Alpha-zinc sulfide (α-ZnS) is the low-temperature polymorph of zinc sulfide, also known as sphalerite in its natural mineral form. It is one of two main crystalline modifications of ZnS, the other being beta-zinc sulfide (β-ZnS, wurtzite structure).
🌍 Origins and Naming
- Mineral Equivalent: Sphalerite (α-ZnS).
- Polymorphism:
- α-ZnS (sphalerite structure): Stable at lower temperatures.
- β-ZnS (wurtzite structure): Stable at higher temperatures.
- Synthetic Form: Produced industrially for pigments, phosphors, and semiconductors.
🔬 Chemical and Structural Properties
- Formula: ZnS
- Crystal System: Cubic (isometric, sphalerite type).
- Structure: Each Zn²⁺ is tetrahedrally coordinated by S²⁻ ions.
- Color: Pure ZnS is white; impurities can cause brown, yellow, or gray tones.
- Hardness: ~3.5–4 on Mohs scale.
- Density: ~4.0 g/cm³.
- Luster: Resinous to adamantine.
- Transparency: Transparent to translucent in pure form.
⚙️ Geological Occurrence
- Natural Form: Sphalerite is the chief ore of zinc, found in hydrothermal veins, sedimentary exhalative deposits, and skarns.
- Associated Minerals: Galena (PbS), chalcopyrite (CuFeS₂), pyrite (FeS₂).
- Localities: Worldwide — notable deposits in the USA (Missouri, Tennessee), Spain, and Australia.
📖 Scientific and Industrial Significance
- Ore Mineral: Sphalerite is the most important zinc ore.
- Semiconductors: Synthetic ZnS is used in optoelectronics, phosphors, and infrared optics.
- Pigments: Historically used as “lithopone” (ZnS + BaSO₄) for paints.
- Luminescence: Doped ZnS (with Cu, Ag, Mn) is used in phosphorescent and electroluminescent materials.
✨ Conclusion
Alpha-zinc sulfide (α-ZnS) is the cubic sphalerite polymorph of ZnS, stable at low temperatures and the dominant natural form. It is both the principal zinc ore and a technologically important material in optics and electronics.
In short: α-ZnS = sphalerite structure, cubic, main zinc ore, also used in semiconductors and pigments.
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