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Recovery o f Platinum f rom Concentrated
Sodium Chloride Brine by
Electrodeposition on Vitreous Carbon
J. E. Harrar and F. 8. Stephens
January, 1984
This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsi- bility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Refer- ence herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recom- mendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof.
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DISCLAIMER
This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency Thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof.
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DISCLAIMER Portions of this document may be illegible in electronic image products. Images are produced from the best available original document.
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Contents
A b s t r a c t . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1
I n t r o d u c t i o n . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1
Exper imental Apparatus and Procedures . . . . . . . . . . . . . . . . 3
Reagents . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3
Apparatus and Procedures f o r Voltammetry . . . . . . . . . . . . . Apparatus and Procedures f o r P la t inum . . . . . . . . . . . . . . 4
4
Recovery Exper iments
R e s u l t s and D iscuss ion o f Vol tammetr ic Measurements . . . . . . . . . 8
R e s u l t s and D iscuss ion o f P la t inum . . . . . . . . . . . . . . . . . . 15
Recovery Exper iments
Conclusions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 18
Acknowledgments . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 9
References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 20
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Recovery of Platinum from Concentrated Sodium Chloride Brine
by Electrodeposition on Vitreous Carbon
J. E. Harrar and F. B. Stephens
Abstract
The voltammetric characteristics of Pt( 11) and Pt( IV) have been
examined at a vitreous carbon electrode i n slightly acidic 3 4 ( ~ 1 5
wt.%) NaCl solutions. Pt(1V) is reduced to Pt(l1) at %O V and Pt(I1)
is reduced to Pt(0) at -0.5 V vs. Ag-AgC1.
platinum metal at -0.5 V is very low on bare carbon, but increases as the
coverage o f platinum increases.
evolved in this medium is -0.85 V. A technique has been tested for
the removal o f sub-part-per-million levels of platinum from the
high-salinity brine by controlled-potential electrolysis using a
reticulated, vitreous-carbon, flow-through electrode. However, at
control potentials negative enough to begin to electrodeposit the
platinum at a significant rate, simultaneous reduction of hydrogen ion
reduces the current and energy efficiency t o an unacceptable level.
The rate of deposition of
The potential at which hydrogen is
Introduction
In a previous study (Harrar and Raber, 1983), in which a number of 6
natural brines were analyzed for precious and strategically-valuable
metals, it was found that one of the brines from the Salton Sea t
geothermal field contained approximately 50 pg/kg o f platinum.
Although this concentration i s very low, the large volumes of fluid that
are currently processed for energy extraction makes such a resource
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attractive if the precious metal could be economically extracted. The
brines of the Salton Sea geothermal field (or KGKA = Known Geothermal
Resource Area) are of extremely high salinity (15-20 wt % salts), and are
composed principally of sodium, potassium, and calcium chlorides.
The fluid that would most likely be processed for metals recovery
would be the relatively low temperature (<90°C) effluent brine from the
power plant facility, after the principal flash stages for energy
extraction.
high-temperature crystallizers for solids removal are currently being
tested, and valuable metals recovery is certainly possible at the higher
temperatures (>200°C) of the wellhead brine.
previous studies in geothermal mineral recovery can be found in our
However, different geothermal plant designs involving
A literature survey of
previous r e p o r t ( h a r r a r and Raber, 1983) and a paper by Maimoni (1983) .
To continue our investigations, two approaches have been examined for
removal of platinum from high-salinity geothermal brines. One involved
the use of various solid chemical media that were known from previous
studies in dilute waters to be effective in precious metal removal. Most
of these media had been tested previously only for non-precious-metal or
gold and silver removal (Acton, 1982) and in low-ionic-strength, low
temperature solutions. The results of this study are being reported
el sewhere (Raber, Thompson, and Gregg 1984).
