Step 1: Understanding the formula for the bulk partition coefficient.
The bulk partition coefficient (\(K_d\)) for the rock is calculated as a weighted average based on the modal abundances and the partition coefficients of each mineral: \[ K_{{bulk}} = (f_1 \times K_{d1}) + (f_2 \times K_{d2}) + (f_3 \times K_{d3}) \] Where:
\(f_1, f_2, f_3\) are the modal abundances of M1, M2, and M3, respectively.
\(K_{d1}, K_{d2}, K_{d3}\) are the partition coefficients of element E in M1, M2, and M3, respectively.
Step 2: Applying the values.
Given:
\(K_{d1} = 1.5, K_{d2} = 1.0, K_{d3} = 0.5\)
\(f_1 = 10% = 0.1, f_2 = 40% = 0.4, f_3 = 50% = 0.5\)
The bulk partition coefficient is: \[ K_{{bulk}} = (0.1 \times 1.5) + (0.4 \times 1.0) + (0.5 \times 0.5) = 0.15 + 0.4 + 0.25 = 0.8 \] Thus, the bulk partition coefficient of element E in the rock is \(0.80\).
The following table provides the mineral chemistry of a garnet. All oxides are in weight percentage and cations in atoms per formula unit. Total oxygen is taken as 12 based on the ideal garnet formula. Consider Fe as Fetotal and Fe\(^{3+}\) = 0. The Xpyrope of this garnet is _.
In the isochemical phase diagram shown below, the curved arrow represents the P-T path. The variance at peak metamorphism is _.
A sediment core of 4 cm diameter and 35.81 cm height was collected. This core had an initial weight of 1000.00 g and upon drying the sediment, the weight decreased by 133.75 g. This core has a void ratio of 0.42857, where void ratio is defined as the ratio of volume of void to the volume of solid (Vv/Vs). The average density of the sediment in the core is ________ g/cm\(^3\).