The formula to calculate the ϕ (phi) value of a sediment grain is:
\[ ϕ = -\log_2 \left( \frac{D}{1} \right) \]
Where:
Given that the diameter D = 0.125 mm, we substitute this value into the formula:
\[ ϕ = -\log_2 (0.125) \]
Since \( \log_2 (0.125) = -3 \), we get:
\[ ϕ = 3 \]
Thus, the correct value of ϕ is: 3.