Dissolution and Precipitation Reactions Between the Madison Limestone and Supercritical CO₂: Implications for Carbon Capture and Storage in Southwest.

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Presentation transcript:

Dissolution and Precipitation Reactions Between the Madison Limestone and Supercritical CO₂: Implications for Carbon Capture and Storage in Southwest Wyoming Steven Levesque

Background-Carbon Capture and Storage Objectives and Hypothesis Outline Background-Carbon Capture and Storage Objectives and Hypothesis Geology: Rock Springs Uplift Experimental Approach Results Summary and Conclusions

Background- Carbon Capture and Storage What is Carbon Capture and Storage? Storage of anthropogenic CO₂ CO₂ is injected within the subsurface into a reservoir rock Ambient conditions allow for supercritical phase of CO₂ CO₂ migration is inhibited by an impermeable cap rock Metz et al. 2005

Objectives and Hypothesis Experimentally simulate a geologic CO₂ storage reservoir Observe any mineral precipitation/dissolution from injection of supercritical CO₂ Hypothesis Reactions among the reservoir rock, brine, and supercritical CO₂ will cause mineral precipitation/dissolution

Geology: Rock Springs Uplift Surdam and Jiao 2007 Located in southwest Wyoming Doubly plunging anticline Modified from Chopping et al 2012

Geology: Rock Springs Uplift Surdam and Jiao 2007 Madison Limestone (12,350 ft)

Madison Limestone (12,350 ft) Mg-rich Dolomite ~10% porosity Surdam and Jiao 2007 Madison Limestone (12,350 ft) Mg-rich Dolomite ~10% porosity

Experimental Approach Purpose: Simulate in-situ reservoir conditions AE Bolted Closure Pressure Vessel (300mL) Duration: 354 hours Temperature: 100˚C Pressure: 345 Bars ~150 mL Brine + 7.5 g Rock, 20:1 water-rock ratio Modified from Wang et al 2013

XRD Analysis

FE-SEM Textural Changes Unreacted Reacted

Water Chemistry Evolution & pH vs. Time

Summary and Conclusions Dolomite dissolution reactions Mineral surface texture changes Increase in Mg and Ca throughout the experiment

Future Work Increase the duration of the experiments Geochemical modeling to predict in-situ changes in pH and mineral assemblages Porosity and permeability analyses Trace element analyses

Acknowledgements Dr. John Kaszuba – Overall mentorship Norbert Swoboda-Colberg –XRD analyses Susan Swapp –SEM assistance Ryan Herz-Thyhsen, Alexa Socianu, Mary Kate McCarney, Quin Miller, Michael Schedel and Rhowe Stefanski – Lab assistance Janet Dewey – Water chemistry analyses Fred McLaughlin and Scott Quillinan (Carbon Management Institute) – Providing rock samples and other necessary data