Step 1: Understanding the Concept:
Allen Hazen's classical particle size distribution parameter defines the effective grain diameter controlling permeability in porous granular media.
Key Formula or Approach:
\[ D_{10} = \text{Effective Grain Size (10\% finer by weight)} \]
\[ K = C \cdot (D_{10})^2 \quad \text{(Hazen's Hydraulic Conductivity Formula)} \]
Step 2: Detailed Explanation:
In hydrogeology, well screen design, and geotechnical engineering:
The effective size (or effective diameter) of a porous soil or aquifer material is universally denoted as \(D_{10}\).
This is defined as the sieve particle diameter such that exactly \(10\%\) of the soil particles by weight are smaller (finer) than this size, and \(90\%\) are coarser.
Hazen demonstrated that hydraulic permeability is primarily governed by this smallest 10% particle fraction.
Step 3: Final Answer:
Therefore, \(x = 10\), matching option (A).