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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)`.
The formula of "fayalite mineral" is

A

`Fe_(2)SiO_(4)`

B

`FeSiO_(4)`

C

`Fe_(2)SiO_(6)`

D

`Fe_SiO_(3)`

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To find the formula of the fayalite mineral in the olivine series, we will follow these steps: ### Step 1: Determine the number of ions in the unit cell In the olivine structure: - The oxide ions (O²⁻) form a face-centered cubic (FCC) lattice. - The number of O²⁻ ions in an FCC unit cell is calculated as follows: - There are 8 corner atoms contributing 1/8 each and 6 face-centered atoms contributing 1/2 each. - Total O²⁻ ions = \(8 \times \frac{1}{8} + 6 \times \frac{1}{2} = 1 + 3 = 4\). ### Step 2: Determine the number of Si⁴⁺ ions - It is given that Si⁴⁺ ions occupy one-fourth of the octahedral voids. - In an FCC lattice, the number of octahedral voids is equal to the number of atoms in the lattice, which is 4. - Therefore, the number of Si⁴⁺ ions = \( \frac{1}{4} \times 4 = 1\). ### Step 3: Determine the number of Fe²⁺ ions - The divalent metal ions (Fe²⁺ or Mg²⁺) occupy one-fourth of the tetrahedral voids. - The number of tetrahedral voids in an FCC lattice is twice the number of atoms, which is \(2 \times 4 = 8\). - Therefore, the number of Fe²⁺ ions = \( \frac{1}{4} \times 8 = 2\). ### Step 4: Write the empirical formula From the above calculations: - Number of Fe²⁺ ions = 2 - Number of Si⁴⁺ ions = 1 - Number of O²⁻ ions = 4 Thus, the empirical formula of fayalite can be written as: \[ \text{Fe}_2\text{Si}_1\text{O}_4 \] ### Step 5: Check for electrical neutrality - Cation charges: \(2 \times (+2) + 1 \times (+4) = 4 + 4 = +8\) - Anion charges: \(4 \times (-2) = -8\) Since the total positive charge (+8) equals the total negative charge (-8), the formula maintains electrical neutrality. ### Final Answer The formula of the fayalite mineral is: \[ \text{Fe}_2\text{SiO}_4 \] ---

To find the formula of the fayalite mineral in the olivine series, we will follow these steps: ### Step 1: Determine the number of ions in the unit cell In the olivine structure: - The oxide ions (O²⁻) form a face-centered cubic (FCC) lattice. - The number of O²⁻ ions in an FCC unit cell is calculated as follows: - There are 8 corner atoms contributing 1/8 each and 6 face-centered atoms contributing 1/2 each. - Total O²⁻ ions = \(8 \times \frac{1}{8} + 6 \times \frac{1}{2} = 1 + 3 = 4\). ...
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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) . 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:

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