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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Improved Modeling of MetalExtraction and Electrowinning
Michael L . Free
Department of Metallurgical Engineering
University of Utah
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Ore leaching has important
application constraints thatneed to be considered to
predict performance
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Importantfactors include
surface
dissolution,product layer
precipitation,
mineralalteration, and
interior
penetration.
host-rock particle
mineral alteration product layer
precipitation product layeracid dissolution of
mineral
Interior penetration
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Valuable Mineral Particle Classification Fully Locked (dominant if the initial size of
valuable mineral particles [vmp] is much
smaller than host rock particles [hrp]) Partially Locked (dominant if the initial size
of valuable mineral particles is similar tohost rock particles)
Liberated (dominant if the initial size ofvaluable mineral particles is much largerthan host rock particles)
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Based on size distributions of
valuable mineral particles and
host rock particles, the
probability for each classification
(fully locked, partially locked, orliberated) can be determined.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
f(r)
rhrp50rvmp50
Partially or
fully locked
valuable
mineralparticle (vmp)
Partially
or fully
liberated
vmp
valuable mineral particle
size distribution
size
Comparison of valuable and host rock particle size distributions
host rock particle
size distribution
hrp size hrp size
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
If the selected valuable mineral particle is larger than the host rock particle,the valuable mineral particle is classified as a liberated particle because it
cannot reside within the corresponding host rock particle:
hrpvmp
Liberation probability can be described by:
)(...)2
()2
( hrpvmpvmp
hrpr vmpr
vmphrphrpLib rrforrr
rfrr
rfP
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Classification of particles can be made by picking andcomparing particles from each distribution:
hrpvmp
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The cumulative fraction of particles below a specified size
can be estimated using a cumulative size probability
function such as the Rosin-Rammler function:
)])([exp(1)(*
s
r
rrP
in which r*is the host rock particle reference size at with 62.3 % of the
material passes as undersize, Pis the probability or fraction of generally
liberated particles at the specified r, ris the particle size that is
evaluated, and sis a constant (generally between 1 and 2). Thus, the
fraction of particles between discrete intervals can be estimated by:
rr
rr
r
rr
rrf ss
])))
2(
([exp])
)2
(
(([exp)2
(**
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The fraction of partially locked nonliberated particles is based on the partial
locking zone volume fraction.
)(;)(
13
3
hrpvmp
hrp
vmphrpkPartialLoc rrfor
r
rrP
zone of partial locking
rvmp
host rock particle (hrp)valuable mineral particle (vmp)
hrpr
vmp
r
Locking classification
is based on center
point position of the
vmp relative to rhrp.
When the center ofthe vmp is between
rhrpand (rhrprvmp)
the vmp is classified
as partially locked.
Otherwise, it is fully
locked.
zone of full locking
Canadian Metallurgical Quarterly, 47(3), 277-284, 2008.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The estimated probability of each classification is found using:
)...]...()(1))][)(exp(1)()(exp(1[ **3
*
**
*
**
*
**
. vmphrp
hr p
vmphron
hr p
hrpvmpn
vmp
hrpvmp
estLockedPartially rrfor
r
rr
r
rr
r
rrP hrpvmp
)))(exp(1)()(exp(*
**
*
**
.hrpvmp n
hrp
hrpvmpn
vmp
hrpvmp
estlibr
rr
r
rrP
).. .))]...()(exp(1)()(exp(1[ **
*
**
*
**
. vmphrp
n
hrp
hrpvmpn
vmp
hrpvmp
estLockedPartially rrforr
rr
r
rrP hrpvmp
).. .]...()())][)(exp(1)()(exp(1[ **3*
**
*
**
*
**
. vmphrp
hrp
vmphron
hrp
hrpvmpn
vmp
hrpvmp
estLockedFully rrforr
rr
r
rr
r
rrP hrpvmp
)......(0 **. vmphrpestLockedFully rrforP
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
This approach describes measured exposed mineral well
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
0.1 1 10 100
FractionofVal
uableMineral
rhrp/rvmp
Liberated
Part.Lock
Full.Lock
Exposed(calc.)
