Spodumene
Spodumene | |
---|---|
File:Spodumene-Quartz-cktsu-45a.jpg | |
Spodumene crystal with quartz | |
General | |
Category | [[Mineral categories|Pyroxene mineral]] |
Formula | LiAl(SiO3)2 |
Strunz classification | [[Strunz classification|]] |
Dana classification | [[Dana classification|]] |
Crystal system | [[Crystal system|]] |
Crystal class | |
Color | Colorless, white, gray, pink, lilac, yellow, green |
Physical properties | |
Cleavage | Perfect on {110} |
Mohs scale hardness | |
Luster | Vitreous |
Streak | White |
Diaphaneity | Transparent to translucent |
Specific gravity | |
Optical properties | |
Refractive index | |
Crystal habit | |
Other characteristics |
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This template is designed for use on pages related to minerals, providing a standardized format to display essential information about various mineral properties. It includes fields for the mineral's name, image, category, formula, classifications (Strunz and Dana), crystal system and class, color, and various physical properties such as cleavage, hardness, luster, streak, diaphaneity, specific gravity, optical properties, refractive index, crystal habit, and other characteristics. Users can fill in the relevant information for each mineral, ensuring a consistent and informative presentation across the wiki's mineral-related articles.
Spodumene is a pyroxene mineral consisting of lithium aluminium inosilicate, LiAl(SiO3)2, and is a source of lithium. It occurs as colorless to yellowish, purplish, or emerald-green crystals, often of great size. Spodumene is an important ore of lithium and is a significant mineral in the production of lithium batteries.
Occurrence[edit | edit source]
Spodumene is typically found in pegmatites associated with other lithium minerals such as lepidolite, petalite, and amblygonite. It is often found in large crystals, sometimes reaching several meters in length. Major deposits are found in countries such as the United States, Canada, Brazil, and Australia.
Varieties[edit | edit source]
Spodumene has several gem-quality varieties:
- Kunzite: The pink to lilac variety of spodumene, named after gemologist George Frederick Kunz.
- Hiddenite: The green variety of spodumene, named after William Earl Hidden, who discovered it in North Carolina.
Uses[edit | edit source]
Spodumene is primarily used as a source of lithium, which is extracted and used in the manufacture of lithium batteries, ceramics, and glass. The gem varieties, kunzite and hiddenite, are used in jewelry.
Extraction and Processing[edit | edit source]
The extraction of lithium from spodumene involves several steps: 1. Mining: Spodumene is mined from pegmatite deposits. 2. Crushing and Grinding: The ore is crushed and ground to liberate the spodumene crystals. 3. Concentration: The spodumene is concentrated using flotation or other methods. 4. Conversion: The concentrated spodumene is heated to convert it from the alpha to the beta form, which is more amenable to lithium extraction. 5. Leaching: The beta-spodumene is leached with sulfuric acid to produce lithium sulfate. 6. Precipitation: Lithium carbonate or lithium hydroxide is precipitated from the solution.
Environmental Impact[edit | edit source]
The mining and processing of spodumene can have significant environmental impacts, including habitat destruction, water pollution, and carbon emissions. Efforts are being made to develop more sustainable methods of lithium extraction.
Also see[edit | edit source]
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Contributors: Prab R. Tumpati, MD