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. Dans-cette-thèse, les différences majeures entre le stockage souterrain de l'hydrogène et le stockage conventionnel du gaz naturel sont alignées pourêtrepourêtre des bio-réactions

. Le-déplacement-dûdûà-la-gravité-lorsque, un réservoir stratifié et saturé en eau, a ´ eté analytiquement modélisé Un nouveau modèle mathématique a ´ eté développé pour décrire le couplage entre l'´ ecoulement bi-phasique multi-composants et des populations microbiennes qui consomment de l'hydrogène pour faire fonctionner leur métabolisme. Des scénarios oscillants, semblablesàsemblablesà l'instabilité de Turing, ontétéontété détecté. Le modèle mathématique a ´ eté implémenté numériquement sur la base de DuMu X . Les scénarios de stockage ontétéontété simulés en incluant une simulationàsimulationà l'´ echelle du champ, avec un modèle géologique réaliste. LesétudesLesétudes ont prouvé que la faible densité et viscosité de l'hydrogène estàestà l'origine du déplacement plus instable de l'eau comparécomparéà l'injection du méthane, De plus, il a ´ eté constaté que la dispersion mécanique et les réactions biochimiques ont une influence importante dans lesétudeslesétudes de prédiction. Les pertes notables d'´ energie peuvent appara??treappara??tre au travers des transformations biochimiques des gaz stockés