Silicate Structures and Silicon-Oxygen Tetrahedrons
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Questions and Answers

What is the fundamental unit in all silicate structures?

  • Silicon trioxide (Si2O3)
  • Silicon dioxide (SiO2)
  • Silicon monoxide (SiO)
  • Silicon-oxygen (SiO4)4– tetrahedron (correct)
  • How many oxygen atoms are bonded to a central silicon cation in the SiO4 tetrahedron?

  • Two
  • Four (correct)
  • Five
  • Three
  • What type of bonds develop in silicate structures due to the attraction of oppositely charged ions and sharing of electrons?

  • Both ionic and covalent bonds (correct)
  • Ionic bonds only
  • Covalent bonds only
  • Hydrogen bonds
  • What is the term used to describe the linking of SiO4 tetrahedrons by shared oxygen atoms?

    <p>Polymerization</p> Signup and view all the answers

    Which type of silicate structure contains isolated groups of SiO4 tetrahedrons?

    <p>Nesosilicates</p> Signup and view all the answers

    What composition do ring silicates, also known as cyclosilicates, have when they are of the sixfold variety?

    <p>$Si_6O_{18}$</p> Signup and view all the answers

    What is the unit composition of single chains in inosilicates?

    <p>SiO3</p> Signup and view all the answers

    When three oxygen atoms are shared with adjoining tetrahedrons, what type of silicate is formed?

    <p>Phyllosilicates</p> Signup and view all the answers

    Which type of silicate is characterized by an SiO2 unit composition?

    <p>Framework silicates</p> Signup and view all the answers

    What is the role of aluminum in silicate structures?

    <p>It can replace silicon in tetrahedral sites.</p> Signup and view all the answers

    Which elements can be found in octahedral coordination with oxygen in silicate structures?

    <p>Mg2+, Fe2+, Fe3+</p> Signup and view all the answers

    How is solid solution involving ions of different charge maintained in silicate structures?

    <p>Through coupled substitutions</p> Signup and view all the answers

    Study Notes

    Silicate Structures

    • The fundamental unit in silicate structures is the silicon-oxygen (SiO4)4– tetrahedron, composed of a central silicon cation (Si4+) bonded to four oxygen atoms.
    • The silicon-oxygen bonds are approximately 50% ionic and 50% covalent, developing from the attraction of oppositely charged ions and the sharing of electrons.
    • The positive charge (+4) of each silicon cation is satisfied by its four bonds to oxygen atoms.

    Polymerization

    • Each oxygen ion (O2–) contributes only half of its total bonding energy to a silicon-oxygen bond, allowing it to also bond to the silicon cation of another tetrahedron.
    • This shared bonding leads to polymerization, where SiO4 tetrahedrons become linked by shared oxygen atoms.

    Types of Silicates

    • Nesosilicates have isolated groups of SiO4.
    • Sorosilicates contain pairs of SiO4 tetrahedrons linked into Si2O7 groups.
    • Ring silicates (cyclosilicates) are closed, ringlike silicates with a composition of Si6O18.
    • Inosilicates are composed of infinite chains of tetrahedrons with a unit composition of SiO3 or Si2O6 (single chain) or Si4O11 (double chain).
    • Phyllosilicates (sheet silicates) are formed when three oxygen atoms are shared with adjoining tetrahedrons, resulting in infinite flat sheets with a unit composition of Si2O5.
    • Framework silicates (tectosilicates) have an infinite three-dimensional network with an SiO2 unit composition, where tetrahedrons share all their oxygen ions.

    Aluminum in Silicates

    • Aluminum, with a radius slightly larger than silicon, can be surrounded by four oxygen atoms arranged tetrahedrally or six oxygen atoms in sixfold coordination.
    • Aluminum can occupy tetrahedral sites as a replacement for silicon and octahedral sites in solid solution with elements such as magnesium and ferrous iron.
    • Aluminum can form ionic bonds with SiO4 tetrahedrons in sixfold coordination.

    Octahedral Coordination

    • Several ions can be present in silicate structures in octahedral coordination with oxygen, including Mg2+, Fe2+, Fe3+, Mn2+, Al3+, and Ti4+.
    • These ions have approximately the same dimensions and can occupy equivalent atomic sites despite having charges ranging from positive two to positive four.
    • Solid solution involving ions of different charge is accomplished through coupled substitutions, maintaining neutrality of the structures.

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    Description

    Explore the fundamental unit of all silicate structures, which is the silicon-oxygen (SiO4)4– tetrahedron. Learn about the bonding between a central silicon cation and four oxygen atoms forming a regular tetrahedron. Understand how these tetrahedrons play a crucial role in holding together the terrestrial crust.

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