Exposed(meas)
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Kinetics are determined using weighted models:Liberated Mineral (Pure Mineral Leaching):
Partially Locked Mineral (Pure Mineral Leaching):
Fully Locked Mineral (Shrinking Core Model):
])1(3
21[
23)( 3/2
2
FLFLeffxw
hrpfFLhrp
DCM
rSrt
))1(1()( 3/1libx
vmpRClibvmp
C
rkrt
])1(1[]
)
3
4(
4[)(
3/2
y
libvmpliblibvmp rkrt
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The combined model, based on valuable mineral association withhost rock particles fits measured data reasonably well.
0
0.050.1
0.15
0.2
0.25
0.3
0.35
0.4
0.45
0.5
0 500000 1000000
F
ractionR
eacted
Time (sec)
Model pH 1.5
Measured pH 1.5
Model pH 2.5
Measured pH 2.5
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The combined model, based on valuable mineral association withhost rock particles fits measured data reasonably well.
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
0 500000 1000000
Fr
actionR
eacte
d
Time (sec)
Model 820 microns
Measured 820 microns
Model 1420 microns
Measured 1420 microns
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Small scale leaching tests nearly always utilizesmall particles to decrease reaction time.Small particles contain a larger fraction of
material that is liberated or partially locked.Knowing the fraction of material in eachcategory allows for a more correct
determination of the relevant constants that
can then be used to predict leaching usinglarger particles provided that the appropriatemineral distribution information is available.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
What is the effect of comminution on theliberated, partially-locked, and fully-locked
valuable mineral particles?
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Consider a cube of valuable mineral in two locations inside
of a host rock particle
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
This estimation method or tool assumes uniform bindingand strength of the valuable and host rock phases.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
3
3
8 )2(D
dP
3
32
4
])2()2([3
D
ddDP
The corresponding sizes and progeny scenario probabilities are:
4 progeny probability with an average of 1/4 of original volume
and (1/4)
1/3
or 0.63 of original size d:
8 progeny probability with an average of 1/8 th of
original volume and 1/2 of original size d:
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
3
2
2
])2
1(2[12
D
dDd
P
2480 1 PPPP
2 progeny probability with an average of 1/2 of original volume and
(1/24)1/3or 0.794 of original size d:
0 progeny probability with an average of original size d:
The resulting probability based size represents a reasonable
estimate of the progeny size resulting from fracturing the host rock
particle to one half of its original size.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The effectiveness of comminution on liberation decreases
rapidly below an initial size ratio of 10 to 1
1
1.1
1.2
1.3
1.4
1.5
1.61.7
1.8
1.9
2
0 20 40 60 80
hrp/v
mpsizereductio
nfactor
(assu
mes50%rhrpred
uction)
initial rhrp/rvmp
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
MODELING OF
ELECTROWINNING
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
electrons
Anode (+) Cathode (-)
H2O
2H++ 0.5 O2
2e-
2e-
V
M2+
M
Electrowinning is the process of reducing metal by applying a negative potential to an electrode (cathode) on which the
metal deposits by means of a power supply and a counter electrode and the associated reaction(s).
Other
reactions
also occur.
Gas bubbles
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The mass of the deposit is related to
Faradays Law, which can be expressed as:
where Mis the mass of metal deposited, imetalis the
current density associated with the measured metal
deposition (assuming 100 % current efficiency), nis the
number of electrons transferred per mole of metal
reduction, Fis the Faraday constant (96,485 Coulombs
per mole of electrons transferred), andAwis the atomic
weight of the metal that is deposited.
nF
tAAiM cathodewmetal
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Energy Consumption is expressed as:
where Eappliedis the overall voltage applied to the
electrochemical cell.
