Le manuscrit est organisé en 7 chapitres, dont l’introduction génerale (Chapitre1).
Les chapitres3,4,5 et6sont écrits en anglais. Les chapitres4, 5et6 sont présentés sous la forme d’articles prochainement soumis à la publication, au sein desquels sont décrites en détail les méthodes expérimentales utilisées.
Le chapitre 2 présente les matériaux minéraux, dispositifs expérimentaux et techniques analytiques utilisés dans les chapitres3à6.
Le chapitre3présente la constitution d’une base de données thermodynamiques pertinente pour le calcul de la spéciation chimique des solutions expérimentales, qui sera utilisée dans la suite du travail. En effet, les bases de données usuelles de PHREEQC, le code de calcul géo- chimique avec lequel seront effectués les calculs de spéciation chimique (Parkhurst et Appelo,
1.3 Structure du manuscrit
1999), ne comportent pas l’ensemble des données pertinentes au système étudié, notamment en présence des ligands organiques en conditions hydrothermales. Ce chapitre présente donc une revue des données pertinentes de la littérature et explique leur extrapolation en tempéra- ture, en vue de construire une base de données thermodynamiques aussi exhaustive et juste que possible.
On y présentera par ailleurs les résultats d’une expérience de mesure de la solubilité de la magnésite en présence de citrate effectuée afin de préciser la valeur de la constante de complexation entre les espèces du citrate et Mg2+à haute température.
Les chapitres4et5 présentent l’étude de l’influence de l’oxalate, du citrate et de l’EDTA sur le processus et la cinétique de croissance cristalline de la magnésite en conditions hydro- thermales, selon deux approches complémentaires.
Le chapitre4présente les résultats des expériences effectuées en réacteur à circulation et vise à quantifier et à modéliser l’influence de l’oxalate, du citrate et de l’EDTA sur la cinétique de précipitation de la magnésite, entre 100 et 146°C. Les résultats obtenus sont la base d’une modélisation cinétique simple de l’influence de l’oxalate sur la carbonatation de la forstérite, présentée en discussion de l’article.
Dans le chapitre5, on présentera les résultats de l’étude effectuée à l’échelle surfacique sur le même système par le biais de la microscopie à force atomique. Ces résultats expérimentaux permettent de confirmer et de préciser certaines hypothèses émises dans le chapitre4quant au mode d’interaction des ligands organiques avec le processus de croissance cristalline de la magnésite.
Le chapitre 6 présente les résultats de l’étude menée sur la solubilité et la cinétique de précipitation de l’hydromagnésite entre 25 et 75°C. Ces données originales seront comparées aux données analogues acquises pour la magnésite, dans le but de tirer des enseignements fondamentaux sur le rôle de l’hydratation des cations Mg2+dans la formation des carbonates de magnésium et afin de déterminer le rôle potentiel joué par l’hydromagnésite dans l’optimisation de la séquestration minérale du CO2.
Un chapitre de Conclusions et Perspectives (chapitre7) viendra, classiquement, clore ce manuscrit, en en rappelant les résultats principaux et leurs conséquences scientifiques et sociétales.
Enfin, une annexe contient un article dont je suis coauteur, publié en 2012 dans la revue Geochimica et Cosmochimica Acta (Saldi et al.,2012). L’article présente une étude détaillée de la cinétique de précipitation de la magnésite en fonction de la chimie des solutions, interprétée grâce à un modèle de complexation de surface. Ces résultats établissent pour la première fois le fait que la précipitation de la magnésite est potentiellement limitante dans le cadre du processus de carbonatation de la forstérite et constituent de ce fait l’une des motivations du travail effectué avec les ligands organiques. En outre, ils constituent une référence pour la cinétique de précipitation de la magnésite en conditions inorganiques et seront à ce titre fréquemment cités et discutés, notamment dans le cadre du Chapitre4.
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