The second technique examined for platinum recovery was electrolytic
For some of the elements, * I
deposition on a substrate of vitreous carbon.
electrodeposition of the metals on inert electrode materials is performed
for both metals recovery (Habashi, 1982; Ettel and Tilak, 1981; Coeuret,
1980), pollution control (Bennion and Newman, 1972; Kuhn, 1972) and for
trace metals analysis (Murthy, Holzbecher, and Ryan, 1982). However, not
only is there no knowledge of the conditions necessary for quantitative
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electrodeposition of trace amounts of platinum from aqueous solutions in
general, but there is also no information on the electrochemistry of
p 1 at i num i n hi gh-chl ori de medi a.
Accordingly, our first objective was t o measure the current/electrode-
potential characteristics of platinum in solutions of NaCl at
concentrations simulating those of the high-salinity geothermal brines. a
Then, using these data, a series of experiments were carried out to
attempt to quantitatively electrodeposit platinum from a flowing stream
of brine. The electrode material selected was vitreous or "glassy"
carbon. This material was selected because of its relative inertness,
and because, for the flowing-stream experiments, it could also be
obtained in the form of reticulated-vitreous carbon (RVC) . This material
(see Wang, 1981) is commercially available and is configured as a rigid,
porous matrix that can be used advantageously in processes requiring
large electrode surface area. Both the current-potential (voltammetric)
and the f low-recovery measurements were performed using 3-electrode
controlled-potential techniques so that the applied cathode potentials
would be precisely known.
Experimental Apparatus and Procedures
Reagents. For the voltammetric measurements, the brine solutions
were prepared from J. T. Baker Ultrex-grade NaCl salt. It was found that
Mallinkrodt ACS reagent-grade NaCl contained sufficient heavy-metal *
impurities to raise the background current to an undesirably high level
in these concentrated solutions. For the recovery experiments, however, i
the larger volumes o f solution precluded use of the Ultrex-grade salt, so
the reagent-grade salt was used.
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Plat inum( 11) and p l a t i n u m ( I V ) s o l u t i o n s were prepared by d i s s o l v i n g ,
r e s p e c t i v e l y , (NH4)2PtC14 and (NH4)2PtC16 s a l t s i n water. These s a l t s
were ob ta ined f rom Engelhard I n d u s t
compounds. The concent ra t ions of p
assays o f t h e compounds as r e p o r t e d
p l a t i n u m recovery experiments, a so
0.002 - M HC1 was used.
t ies as n o m i n a l l y h i g h - p u r i t y
a t inum were c a l c u l a t e d f r o m t h e
by t h e manufacturer. For t h e
u t i o n c o n t a i n i n g 0.168 mg P t / m l and
Apparatus and Procedures f o r Voltammetry. To i n v e s t i g a t e t h e
vol tammetry o f p la t inum, equipment c o n s i s t e d o f an EG&G Pr ince ton A p p l i e d
Research Model 174A Po larograph ic Analyzer, Model 303 S t a t i c Mercury Drop
E l e c t r o d e Assembly, and a Houston X - Y recorder .
carbon e l e c t r o d e was s u b s t i t u d e d f o r t h e mercury c a p i l l a r y i n t h e c e l l
assembly.
p laced i n t h e c e l l , and 1 m l o f a s tock s o l u t i o n o f e i t h e r P t ( I 1 ) o r
Pt (1V) was p i p e t t e d i n t o t h e c e l l t o g i v e a p l a t i n u m c o n c e n t r a t i o n o f 2 x
A model GO173 g l a s s y
To prepare a s o l u t i o n f o r voltammetry, 5 m l o f b r i n e was
lo-' - M.
S o l u t i o n s were deoxygenated b y b u b b l i n g h i g h - p u r i t y n i t r o g e n through them
f o r a t l e a s t 4 min. p r i o r t o t h e vo l tammetr ic scans. N i t r o g e n was f lowed
over t h e t o p of t h e s o l u t i o n s d u r i n g t h e scans.
made a t an ambient temperature o f 22-25OC.
