissolution through a purification train. The classic, and still most generally
useful, device for circulation (or transfer) of gases is the Toepler pump,
with which rates of about a liter per minute may be obtained. Other circulat-
ing pumps which may be useful in particular instances have been designed.
These consist essentially of a chamber designed to permit only unidirectional
flow of gas and a means of producing periodic pressure changes within the
chamber. Alternate heating and cooling of the gas in the chambet has been
used to achieve flow rates of 0,5 liters per hour. 3 An iron piston enclosed
in glass and electromagnetically operated has produced rates of a few liters
per minute ,1 Pressure differentials de.vel.dped were. not noted in the reference
but are probably small. Another achieves aimilarly. high flow rates by pulsing
the chamber pressure by means of a fnyla.r diaphragm driven by high preasure
gas. 13 .
Ultimately the radiochemist must concern himself with the physical
properties of the rare gases. Table 1 summarizes some data which may be
of interest,
Table 1
He Ne A.r Kr Xe Rn
Atmospheric abundance 5.25 1,82 0.934 1.14 8.7 6x107'%
(Volume %) x107* x1073 x10"% x107°
Boiling Point (°C) -269 -246 -186 -153 -107 -65
Melting Point (°C) -272 -249 -189 -157 -112 -71
' (25 atm.)
Atomic diameter in 3.57 3.20 3,82 3.94 4.36 _——-
crystal (angstroms)
Distillation and adsorption techniques are those which first come to mind
for separation of the rare gases. The pure rare gases have of course been
successefully produced commercially by the fractional distillation of air, with
the exceptions of helium which is extracted from certain Texas natural gases
and radon which is obtained as 2 member of the 4n+2 natural radioactive decay
séries. Fractional distillation is discussed in most texts on physical chem-
istry and the ‘fractionation of rare gases from air is discussed in numerous
places. 17-20 Glueckauf used 2 procedure combifiing fractional distillation of
air and adsorption techniques in the detg_rmination-of krypton and xenon con-
tents of the atmosphere. 21 It is very unlikely that the radiochemist will have
need to use such low temperature fractionation columns in the laboratory so
there will be no d'iscussion. of the method here.
On the other hand, simple distillation and condensation processes will
be used in practically every experiment in transferring gases or effecting
rough separations. Thus a plot ( for low temperatures) of vapor pressures as
a_fu.nction of temperature for rare gases and other volatile species commonly
encountered will prove very handy to the radiochemist. The reader is refer-
red to the generally ava.fl.able Handbook .of Chemistry and Physuca22 for data
necessary for such a plot. Dushma.nZ (page 781 et seq.) also tabulates vapor
preasuré data for a number of substances at low temperatures. In order of
decreasing volatility (decreasing vapor pressure at a given temperature below
the critical temperature) the common gases are NZ' A and 02. Kr, Xe, Rn
and COZ-. and HZO' Gases listed in pairs have vapor pressure curves at low
temperatures which are very similar,
Efficiencies of processes such as the transfer of a gaseous species con-’
tained in a system to a cold trap attached to the system are determined by the
relation of the initial pa.rt-ia.l. pressure of the species in the system to the vapor
pressure of its solid or liquid after condensation in the cold trap, As an ex-
ample, the vapor pressure of solid Kr at -195°C ie 2-3 'mm Hg, so roughly
99%' of the Kr in a system at 20 cm Hg pressure may be collected in an attached
small cold trap at -195°C. As liquid nitroger is generally the coldest con-
veniently available refrigerant, Kr is often manipulated by condensation at
this temperature. The resultant losses decrease with increasing initial krypton
pressure and may be minimized by using- the emallest systeme and the [a.rgest
amounts of krypton carrier practicable -- usually they may be made small
‘enough that they are acceptable for the sake of epeed and convenience. If one
must of necessity collect krypton at pressures comparable to 2-3 mm Hg from
a system, he must resort to lower temperature refrigerants, refrigerated
adsorbents such as charcoal, or Toepler pumps. Presence of small amounts
of noncondensible gases may seriously lower the rates of transfer procegses |
such as the above krypton condensation, due to the relative slowness of gas-
eous -interdif_fusio_n processes. Thus one wishes a vacuum system with a base
pressure orders of magnitude lower than the lowest vapor pressures involved
in nganipulazions ‘he may wish to perform. Systems with base pressures of
10 to 10 © mm Hg are easily constructed and will suffice for the'manipula-
10
tions involved in most rare gas radiochemistry (assuming that macro rather
than tracer amounte are involved). |
Removal of only the least volatile species from a gas stream is feasible
when a temperature can be found at which its vapor pressure ie sufficiently
less than its partial pressure in the gas stream that condensation is essen-
tially complete, while the vapor preseuree of other constituents are higher
than their partial pressures over the t:rap'. Assuming equilibrium conditions
and insolubility of the other epecies in the condensed phase, passage of the
g3s stream through the cold trap effects the desired separation quite simply.
Iflc;ondensa.t'ion occurs under equilibrium conditiona, the fraction of species
lost (passing through the trap with the gas stream) is the ratio of its vapor
pressure at trap temperature to its partial pressure in the influent gases. To
' improve the approach to equilibrium conditions, flow rates are limited and
cold traps packed with some material to provide a large contact area and to
prevent mechanical blow-through of condensed materials. Glass wool, beads
or ringe are materials commonly used for this purpoae. Stainless steel bails
(3/16 in.) combined with suitable glase wool plugs have aleo proved very sat-
isfactory. Such a packing has the advantage that the steel may be warmed by
the induction of eddy currents in it to achieve rapid and efficient removal of
condensed materials. Time for thermal equilibrium to be reached in traps
must always be allowed before initiating gae flow. As cooling of trap packings
under vacuum may be quite slow, temporary introduction of some easily re-
movable gas such as helium to improve heat transfer is often useful.
