V J \ I X THE EXTRACTION AND PURIFICATION OF CAESIUM SALTS BY JOHN DRISCOLL CONATY THESIS FOR THE DEGREE OF BACHELOR OF SCIENCE IN CHEMISTRY COLLEGE OF LIBERAL ARTS AND SCIENCES UNIVERSITY OF ILLINOIS 1922 to UNIVERSITY OF ILLINOIS i92_2__ THIS IS TO CERTIFY THAT THE THESIS PREPARED UNDER MY SUPERVISION BY JQHK_DftI_SC_OLL_C^^^ ENTITLED__THS_MTMQTI_Qli_ANp__PURl£XCMIM__QF_Cj^_SIU^^ IS APPROVED BY ME AS FULFILLING THIS PART OF THE REQUIREMENTS FOR THE DEGREE OF Bac_he_lo_r p_f__Scjience__i^^^^^ Instructor in Charge Approved : /I Ct / q HEAD OF DEPARTMENT OF C_HEMI_ST_RY_ i Digitized by the Internet Archive in 2016 https://archive.org/details/extractionpurifiOOcona Acknowledgement . The author wishes to ta,ke this opportunity to express his sincere thanks to Professor B.S. Hopkins at whose suggestion this work was carried out and to whose aid and advice its successful completion is largely due. Tabla of Contents. I. Historical II. 3xtraction of Caesium from Hollucita A. Decomposition of the Llaterial B. Precipitation of Caesium as the Double Lead Salt According to the Method of ¥ells. Page 2. e. Precix-)i tation of Caesim as the Double Antimony Salt According to the Method of Godeffroy Page 3. D. Discussion of the Results and Precautions Page 3. Page 1. Page 2. E. Diagram of Method for the Extraction of Caesiura from Pollucite as Cs^Sb^Clg Page 5. III. PractionG.1 Crystallization of the Alums of the Alkali Metals A. Historical Page 6. B. Plan for Systematic Practional Crystallization of the Alkali Metals Page 7. C. Results Obtained fro.m Praction- ation Page 8. D. Solubility of cs and Rb in the Presence of yunmoniua Alum Page 9. « ' ' ' v; - '• '■■ T '<\rm '■<. ,^'ifr/ 'V'^,,f pi ‘ ■' ra«P^ ^ ^«|!k^?v 4.7 /I ft " f- ' ♦ ■•■ - ' ' .V , ^ ^ -- - '• • . ,.Ki< f.*;c<«?fc 4iC Uw 'f'". ■ ’^!™' V *' '-^ - -■'■ '■ ■’ • r U'i Xj»Ji'z«ife.... *'iu ji? poi!i^ j;«o^p?^^-. p, ■ ' - .- \ ji»t-’.'" ■'M' » .rjuittxiO Cj ftci '->^,1 iv* ‘ V?. ♦ . ' '. 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The filtrate snov/ed tjie spectral lines tor sodi’um, potassium and litnium, “and, "besides tnese, tv/o splendid lines near the blue strontum line Bunsen and Kirchiiolf add: “As no elementar 3 ,' oody produces two blue lines in tni s portion of the spectru.'a we may consider tne existence of tni s Hitherto unknown alkaline element was placed beyond doubt. The tacility witii whicn a few tnousandtns of a miliigrtim of tni s bod;^’" may be recognized by tne brigiit blue of its in- candescent vapor even wnen mixed witn large quantities of more common alkalies, has induced us to propose for tne name caesium (and tiie ^'mbol (js) derived from tne Latin caeslus, used to designate tne blue of tne clear sky". Caesium is found widely distributed in nature in small amounts Lepidolite (Li ,E,Na,F,Al(Si 03 ) j) a mineral occurring in considerable quantities near Pala, San Diego Co., Calif., also at Paris and nebron, :ie . , contains from .3-1% Cs^O. Pollucite a mineral occurring on tne island of Elda and at Hebron, Me,, contains from 30-35% CS 2 O . it MB ' ; ’rrj.M'jv ;uvi , • '^- ■:■'^■^■ •. . .4 r^\fi^ /..'