Sheet Silicates Structure Overview

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Questions and Answers

What cation is associated with the Gibbsite structure?

  • Fe+2
  • Ca+2
  • Mg+2
  • Al+3 (correct)

In which structure are 2 out of 3 octahedral sites occupied?

  • Brucite structure
  • Neither structure
  • Gibbsite structure (correct)
  • Both structures equally

Which of the following cations is found in Brucite?

  • Mg+2 (correct)
  • Al+3
  • Li+
  • Na+

What type of sheet silicate is Gibbsite classified as?

<p>Dioctahedral (A)</p> Signup and view all the answers

What is the formula for Gibbsite?

<p>Al(OH)3 (C)</p> Signup and view all the answers

What structural characteristic differentiates the Brucite and Gibbsite structures?

<p>Brucite contains solely +2 cations. (A), Brucite has all octahedral sites occupied. (C)</p> Signup and view all the answers

Which statement best describes the occupancy of octahedral sites in Gibbsite?

<p>It has two out of three octahedral sites occupied. (D)</p> Signup and view all the answers

Which of these cations is associated with Brucite?

<p>Mg+2 (A)</p> Signup and view all the answers

What type of sheet silicate is Brucite classified as?

<p>Trioctahedral sheet silicate (C)</p> Signup and view all the answers

What is the chemical formula of the octahedral layer in Gibbsite?

<p>Al(OH)3 (A)</p> Signup and view all the answers

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Study Notes

Sheet Silicate Structure

  • Sheet silicates consist of two types of layers: tetrahedral layers and octahedral layers.
  • Octahedral layers can have different structures depending on the cations present.
  • Brucite: When the cations are +2 ions like Mg+2 or Fe+2, the octahedral layer takes on the structure of Brucite [Mg(OH)2].
  • Gibbsite: When the cations are +3 ions like Al+3, the octahedral layer takes on the structure of Gibbsite [Al(OH)3].
  • In the Brucite-like structure (trioctahedral sheet silicate), all octahedral sites are occupied.
  • In the Gibbsite-like structure (dioctahedral sheet silicate), only 2 out of 3 octahedral sites are occupied.

Sheet Silicates Structures

  • Brucite and Gibbsite are important structural components in sheet silicates.
  • Both are octahedral layers with hydroxyl groups (OH-) surrounding cations
  • Brucite has a trioctahedral structure with all octahedral sites occupied
  • Gibbsite has a dioctahedral structure with only 2 out of 3 octahedral sites filled.
  • Brucite forms when the cations have a +2 charge, such as Mg+2 or Fe+2
  • Gibbsite forms when the cations have a +3 charge, such as Al+3

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