Skip to main content
Log in

Antimony Mobilization through Two Contrasting Gold Ore Processing Systems, New Zealand

  • Technical Article
  • Published:
Mine Water and the Environment Aims and scope Submit manuscript

Abstract

Antimony, a toxic metalloid similar to arsenic, is present at variable levels in most gold-bearing rocks. Antimony is soluble in the surface environment, so antimony (Sb) mobilization in mine waters is an environmental issue around gold mines. The Reefton gold mine was originally developed in gold-bearing quartz veins; Sb concentrations were low (<100 mg/kg) compared to arsenic (As) concentrations (>1,000 mg/kg), and the mine waters had low dissolved Sb (<0.1 mg/L). A second stage of gold mineralization at Reefton involved brecciation and cataclasis of quartz veins and wall rocks, with addition of stibnite (Sb2S3). Processing of this ore has resulted in higher dissolved Sb in mine waters (0.1–1 mg/L), even after water treatment that removes most dissolved As (to 0.01 mg/L) by adsorption to suspended iron oxyhydroxide. Competition between As and Sb for adsorption sites on iron oxyhydroxide particles may have resulted in partial exclusion of the more weakly adsorbed Sb. The high rainfall (2,000 mm/year) at Reefton ensures adequate dilution of mine waters after discharge. The Macraes gold mine has no stibnite, and most Sb is in solid solution in the abundant arsenopyrite (Sb up to 2,000 mg/kg). Pit waters have both Sb and As dissolved up to 0.1 mg/L, partly because of evaporative concentration in a low-rainfall environment. Macraes tailings waters have high As (up to 3 mg/L) but negligible Sb (<0.001 mg/L). Reefton mine gold-bearing concentrate, containing stibnite, is transported 700 km to be processed by autoclave oxidation and cyanidation at the Macraes mine. This introduction of additional Sb to the Macraes site substantially increases the Sb content of the process stream periodically. Tailings from this process have up to 3 wt% Sb, dispersed through As-rich iron oxyhydroxides that are formed in the autoclave. The Sb-rich tailings are strongly diluted (approximately 100:1) by the Macraes tailings, and adsorption of Sb to iron oxyhydroxides in the tailings piles ensures that there has been no increase in the Sb content of the tailings water since the Reefton concentrate has been added at Macraes.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8

Similar content being viewed by others

References

  • Adriano DC (1986) Trace elements in the terrestrial environment. Springer, Heidelberg, p 533

    Google Scholar 

  • Ainsworth N, Cooke JA, Johnson MS (1990) Distribution of antimony in contaminated grassland: I: vegetation and soils. Environ Pollut 65:65–77

    Article  Google Scholar 

  • Ashley PM, Craw D (2004) Structural controls on hydrothermal alteration and gold-antimony mineralisation in the Hillgrove area, NSW, Australia. Miner Depos 39:223–239

    Article  Google Scholar 

  • Ashley PM, Craw D, Graham BP, Chappell DA (2003) Environmental mobility of antimony around mesothermal stibnite deposits, New South Wales, Australia and southern New Zealand. J Geochem Explor 77:1–14

    Article  Google Scholar 

  • Ashley PM, Craw D, Tighe MK, Wilson NJ (2006) Magnitudes, spatial scales and processes of environmental antimony mobility from orogenic gold-antimony mineral deposits, Australasia. Environ Geol 51:499–508

    Article  Google Scholar 

  • Blowes DW, Jambor JL, Hanton-Fong CJ, Lortie L, Gould WD (1998) Geochemical, mineralogical and microbiological characterization of a sulfide-bearing carbonate-rich gold-mine tailings impoundment, Jontel, Quebec. Appl Geochem 13:687–705

    Article  Google Scholar 

  • Christie AB, Brathwaite RL (2003) Hydrothermal alteration in metasedimentary rock-hosted orogenic gold deposits, Reefton goldfield, South Island, New Zealand. Miner Depos 38:87–107

    Article  Google Scholar 

  • Craw D (2000) Water-rock interaction and acid neutralization in a large schist debris dam, Otago, New Zealand. Chem Geol 171:17–32

    Article  Google Scholar 

  • Craw D (2002) Geochemistry of late metamorphic hydrothermal alteration and graphitisation of host rock, Macraes gold mine, Otago Schist, New Zealand. Chem Geol 191:257–275

