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 |
A hypothetical garnet peridotite composed of 60% olivine, 25% orthopyroxene, 10% clinopyroxene and 5% garnet undergoes 10% batch melting described by $\frac{C_L}{C_o} = \frac{1}{F+D-F*D}$ where F is degree of melting and D is bulk partition coefficient. The ratio of Ce in the melt to the original rock will be ___________ (round off to 2 decimal places).
(The $K_D$ values of Ce for olivine, orthopyroxene, clinopyroxene and garnet are 0.001, 0.003, 0.10 and 0.02, respectively)