A diffusion model for land subsidence

Massimiliano Ferronato, Giuseppe Gambolati, Mario Putti, Pietro Teatini & Massimiliano Ferronato
In classical hydrogeology land subsidence due to fluid withdrawal is typically predicted by decoupling the flow model from the structural model. The pore pressure solution obtained from the flow model is used as an external source of strength in the structural equations to compute the porous medium deformation. Though the horizontal displacement can be of some interest as well, usually the attention is devoted to the vertical displacement, which allows for the prediction of subsidence...
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