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Published byDevyn Blatchford Modified over 9 years ago
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Experimental investigation of supercritical CO2 reactivity
Centre de Géosciences Experimental investigation of supercritical CO2 reactivity Olivier Regnault a, Vincent Lagneau a, Hubert Catalette b a ENSMP-CIG 35 rue Saint Honoré, Fontainebleau Cedex – b EdF R&D Département étude des matériaux, Site des Renardières Route de Sens, Ecuelles, Moret sur Loing Cedex French-Serbian European Summer University 16 – 25 October 2006 Renewable Energy Sources and the Environment
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sc-CO2 potential reactant
Context of the study Cap-rock Aquifer silicate dissolution + carbonate precipitation dissolved CO2 main reactant sc-CO2 potential reactant Pure sc-CO2 cross dissolution scCO2/H2O H2O/aqCO2 ? CO2 Injection well
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Experimental conditions
Pressure ≈ 160 bars Temperature = 200°C Duration = 45 days X CO2 P (bar) Anhydrous sc-CO2 H2O/CO2
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Selection of minerals Selected pure minerals consistent with the mineralogy of a geological formation and the cements of the borehole seals : Anorthite (Feldspar, CaAl2Si2O8) Phlogopite (Mica) Forsterite (Olivine, Mg2Si2O5) Portlandite Ca(OH)2 Those minerals have been crushed to enhanced the reactive surface and provite fresh surfaces.
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Schematic section of the experimental device
Experimental protocol Schematic section of the experimental device Autoclave Injection pit Titanium cell Thermal compressor P T sc-CO2 Powdered pure minerals
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Anorthite behaviours with a H2O/CO2 fluid (I)
Figure of dissolution and clay growth Tridymite (SiO2)
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Anorthite behaviours with a H2O/CO2 fluid (II)
Calcite (CaCO3) Aragonite (CaCO3)
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Anorthite behaviours with anhydrous CO2
before reaction carbonate and clay growth fibrous calcite
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Conclusions and Prospect
An effective mineral reactivity exits and ought to be considered for CO2 sequestration studies. The strong reactivity of portlandite Ca(OH)2 suggests potential reaction with cements structures arround the borehole : possible decrease of the sealing properties. A new experiment is actually carried out : quantify and measure first the portlandite carbonation kinetics.
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