Table Of ContentOTHER  TITLES  IN  THE  SERIES  ON 
ANALYTICAL  CHEMISTRY 
Vol.  1.  WEISZ—Microanalysis  by  the Ring  Oven  Technique 
Vol. 2.  CROUTHAMEL (Ed).—Applied  Gamma-ray  Spectrometry 
Vol. 3.  VICKERY—The Analytical  Chemistry  of the Rare  Earths 
Vol. 4.  HEADRIDGE—Photometric  Titrations 
Vol. 5.  BUSEV—The Analytical  Chemistry  of  Indium 
Vol. 6.  ELWELL AND GIDLEY—Atomic  Absorption 
Spectrophotometry 
Vol. 7.  ERDEY—Gravimetric  Analysis,  Part  1 
Vol. 8.  CRITCHFIELD—Organic Functional  Group  Analysis 
Vol. 9.  MOSES—Analytical  Chemistry  of the  Actiniae  Elements
THE  ANALYTICAL 
CHEMISTRY 
OF  THORIUM 
by 
D.  I.  RYABCHIKOV  and  Ε.  K.  GOL'BRAIKH 
Translated by 
A.  D.  NORRIS 
LECTURER IN PHYSICAL CHEMISTRY 
THE UNIVERSITY OF HULL 
Translation edited by 
R.  BELCHER  and  L.  GORDON 
P E R G A M ON  PRESS 
OXFORD  ·  LONDON  ·  NEW  YORK  ·  PARIS 
1963
PERGAMON  PRESS  LTD. 
Headington  Hill  Hall,  Oxford 
4 and 5 Fitzroy  Square,  London,  W. 1 
PERGAMON  PRESS  INC. 
122 East  55th  Street,  New  York,  22,  Ν. Y. 
GAUTHIER-VILLARS  ED. 
55 Quai  des  Grands-Aug  us tins, Paris,  6e 
PERGAMON  PRESS  G.m.b.H. 
Kaiserstrasse  15, Frankfurt  am  Main 
Distributed in the Western Hemisphere by 
THE MACMILLAN  COMPANY  * NEW  YORK 
pursuant to a special arrangement  with 
Pergamon Press Limited 
Copyright  ©  1963 
Pergamon Press Ltd. 
Library of Congress Catalogue Card Number  63-10065 
This translation  has been made from  the  Russian 
ANALITICHESKA  Y A KHIMIYA  TORI Y A 
Published  in Moscow,  1960, by IzdateVstvo  Akademii  Nauk,  SSSR 
Set  in Monotype  Times  New  Roman  10 on 12 pt.  and printed  in Great  Britian  by 
J. W. ARROWSMITH  LTD.,  BRISTOL
GENERAL  INTRODUCTION TO  THE  SERIES 
THE V. I. Vernadskii  Institute  of  Geochemistry  and  Analytical 
Chemistry of the Academy of Sciences of U.S.S.R. has embarked 
on the publication  of a series of monographs  on the  analytical 
chemistry  of various  elements. The  series will include about  50 
volumes in all, and will be issued over a period of about 5 years. 
The need for such a series has been felt for a long time, and now 
that a large amount of experimental material has been accumulated 
in many laboratories it has become both possible and  necessary 
to proceed. The projected series will be the first of its kind. 
The analytical chemistry of any element and its compounds is 
in these days a complex subject with many aspects, both because 
of the complicated  nature  of the  results required  and  the  wide 
concentration range which must be reckoned with, and because of 
the  variety of  available  methods. A general plan  has been  laid 
down for the monographs, both as to contents and as to arrange-
ment of material. 
Each monograph will contain general information on the proper-
ties of the chosen element and its compounds. A description will 
then be given of those chemical reactions which are of importance 
for  analytical  purposes,  followed  by  an  account  of  physical, 
physico-chemical  and  chemical  methods  which  may  be  used  in 
the quantitative determination of the element—commencing  with 
the analysis of the ores, and continuing with end products  such 
as metals, alloys, oxides, salts and other compounds and materials. 
As a general rule the principles of the method  of  determination 
are first given, and are then followed when necessary by a detailed 
description  of the whole process. Rapid methods of analysis are 
noted where necessary, and a separate place is given to the methods 
of determination of the so-called impurity elements in pure mat-
erials. 
Attention is given to the precision and sensitiveness of methods, 
in accordance with the general tendency towards increased sensi-
tiveness in methods used to determine trace quantities of impurity 
elements. 
