Solution:Lacey's silt theory–According to Lacey, for a given discharge on silt factor (silt charge) all the dimensions such as width depth and longitudinal slope are all fixed by nature.
• If channel section is too small and slope too steep scour will occur till regime is attained. On the contrary, if section is too large and slope too flat, silting will take place till final regime is established.
• Still supporting eddies are generated from perimeter of the channel and not only from bed with. Hence, Lacey considered the hydraulic mean depth as the variable for silt supporting.