posted on 2022-11-22, 21:13authored byDominique Guérillot, Jérémie Bruyelle
<p dir="ltr">The fluid injection in sedimentary formations may generate geochemical interactions between the fluids and the rock minerals, e.g., CO<sub>2</sub> storage in a depleted reservoir or a saline aquifer. To simulate such reactive transfer processes, geochemical equations (equilibrium and kinetics equations) are coupled with compositional flows in porous media in order to represent, for example, precipitation/dissolution phenomena. The aim of the decoupled approach proposed consists in replacing the geochemical equilibrium solver with a substitute method to bypass the huge consuming time required to balance the geochemical system while keeping an accurate equilibrium calculation. This paper focuses on the use of artificial neural networks (ANN) to determine the geochemical equilibrium instead of solving geochemical equations system. To illustrate the proposed workflow, a 3D case study of CO<sub>2</sub> storage in geological formation is presented.</p><h2>Other Information</h2><p dir="ltr">Published in: Computational Geosciences<br>License: <a href="https://creativecommons.org/licenses/by/4.0" target="_blank">https://creativecommons.org/licenses/by/4.0</a><br>See article on publisher's website: <a href="http://dx.doi.org/10.1007/s10596-019-09861-4" target="_blank">http://dx.doi.org/10.1007/s10596-019-09861-4</a></p>
Funding
Open Access funding provided by the Qatar National Library.