Lacey’s regime theory for stable channel design in alluvial soil is applicable when flow is in:
APurely non-scouring supercritical flow
BRigid boundary lined canal
CNon-coherent boundary condition
DTrue regime condition with silt factor f
Explanation
Lacey’s regime theory applies to stable alluvial channels carrying silt-laden water where channel cross-section and slope adjust naturally under a true regime condition governed by a silt factor f.

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