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Solvent extraction in analytical geochemistry : a thesis presented in partial fulfilment of the requirements for the degree of Doctor of Philosophy at Massey University of Manawatu

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8 0 L V E N T E X T R A C T I 0 N I N

A N A L Y T I C A L G E 0 C H E M I S T R Y

A thes i s

presented in partial fulfilment o f the requirements for the degree o f

Doctor of Phi l o s ophy at

Mas s ey Univers i ty of Manawa tu

Colin Ralph Bo swell

1966

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ACKNOWLEDGEMENTS

The author is indeb t ed to hi s sup ervis or, Dro R,R. Brooks 9 for his guidanc e , advi c e and enthus iasm9 wi t h­

out which thi s work c ould never have been undertaken;

n.l s o to the members of hi s supervis ing c ommi ttee 9 Dr . C . V . Fife nnd Dr. J . C . Hawke 9 for their valuable a s s i s tanc e and advice .

He is gra teful to Geo l o gical Divi s i on D.S. I . R . for the provi s i on of the many spec imens provided by them;

Profes sor A.T . Wil s on, Vi c toria Univers i ty of Wellington for the samples of Antarctic lake wa ters and to Chemi s try Divi s i on , D.S. I.R. for the . loan of their 120-tub e Cra i g c ountercurrent s olvent extra c t i on appara tus .

The author would a l s o l ike to thank hi s wife for her enc oura gement and pat i enc e during the c ours e of thi s s tudy .

"No man i s an Iland9 intire of i t s elfe "

(

Donne � 1623

)

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ABSTRACT

A procedure c onbining s o lvent extrac ti on enrich­

oent techniQues and spectrographic analys is wa s developed for the QUanti tative deteroina tion of nany trace elenents in a wide range of s ilicate rocks and in a s eries of hi ghly saline Antarc t i c lake wat ers .

Since a great deal of the work depended on s pec­

trographi c ana lys i s 9 an inves t i gation wa s carried out t o improve the precis ion and sens i t ivi ty o f exis ting methods .

An inproved me thod for the det ermina t i on of spec tral line intens ities wa s developedq Thi s was ba s ed on the author's nodifica t i on of the partial S e idel func t i on , referred to as B-func tions. A convers i on table for the s e is given . A s cale cal ibrat ed in B-funct i ons wa s inco rpora ted into a Hilger micropho tome t er enabl ing euch values to be obtained direc tly wi thout the us e of c onvers i on tabl e s . B-va lue s can b e plotted directly o n to the linear ordina t e of s emi­

l o g paper if the s elf-cal ibra t i on nethod is us ed for eval­

uo.t:Lng line intens i t ies. Thi s result s in a s tra ightening of the characteristic curve with an a t tendant t ine saving and o.n improvement in the accuracy of the ba ckground ex­

t rapo lation . A nomographic t echniQUe wa s a l s o developed for use in conjur�c t i on with this scale and resul ted in a rapid evaluation of line intens i ti e s but with s ome l o s s in prec i s i on.

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Cathode exc i tation as dist inct from ca thode­

layer was c ompared with anode exc i ta t i on under the same

c ondi t ions. Da ta on 33 elements were used t o study rela t ive self-absorp t i on Dffects , absolute s ens i t ivi t i es , volatil­

isat i on curves , times for complete c ombustion9 and ba ckground effects . Data on

14

elements and 3 5 l ine pa irs were used to s tudy reproduc ib i l i t i es in the three ma tri c es, NaCl , CaCl2 and carbon . I t was shown that ca thode exc i ta t i on i n a

carbon ma trix afforded the grea t est pre c is i on for a number of the more vo latile elements. Anode exc i ta t i on provided generally better pre c is i on if a NaCl ma trix was used.

CaCl2 was a very unsat isfa c tory rn.a trix . li1or the more vola ti le elements ca thode exc i ta t i on provided a higher sens i t ivity than anode exc i ta ti on but with increased back­

ground and cyanogen emiss i on .

