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Heap leaching of copper ores opportunity through science Jochen Petersen
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Heap leaching of copper ores – opportunity through science

May 10, 2023

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Page 1: Heap leaching of copper ores – opportunity through science

Heap leaching of copper ores –

opportunity through science

Jochen Petersen

Page 2: Heap leaching of copper ores – opportunity through science

2

A typical heap leach operation

Page 3: Heap leaching of copper ores – opportunity through science

Heap leach process

Page 4: Heap leaching of copper ores – opportunity through science

?

What is going on inside a heap

Page 5: Heap leaching of copper ores – opportunity through science

Grain/Surface Scale

Particle Scale

Agglomerate Scale

Heap Scale

What is going on inside a heap

Page 6: Heap leaching of copper ores – opportunity through science

6

Solution flow downwards

Heat generationthrough reaction

Gas (humid air) transport up

Surface evaporation and radiation

The heap scale in heaps

Page 7: Heap leaching of copper ores – opportunity through science

gas flow through

pore network

Solution ‘seeps’ along preferential channels

on air-liquid contact surfaces

The agglomerate scale in heaps

Page 8: Heap leaching of copper ores – opportunity through science

inner particle pores

sessile and planktonic micro-organisms

individual

particle

stagnant solution space

mobile solution space

The particle scale in heaps

Page 9: Heap leaching of copper ores – opportunity through science

Key chemistry in copper heaps

Acid leaching of malachite

𝐶𝑢2𝐶𝑂3(𝑂𝐻)2+2𝐻2𝑆𝑂4 → 2𝐶𝑢𝑆𝑂4 + 𝐶𝑂2 + 3𝐻2𝑂

Ferric leaching of covellite

CuS + 2Fe3+ → Cu2+ + 2Fe2+ + So

Chloride facilitate leaching of chalcopyrite

CuFeS2 + 3Cu2+ − Cl− → 4Cu+ + Fe2+ + 2So

Ferrous re-oxidation (biologically accelerated)

4Fe2+ + O2 + 4H+ → 4Fe3+ + 2H2O

Cuprous re-oxidation (rapid in chloride solution)

4Cu+ + O2 + 4H+ − (Cl−) → 4Cu2+ + 2H2O

Sulfur oxidation (chemically or biologically facilitated)

2S + 3O2 + 2H2O → 2H2SO4

Page 10: Heap leaching of copper ores – opportunity through science

Reaction network at particle surface

Fe2+

Fe3+

H+

O2,

CO2

acid migration or flow throughliquid film

solution phase solid phasegas phase

re-oxidation of ferrous (biological or direct)

Fe2+

Cu2+

reaction with gangue grains

𝐹𝑒𝐶𝑂3+ 𝐻2𝑆𝑂4→ 𝐹𝑒𝑆𝑂4 + 𝐻2𝑂 + 𝐶𝑂2

H+

Fe(OH)3 precipitation

𝐹𝑒3+ + 3𝐻2𝑂 → 𝐹𝑒 𝑂𝐻 3 + 3𝐻+

diffusion through micro-pores

reaction with mineral grains

𝐶𝑢𝑆 + 𝐹𝑒2 𝑆𝑂4 3 →

𝐶𝑢𝑆𝑂4 + 2𝐹𝑒𝑆𝑂4 + 𝑆0

Page 11: Heap leaching of copper ores – opportunity through science

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Is heap leaching a competitive technology?

• Slow process, residence time of months to years

• Poorer extraction (70-80%)

• Large physical footprint

• Long-term environmental burden uncertain

BUT

• Low energy requirements (crushing instead of milling)

• Simple, low-cost technology, can operate at remote sites

• Spent heaps comparable to tailings dams from minerals processing

Heap Leaching vs. Conventional Processing

Page 12: Heap leaching of copper ores – opportunity through science

12

Heap Leaching vs. Conventional Processing

ROM ore

Primary crushing

Heap leachingComminution and

flotation

Atmospheric leaching

SX/EW

Copper cathode to market Concentrate to market

Route 1

Route 3

Route 2

Page 13: Heap leaching of copper ores – opportunity through science

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In heaps, inventory cost is directly linked to tons of ore under leach/ leach time

Heap Leaching vs. Conventional Processing

Page 14: Heap leaching of copper ores – opportunity through science

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Why is heap leaching often so slow?