The pH o f t h e c e l l s o l u t i o n s was i n t h e range o f 4 t o 6.
A l l measurements were
Apparatus and Procedures f o r P la t inum Recovery Experiments. The f l o w
e l e c t r o l y s i s c e l l shown i n F i g u r e 1 was used f o r t h e recovery
experiments.
p rev ious designs ( S t r o h l and Curran, 1979; Wang and Dewald, 1983) a re t h e
dua l counter - and r e f e r e n c e e l e c t r o d e s and t h e use o f low-temperature
(140OC) heat -shr inkab le T e f z e l t o encase t h e RVC. The lower temperature
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Features o f t h i s f low- th rough R V C c e l l t h a t d i f f e r from
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Solution Sol ut ion outlet inlet
Figure 1. Flow electrolysis cell for removal of platinum from simulated geothermal brine. 1. Reticulated vitreous carbon working electrode. 2. Heat-shrinkable Tefzel tubing. 3. Glassy carbon rod counter electrodes. 4. Ag-AgC1 reference electrodes. 5. Ace threaded-glass connectors. 6. Teflon plugs. 7. Viton O-Rings. 8. Zirconium electrical connection to working electrode.
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would min imize chemical m o d i f i c a t i o n o f t h e R V C d u r i n g f a b r i c a t i o n o f t h e
assembly.
I ~ V C and e f f e c t b e t t e r c o n t r o l o f i t s p o t e n t i a l . I n opera t ion , each
counter e l e c t r o d e and each r e f e r e n c e e l e c t r o d e i s connected e x t e r n a l l y t o
i t s t w i n .
The dual e l e c t r o d e s reduce t h e p o t e n t i a l g r a d i e n t th rough t h e
The work ing-e lect rode c y l i n d e r o f K V C was c u t b y means o f a c o r k
b o r e r f r o m p ieces o f R V C ob ta ined f r o m Energy Research and Generation,
Inc. Two grades o f R V C were t e s t e d : 45s ( s45 pores/ in . and 800 f t /ft
2 3 s u r f a c e area) and 100s ($100 pores/ in . and 2000 f t /ft sur face area) .
2 3
For t h e 45s-grade m a t e r i a l , our work ing e l e c t r o d e volume o f $4.5 cm
would have an e f f e c t i v e s u r f a c e area of 118 cm . By comparison, t h e
2 s u r f a c e area o f t h e vo l tammet r ic work ing e l e c t r o d e was 0.096 cm . 2
The counter e l e c t r o d e s were rods o f g l a s s y carbon ob ta ined f r o m
Polycarbon, Inc.
t h e t o p w i t h an i n s u l a t i n g f i l m o f N a r l i n e r s t r i p p a b l e f i l m , and
conver ted t o AgCl a t t h e t i p b y immersion i n aqua r e g i a .
bodies were f a b r i c a t e d f r o m Ace Glass Co. s i z e 15 threaded connectors,
and t h e R V C e l e c t r o d e was h e l d i n p l a c e b y T e f z e l tub ing , which, as
mentioned, c o u l d be shrunk a t t h e r e l a t i v e l y low temperature o f 14OOC.
The r e f e r e n c e e l e c t r o d e s were rods o f s i l v e r , coated a t
The g l a s s c e l l
A new R V C e l e c t r o d e was used f o r each exper iment; a f t e r reassembly b y
heat s h r i n k i n g t h e T e f z e l o n t o t h e RVC, and i n s e r t i n g t h e T e f l o n plugs, a
needle was used t o p i e r c e t h e T e f z e l and then a 0.5-mm-dia z i rcon ium w i r e
was i n s e r t e d as shown i n F ig . 1 t o make e l e c t r i c a l connect ion t o t h e
RVC.
sealant . A Technicon AutoAnalyzer p e r i s t a l t i c pump and a p p r o p r i a t e s i z e s
of Tygon t u b i n g were used t o pump b r i n e th rough t h e e l e c t r o l y s i s c e l l .