The extra c t i on of the elements Au, Zn , Cd, Hg,

Ga� In, Tl, Sn, Pb , As , Sb and Bi from hydrochlori c a c i d into the three solvents cyclohexanone 9 cyclohexanol and

cycl ohexane was studied as a· func t i on of a c i d concentra tion.

Cyclohexanone is a more effic i ent, but less selective extrac t�nt , than cyclohexanol, Cyclohexane has l i t tle extrac t ing power for these elements.

Solvent extra c t i on of hydr ochl o r i c a c i d sol­

uti ons of a ser i es of hi ghly sal ine Antarc t i c lake wa t ers int o cyclohexanone was used. to enrich the elements Zn, Pb, In1 Bi, Fe , Mn , Mo prior to spectrographi c ana lys is . For

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thi s , the perc ent extra c t i on of F e � rJn and Mo into cyclo-

hexanone from 3N hydrochloric acid wa s obta ined . Thi s

inves tigation has shown tha t one of the s e lakes 9 Lake Bonney 9 ha s mos t probably had a s ea w�ter origin o It i s also

po s s ible that another of the s e lakes9 Lake Fryxel l 9 may a l s o have conta ined s ea wa t er i n the pa st . From the rela t iv e abundanc e o f the vari ous elements in the o ther lakes , i t wa s possible t o c onduct a geochemical rec onna i s sance of the areas surrounding the lake s . Thi s sugges t ed trillt the two mo s t likely areas for minera l i sa t i on in the McMurdo Oas i s area of Antarctica are the regi on surrounding and feeding wa t er to Lake Hoare and the regi on surrounding Lake Joyc e o

A c ons idera t i on of the theory of di s c ontinuous c ount ercurr ent l i quid-liquid extra c t i on ha s shown that i t is pos s ible to s imultaneous ly determine the extra c ti on chara cteri s t i c s of a large number of element s for a given s olvent system o If thi s t echni que is c oupl ed with spec tro- graphic analys is the determina t i on is particulnrly rapi d o The extra c t i on of the elements Ti , V, er , �Jn, Fe , Co , Ni 9 Zn9 Ga , As, Nb, M o 9 Ru, Rh, Pd , Ag, Cd, In, Sn, Sb , La , vv , Re, Os , Ir , Pt , Au, Hg 9 Tl , Pb and Bi from hydrochloric a c id into me thyl is obutyl ket one wa s s tudi ed a s a functi on o f a c id conc entra t i on . The da ta were obta ined b y s tudy- ing spectrographically the distributi on pa t terns of the elements after equi libra t i on on a di s c ontinuous c ount er- current l i quid-liquid extrac t i on appara tus . A c ompari s on

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of s ome of the da ta s o obta ined with results for the same sys t em as reported by other workers showed that the tech­

nique is val id and ac curat e .

Us ing thes e da ta i t was pos s ible to devi s e a s cheme vvhich c ould s epara te Fe from the ma j or i ty of the

(

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trace elements extrac ted by cyclohexanone from a hydrochloric a c i d solut i on of a rocko By a c ombina t i on of ba tch extra c t­

i on with cyclohexanone and c ountercurr ent di s tr ibut i on w i th methyl is obutyl ketone i t was possible t o ob tain quanti ta tive da ta for Zn and Ga and s emiquant i tative da ta for In in a

wide range of s i licate rocks by spec trochemi cal analys i s . By the us e of extra c t i on int o cyclohexanone c oupl ed w i th a t omic abs orpti on spectrome try i t wa s p o s s ible to det ermine the c onc entra t i on of Pb, Cd and Bi in the same sui t e of r ocks .

By the us e of thes e �echni ques i t wa s pos s ibl e t o obtain fresh abundance da ta for the above elements in the four s tandard r ocks , G-1J W-1 9 C�\S syeni t e and C�\S

sulphj_de .

