Step 1: Recall the formula for effective permeability.
For two-dimensional seepage in anisotropic soils, the effective permeability is calculated using the geometric mean: \[k_{eff} = \sqrt{k_x \cdot k_y}.\]
Step 2: Parameter substitution.
The formula is independent of specific values; the effective permeability is determined by the geometric mean.
Step 3: Final result.
Therefore, the effective permeability is $(k_x k_y)^{1/2}$.