Connection t o t h e p o r t s of t h e c e l l were made v i a Cheminert f i t t i n g s .
The b r i n e was f lowed th rough an i n - l i n e , 1-pm Gelman f i l t e r b e f o r e
The w i r e was t h e n sealed a t t h e o u t s i d e w i t h Dow-Corning 3145 RTV
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B
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entering the cell.
was pumped through the cell consisted of a 2-liter FEP Teflon bottle.
The cap of the bottle was fitted with a fritted-glass gas-dispersion tube
for deoxygenation of the solution, and a section of Teflon tubing
reaching to the bottom of the bottle for withdrawal of the solution.
The reservoir for the platinum-containing brine that
This tubing was connected to the pump tubing via a 3-way Teflon-plug
stopcock so that the cell could first be flushed with brine that did not
contain platinum. e
At the beginning of each experiment, exactly 1-liter of brine was
placed in the 2-liter reservoir, 1.000 ml of the stock Pt(I1) solution
containing 168 pg Pt was pipetted into the brine and mixed. The pH of
this test solution was 5.1.
purity nitrogen, and then, while the flow of nitrogen continued, brine
without platinum was pumped through the cell, most of the air bubbles
were removed by tapping the cell, and the working electrode was
The solution was deoxygenated with high-
preconditioned for a few minutes by polarization at the test reduction
potential. Then, without interrupting the electrolysis current, and
after at least 15-min. deoxygenation, the stopcock was turned to begin
the flow of Pt-containing brine to the cell.
The potentiostat was an EG&G Princeton Applied Research Model 173
with Model 176 Current Follower.
(bel) Model 731 Uigital Integrator. All experiments were carried out at
Currents were integrated using an ECO
b an ambient temperature of 22-25OC.
After the electrolysis, the Tefzel tubing surrounding the RVC
electrode was cut, and the KVC was flushed thoroughly and quickly with
water.
vial and dried in a desiccator.
i'
The KVC sample was then placed in a HN03-cleaned polyethylene
The samples were analyzed for platinum
by neutron activation analysis by General Activation Analysis, Inc. (San
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Diego) u s i n g t h e f o l l o w i n g procedure. The samp
standards were i r r a d i a t e d f o r 30 min. i n a T R I G
a t a f l u x o f 1.8 x lo1‘ n/cm -sec. The element 2
es p l u s comparator
L Mark I n u c l e a r r e a c t o r
p l a t i n u m produces gold-199
w i t h a h a l f - l i f e o f 3.15 days.
were counted on a Ge(L i ) d e t e c t o r coupled t o a mul t i channe l gamma-ray
spectrometer.
0.5 p g .
A f t e r a decay o f n i n e days, t h e samples
The l i m i t o f d e t e c t i o n o f p l a t i n u m i n t h e R V C samples was
Resu l ts and D iscuss ion o f Vol tammetr ic Experiments
The predominant species o f p l a t i n u m t h a t would be present i n t h e 2- 2- a r e PtC16 o r P t C I 4 , depending i n
o r +2 o x i d a t i o n s t a t e . Reduct ion
concent ra ted-ha l ide geothermal b r i n e s
whether p l a t i n u m i s present as t h e +4
o f t h e these species a t a cathoae wou d i n v o l v e t h e r e a c t i o n s :
P t C l 6 ’ - + 4e- - P t meta l + 6 C1- ( 3 )
React ions ( 1 ) and ( 2 ) would r e p r e s e n t t h e e l e c t r o d e p o s i t i o n process if i t
occur red as a s tepwise r e d u c t i o n of t h e P t ( I V ) th rough P t ( I 1 ) t o P t ( 0 ) ;
o r React ion ( 3 ) would represent t h e process i f P t ( I V ) were reduced
d i r e c t l y t o t h e metal .