/’•’irr ■ » ■- ^.' ' ^ : . K.- /^utfO#TI^E' ^’1 . y |£' *V' . >.'- V V .' ^ L-l 1 . > fli't t.t;’ «^»v> .4 /l;.. p^n v-Ji. .r. "-■‘ ‘ 0 « .1. 1' ivj^j e,»^>^5. U4.-*ji| ■ ,' ' ’'■ W, " ‘ : • t i,X : tici. tiMpfaM’ f' . iiajs^c%.t« i *'^• HL ■ '■ i ' « *^>2n oicf "■‘' ■ ' ■■ • ■ ■■r ,.,,Xigta XA*>j^i'‘, -.At #-' - '*< vf(j».;t(4' ''t'rWiy^c^.u-'sAi Tp^cclj ■ ■■ • ^ V. ■ ■ ' ' r-foM - Utirift >^X 'rc‘*7*^ AMI* »* • i '' . #xif^(x>WM (^4 . j' - fJ >f . m .r . ■ ^ :'r S' ■*; I ' li? Mt i:- i^4ic!f' MAjr jVi.c *m 1 t% * ^-C#.^S^^rtUJt ^7 'i, f,#r,.«'.i‘ r » ' -.- i-T. .A - V .• ..f ■ T ‘T f ■ , v^, ^ • .tg 'iii^ff .'lirtr. R^4#ai V ..i’ r " ' '3^ V ' i.' ' . 1 *« » )^-m Xtn|t;aMH. ( j. U i ' i^'tl. X, .till ' p^U4)5.X ”L. t . f ' • . i ?r-*'. i,ftn f.).i«4oo* ‘ , .*i„ ,'i5n:e»u i/»4 • tiwi ♦ V’ - ' -fc " ■ ■ " '.'Js" :d 4‘i^*oi£ ’^i^#b'tksL^ €iJX«;' J §fS V . ,1 ' y . '■": . h ^ .iV 'i*. . 'V'- . iMllj. .1.iS Vi'^' ',4a'{ •.-«?« 2 . ^traction of Caesium from Pollucita Decomposition of tlie Material Tile mineral was finely pulverized by grinding in a Ijall mill, placed in large evaporating disn.es and digested from 48 to 60 hours v/itn dilute nydrocnioric acid (sp.gr. I.l2). At the end of this period tne mixture was evaporated to di%*- ness on tne water datn alter wnicn it was carefully heated over a free flame to dehydrate tne silicic acid. The material was then taken up with v/ater and enough dilute hydrochloric acid added to dissolve the iron salts, and the silica filtered off . Precipitation of Caesiun as the Double Lead 8alt According to the Method of Wells Several methods are described in the literature for the isolation of caesium from the nydrocnioric acid extract. Wells'^ has recommended the use of tne yellov/ salt 2CsCl PbCl^ in which tne precipitation is made by adding a hot concentrated solution of tne calculated amount of lead nitrate to the crude hydrochloric acid extract. Chlorine gas is then passed in until the solution is saturated. After allowing to stand for ten to twelve hours tne solution is decanted from the pre- cipitate of 2GsCl PbCl^. Tne precipitate is then boiled with ammonium carbonate after which the Pb O 2 filtered off. only one run was made on a samx^ls of Maine pollucite as tne yield of caesiuia chloride v/as veiy small as compared with the heavy and large amount of precixJitate forraed and the r 'f 'fh t ii’ ■ i •• ■•iV. ■».* >• ^ .. • "'V'' /, ^ f-'.> • ■ ' /A-. . ' T'.v -i ' '*i‘ ■ ^ :. r V., of'i; , 4 ".‘l V k ; .< J » .. mK- t V^jyv^;otV ta ••n-’' arju^j cltf^fviX •a 10 Bni4’A»v . n^T-.* " * ^'.' ' #j' ■ »**-•"■ IT c'r xj>-- nr, . oy ...j ■'’Ji ■'» bu* ,':%^v3 'It- ,;>;Ar.au % VTVc-i;i^'rr;(|,ltiiJi'.S./^^^ j *■0 a?l: •. »i{J ^•^o‘d#i5<>it Q^jb ,t/jl f ^ ^ "^T rt... r' ftflj i J' I . Sr 'J, J ,7> ‘ ■ •* ’■, t* J c 'iitom-.