tEAitIEEnergy appliedcathodecathodeapplied
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Substitution of the equation for mass of thedeposit into the expression for energy
consumption per unit of metal leads to:
metalw
appliedcathode
iA
EnFi
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The current efficiency, , is the ratio of theamount of current theoretically needed to deposit
a unit mass of metal divided by the actual current
consumed at the cathode per unit mass of metal,which can be expressed mathematically as:
cathode
metal
i
i
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Consequently, both voltage and current density
information must be determined to determine theenergy consumption per unit of metal produced.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Voltage and current information can bedetermined by appropriate application
of thermodynamics, mass transport, and
electrochemical kinetics.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The general form for chemical equationscan be expressed as:
where vjis the stoichiometric coefficient of the
species,Xis the chemical formula of species j,
zjis the charge of species j, nis the number ofelectrons in half-cell reactions, which must be
written cathodically or as reduction reactions.
j
jz
jjXvne
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Specific equations considered in thisexample include:
23 FeeFe
424
3 FeSOSOFe
24
2
4 SOFeeFeSO
424 HSOSOH
22 HeH
OHeHO 22 244
CueCu
2
2
ZneZn 22
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The free energy of a reaction is expressed
as:
in which R is the gas constant, T is the absolute
temperature, and ajvjis the activity of species j.
The standard free energy of a reaction, Gro, is
expressed as:
j
jv
jorr aRTGG ln
o
jfjj
or GvG
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
At equilibrium, the free energy of the reaction equalszero and the equilibrium constant may be used to
represent the equilibrium activity relationship between
the species:
where:
KRTGor ln
j
jvjeq aK
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The activity of an ion in aqueous media can be expressed
as:
The equilibrium electrochemical potential for
each half-cell reaction in the system isdetermined based on free energy using the
Nernst Equation:
jjj ma
jjv
jo
eq anF
RTEE ln
RT
GE
oro
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The rate of each half-cell reaction can be expressed by:
in which iis the current density, a
is the anodic charge transfer
coefficient, Fis the Faraday constant, is the surface overpotential
or the difference between the surface potential (Esurf) and the
equilibrium reaction potential (Eeq), Ris the gas constant, Tis the
absolute temperature, kis constant that is directly related to the
equilibrium exchange current density, Cbis the bulk concentration,
Csis the surface concentration, and is a factor that depends uponreaction mechanisms and related factors and it is usually between
0.25 and 1 and cis the cathodic charge transfer coefficient. :
)]exp()()exp()(['RT
F
C
CC
RT
F
C
CCki cc
bc
scbc
aa
ba
saba
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The transfer of electrons and charge must balance, thusthe system of Butler-Volmer equations that applies to a
given reaction scenario is subject to the constraint that:
When all currents are associated with the same
homogenous surface:
0 I
0
i
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The current density of ion transport consists
of the sum of the ion flux densities of all ions
in the system:
where Njis the flux density of species j, cjis
the concentration of species j and uj, the ion
mobility of species j, is:
jj jjj jjj jjjj jj cDzFczFVcuzEFNzFi
22
RT
Du
jj
jj
r
RTD
6
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The effect of gas generation on solution
conductivity, which is inversely related toresistivity, is often approximated using the
Maxwell equation:
Where k is the conductivity adjustment factor and f is the
void fraction associated with gas generation. In this
investigation the proportionality constant relating current
density associated with oxygen production and voidfraction was determined using experimental data (0.0002
m2/A within the range of 50 to 2000 A/m2for the oxygen
evolution reaction).
21
1
f
f
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Fluid flow can be determined using the Navier-
Stokes equation:
in which is the density of the fluid, Vis the
velocity,pis the pressure, gis the gravitational
acceleration, his height, and is viscosity.