P t ( 1 I ) t o t h e metal.
React ion ( 2 ) corresponds t o t h e r e d u c t i o n o f
There i s some disagreement i n t h e l i t e r a t u r e as t o t h e exac t values
of t h e s tandard p o t e n t i a l s of React ions 1 t o 3 ( M i l a z z o and C a r o l i , 1978;
L l o p i s and Colom, 1976; Lingane, 1958). However, a l l o f t h e values f o r
c h l o r i d e media l i e between +0.5 and +0.75 V v s . t h e s tandard hydrogen
e l e c t r o d e (SHE), and i t m i g h t be expected t h a t t h e e l e c t r o d e p o s i t i o n o f
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platinum could be effected at quite positive, or at least relatively low
negative potentials. Unfortunately, however, both polarographic and
voltammetric studies (Llopis and Colom, 1976, et seq.) have revealed that
a rather large overpotential is associated with these reactions at
practical current densities. Although there are no reported
investigations of the voltammetry of platinum using carbon electrodes, or
in strong halide media, several studies of the reduction of platinum
chlorocomplexes at platinum metal electrodes (Llopis and Colom, 1976) b
have shown that reactions (l), (Z), and ( 3 ) take place in the vicinity of
-0.2 to -0.4 V vs. SHE. Accordingly, we anticipated in our studies with
vitreous carbon that we would also be dealing with this electrode
potential region. A practical difficulty with this characteristic is
that hydrogen ion is also reduced (to H2 gas) in this potential region,
and this process would tend to obscure and interfere with the platinum
electrodeposition to a greater extent as the solution pH is lowered. Our
hope, therefore, was to demonstrate that platinum could be quantitatively
deposited from solutions under typical hypersaline geothermal brine
conditions, without consumption of a large fraction of the current by
hydrogen ion reduction.
Our examination of the voltammetry of platinum was limited in the
3 - M ($15 wt % ) present work to one specific set of brine conditions:
WaCl, a pH range of 4 to 6, and ambient ( 2 2 - 2 5 O C ; ) temperatures. Higher
temperatures such as those typical o f real geothermal fluids would not be
expected to change the relevant electrode potentials or reaction
characteristics significantly, thus it was felt that ambient temperature ("
tests would be sufficient to determine whether the electrolytic approach
was promising. Atmospheric-flashed hypersaline brine has a pH of 5 to 6,
thus the acidity conditions of these experiments are typical of those
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found in the field.
chlorocomplexes, any chloride concentration in the range of 0.2 to 4 - M
probably would yield about the same characteristics for the platinum
species electrochemistry. What is not definitely known is the oxidation
state of the platinum in the real geothermal brine, but because the brine
is anoxic, contains H2S, and is generally mildly reducing even after
loss of the H2S through flashing, the platinum is probably present as
Pt(I1).
briefly investigated to learn the effect of the platinum speciation on
the electrodeposition process.
Because of the stability of the platinum
However, the characteristics of both Pt(1V) and Pt(I1) were
Figure 2 shows the results of a series of voltammetric scans of a
solution of Pt(I1) as PtClt- in 3 - M NaC1. Note that this solution of
platinum corresponds to 400 ppm Pt vs. the 50 ppb Pt or less that might
be present in a real geothermal brine.
higher concentrations of platinum to study its electrochemical
characteristics because the typical background currents in voltammetry
would completely obscure the platinum reduction at concentrations below
1 ppm.
starting with a clean, bare, glassy-carbon electrode.
completed, the potentiostat was disconnected and the solution stirred
briefly.
Very little reduction of the Pt(I1) is evident at first, but as platinum
metal accumulates on the electrode (in effect making it a platinum
electrode), it becomes easier to reduce the Pt(I1) species, and the
height of the current peak seen in Fig. 2 increases.
of reduction of Pt(I1) on a pure glassy carbon surface is very low, thus
it would be necessary in an efficient recovery process to first
predeposit platinum on the electrode to ensure rapid subsequent
deposition of the platinum to be recovered.