->t‘ 'I 'lo > Lv* 3 - {vf^idb ’Bi " , t»>ro ?- f?i i V n . j/^ ») Ik iti(- •J'"X3 ^ * -■ -ntf / . , ♦ivfjrtts .. .i.ji/ rrji*^'' E,tif rii j x*i^\*^iu£Tto 'To .1.1,^ .jrlo-s ’ * . i:i o *6c i *>;> X *7 ‘yi * • ' * "» '" ' ' * * ■ * ' *' ' '' '*5 ' “■ ■. r^i^ 1^1^ W ji- . &ioii Cii'x./ */: ,«5st»f,c»r xXa.f 6 cf ■ li®ll ■- ■- ■ O ,■■*’■; ' ■'yw V* : (} » *t ^iiro ‘>»sesXX/ J‘i r'U; sliua i .-i>. t ^ ■5'T 1* / ■ ' ^ i/:%''fiii ^ « ,'» piwVJ.Vi'i ■x: ''^^ '^'^i 4 i *■■'■■• ';)i:4„ ■■ ^aV V'^^4-V :.\;.l';i(VVV)^ c J#o':4^: •fife' * * *-i ”■ ’ . ■ * ■ ‘ . >4' ' ■*'. ' ® ■"., ,• ■•' ■ « ’ ' -’ ? ,T ''C;^' f.->^ %‘fc ' d j5?i!v^44 T{ ''^.‘K/-€m -v Xs^y ♦4<3R-Tlu» / ,. y %■ •• j ,' 'T^" ' ^ "' ' >.r Jgr^.‘ *« * ?.»’ f’cx-^' ftj rs. u^tii•i _ V .V - ’‘iA , #,.,-A.'’;.i , ^ ■ i^air ■ a f>>‘;- .' 4, vS ' cl>t-t.-;. ■^v'j' i»K.^ •’^.’ *’ - ' ■ ;-»i ‘ ‘^1 ^t.i:. R-. i 1‘S^v.--; ' 5 Diagram of K<9thod for the ijjxtraction of Caesian from Pollucite as GSjSb^Clg SiO^ ^tc. Pollucit e Boil HCl sp.gr. 1.12 48-60 hours Uvaporatiou and Filtration Solution; Alkali ..petals, CsCl PbO. Recr>" stall! zed from hot water 6 Fractional stall izat ion of the Alums of the Alhali Metals. The soluhilities of the alums of sodium, ammoniura, potassium, caesium and rubidium as stated in Comey are as f ollov/s: Parts in 100 Parts V/ater T «mp . Pota.ssi'om alum 13.5 17® Ammonium alum 8.74 17.5 SodiuTi alun 103.1 10 ® Rubidium alum 2.27 I 7 P Caesium alum 0.619 17® Rohinson and Hutchins^ v/ere the first to point out this difference in solubility and recommended it as a me.ans of separating caesium and rubidium from lithiun and potassium in lepidolite after the mineral had been decomposed v\ritn hydrofluoric acid. They also pointed out the difference in solubility of caesium and ruoidiuin alums and recommended a fractional crystallization for the separation of these elements. Hov;ever, tne difference in solubility of ca.esiua and rubidium aluas is not great enough to allovr a rapid separation of these elements, v/hile the difierence in solubility of the alums of the rare metals and those of the common ones is suificient to make a sati sfactoiy method of separation. 7 . Plan for Systematic Practional cry atallizc tion of Alums 01 tne Alkali Metals. i M The pollucite was decomposed in tne usual manner with | ny drocnloric acid and after evaporation and filtro,tion of | tne silica the hydrochloric acid extract was concentre ted i witn sulfuric acid. On cooling the mixed aluius ciystaliized | r out. 