Ores are naturally occurring materials from which minerals, typically metals, can be extracted economically. Here are the key properties of ores:
1. Mineral Composition
– Metallic Ores: Contain metals (e.g., hematite for iron, bauxite for aluminum).
– Non-Metallic Ores: Contain non-metals (e.g., halite for salt, gypsum for plaster).
2. Grade (Purity)
– The percentage of valuable metal/mineral in the ore.
– High-grade ores have more extractable material (e.g., 60% iron in hematite vs. 30% in taconite).
3. Gangue Materials
– Unwanted impurities like silica, clay, or limestone that must be removed during processing.
4. Physical Properties
– Color & Luster: Varies (e.g., shiny metallic pyrite vs. dull bauxite).
– Hardness: Affects mining difficulty (e.g., soft coal vs. hard diamond-bearing kimberlite).
– Density: Heavy ores (e.g., galena for lead) can be separated by gravity methods.
5. Chemical Properties
– Reactivity: Determines extraction method (e.g., electrolysis for aluminum from bauxite).
– Solubility: Some ores are leached using acids/alkalis (e.g., gold cyanidation).
6. Formation & Occurrence
– Primary Ores: Formed directly from magmatic processes (e.g., chromite in ultramafic rocks).
– Secondary Ores: Formed by weathering/sedimentation (e.g., bauxite from aluminum-rich rocks).
7. Magnetic & Electrical Properties
– Magnetite is magnetic; cassiterite conducts electricity—useful for separation techniques.
8. Economic Viability
– Depends on market demand, extraction costs, and processing technology.
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