It is necessary to use these
Figure 2 shows a series of successive scans of potential,
As each scan was
Then the succeeding scan was initiated with a quiet solution.
Apparently the rate
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a
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T 100 p A
I
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I I 1 I 1 I 0.4 0.2 0 -0.2 -0.4 -0.6 -0.8 -1.0 -1.2
Potential, V vs. Ag-ASCI
F i g u r e 2. RedGction o f P t ( I 1 ) t o P t ( 0 ) on a g lassy carbon e l e c t r o d e i n 3 - M (s15 wt.%) NaC1.
P t ( I r ) = 2 x 10-3 - M Scan Rate = 100 mV/sec
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The p o t e n t i a l r e g i o n where P t ( I 1 ) i s reduced i s i n general agreement
w i t h p rev ious work u s i n g p l a t i n u m e l e c t r o d e s as no ted above.
Ag-AgC1 re fe rence e l e c t r o d e i s +0.2 V vs. t h e SHE).
r i s e i n c u r r e n t a t -0.85 V (F ig . 2) i s due t o t h e r e d u c t i o n o f hydrogen
i o n t o hydrogen gas, thus i t i s r a t h e r c l o s e t o t h e p o t e n t i a l r e q u i r e d t o
reduce t h e P t ( 11).
(The
The n e a r l y v e r t i c a l
The p l a t i n u m meta l t h a t has been depos i ted on t h e g l a s s y carbon
e l e c t r o d e can be removed b y e l e c t r o l y t i c s t r i p p i n g as shown b y t h e curves
o f F i g . 3. I n these experiments, t h e p l a t i n u m was depos i ted f o r a g i v e n
l e n g t h o f t i m e b y h o l d i n g t h e e l e c t r o d e a t -0.7 V w i t h a g i t a t i o n o f t h e
s o l u t i o n b y t h e b u b b l i n g o f n i t r o g e n .
rep laced by 3 - M b r i n e n o t c o n t a i n i n g P t ( I I ) , and deoxygenation was
c a r r i e d o u t f o r 4 min. w h i l e t h e p o t e n t i a l o f -0.7 V was mainta ined on
t h e e lec t rode. Then t h e q u i e t , deoxygenated s o l u t i o n s were scanned f r o m
-0.7 t o +0.5 V w i t h t h e r e s u l t s shown i n F ig . 3.
p l a t i n u m can be removed i n t h i s manner migh t be u s e f u l i n an e l e c t r o l y t i c
recovery process because t h e carbon e l e c t r o d e m a t e r i a l would n o t have t o
be dest royed and c o u l d be reused.
The s o l u t i o n i n t h e c e l l was then
The f a c t t h a t t h e
2- F i g u r e 4 shows t h e behav io r of Pt (1V) as PtC16 i n t h e h i g h - s a l i n i t y
b r i n e . No background c u r r e n t c u r v e i s shown; i t i s t h e same as t h a t i n
F ig . 2. The curves f o r p l a t i n u m r e d u c t i o n were ob ta ined i n a s e r i e s of
s t a r t i n g w i t h a bare carbon sur face, and again show t h e
r e d u c t i o n o f P t ( I 1 ) as p l a t i n u m meta l b u i l d s up on t h e
r s t peak i n F ig . 4, which i s due t o t h e r e d u c t i o n of
i s a p p a r e n t l y n o t s e n s i t i v e t o t h e surface composi t ion
No f u r t h e r work was done t o unravel t h e c o n t r i b u t i o n
o f t h e two consecut ive r e a c t i o n s t o t h e c u r r e n t - p o t e n t i a l c h a r a c t e r i s t i c s ;
i t i s e v i d e n t t h a t t h e c o n s t a n t - p o t e n t i a l e l e c t r o d e p o s i t i o n c o n d i t i o n s
-1 2-
consecut ive scans
increased r a t e o f
e lec t rode. The f
Pt(1V) t o P t ( I I ) ,
o f t h e e lec t rode.