Conservation of mass in fluid flow leads to theequation of continuity:
VhgpVVt
V 2])([
0)(
V
t
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The effect of the auxiliary cathode reactions and shortcircuits on current efficiency can be mathematically
written as:
The corresponding effect on current efficiency is,
therefore:
othermetalcircuitshortauxilliarymetalcathode iiiiii
othermetal
metal
ii
i
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Comparison of measured and predicted data
Table 1: Comparison of model predictions and experimentaldata* for current efficiency and energy consumption for zincelectrowinning (55 gpl Zn, 35oC, 500 A/m2)
H2SO4
Concentration
(gpl)
Predicted
Current
Efficiency
Measured
Current
Efficiency
Predicted
Energy Use
(kWhr/ton)
Measured
Energy Use
(kWhr/ton)
65 98.1 97.4 2730 2912
110 96.1 95.7 2730 2870
155 93.5 93.6 2671 2773
*G. W. Barton and A. C. Scott, Validated Mathematical Model for a Zinc
Electrowinning Cell, J. of Applied Electroch., 22(2), 1992, 104-115.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Comparison of measured and predicted data
Table 1: Comparison of model predictions and experimentaldata* for current efficiency and energy consumption for zincelectrowinning (55 gpl Zn, 35oC, 500 A/m2) (US$ 0.03/kwhr)
H2SO4Concentration
(gpl)
PredictedCurrent
Efficiency
MeasuredCurrent
Efficiency
Predicted Cost($US/ton)
Actual Cost($US/ton)
65 98.1 97.4 81.90 87.36
110 96.1 95.7 81.90 86.10
155 93.5 93.6 80.13 83.19
*G. W. Barton and A. C. Scott, Validated Mathematical Model for a Zinc
Electrowinning Cell, J. of Applied Electroch., 22(2), 1992, 104-115.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Energy Use per Ton of Cu versus Current Density
1000
11001200
1300
1400
1500
1600
1700
1800
1900
2000
0 200 400 600 800
Current Density (A/m2)
Energ
yPerMetricTon
(kWhr/ton
Measured
Predicted
42 gpl Cu2+, 160 gpl
H2SO4, 0.06 gpl
Fe3+, and 0.06 gpl
Fe2+at 60oC using a
lead anode in a cell
with electrodes
spaced 1 cm apart.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Energy Cost per Ton of Cu versus Current Density
42 gpl Cu2+, 160 gpl
H2SO4, 0.06 gplFe3+, and 0.06 gpl
Fe2+at 60oC using a
lead anode in a cell
with electrodes
spaced 1 cm apart.
45
47
49
51
53
55
0 200 400 600 800
Current Density (A/m2)
Electrici
tyCostPerMetricTo
n($US/ton)
Measured
Predicted
(Assumes $0.03 per kilowatt hour)
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Another factor that affects electrowinning performance is the
physical qualities of the cathode such as roughness and
nonuniform deposition. If the cathode has areas of high
growth, short-circuiting may occur, which lowers currentefficiency and requires additional maintenance and personnel
costs. Areas of high growth are often associated with areas
with high rates of deposition. Some of these effects can be
determined by appropriate modeling as well as by control ofsurface roughness.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Electrodeposit roughness has a substantialimpact on the properties of the deposited film
or the crystals that are harvested from
cathodes
Rough deposits can lead to short circuiting in
electrolysis or entrapment of electrolyte or
gasses.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Electrodeposit roughness is generallycontrolled by:
Initial Surface Topography
Coating Thickness
Nucleation
Growth
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
substrate
Height from low
to high point
Original nucleus
Low nucleus density results
initially in rough surfaces
High nucleus density results
initially in smoother surfaces
Roughness on smooth surfaces is a
function of nucleation and growth.
growth
Initial surface roughness is reduced by higher nucleus density
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Nucleation and growth are the resultof the electrochemical and physical
properties that can be described
using thermodynamics,
electrochemical kinetics, ion
transport, fluid flow, and nucleation
equations.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Effect of mass transportFor mass transport controlling the current flow inthen the expression for the diffusion controlled
deposition rate, iLis
iL=nFDCb/
where iLis the diffusion controlled deposition rate (Amp/area),
F is Faraday constant,
n is the number of electrons transferred,D is the diffusivity of the reacting species,
is the thickness of the diffusion boundary layer
Cbis the bulk concentration.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Often, the combination of diffusion and electrochemical kinetics
are sufficient to predict electrochemical reaction rates
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
The closer the deposition current is to themass transport limited current density understeady-state conditions, the closer the
surface concentration of depositing speciesapproaches zero. As the surface
concentration approaches zero, the lower theNernst Potential becomes and the greater therequired applied potential becomes to beginnucleation. Consequently, as i/ilapproaches
one, it becomes difficult to initiate newnuclei, thereby increasing the tendency for
growth from limited nuclei.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
ion flux lines ion flux lines
asperity asperity
Under mass transport controlled electrodeposition, surface asperities receive
more of the available flux of depositing ions than areas between asperities.Consequently, asperities grow faster than other areas. As the asperities grow
rapidly and nuclei initiate and grow on the asperities, dendritic, granular
deposits become the dominant morphology.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Nucleation and Growth are OftenPartially Controlled Using Additives:
A balance between activators, inhibitors, and
modifiers or smoothing agents is often used tocontrol electrodeposit morphology.
