Caisson Soil Seepage Analysis > 기술자료실

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Caisson Soil Seepage Analysis

Introduction

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Soil seepage is governed by the same equations as heat transfer (the diffusion equation). 

It is thereby possible to use the Strand7 heat solver to solve seepage problems, including 

pore pressure and flow rates. In the following example, this method is applied to an axisymmetric 

mesh representing a hole being bored in a mud flat. The ground water level is assumed to be 

flush with the mud surface. The axisymmetric mesh is annotated below.