    Article  Google Scholar 

  • Craw D (2003) Geochemical changes in mine tailings during a transition to pressure-oxidation process discharge, Macraes Mine, New Zealand. J Geochem Explor 80:81–94

    Article  Google Scholar 

  • Craw D (2006) Pressure-oxidation autoclave as an analogue for acid-sulfate alteration in epithermal systems. Miner Depos 41:357–368

    Article  Google Scholar 

  • Craw D, Nelson M (2000) Geochemical signatures of discharge waters, Macraes mine flotation tailings, east Otago, New Zealand. N Z J Mar Freshw Res 34:597–613

    Article  Google Scholar 

  • Craw D, Windle SJ, Angus PV (1999) Gold mineralization without quartz veins in a ductile-brittle shear zone, Macraes Mine, Otago Schist, New Zealand. Miner Depos 34:382–394

    Article  Google Scholar 

  • Craw D, Koons PO, Chappell DA (2002) Arsenic distribution during formation and capping of an oxidized sulfidic minesoil, Macraes mine, New Zealand. J Geochem Explor 76:13–29

    Article  Google Scholar 

  • Craw D, Falconer D, Youngson JH (2003) Environmental arsenopyrite stability and dissolution: theory, experiment, and field observations. Chem Geol 199:71–82

    Article  Google Scholar 

  • Craw D, Wilson NJ, Ashley PM (2004) Geochemical controls on the environmental mobility of Sb and As at mesothermal antimony and gold deposits. Trans Inst Mining Metall (Appl Earth Sci) 113:B3–B10

    Article  Google Scholar 

  • Dzombak DA, Morel FMM (1990) Surface complexation modeling: hydrous ferric oxide. Wiley Interscience, New York City, p 393

    Google Scholar 

  • Filella M, Belzile N, Chen Y-W (2002) Antimony in the environment: a review focused on natural waters. I. Occurrence. Earth Sci Rev 57:125–176

    Article  Google Scholar 

  • Giggenbach WF, Sheppard DS, Robinson BW, Stewart MK, Lyon GL (1994) Geochemical structure and position of the Waiotapu Geothermal Field, New Zealand. Geothermics 23:599–644

    Article  Google Scholar 

  • Goldfarb RJ, Groves DI, Gardoll S (2001) Orogenic gold and geologic time: a global synthesis. Ore Geol Rev 18:1–75

    Article  Google Scholar 

  • Haffert L, Craw D (2008) Mineralogical controls on environmental mobility of arsenic from historic mine processing residues, New Zealand. Appl Geochem 23:1467–1483

    Article  Google Scholar 

  • Hedenquist JW, Arribas AR, Gonzalez-Urien E (2000) Exploration for epithermal gold deposits. In: Hagemann SG, Brown PE (eds) Gold in 2000, vol 13. Reviews in Economic Geology, pp 245–277

  • Hewlett L, Craw D, Black A (2005) Comparison of arsenic and trace metal contents of discharges from adjacent coal and gold mines, Reefton, New Zealand. Mar Freshw Res 56:983–995

    Article  Google Scholar 

  • Kang M, Kamei T, Magara Y (2003) Comparing polyaluminum chloride and ferric chloride for antimony removal. Water Res 37:4171–4179

    Article  Google Scholar 

  • Krause E, Ettel VA (1988) Solubility and stability of scorodite, FeAsO4.2H2O: new data and further discussion. Am Miner 73:850–854

    Google Scholar 

  • Langmuir D (1997) Aqueous Environmental Geochemistry. Prentice-Hall, Upper Saddle River, NJ, USA, p 600

    Google Scholar 

  • Lottermoser BG (2003) Mine wastes: characterization, treatment and environmental impacts. Springer, Berlin, p 277

    Google Scholar 

  • McComb KA, Craw D, McQuillan AJ (2007) ATR-IR spectroscopic study of antimonate adsorption to iron oxide. Langmuir 23:12125–12130

    Article  Google Scholar 

  • Mercer KL, Tobiason JE (2008) Removal of arsenic from high ionic strength solutions: effects of ionic strength, pH, and preformed vs in situ formed HFO. Environ Sci Technol 42:3797–3802

    Article  Google Scholar 

  • Mitchell M, Maw L, Angus PV, Craw D (2006) The Macraes gold deposit in east Otago. In: Christie AB, Brathwaite RL (eds) Geology and exploration of New Zealand mineral deposits, vol 25. Australasian Institute of Mining and Metallurgy Monograph, pp 313–318

