Bligh’s Creep Theory
Bligh’s creep theory states that, the percolating water creeps along the profile of the bottom of hydraulic structure, which is in contact with the subsoil. The creep length is the path traced by the percolating water. Hydraulic gradient is constant throughout its passage and it is the loss of head per cubic length. The creep length must be made as big as possible to prevent the piping action. By proving deep vertical cut-off or sheet it can be achieved.
According to Bligh’s creep theory, the total length for first drawing: L=B and for second drawing: L = B + 2 (d1 + d2 +d3).
If the total loss of head is H, then the loss of head per unit length of the creep shall be,

Bligh called the loss of head per unit length of creep as percolation coefficient. The reciprocal, (L/H) of the percolation coefficient is known as the coefficient of creep C.
Assumptions
Design criteria for Bligh’s creep theory
Safety against piping
The length of creep should be sufficient to offer safe hydraulic gradient according to the type of soil.
Safe creep length = L = CH, C = 1/c.
Limitations of Bligh’s theory
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