The cyclohexanone

/

hydrochloric a c i d extra c t i on sys tem provides a sa ti sfa c t ory enrichment t echni que for the spectrographi c analys i s of trace elements in ma terial wi th a low Fe c ontent . For ma t er ial c onta ining a high

c oncentra t i on o f Fe.9 i t is neces sary to combine thi s tech­

ni que with di s c ont inuous c ount ercurrent l i quid-liquid

extra c t i on t o s eparat e the_Fe b efore spectrographi c ana lys i s .

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However � Qnder these c ondi ti ons? c erta in elements can be de termined by direct a t omic abs orpt i on spectrometry o f the cyclohexanone extrac to

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CONTENTS

INTRODUCTION Pa ge

1 PART I

The Development of Improved Spectrochemical

Tec.hniques . , 16

17

PART I I

(

a

)

Improved me thods for the determin­

ation of spectral line intens i t i e s

(

b

)

A compari s on of ca thode and anode

excitation

3 1

A Study of the Extrac t i on of a Number of

Elements into Certain Cyclic Solvents .

43

PART I I I

(

a

)

Introduction and Pr eliminary

Inve s t i ga t i on

43

(

b

)

An investiga t i on of cyclohexanone , oyclohexo.nol o.nd cyclohexo.ne. a s

extra cting s o lvents for the chloro­

complexes o f Au, Zn , Cd, Hg, Ga , In , Tl , Sn, Pb 9 As , Sb , Bio 47 .

(

c

)

Results and Discus s i on 52

(

d

)

Preliminary inves t i gations into the

geochemical applications of the cyclohexanone

/

hydrochloric acid

extrac t i on sys t em 5 7

The Use o f Cyclohexanone for the Determin­

a t i on of Zn , Pb , In , Bi , Fe , Ivi:n, Mo in the

Lakes of McMurdo Oa s i s, Antarctica . 61

PART IV

(

a

)

Introduc t i on 61

(

b

)

Development and applica t i on of a

quanti ta tive proc edure. 66

(

c

)

Re sults and D i s cus s i on . 77 The Devel opment of D i s continuous Count er-

current Extrac t ion for Inorganic Sys t0ms .

89

(

a

)

Introduc t ion

89

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PART V

(b )

(c )

(d ) (e )

The us e of di s c ontinuous c ountercurrent l i Quid-liQU�d extra c t i on for det er­

mining the extra c t i on of the elements Cu, li.g� J�.u9 Zn9 Cd9 Hg, Ca 9 In, Tl, Sn, Pb 9 As , Sb , Bi 9 Ru9 Pd9 Ir and Pt from

3N

hydrochloric acid int o cyclohexanone A s tudy of the extra c t i on of certa in elements in the methyl i s obutyl ket one/

hydrochloric acid sys tem using

dis c ontinuous c ountercurrent l i Quid­

l i Quid extra c t i on . Results and Discus s i on

Inves ti ga t i ons int o the us e of dis­

continuous c ountercurrent extra c t i on for the s epara t i on of Fe .

The Det ermina t i on of Bismuth9 Cadmium9 Gallium, Lead and Z inc in Silicate Rocks .

PART VI

(a ) Tho development of QUant i ta tive proc edure s.

(b ) Results and Discus s i on . Conclus i ons and Cri t i cal Evalua t i on REFERENCES

96

99 101

107

112

112

1 26

13 7

143

Referensi

Dokumen terkait

Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only.. The thesis may not be reproduced elsewhere without the permission

Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only.. The thesis may not be reproduced elsewhere without the permission

Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only.. The thesis may not be reproduced elsewhere without the permission

Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only.. The thesis may not be reproduced elsewhere without the pennission

Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only.. The thesis may not be reproduced elsewhere without the permission

Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only.. The thesis may not be reproduced elsewhere without the pennission

Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only.. The thesis may not be reproduced elsewhere without the pennission

Pe1mission is given for a copy to be downloaded by an individual for the purpose of research and private study only.. The thesis may not be reproduced elsewhere without the permission