P
‘a
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i
0.8 0.6 0.4 0.2 0 -0.2 -0.4 -0.6 -0.8 -1 .o Potential, V vs. Ag-ASCI
Figure 3. Anodic stripping of platinum from a glassy carbon electrode in 3 - M (c15 wt.%) NaC1.
Scan Rate = TOO mV/sec
Peak 1:
Peak 2:
After 4 min deposition from Pt(I1) solution
After 20 min deposition from Pt(I1) solution
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0.4 0.2 0 -0.2 -0.4 -0.6 -0.8 -1.0 -1.2
Potential, V vs. Ag-AgCI
F i g u r e 4. Reduct ion o f P t ( I V ) t o P t ( I 1 ) and P t ( 0 ) on a g l a s s y carbon e l e c t r o d e i n 3 - M (*15 wt .%) NaC1.
P t ( 1 v ) = 2 x 10-3 - M
Peak 1: P t ( I V ) + P t ( I 1 ) Peak 2: ( P t ( I 1 ) .+ P t ( 0 )
Scan Rate = 100 mV/sec
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Page 19
must be selected to ensure that Pt(I1) is reduced, whether the geothermal
platinum is present as either Pt(I1) or Pt(1V).
Results and Discussion of Platinum Recovery Experiments
Based on the results of the voltammetric measurements, it is obvious *
that the control potential would have to be at least as negative as
i -0.6 V vs. Ag-AgC1 for complete electrodeposition of the platinum. The
two complicating factors are the need to predeposit platinum t o
"sensitize" the carbon electrode and the proximity of the platinum
reduction wave to that of hydrogen ion. A series of electrolytic
recovery experiments were performed, first at -0.60 V to examine the
effect of RVC porosity and flow rate, and then at more negative
potentials. The results are presented in Table 1.
These results show that the recovery of platinum was not very
sensitive to the porosity (surface area) of the RVC, but was influenced
significantly by the flow rate. The lowest flow rate, 1 ml/min, was
comparable to the flow rate found by Strohl and Curran (1979) to be
necessary for quantitative electrolysis of several other species using
t h e same porosity and similar size electrode o f RVC. No preplating o f
platinum on the electrode was performed before the experimental runs,
thus some of the lower recoveries found for the faster flow rates was due
t o this. At the lowest flow rate, ~ 1 7 h was required for a run; this
was believed to include enough time for.sensitization of the electrode
'I without loss of a significant fraction o f the platinum.
The data in Table 1 also show that, even at the most negative
potential, -0.80 V, the % recovery of the platinum was still relatively
poor.
reference electrodes, the actual potential on the interior of the RVC
It is known that, because of the positioning of the counter and
-1 5-
Page 20
Table 1. Recovery o f P la t inum f rom NaCl B r i n e by E l e c t r o l y t i c Reduction.
P t Taken: 168 pg as PtC14 2- NaCl : 3 - M (%15 w t % ) P t Concentrat ion: 168 pg/ l i t e r pH: 5.1
Working E lec t rode
P o t e n t i a l , V vs Ag-AgCl
none (b lank) -0.60
none (b lank ) -0.60
none (b lank ) -0.60
none (b lank ) -0.60
non (b lank ) -0.60
none (b lank ) -0.60
-0.75 -0.80
R VC
P o r o s i t y
Grade I
4 5s 4 5s
100s 1 00s
4 5s 4 5s
100s 100s
4 5s 4 5s
100s 100s
100s 100s
Flow
Rate
m l / m i n
11.5 11.5
11.5 11.5
3.9 3.9
3.9 3.9
1 .o 1 .o
1 .o 1 .o 1 .o 1 .o
P t Recovered
<o. 5 2.0, 1.8, 1.9
<o. 5 1.6, 1.3
(0.5 5.2,4.9
<O. 5 7.4. 7.8
(0.5 19,11
(0.5 12912
22 29,33
%
Recov e ry
1.1
0.8
3.1
4.5
9
7
13 18
\
'6
-1 6-
Page 21
matrix is less negative than the control potential at the exterior edges
(Fleischmann and Oldfield, 1971).
