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Kinetics of quartz alkaline dissolution in clayey sandstones

Conference · · Am. Chem. Soc., Div. Pet. Chem., Prepr.; (United States)
OSTI ID:6728293

The dissolution of minerals constitutive of sandstone rocks is one of the points to be evaluated for numerous oil production processes where the use of alklaline agents can be considered: alkaline flooding, surfactant flooding, polymer flooding. Alkaline agents have been also set forth to prevent well bore damage. It has been shown that at moderate temperature, quartz, among the numerous minerals constituting clayey sandstones, could be the determining species as far as dissolution is concerned. In this paper the particular influence of the aluminum appearing during the alkaline dissolution of such sandstones is specified. The influence of pH and contact time is examined by means of dissolution experiments, in which solubilized silicon and aluminum concentrations are measured. The interpretation of the experimental results is proposed with a tentative model. This model takes into account a kinetic scheme for the quartz dissolution-condensation, involving the silicon and aluminum adsorption equilibria.

Research Organization:
Institut Francais du Petrole, Rueil-Malmaison (FR)
OSTI ID:
6728293
Report Number(s):
CONF-880659-
Journal Information:
Am. Chem. Soc., Div. Pet. Chem., Prepr.; (United States), Journal Name: Am. Chem. Soc., Div. Pet. Chem., Prepr.; (United States) Vol. 33:1; ISSN ACPCA
Country of Publication:
United States
Language:
English