The partition coefficient ($K_D$) describes how a specific element distributes between two immiscible phases (in this case, solid olivine and liquid magma) at equilibrium.
The formula is:
$ K_D = \frac{\text{Concentration in Solid}}{\text{Concentration in Liquid}} $
For Nickel (Ni) between olivine and basaltic magma, this is:
$ K_{D(\text{Ni, olivine/melt})} = \frac{C_{\text{Ni, olivine}}}{C_{\text{Ni, melt}}} $
We are given:
We need to calculate the concentration of Ni in the crystallizing olivine ($C_{\text{Ni, olivine}}$).
Rearranging the formula to solve for $C_{\text{Ni, olivine}}$:
$ C_{\text{Ni, olivine}} = K_{D(\text{Ni, olivine/melt})} \times C_{\text{Ni, melt}} $
Substituting the given values:
$ C_{\text{Ni, olivine}} = 5 \times 20 \, \text{ppm} $
$ C_{\text{Ni, olivine}} = 100 \, \text{ppm} $
Therefore, the concentration of Ni in the olivine that crystallizes from this magma is 100 ppm.
| Mineral | Modal abundance (%) | Partition coefficient |
| Clinopyroxene | 45 | 0.506 |
| Orthopyroxene | 40 | 0.42 |
| Olivine | 10 | 0.045 |
| Plagioclase | 05 | 0.019 |
Choose the CORRECT combination for the following four statements.
Statement I: Anhydrous partial melting of peridotites produces basaltic magma.
Statement II: Hydrous melting of peridotites produces andesitic magma.
Statement III: Congruent melting of minerals produces liquids of compositions identical to the minerals.
Statement IV: Incongruent melting of minerals produces liquids of different compositions and new solids.