'i'nis is the most advantageous and rapid method to ( remove caesiuiri from pollucite. The mixed alums vdiile con- ! f taining traces of iron were in two to three ciy stallizations t free from iron. s. Tile alujTis (1) from 3400 grams of pollucite containing approximately 12/^ CS 2 O were subjected to ^'Stematic fra.ctional cry stall iza,ti on by dissolving in not water and stirring vigorously wnile tii9 solution yjaz cooling to destroy the supersaturated solutions which these alums especially caesium tend to form. The motner liquor v/as concentrated until on cooling it yielded a second crop of ci^’stjils, (6) and the ne \7 mother liquor concentrated again to yield a third crop of cr;>’stals (12) and so on. The crystals in the first crystallizing disn (2) were d.issolved in not water and allow- ed to crystallize again (4) the supernatant liquid (5) being used to dissolve the^ second crop of cr;>'stals (6) and allowed to re cr;>' stall ize tni s scheme being continued in all the dishes. The cr;>*stals separa.ting in the first dish wrere repeatedly recrystallized from hot v/ater. By tnis system tne cry^stals in tne first of the series were tJie more insoluble alur^s of caesium (and rubidium) while those in tne lov\rer end of tne series were tne more soluble alums namely sodium and potassium. Results Obtained from Rractionation of the Alums. After the alums from the pollucite were recrystallized nine times the crystals in the insoluble end of tne series gave strong tests for caesium and traces of sodium, and potassium while the crystals in the more soluble end (ninth dish) gave strong tests for sodium and potassium a.nd traces of caesium. W'i) JmV' I?N^’ . • 7 ’CK r , '. . ' ■ J • . il,” V '* ' ,, ,.. :^L * * ^■f!" •. . ', .'•7^': :.-A-‘ , ’’(kV? i, ‘>>;A*i,- C'X )' ' <>1AB|. . ;’>4» fU 94 i yl* W ; . ■ 'i '■• n -xiSSt Jloii.6«j>r' ■ ;f ’*v. ■■■'■w^.r4t,v/J " ■ . * ' . '^r':' , '"0.4 ,> ■•: '..'^Vifl , i’V4 ^V ,,v,r .V, ..'W^ ,V-. V ■ 'MM : / \ ' V-- ■' . •* ' ■•" v-'V^’^ ’^r- ■■" •>w#> . .. v'f.) + ■• t ,L i ‘.' i'V ♦■r>' r^v * ? * /.H) \lim ^ ^ ^ ^ ^ -‘ ««l it> 1 - -■"sj" <.'•• tr,i =^r-,.'= , . ti», . v/-'. 'v' ^ _.. 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After the process of ciy' stall i aati on was carried througii twenty-four crystallizations the spectruLu saioived no evidence of tne presence of rubidium in the tv/enty -fourth dish v/hile the first dish showed nearly pure caesium with traces of sodium. Solubility of Caesium and Rubidium in the Presence of Ammonium Alum. 7 browning and Spencer have determined the solubility of caesium ana rubidiuiL in a saturated solution of ammonium aluiii. They found that Ic.c. of a solution of RbCl containing 0.0002gm. v.'ould give a perceptible precipitate v/hen treated with 5c. c. of a saturated solution of ammonium alum and that Ic.c. of a csCl solution containing .00005gm. cs v/ould give a precipitate of caesiun} a.lum. u r •>.« t ••'-'i Jii -i ’^v' V ' S 'i> ' . ■ ► ,.-'f /',.*' H i: , . , I ' ' p? ^ ^ r— ■ — ' ' , 'V.'”"' > ' )‘. • y ■'-» V--- ■■'vtairMS • •• s' •■, w • ■' ■ ■’■'■ ■fii ■'ti, - : -^SPJH ' '■■*■' , i . ?' , / V '*'4 '■. »'!»■«■ -■ nr. I •^VTV ' 0 ! .. ■».;.' 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