The monographs will contain a comprehensive list of references 
ix
χ  GENERAL  INTRODUCTION  TO  THE  SERIES 
to  recent  literature,  which  should  be  especially  useful  to  a  wide 
circle  of  chemists,  and  especially  analytical  chemists  in  research 
institutes  and  factory  laboratories  and  in  various  other  aspects 
of public life, as well as for teachers  of chemistry  and  students  in 
higher  academic  establishments. 
The preparation of the monographs has been placed in the  hands 
of the most eminent specialists in the particular  fields  of  analytical 
chemistry  concerned.  The  separate  volumes  will  be  issued  inde-
pendently  as  they  are  ready.  The  monograph  on  thorium  is  at 
present prepared,  and  those  on  the  analytical  chemistry  of  pluto-
nium, lithium and  gallium, amongst  others, are under preparation 
for the  press. 
We  should  welcome  suggestions  and  opinions  from  readers  of 
the  monographs. 
The  Editorial  Board.
FOREWORD 
THE use of thorium as a raw material for the manufacture of nuclear 
fuel,  as well as in other  recently  developed  technical  fields,  has 
stimulated a comprehensive study of the element. A large number 
of works have been published in recent years, giving detailed infor-
mation on the properties of the metal and its compounds, especially 
those used  in the isolation  and  determination  of the element in 
natural  and  industrial  materials.  The  literature,  especially  that 
published  abroad, contains  reviews  of the chemistry and  analy-
tical chemistry of thorium by C. J. Rodden and J. C. Warf [1710], 
G.  Moeller,  D.  Schweitzer  and  D.  Starr  [1503], G.  T.  Seaborg 
[1816-20] and J. Katz [1180], and others. Unfortunately,  however, 
these reviews are far  from  comprehensive,  and  leave  untouched 
many investigations reported in various journals. 
Because  of this  we have  attempted  here to  give a  systematic 
treatment  of the available factual  material. The more than 2000 
references to work used in the preparation  of this volume  com-
prise the great majority of those published in the last decade, but 
it is impossible even for such a survey to keep pace with the new 
publications, which appear constantly in a science which is develop-
ing so rapidly. 
In addition to the strictly analytical section of this book, a chapter 
is provided on the physico-chemical characteristics of the element. 
The four  following  chapters  describe the chemical and  physico-
chemical methods of determining thorium, its removal from  ele-
ments occurring with it, and its determination in various natural 
and industrial materials, as well as the determination of impurities 
in the metal. References to literature not actually used in the book, 
but likely to be of interest to analytical chemists and  specialists 
in other fields of science, are given in the text in smaller print. 
We have arranged the material in relation to the importance of 
the various reagents, and have adhered to the commonly accepted 
classification of organic substances. 
The authors wish to express their gratitude to their colleagues in 
the Institute who have helped with advice during the preparation 
of the manuscript  for  the press, and  would  particularly  express 
xi
xii  FOREWORD 
their appreciation to Correspondent-Member  of the Academy of 
Sciences  of  U.S.S.R.  I.  P.  Alimarin,  to  Doctors  of  Chemical 
Science P. N. Palei and V. I. Kuznetsov, to Candidates of Chemi-
cal Science A. A. Nemodruk  and  A. N. Ermakov, as well as to 
Candidate  of  Chemical  Science  V.  K.  Belyayev  and  Scientific 
Assistant M. P. Volynets for their help in the literature survey. 
D.  I.  RYABCHIKOV 
Ε.  K.  GOL'BRAIKH
PREFACE 
THE writer  notes with interest that  the Academy  of  Sciences of 
the U.S.S.R. is sponsoring the publication of some fifty  volumes 
on the analytical chemistry of the elements. These volumes should 
prove of great value to those working in this field, particularly as 
they will undoubtedly cover recent U.S.S.R. work. 
The present inaugural volume on the Analytical Chemistry of 
Thorium must be regarded  as one of the most important  of the 
series, dealing as it does with an important atomic energy material. 
Its translation under the aegis of the Pergamon Institute will be 
greatly welcomed. It is noted that the volume on plutonium  will 
be one of the next to follow. 
The references given in the Russian text appear to cover the subject 
up to the end of 1955, with a few 1959 entries. The present writer 
has supplied further references (with titles of papers) to the end of 
1961, with some 1962 entries. It is thought that this supplementary 
bibliography should add to the value of the book. No attempt has 
been made to classify the supplementary references, as this would 
lead to much  overlapping. The entries are alphabetical by  first-
named Author, and their serial numbers are followed by the letter 
"S". 
