Gold extraction
Gold extraction refers to the industrial processes used to recover gold from its primary lode deposits in hard rock or secondary placer deposits in alluvial gravels, involving physical separation, chemical leaching, and refining to produce doré bars or pure metal.[1] Primary methods include placer mining, which employs gravity separation via panning, sluicing, or dredging to concentrate heavy gold particles from unconsolidated sediments; open-pit or underground hard rock mining to access vein or disseminated ores; and heap leaching or tank leaching with cyanide solutions to dissolve gold from crushed ore.[2] These techniques have evolved from ancient panning in riverbeds dating back over 6,000 years to modern mechanized operations that recover gold at concentrations as low as 1-5 grams per tonne of ore.[3] The economic significance of gold extraction stems from gold's role as a store of value, monetary reserve, and material in electronics, dentistry, and aerospace, with global production exceeding 3,000 tonnes annually as of recent years, predominantly from large-scale operations in countries like China, Russia, and Australia.[4] Cyanidation, introduced in the 1880s, revolutionized recovery by enabling efficient extraction from low-grade ores, though it requires careful management of toxic reagents.[5] Artisanal small-scale mining, often using mercury amalgamation, accounts for about 20% of global output but poses heightened risks due to rudimentary technology.[6] Notable controversies surround environmental externalities, including acid mine drainage, heavy metal contamination from mercury (estimated at 1,400 metric tons used annually in processing), and cyanide spills that have devastated aquatic ecosystems, as seen in incidents like the 2000 Baia Mare spill in Romania.[6][7] Despite regulatory advances like the International Cyanide Management Code, abandoned mine sites continue to impose cleanup costs on taxpayers, underscoring the tension between gold's enduring value and the causal chain of ecological degradation from extraction activities.[8]Ore Characteristics
Types of Gold-Bearing Ores
Gold-bearing ores are classified primarily by the mineralogical form of gold and its associations, which dictate processing requirements and recovery rates. Free-milling ores contain gold that liberates readily during grinding, typically as native gold or electrum particles larger than a few micrometers, allowing over 90% recovery through direct cyanidation.[9] These ores often feature gold disseminated in quartz veins or associated with minimal sulfides, as seen in many mesothermal vein deposits where visible gold occurs alongside pyrite or arsenopyrite in low concentrations.[10] In contrast, refractory ores yield less than 80% recovery via standard cyanidation due to gold being locked within host minerals or interfered with by associated materials.[11] Refractory ores subdivide into sulfidic and carbonaceous types. Sulfidic refractory ores encapsulate submicroscopic gold within sulfide minerals such as pyrite (FeS₂) or arsenopyrite (FeAsS), necessitating pretreatment like roasting, pressure oxidation, or bioleaching to expose the gold for leaching; these predominate in orogenic and volcanic-hosted deposits with grades often below 5 g/t Au.[12] Carbonaceous refractory ores contain organic carbon that adsorbs dissolved gold complexes during cyanidation—a phenomenon termed preg-robbing—reducing recovery to under 50% without mitigation, commonly in Carlin-type deposits where gold averages 1-3 g/t and associates with fine pyrite and kerogen.[11] Double-refractory ores combine both sulfides and carbonaceous matter, demanding integrated treatments like flotation followed by oxidation and carbon removal.[13] Other notable ore types include telluride ores, where gold forms compounds like calaverite (Au₂Te₄) or sylvanite ((Au,Ag)₂Te₄), requiring specific roasting or leaching to break tellurium bonds; these occur in epithermal systems with grades up to 10 g/t Au.[12] Polymetallic ores associate gold with base metals in sulfides, as in iron oxide copper-gold (IOCG) deposits, complicating extraction due to penalties for copper or arsenic content.[10] Placer ores, though sedimentary rather than primary, consist of free native gold particles in alluvial gravels, easily concentrated by gravity without chemical processing.[14]| Ore Type | Key Characteristics | Typical Gold Form | Recovery Method Example |
|---|---|---|---|
| Free-milling | Gold liberated by grinding; low sulfide content | Native gold, electrum (>1-10 μm) | Direct cyanidation (>90%) |
| Sulfidic refractory | Gold locked in sulfides; fine dissemination | Invisible gold in pyrite/arsenopyrite | Pressure oxidation + cyanidation |
| Carbonaceous refractory | Preg-robbing by organic carbon; often with sulfides | Submicron gold particles | Roasting or bioleaching + CIL |
| Telluride | Gold bound to tellurium; epithermal origin | Au-Ag tellurides (e.g., calaverite) | Alkaline chlorination or roasting |