UPSC MainsGEOLOGY-PAPER-II201620 Marks
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Q7.

Give an account of the atomic structure, chemical composition, and physical and optical properties of the minerals of mica group.

How to Approach

This question requires a detailed understanding of the mica group of minerals. The approach should be to first define mica and its general characteristics, then delve into the atomic structure, chemical composition, and finally, the physical and optical properties of key mica minerals – Muscovite and Biotite. A comparative table highlighting the differences between these two common micas will be beneficial. Focus on relating properties to the atomic structure and chemical composition.

Model Answer

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Introduction

Mica is a group of phyllosilicate minerals, known for their perfect basal cleavage, resulting in thin, flexible, and easily separable sheets. These minerals are widely used in various industries, including electrical insulation, paints, and cosmetics. The term 'mica' is derived from the Latin word 'micare', meaning 'to glitter', reflecting their characteristic sheen. Understanding the atomic structure, chemical composition, and properties of mica minerals is crucial for their identification, classification, and application in diverse fields. This answer will focus on the two most common members of the mica group: Muscovite and Biotite.

Atomic Structure of Mica Minerals

Mica minerals possess a layered structure. The basic building block is a sheet silicate, where silicon and oxygen atoms are arranged in a tetrahedral framework. These tetrahedra are linked together to form a continuous sheet. Within each sheet, cations like potassium (K+), magnesium (Mg2+), iron (Fe2+), and aluminum (Al3+) occupy interstitial sites. These sheets are held together by weak Van der Waals forces, allowing for easy cleavage along the basal plane. The general formula for mica is X2Y4-5Z5-6O10(OH,F)2, where X represents a large cation (like K+), Y represents smaller cations (Mg2+, Fe2+, Al3+), and Z represents Si4+ and Al3+.

Chemical Composition

Muscovite (White Mica)

Muscovite has the chemical formula KAl2(AlSi3O10)(OH)2. It is a potassium aluminum silicate hydroxide. The presence of potassium ions contributes to its relatively high resistance to weathering. It’s essentially a silicate with potassium as the dominant large cation.

Biotite (Black Mica)

Biotite is a complex solid solution series with the general formula K(Mg,Fe)3(AlSi3O10)(OH)2. It contains varying amounts of magnesium and iron, giving it a dark color. The iron content is responsible for its darker hue, ranging from black to dark brown. Biotite can also contain significant amounts of titanium and other trace elements.

Physical Properties

Muscovite

  • Cleavage: Perfect basal cleavage – splits into thin, flexible sheets.
  • Hardness: 2.5 – 3 on Mohs scale.
  • Specific Gravity: 2.8 – 3.0
  • Luster: Pearly to vitreous.
  • Color: Colorless, silver, or pale shades of green, yellow, or brown.
  • Streak: Colorless

Biotite

  • Cleavage: Perfect basal cleavage.
  • Hardness: 2.5 – 3 on Mohs scale.
  • Specific Gravity: 2.8 – 3.4 (higher than Muscovite due to iron content).
  • Luster: Vitreous to pearly.
  • Color: Black, dark brown, or greenish-black.
  • Streak: Colorless to grayish

Optical Properties

Muscovite

Muscovite is generally transparent to translucent. It exhibits a slight birefringence, meaning it splits light into two rays, causing double refraction. Under a microscope in polarized light, it shows a characteristic interference color pattern. Its refractive indices are relatively low.

Biotite

Biotite is typically opaque to translucent. It also exhibits birefringence, but the higher iron content results in stronger absorption of light, leading to a darker appearance. Pleochroism is a prominent optical property of biotite, meaning it displays different colors when viewed from different angles under polarized light. Its refractive indices are higher than those of muscovite.

Comparative Table: Muscovite vs. Biotite

Property Muscovite Biotite
Chemical Formula KAl2(AlSi3O10)(OH)2 K(Mg,Fe)3(AlSi3O10)(OH)2
Color Colorless, silver, pale shades Black, dark brown, greenish-black
Specific Gravity 2.8 – 3.0 2.8 – 3.4
Iron Content Low High
Transparency Transparent to translucent Opaque to translucent
Pleochroism Absent or weak Prominent

Conclusion

In conclusion, the mica group minerals, particularly Muscovite and Biotite, are characterized by their unique layered atomic structure and perfect basal cleavage. Their chemical compositions, dominated by silicate structures with varying cations, dictate their distinct physical and optical properties. Muscovite, with its potassium-rich composition, is lighter in color and transparent, while Biotite, containing significant iron and magnesium, is darker and often opaque. Understanding these differences is crucial for their identification and application in various geological and industrial contexts.

Answer Length

This is a comprehensive model answer for learning purposes and may exceed the word limit. In the exam, always adhere to the prescribed word count.

Additional Resources

Key Definitions

Phyllosilicate
A class of sheet silicate minerals, characterized by their layered structure, where silicon-oxygen tetrahedra are arranged in sheets. Mica minerals belong to this group.
Birefringence
The splitting of a ray of light into two rays when it passes through an anisotropic material (like mica), resulting in the formation of two images with slightly different refractive indices.

Key Statistics

Global mica production was estimated at 340,000 metric tons in 2022, with India being a major producer and exporter.

Source: US Geological Survey, Mineral Commodity Summaries 2023 (Knowledge Cutoff: 2023)

India accounts for approximately 60% of the world’s mica reserves.

Source: Ministry of Mines, Annual Report 2021-22 (Knowledge Cutoff: 2022)

Examples

Mica in Electrical Insulation

Muscovite mica is extensively used in the manufacture of electrical capacitors due to its high dielectric strength and resistance to heat and chemicals. It provides excellent insulation in high-voltage applications.

Frequently Asked Questions

What causes the perfect cleavage in mica?

The perfect cleavage in mica is due to the weak Van der Waals forces holding the silicate sheets together. These forces are much weaker than the covalent bonds within the sheets, allowing them to easily separate along the basal plane.

Topics Covered

GeologyMineralogySilicate minerals, Sheet silicates, Mineral chemistry