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The "OLIVINE" series of minerals consist...

The `"OLIVINE"` series of minerals consists of crystal in which `Fe^(2+)` and `Mg^(2+)` ions may substitute for each other causing susbstitutional impurity defects without changing the volume of unit cell. In `"OLIVINE"` series of minerals, `O^(2-)` ions exist as fcc with `Si^(4+)` occupying one-fourth of `OVs` and divalent metal ions occupying one-fourth of `OVs` and divalent metal ions occupying one-fourth of `TVs`. The density of "forsterite" (magnesium silicate) is `3.21 g cm^(-3)` land that of "fayalite" (ferrous silicate) is `4.34 g cm^(-3)`.
If in "forsterite mineral" bivalent `Mg^(2+)` ions are to be replaced by unipositive `Na^(o+)` ions, and if `Na^(o+)` ions are occupying half of `TV_(s)` in`fcc` lattice, the arrangement of rest of the constituents is kept same, then the formula of the new solid is:

A

`Na_(2)SiO_(4)`

B

`Na_(2)SiO_(3)`

C

`Na_(4)SiO_(4)`

D

`Na_(2)Si_(2)O_(6)`

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To solve the problem, we need to determine the formula of the new solid formed when bivalent \( \text{Mg}^{2+} \) ions in forsterite are replaced by unipositive \( \text{Na}^{+} \) ions, occupying half of the tetrahedral voids in the FCC lattice. ### Step-by-Step Solution: 1. **Identify the Composition of Forsterite:** - Forsterite is represented as \( \text{Mg}_2\text{SiO}_4 \). - In this structure: - There are 2 \( \text{Mg}^{2+} \) ions. - There is 1 \( \text{Si}^{4+} \) ion. - There are 4 \( \text{O}^{2-} \) ions. 2. **Determine the Number of Tetrahedral and Octahedral Voids:** - In an FCC lattice, there are 8 tetrahedral voids and 4 octahedral voids. - Since \( \text{Na}^{+} \) ions occupy half of the tetrahedral voids: - Number of \( \text{Na}^{+} \) ions = \( \frac{1}{2} \times 8 = 4 \). 3. **Determine the Number of Silicon and Oxygen Ions:** - The number of \( \text{Si}^{4+} \) ions remains the same as in forsterite: - Number of \( \text{Si}^{4+} \) ions = 1 (occupying one-fourth of the octahedral voids). - The number of \( \text{O}^{2-} \) ions also remains the same: - Number of \( \text{O}^{2-} \) ions = 4. 4. **Write the New Formula:** - The new solid will have: - 4 \( \text{Na}^{+} \) ions, - 1 \( \text{Si}^{4+} \) ion, - 4 \( \text{O}^{2-} \) ions. - Therefore, the formula of the new solid is \( \text{Na}_4\text{SiO}_4 \). 5. **Check for Electrical Neutrality:** - Cations: \( 4 \times (+1) = +4 \) from \( \text{Na}^{+} \). - Anions: \( 4 \times (-2) = -8 \) from \( \text{O}^{2-} \). - The total charge is balanced, confirming electrical neutrality. ### Final Answer: The formula of the new solid is \( \text{Na}_4\text{SiO}_4 \). ---

To solve the problem, we need to determine the formula of the new solid formed when bivalent \( \text{Mg}^{2+} \) ions in forsterite are replaced by unipositive \( \text{Na}^{+} \) ions, occupying half of the tetrahedral voids in the FCC lattice. ### Step-by-Step Solution: 1. **Identify the Composition of Forsterite:** - Forsterite is represented as \( \text{Mg}_2\text{SiO}_4 \). - In this structure: - There are 2 \( \text{Mg}^{2+} \) ions. ...
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The "OLIVINE" series of minerals consists of crystal in which Fe^(2+) and Mg^(2+) ions may substitute for each other causing susbstitutional impurity defects without changing the volume of unit cell. In "OLIVINE" series of minerals, O^(2-) ions exist as fcc with Si^(4+) occupying one-fourth of OVs and divalent metal ions occupying one-fourth of OVs and divalent metal ions occupying one-fourth of TVs . The density of "forsterite" (magnesium silicate) is 3.21 g cm^(-3) land that of "fayalite" (ferrous silicate) is 4.34 g cm^(-3) . The formula of "fayalite mineral" is

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