1887

Abstract

pressure by time then we convolve the two functions: transient pressure of the delta function by time and displacements of particles of sediments Finally we convolve the obtained results and the transient pressure of the delta function by the pore length. The process of transient of pressure in pore when a step function of pressure is applied to the beginning of that pore was described by Chandler (1981) as: ⎡ ∞ 1 2 1 ⎛πnl ⎞ ⎛ n π C t ⎞⎤ P l t) = P ⎢1 − − ∑ sin⎜ ⎟ ⋅ exp ⎥ = P ⋅ ⎢⎣

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/content/papers/10.3997/2214-4609-pdb.13.B041
2005-09-04
2020-09-21
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