  • Mok WM, Wai CM (1990) Distribution and mobilization of arsenic and antimony species in the Coeur d’Alene River, Idaho. Environ Sci Technol 24:102–108

    Article  Google Scholar 

  • Mori C, Orsini A, Migon C (1999) Impact of arsenic and antimony contamination on benthic invertebrates in a minor Corsican river. Hydrobiologia 392:73–80

    Article  Google Scholar 

  • Nesbitt BE, Muelenbachs K, Murowchick JB (1989) Genetic implications of stable isotope characteristics of mesothermal Au deposits and related Sb and Hg deposits in the Canadian Cordillera. Econ Geol 84:1489–1506

    Article  Google Scholar 

  • Petrie BS, Craw D, Ryan CG (2005) Geological controls on refractory ore in an orogenic gold deposit, Macraes mine, New Zealand. Miner Depos 40:45–58

    Article  Google Scholar 

  • Pitcairn IK, Teagle DAH, Craw D, Olivo GR, Kerrich R, Brewer TS (2006) Sources of metals and fluids in orogenic gold deposits: insights from the Otago and Alpine Schists, New Zealand. Econ Geol 101:1525–1546

    Article  Google Scholar 

  • Reed MH (1997) Hydrothermal alteration and its relationship to ore fluid composition. In: Barnes HL (ed) Geochemistry of Hydrothermal Ore Deposits. Wiley, New York City, pp 303–366

    Google Scholar 

  • Roddick-Lanzilotta AJ, McQuillan AJ, Craw D (2002) Infrared spectroscopic characterisation of arsenate(V) ion adsorption from mine waters, Macraes Mine, New Zealand. Appl Geochem 17:445–454

    Article  Google Scholar 

  • Seal RR, Hammarstrom JM (2003) Geoenvironmental models of mineral deposits: examples from massive sulfide and gold deposits. In: Jambor JL, Blowes DW, Ritchie AIM (eds) Environmental aspects of mine wastes, vol 31. Mineralogical Association of Canada. Short course, pp 11–50

  • Shotyk W, Krachler M, Chen B (2005) Anthropogenic impacts on the biogeochemistry and cycling of antimony. In: Sigel A, Sigel H, Sigel RKO (eds) Biogeochemistry, availability and transport of metals in the environment, metal ions in biological systems, vol 44. M Dekker, New York City, pp 177–203

    Google Scholar 

  • Tien VN, Chaudhary DS, Ngo HH, Vigneswaran S (2004) Arsenic in water: concerns and treatment technologies. J Ind Eng Chem 10:337–348

    Google Scholar 

  • Vink B (1996) Stability relations of antimony and arsenic compounds in the light of revised and extended Eh-pH diagrams. Chem Geol 130:21–30

    Article  Google Scholar 

  • Waychunas GA, Fuller CC, Rea BA, Davis JA (1996) Wide-angle X-ray scattering (WAXS) study of “two-line” ferrihydrite structure: effect of arsenate sorption and counterion variation and comparison with EXAFS results. Geochim Cosmochim Acta 60:1765–1781

    Article  Google Scholar 

  • Wilson N, Webster-Brown J, Brown K (2007) Controls on stibnite precipitation at two New Zealand geothermal power stations. Geothermics 36:330–347

    Article  Google Scholar 

Download references

Acknowledgments

This research was financed by the NZ Foundation for Research Science and Technology, and the University of Otago. The NZ Branch of Australasian Institute of Mining and Metallurgy provided a scholarship to LM for the study. The project would have been impossible without the enthusiastic co-operation and support from Oceana Gold Ltd personnel at both Reefton and Macraes mines, especially Debbie Clarke, Simone Vellekoop, Russell Pearce, Craig McIntosh, Brent Hill, Nick Whetter, Mark McCulloch, Tony Frater, Quenton Johnston, Melanie Rosak, and Pat Chave. Kat Lilly, Brent Pooley and Damian Walls provided expert laboratory assistance. Comments by two anonymous reviewers helped to improve the substance and presentation of the manuscript.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Dave Craw.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Milham, L., Craw, D. Antimony Mobilization through Two Contrasting Gold Ore Processing Systems, New Zealand. Mine Water Environ 28, 136–145 (2009). https://doi.org/10.1007/s10230-009-0071-y

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10230-009-0071-y

Keywords

Navigation