In like fashion several condensed materials of widely differi.izlg volatil-
ities may often be separated by warming to a suitable tempéra.ture and distilling
the more volatile components into another cold trap. It is often necessary to
melt and refreeze the condensate remaifii.ng behind several times, each time
removing the volatile material evolved to the other cold trap, to effect com-
plete removal of occluded or dissolved traces of the volatile materials (e.g..
the distillation of CO, from CO,
The subject of trap refrigerants should be touched on briefly, Liquid
-ice condensate at dry-ice temperature),
nitrogen (-195.8°C}, dry ice (-78. 5°C), and ice (0°C) are commonly available
in most laboratories, -Fortuna.teljr temperatures lower than that of liquid
nitrogen will usually not be required in handling rare gases other than helium
and neon, It might be noted that pumping on liquid nitrogen will cool it by
evaporation to its triple point (-210, 9°C, 96.4 mm Hg). Témpera.tu.rea inter -
mediate to those of liquid nitrogen, dry ice, and ice are often necessary and
are commonly obtained by cooling a suitable liquid with liquid nitrogen or dry
ice to obtain a partially frozen '"slueh'" at the melting point. Slush or liquid
refrigerants provide better heat transfer from the trap than solid refrigerants,
11
thus dry ice is usually mixed with acetone to provide a slush refrigerant at
-78.5°C. Discussion of cold baths may be found in most texts where vacuum
24,25 The author has found the following baths par-
techniques are discussed.
ticularly useful in working with rare gases: acetone, -95°C, n-pentane, -130°C,
and isopentane, -160°C.
It is usually most convenient to refrigerate traps through which large
~ quantities of gas will flow with liquid nitrogen, dry ice, or ice since such
traps are easily replenished in place on the line. '"Slush-cooled' traps at
other temperatures may usually be reserved for 6pe1-a.tions where they need
take up only small amounts of heat.
Adsorption and Adsorption Techniques
By far the majority of separations of rare gases to be found in the litera-
ture have employed adsorption techniques. Of the large number of adsorbent
rnaterials available, a.ctivated- charcoal has most often been us.ed because it
has the largest surface area (largest adsorptive capacity) per unit mass and
because the rare gases adsorb on charcoal to widely differing extents.
For a given adsorbate gas and adsorbent material the amount adsorbed
per unit mass of adsorbent, called v and usually expressed as cc STP
(Standard Temperature and Pressure,i.e., 0°C and 760 mm Hg) of gas per
gram adsorbent, is a function of temperature of the adsorbent and partial
pressure of the gas over the adsorbent. Three functional relationships among
these variables are of interest: 1) Isotherms showing the dependence of v
on P at constant temperature; 2) Isosteres relating P and T at constant v;
and 3) Isobars relating v and T at constant P. In experimental studies of
adsorption the isotherms are most usually determined at a series of tempera-
tures. From these data the other relationships may be obtained if desired.
The Clausius-Clapeyron equation also relates heats of adsorption and the pres-
sure change with temperature (shape of the isostere),
A number of equations have been used to exp-resa adsorption isotherms,
most of which are empirica.l in nature. Langmuir first derived the hyperbolic
isotherm for monolayer adsorption from theoretical considerations. 26
Brunauer, Emmett, and Teller27 later .derived equations for multilayer ad-
sorption which reduce to Langmuir's equation in the case of a monolayer. The
hyperbolic isotherm may be written v = vsbP/(l +bP), P = v/b(vs—v) , or
P/v = l/b\a"3 + P/vs » where Vg is the cc STP of adsorbate requiret_:l to
form a monolayer per gram of adsorbent, and b is a constant dependent on
temperature and the nature of the adsorbate and adsorbent. The last form is
particularly useful for the extension of data by interpolation since the plot of
P/v versus P is linear. At low pressures, or perhaps more definitiw;rely low
12
v , it is found that adsorption obeys Henry's law (v = kP), and interpolation .on
a linear plot of P- versus v is possible. It will be noted that for P much less
than 1/b, or v much less than Vg the hyperbolic isotherm reduces to Henry's
law with k equal to ‘m_rB . Freundlich's parabolic equation (semi-empirical in
nature) is often useful for linear interpolation on a log-log plot in cases where
it is obeyed: v = KP /n . Peters and Weil28 studied the adsorption of argon,
krytpon and xenon on charcoal and calculated the constants in the Freundlich
equation from their data at several temperatures, These are given in Table
2 for handy reference. Adsorption data for a number of gases on charcoal are
tabulated in Chapter 8 of Dushman. 23 The adsorption process releases heat
and as expected from LeChatelier's principle adsorption decreases with in~
creasing temperature, other factors remaining constant. Adsorption increas-
es with increasing pressure. Adsorption of different gases tends to increase
with decreasing volatility (extent of adsorption tends to increase in the same
order as the boiling points of the gases),
Table 2. Adsorption constants for argon, krypton
and xenon: v = KPl/n
T°C K 1/n
Argon -80 0.500 0.950
-18 .0.0764 1.0
0 0.0581 1.0
Krypton -80 : 2.927 0.711
-18 - 0.497 . 0.885
) 0.340 1.0
Xenon _ -80 15.99 0.574
' -18 2.458 0.692
0 1.583 0.77
Theoretical treatments discuss adsorption in terms of: 1) formation of
a monolayer of adsorbate on the surface, 2) formation of multilayers on plane
surfaces, and 3) capillary condensation in small pores. Adsorption of a gas
is considered the result of van der Waal's forces of the same type involved in