According to Lacey's regime equations, we have the following relationships for designing hydraulic structures across alluvial channels:
- The equation for the depth of scour is:
\[
D = 0.470 \times \left( \frac{Q}{f_s} \right)^{1/3}
\]
where \( D \) is the depth of scour, \( Q \) is the discharge, and \( f_s \) is the silt factor.
- The equation for the perimeter is:
\[
P = 4.75 \times \sqrt{Q}
\]
where \( P \) is the perimeter and \( Q \) is the discharge.
- The equation for the silt factor is:
\[
f_s = 1.76 \times \sqrt{d}
\]
where \( f_s \) is the silt factor and \( d \) is the diameter of the particle.
Thus, the correct statements are (B) and (D). The depth of scour \( D \) is calculated based on the discharge and silt factor, and \( P \) is the perimeter based on the discharge.