Smoothing agents often consist ofmacromolecules.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Base solution: 0.1 M CuCl, 4 M NaCl, and 0.01 M HCl
Experiment condition:i = -15 mA/cm2, 1,000 RPM, and deposition time = 15 hours
a) no additive b) 0.013 g/L gelatin
The colors indicate the height of the copper deposit.
Using organic additives to obtain smooth copper electrodeposits
from halide media.
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
0
10
20
3040
50
60
70
8090
100
0 0.5 1
RSMRoughness(m)
i/iL
no additivegelatin 0.1% by volume
Q = 6000Coulombs/cm2
Comparison of RMS roughness and i/ilvalues for electrodeposits (6000
Coulombs per centimeter squared) obtained from a bath containing 0.1
mol/L CuCl, 4.0 mol/L NaCl and 0.01 mol/L HCl under direct current
conditions 25 mA/cm2).
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Department of Metallurgical Engineeri ng, University of Utah
Nucleation is Controlled by: Species Concentrations
Applied Potential Substrate Properties
N l ti
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Department of Metallurgical Engineeri ng, University of Utah
Nucleation
The steady-state nuclei formation rate can be described
mathematically by the equation:
2exp
formation
s
dNN
dt T
where Nformationis the number density of new nuclei, tistime, Nis the baseline rate of nuclei formation, is aconstant (and Nare functions of valence, geometry,surface energy, and frequency of attachment and
detachment), Tis temperature, sis the surfaceoverpotential. (R. T. C. Choo, J. M. Toguri, A. M El-Sherik, U.Erb,J.Appl.Electrochem., , 384, (1995). E. B. Budevski, in Comprehensive Treatiseof Electrochemistry, Vol. 7, B. E. Conway, J. OM. Bockris, E. Yeager, S. U. M.
Khan, and R. E. White, Editors, Plenum, New York, p. 441, 1983.)
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Department of Metallurgical Engineeri ng, University of Utah
Copper nucleation on chloride media on copper
Solution:Base solution with 0.1 % by volume Gelatin
Experiment condition: Stationary copper electrode, 1 sec deposition
microns
m
icrons
0 155
3
0.1
0.2
0.3
0.4
0.5
microns
m
icrons
0 155
103
0.1
0.2
0.3
0.4
0.5
0.6
0.7
a) 100 mV below OCP b) 200 mV below OCP
103
OCP = open circuit potential
Effect of gelatin concentration on RMS Roughness
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0
5
10
15
20
25
30
35
0 0.2 0.4 0.6 0.8 1 1.2
% by volume gelatin
RMS
Roughness(m
)
Effect of gelatin concentration on RMS Roughness
The surface morphology remains almost the same when the gelatin
Concentrations are in the range of 0.01 to 1% by vol.
Solution:Base solutionExperiment condition:i = -25 mA/cm2, 3 hours plating, and 1000 RPM
Department of Metallurgical Engineeri ng, University of Utah
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Gelatin chemistryTypical structure:
-Ala-Gly-Pro-Arg-Gly-Glu-4Hyp-Gly-Pro-
Descriptions:
preparing by the thermal denaturation of collagen,
containing between 300 - 4000 amino acids.
containing approximately 33% glycine, 22% proline and 11% hydroxyproline
11% glutamic acid, 11% arginine, and 11% alanine.