A.E.R.E.  Harwell  R.  W.  CLARKE 
xiii
CHAPTER  I 
OCCURRENCE OF THORIUM AND ITS MOST 
IMPORTANT  PROPERTIES 
ORES  AND  DISTRIBUTION  OE  THORIUM 
Thorium was discovered by Berzelius in 1828 during his investi-
gations of a mineral later called thorite, obtained from the island 
of Loveoya, near Brevik in Norway [371, 820]. It was given its name 
in honour of Thor, a god in Scandinavian mythology, as early as 
1817, when Berzelius formed the erroneous view that the phosphate 
of a rare earth  element  of the yttrium subgroup, occurring in a 
mineral obtained  from  Finnbo, belonged to a new, at that  time 
unknown, element [369, 370]. For the history of the discovery of 
thorium see also [364, 1555]. 
The element is widely distributed in the earth's crust [22, 42, 105, 
198, 220, 1564], of which, according to  Vinogradov  [47] it  con-
stitutes 8 χ 10~4 per cent. It is, however, only rarely encountered in 
appreciable  concentrations.  The thorium  content  of basic  rocks 
is considerably smaller than that of acidic rocks [42, 1629, 1698]. 
Thus, its proportion by weight is 1-2 χ 10-3 in granites, compared 
with  5xl0-4  in  dunites  [47,  198]. The  thorium  content  of  the 
hydrosphere  varies  between  10~5 and  10~9 g/1. [144,  178, 1153, 
1609, 1610, 1835, 2047-8]. Its weight proportion in iron meteorites 
varies from  0-9 χ 10-6 to 4-3 χ 10-8 per cent, while that in  stone 
meteorites is 2-4 χ 10~5 per cent [189]. 
Thorium minerals are most often encountered in igneous rocks, 
pegmatites,  veins  and  alluvia,  of  which  the  last  are  the  most 
important industrial sources. 
Almost  all  thorium  minerals  are  resistant  to  natural  attack, 
so that there is little tendency for the concentration of the metal 
in secondary minerals as a result of such attack. 
The  most  important  thorium  minerals  are  monazite,  thorite, 
and  thorianite.  Although  monazite  contains  only  from  1-4-28 
1
2  THE  ANALYTICAL  CHEMISTRY  OF  THORIUM 
per  cent  of  thorium  [177], the  monazite  deposits  are  the  most 
important primary sources of the metal. Thorium is a major com-
ponent  of  thorite  and  thorianite.  but  these  minerals  are  quite 
rare and have no practical importance. 
Recent  evidence  [1560,  1856, 2036] discloses the  discovery  of 
vein deposits containing thorium  in the White  Mountains,  near 
Powderhorn  in  Colorado,  as  well as in  California  [1560], New 
Mexico,  Montana,  Wyoming  and  Idaho  [1981].  Deposits  of 
industrial importance [4, 139, 303, 1021, 1384, 1921, 2027] occur 
in Brazil, India, Ceylon, Tasmania, Nigeria, and the Scandinavian 
peninsula. In the U.S.A., in addition to the locations  mentioned 
above, deposits occur in Colorado, North Carolina and  Virginia 
and other states. 
A large part of the world production is obtained from  Brazil, 
India, Ceylon and U.S.A.  [925, 1193, 1336, 1513, 2028]. Reserves 
of monazite in India are estimated to exceed 2,000,000 tons. Indian 
monazite from the Malabar coast and Travancore contains  from 
8 to 10 per cent of thoria, TI1O2, while Brazilian monazite from the 
Baia  coasts  and  Santo  Esperito  contains  on  the  average  ca.  6 
per cent [1744]. 
Monazite  is  obtained  in  U.S.A.  from  the  sand  dunes  near 
Jacksonville in Florida,  and from  California,  Colorado,  Oregon 
and  Washington  [1981], as well as from  the auriferous  sands of 
Central  Idaho.  Concentrations  of  monazite  with  around  7-5 
per cent thoria occur in isolated places in the iron-mining region 
of Marquette in northern Michigan [2018]. 
Monazite sands are also encountered in large quantities along the 
sea shores, in river beds and in coastal banks in western Taiwan. 
The thoria content of the last named varies from  4-2 to 6-8 per 
cent [2142]. 
Information  presented  at the First Geneva Conference  on  the 
Peaceful  Uses  of  Atomic  Energy  reveals  that  new  sources  of 
thorium have been found in South Korea [2142], Sweden [1919], 
Norway  [1848], Jugoslavia  [1702],  Greece,  Thailand  and  Aust-
ralia [1642]. 
The nominal price per metric ton of monazite concentrates has 
changed thus with time: $120-180 in 1922-29; $50-75 in 1929-46; 
$100-150 in  1947; and  $140-200  in  1948. Since  1949 the  price 
price has further increased to $245[1744].