• Slow reaction kinetics at low temperatures

• Unliberated minerals in large particles

• Low aeration rates and poor gas-liquid mass transfer

• Solution channelling and stagnant zones

• re-adsorption of Cu onto precipitated Fe phases

Limitations of Heap Leaching

Page 15: Heap leaching of copper ores – opportunity through science

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Mineral extraction from large particles

• X-ray tomography shows shrinking shell and unreacted core

Limitations of Heap Leaching

Page 16: Heap leaching of copper ores – opportunity through science

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Gas-liquid mass transfer

• rate limited by low O2 solubility and interfacial area

• O2 solubility limited by temperature, solution salinity and air

pressure

0

2

4

6

8

10

12

14

0 20 40 60 80 100

Temperature ('C)

Ox

yg

en

so

lub

ilit

y [

pp

m]

pure water, dry air

0.15 M salinity, dry air

0.15 M salinity, sat. air

high salinity, high altitude

Limitations of Heap Leaching

Page 17: Heap leaching of copper ores – opportunity through science

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Solution Flow through Heaps

Drip point Drip point Drip pointa) b) c)

Page 18: Heap leaching of copper ores – opportunity through science

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Lag due to bio-colonisation

Metal attenuation due to

sorption on surface precipitate

Copper attenuation on Fe precipitates

Page 19: Heap leaching of copper ores – opportunity through science

• Progressive ‘cementation’ of heap ore by Fe-precipitates

Fresh Ore

After 1 month

of leaching

After 3 months

of leaching

Fe precipitation in column bioleaching

Page 20: Heap leaching of copper ores – opportunity through science

• Nano SEM studies of freshly precipitated Fe-OH

• Network structure of precipitate offers large surface formetal sorption and inhibits solution flow

Fe precipitation in column bioleaching

Page 21: Heap leaching of copper ores – opportunity through science

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gas flow throughpore network

Solution ‘seeps’ through open pore spaces as a front

Transport-reaction modelling

Fe2+

Fe3+

Cu2+

H+

O2, CO2

Bulk flow diffusion through

Stagnant pores

Heap Modelling

Page 22: Heap leaching of copper ores – opportunity through science

HeapSim Model

Heap Modelling

Overall Mineral Conversions and Zinc Extraction

0%

20%

40%

60%

80%

100%

0 50 100 150 200 250

Leach time [d]

Con

ve

rsio

n

Sphalerite

Galena

Pyrite

Zn Extraction

Col 116 data

Zinc Concentration in Effluent

0

10

20

30

40

50

60

70

0 50 100 150 200 250

Leach Time [d]

Zn C

once

ntr

ati

on [

g/L]

Iron Concentration in Effluent

0

5

10

15

20

0 50 100 150 200 250

Leach Time [d]

Fe C

oncentr

ati

on [

g/L]

pH in Effluent

0.0

0.5

1.0

1.5

2.0

2.5

3.0

0 50 100 150 200 250

Leach Time [d]

pH

Potential (vs. Ag/AgCl) in Effluent

300

320

340

360

380

400

420

440

460

480

500

0 50 100 150 200 250

Leach Time [d]

Pote

nti

al (v

s. A

g/A

gCl)

[m

V]

Temperature with Depth and Time

20

25

30

35

40

45

50

55

60

65

70

0 1 2 3 4 5 6 7

Heap Depth [m]

Tem

pera

ture

[°C

]

Progression with each line: 9.2 days

Marmatite ZnS Conversion with Depth and Time

0%

10%

20%

30%

40%

50%

60%

70%

0 1 2 3 4 5 6 7

Heap Depth [m]

Zn

S C

on

versio

nProgression with each line: 9.2 days

Page 23: Heap leaching of copper ores – opportunity through science

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Key insights from modelling

• Complex distributions of reagent and heat distribution throughout

heaps determines local rates of leaching;

• Ambient conditions have significant impact on oxidative heap leaching;

• Optimal heap design varies strongly with ore characteristics;

• There are ‘speed limits’ to the maximum rate of leaching:

• Supply rate of acid (rare)

• Reagent distribution through stagnant (diffusion) zones

• Mineral liberation in large particles

• Supply rate of oxidant (air) – gas liquid mass-transfer

• Formation of adsorption buffers

Page 24: Heap leaching of copper ores – opportunity through science

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Conclusions

• Heap leaching is a technically simple process, but of immense physical

complexity at all scales.

• The interplay of these complexities is difficult to grasp, yet under-

standing them offers opportunities to conduct the process

efficiently.

• Economic analysis indicates if heaps can be made to operate reliably at

their optimum, they would be a serious technology of choice.

• Heaps do have a future!

Page 25: Heap leaching of copper ores – opportunity through science

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The National Research Foundation (NRF) of South Africa

is acknowledged for funding this research through their

Incentive Funding for Rated Researcher programme.

Thank You