Multi‐scale simulation of rock compaction through breakage models with microstructure evolution

<p>Regional subsidence due to fluid depletion includes the interaction among multiple physical processes. Specifically, rock compaction is governed by coupled hydro-mechanical feedbacks involving fluid flow, effective stress change and pore collapse. Although poroelastic models are often used...

Full description

Bibliographic Details
Main Authors: G. Buscarnera, Y. Chen, J. Lizárraga, R. Zhang
Format: Article
Language:English
Published: Copernicus Publications 2020-04-01
Series:Proceedings of the International Association of Hydrological Sciences
Online Access:https://www.proc-iahs.net/382/421/2020/piahs-382-421-2020.pdf