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Stishovite: The Deep Earth's Dense Silica Marvel

An exploration into the high-pressure polymorph of silicon dioxide, its unique structure, and its significance in geological science.

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What is Stishovite?

A High-Pressure Polymorph

Stishovite represents an exceptionally dense, tetragonal crystalline form of silicon dioxide (SiO2). It is a polymorph, meaning it shares the same chemical composition as other forms of silica, such as quartz, but possesses a distinct crystal structure due to differing formation conditions.

Rarity and Significance

While exceedingly rare on the Earth's surface, stishovite is theorized to be a predominant form of silicon dioxide within the planet's lower mantle. Its existence provides critical insights into the mineralogy and physical conditions of the deep Earth.

Naming and Discovery

The mineral was named in honor of Sergey Stishov, a Soviet physicist who first synthesized it in 1961. Its natural occurrence was subsequently identified in 1962 by Edward C. T. Chao within samples from Meteor Crater.

Crystal Structure and Chemistry

Rutile-like Framework

The crystal structure of stishovite is notably similar to that of rutile (TiO2). A key distinction from other common silica polymorphs lies in the coordination geometry of silicon. In stishovite, silicon atoms adopt an octahedral coordination, being bonded to six oxygen atoms. Conversely, the oxygen atoms are typically three-connected.

Crystallographic Data

Stishovite crystallizes in the tetragonal system, belonging to the space group P42/mnm. Its unit cell parameters are approximately a = 4.1772(7) ร… and c = 2.6651(4) ร…, with two formula units (Z=2) per unit cell.

Chemical Formula

The fundamental chemical composition of stishovite is silicon dioxide, represented by the formula SiO2. This simple formula belies the complex structural arrangement dictated by extreme pressure conditions.

Physical Characteristics

Appearance and Optics

Pure stishovite is colorless. It exhibits a vitreous luster and ranges from transparent to translucent. Optically, it is uniaxial with a positive sign. Its refractive indices are measured as nฯ‰ = 1.799โ€“1.800 and nฮต = 1.826โ€“1.845, with a birefringence (ฮด) of 0.027.

Density and Hardness

Stishovite is remarkably dense, with a calculated specific gravity of 4.29 and a synthetic value of 4.35 g/cmยณ. It ranks as the second densest polymorph of silica, surpassed only by seifertite. On the Mohs scale of mineral hardness, stishovite registers a formidable 9.5, making it exceptionally resistant to scratching.

Thermal Behavior

Stishovite does not possess a distinct melting point under standard conditions; instead, it decomposes. This characteristic is typical of minerals formed under extreme pressure and temperature regimes.

Formation and Occurrence

Impact Events

The most common terrestrial occurrences of stishovite are found within impact craters, such as Meteor Crater. It forms under the immense shock pressures (exceeding 10 GPa) and high temperatures generated during hypervelocity meteorite impacts into quartz-bearing rocks.

Deep Earth Conditions

Minute quantities of stishovite have also been identified within diamonds and in ultra-high-pressure metamorphic rocks originating from the Earth's mantle. This suggests that stishovite may be a stable and potentially abundant phase in the deep mantle, conditions that are difficult to replicate and study directly.

Natural Crystal Size

Large natural crystals of stishovite are exceptionally scarce, typically found as small fragments measuring only 1 to 2 millimeters in length. Distinguishing these from common quartz often requires detailed laboratory analysis.

Laboratory Synthesis

Recreating Extreme Conditions

Stishovite can be synthesized in laboratory settings by recreating the high-pressure and high-temperature conditions under which it naturally forms. This is achieved through methods such as isostatic pressing or shock wave experiments, effectively mimicking the geological processes of meteorite impacts or deep mantle environments.

Exceptional Hardness

A Benchmark in Material Science

For a considerable period, stishovite was recognized as the hardest known oxide, with a Vickers hardness rating around 30 GPa. While the discovery of boron suboxide has since revealed an even harder oxide, stishovite's extreme hardness remains a significant characteristic, underscoring the material properties achievable under immense pressure.

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References

References

  1.  Stishovite. Mindat.org.
  2.  Stishovite. Webmineral.com.
A full list of references for this article are available at the Stishovite Wikipedia page

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Important Notice

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