Department of Metallurgical Engineeri ng, University of Utah
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Effect of amino acids
0
5
10
15
20
25
3035
40
0 0.02 0.04 0.06 0.08 0.1 0.12
Concentration (Molarity)
RMSRoughness(m)
Glycine
Proline
Solution:Base solutionExperiment condition:i = -25 mA/cm2, 3 hours plating, and 1,000 RPM
Glycine and proline do not significantly smoothen the surface
morphology as separate entities.
Department of Metallurgical Engineeri ng, University of Utah
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Department of Metallurgical Engineeri ng, University of Utah
Assumptions:
1) spherical shape additive molecules.2) depositing ions access to the surface via pore area between the additive molecules
not through the additive molecules.
Hence, the diffusion through the pore area between the adjacent molecules is used to evaluate the effect of
the polymeric additives in electrodeposit nucleation.
Effective
adsorbate
layer
Effective
adsorbate
layer
Deposition surface
Effective
pore
M+ M+ M+
Side view
3 additive molecules
Top view
additive
additive additive
Depositing ions
Depositing ions
Depositing ions
Effect of additive sizes on nucleation rate density
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Department of Metallurgical Engineeri ng, University of Utah
View of Unit Cell of Macromolecules or Spheres
Top view of Ions diffusing through a pore between additive
molecules or nanoparticles on an electrode that have movedapart by diffusion during the time needed by the depositing
ions to diffuse to the surface
Additive orparticle DepositingionsDepositing
ions
Additive or
particle
Additive or
particle
Unit cell length
(2r +(2Dt)0.5)
Relevant equations
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Department of Metallurgical Engineeri ng, University of Utah
Relevant equations
electroactD
rt 2
2
Simultaneous solution of these equations can be performed to determine
the effects of adsorbate molecules on surface nucleation.
Finding Cs
Knowing Cs helps to find s
Obtaining relative nucleation rate density
a nat.rxnp c nat.rxnpspore o
b
F(E-E ) - F(E-E )Ci = i [exp( )-exp( )]
C RT RTPoreEst
Appl Pore
tot
Ai =i
A2
ads ads
poreEst ads
r 3r+(r+ 2D t )( 3(r+ 2D t ))-rA = ;..for( 2D t
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Department of Metallurgical Engineeri ng, University of Utah
Molecular weights can confine the plating so that
the nucleation rate density increases at a reasonable size.
Theoretical values vs. Experimental values
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
1
0 50 100 150 200 250 300
Effective Adsorbate Radius (nm)
RelativeNuc
leationRateDensity
Theoretical Values
Experimental Values SiO2
Experimental Values PEG &PEO
Deposit Morphology Modeling (effect of fluid flow and current)
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
68
Arrows
represent
local fluid
velocityvectors.
Colors
represent
depositing
species
conc.
White
above the
thin darklower line
represents
the deposit.
Modeled using Comsol Multiphysics Software with significant modifications
Deposit Morphology Modeling (effect of fluid flow and current)
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69Modeled using Comsol Multiphysics Software with significant modifications
Arrows
represent
local
currentvectors.
Colors
represent
depositing
species
conc.
White
above the
thin darklower line
represents
the deposit.
Axis
values
are in
cm
2 5
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Comparison of RMS roughness and i/ilvalues for predicted and
measured results. Predictions were based on a solution obtained using
the previous equations associated with copper electrodeposits obtained
from a bath containing 0.1 mol/L CuCl, 4.0 mol/L NaCl and 0.01 mol/L HCl
under direct current conditions.
0
0.5
1
1.5
2
2.5
0.00 0.20 0.40 0.60 0.80
i/iL
RM
SROUGHNES
S(m) EXPERIMENTAL DATA
MODEL PREDICTION
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DEPARTMENT OF METALLURGICAL ENGINEERINGCOLLEGE OF MINES AND EARTH SCIENCES
Improved methods of modeling
provide tools to more appropriately
include natural phenomena inpredictions that can be used to
optimize performance of metal
extraction and electrowinningoperations