employing a significantly more negative control potential. However, in
this instance we must try to establish as negative a potential as
possible for complete platinum reduction on the interior surfaces of the
RVC, while minimizing hydrogen ion reduction and gas evolution on the
edges. At the pH of this brine, 5 to 6, and conceivable, practical
electrolysis cell designs, this would be very difficult to achieve.
In general, this can be compensated by
A control potential still more negative than -0.80 V could be used,
but then additional electrolysis current would be wasted. In our
experiments, initial currents were 4-8 mA at -0.60 V and 15-30 mA at
-0.80 V. In every experiment, the current decayed to ~ 0 . 5 mA at the
end of the electrolysis.
"desensitization" is not known; however, it should be noted that many of
the impurities in the NaCl that was used to prepare the brine also would
be codeposited with platinum under these conditions.
measured total charge that was passed, at the flow rate of 1.0 ml/min,
the average current was ~ 0 . 7 mA at -0.60 V and ~2 mA at -0.80 V.
comparison, only -2 PA would be consumed in quantitatively depositing
163 ug of platinum, thus the current efficiency of the process here was
very low. Real geothermal brines containing additional trace metals
would require still more current; however, if the recovery were carried
out using controlled-potential techniques, only Pb( 11), which is found at
-50-100 mg/l concentrations in hypersaliie geothermal brines, would be
important. Copper, gold, silver, and cadmium, if present, also would
codeposit; but manganese and zinc, which are present n high
concentrations in some brines, woula reqJire potentia s more negative
than -1.0 V vs. Ag-AgC1 (Kolthoff and Liligane, '1952).
The reason for this decay or apparent
Based on the
By
-1 7-
Page 22
Conclusions
Our objective in these experiments was to determine whether platinum,
as the chlorocomplex in high-salinity brine, could be deposited
electrolytically as the metal on a relatively inexpensive substrate with
reasonable current efficiency. Reticulated vitreous carbon was found to
be a convenient material to use as a working electrode, and
electrodeposition o f the platinum was clearly observed at millimolar
concentrations (a few hundred ppm). However, the process was found to
require a significant overpotential, especially at the uncoated carbon
surface. For the slightly acidic solutions typical of the hypersaline
geothermal brine, the required control potential is close to that o f the
reduction of hydrogen ion.
process were thus unacceptably low for the very low concentration level
(<1 ppm) found in the geothermal brine.
The current and energy efficiency of the
If the pH of geothermal brine that could be used as the input to the
recovery process were higher, e.g., neutral or slightly alkaline, or if
the concentrations of platinum in the brines were higher, then the
electrodeposition technique would become much more favorable.
negative control potential could then be used to obtain quantitative
deposition of the platinum, and the interference by hydrogen-ion
reduction would be lessened.
brine in a processing plant by the addition of alkali, merely to
facilitate platinum recovery, would not, however, prove to be economical,
because of the amount of alkali that would be required.
electrolytic removal o f platinum had been successful, it is probable that
the platinum could also be stripped from the carbon electrolytically by
changing the control potential, thus avoiding destruction o f the
deposition substrate.
A more
Deliberately raising the pH of a geothermal
I f the
-1 8-
c
Page 23
It appears that the activated charcoal extraction technique
investigated by Raber, Thompson, and Gregg (1984) should be the method
o f choice for precious metal recovery.
Acknowledgement 4
H. C. Crampton assisted in the fabrication o f the flow-through
electrolysis cell. L
0
-7 9-
Page 24
References
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