CarbFix Mineral storage of CO2 in basalt - CO2Geonet
CarbFix Mineral storage of CO2 in basalt - CO2Geonet
CarbFix Mineral storage of CO2 in basalt - CO2Geonet
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<strong>CarbFix</strong> <strong>M<strong>in</strong>eral</strong> <strong>storage</strong> <strong>of</strong> <strong>CO2</strong> <strong>in</strong> <strong>basalt</strong>Bergur Sigfússon (1), Sigurdur R. Gislason (2), Mart<strong>in</strong> Stute(3), Eric H. Oelkers(4), Susan Stipp (5)E<strong>in</strong>ar Gunnlaugsson(1), Holmfridur Sigurdardottir(1), Edda Sif Aradóttir(1), Ingvi Gunnarsson (1),Helgi Alfredsson(2), Juerg M. Matter(3), Domenik Wolff-Boenisch(2), Andri Stefansson(2), GudniAxelsson(6) Kiflom Mesf<strong>in</strong>(2), Iwona Galeczka(2), Snorri Gudbrandsson(2) Gabrielle Stockman(2),Alex P. Gysi(2) Therese K. Flaathen(2), Mahnaz Rezvani Khalilabad(2), Knud Dideriksen (5), JonasOlsson (5) and Fidel Grandia (7), Wallace S. Broecker(3)(1) Reykjavik Energy, Iceland (2) Institute <strong>of</strong> Earth Sciences, University <strong>of</strong> Iceland, Iceland (3) EarthInstitute, Columbia University, USA, (4) CNRS, Université Paul Sabatier, France, (5) Nano-ScienceCenter, University <strong>of</strong> Copenhagen, Denmark, (6) Iceland Geosurvey, Iceland, (7) Amphos21, Spa<strong>in</strong>.
The <strong>CarbFix</strong> ConceptPhoto: J. AleanPhoto: H. SigurdardottirBasalt CO 2 dissolved <strong>in</strong> Water Carbonates• Basalt conta<strong>in</strong>s m<strong>in</strong>erals which can be used for carbon fixation• Bedrock > 90% <strong>basalt</strong>ic• Excellent <strong>in</strong>frastructure for experiment at the Hellisheidi powerplant• Group <strong>of</strong> scientist, eng<strong>in</strong>eers and technicians• Initially eight PhD and two MSc students
IPCC (2005)
• Icelanders ~4-5 Mt CO 2 /yr– Industrial processes 41%– Transport 23%– Fish<strong>in</strong>g <strong>in</strong>dustry 14%– Agriculture 12%– Waste 6%– Geothermal energy 4%Iceland - CO 2 Emission• Hellisheidi Geothermal Power Plant (300 MWe):– 20-40 g CO 2 /kWh• Fossil fuel sources:– 600-1000 g CO 2 /kWh• Magma: ~ 2 Mt CO 2 /yrSigfús Már PéturssonSigurður R Gíslason
Natural ProcessesCO 2 fully dissolved <strong>in</strong> fresh waterand <strong>in</strong>jected down to 540 mCO 2 <strong>in</strong> geothermal steamfrom wells at HellisheiðiFumarolesand hot spr<strong>in</strong>g areasAdd carbonates tothe alteration capGeothermal systemsAlteration capSolidify<strong>in</strong>g magmaHeat conductionand naturalCO 2 release
2 L / s <strong>of</strong> waterpumped to the<strong>in</strong>jection site0.07 kg/s <strong>of</strong>pure CO 2 gas or gasmixture pumped andmixed with the waterThe CO 2 rich waterwill mix with thegroundwater, travelthrough the rockdownstream fromthe <strong>in</strong>jection site andreact with the <strong>basalt</strong>~2.000 t CO 2 /yrmixed with waterand pumped down to~500 m depth.The HellisheiðiPower Plant:Releasesaround 40.000tons <strong>of</strong> CO 2 /yr.The CO 2orig<strong>in</strong>ates fromthe heat source;cool<strong>in</strong>g magmaAlfredsson (2009)
Safety Strategy• Prepare– Site selection and tests– Model<strong>in</strong>g– Consultation and Licenses• Inject dissolved CO 2 <strong>in</strong> waterJuerg Matter• Monitor <strong>in</strong>jection and report• Remedy– F<strong>in</strong>e tune <strong>in</strong>jection– Calibrate models Guðmundur LárussonGuðmundur LárussonOrkust<strong>of</strong>nun
Experiments 2012-2013• Injection <strong>of</strong> CO 2 mixedwithH 2 S from the powerplant.– Elevated safety precautions• 130 tons <strong>of</strong> mixture already <strong>in</strong>jected <strong>in</strong>to two different reservoirs– Low temperature (20-50°C) at 400-800 meters where CO 2m<strong>in</strong>eralisation is predicted to be high– High temperature (>250°C) below 800 meters where H 2 Sm<strong>in</strong>eralisation si predicted to be high• Ongo<strong>in</strong>g <strong>in</strong>jection <strong>in</strong>to the low temperature reservoir withextensive monitor<strong>in</strong>g.• Ongo<strong>in</strong>g preparations for further treatment <strong>of</strong> gas (separation <strong>of</strong>CO 2 and H 2 S) and re-<strong>in</strong>jection from one turb<strong>in</strong>e (15-20% <strong>of</strong> thepowerplant‘s emissions)
Already successful solubility trapp<strong>in</strong>g, IF m<strong>in</strong>eral trapp<strong>in</strong>g successful:• Possible to demonstrate a “near zero CO 2 emission” geothermal power plant.• Valuable early experience, <strong>in</strong>frastructure and knowledge base needed for thefuture large-scale <strong>in</strong>jection <strong>of</strong> CO 2• Long term response <strong>of</strong> <strong>in</strong>jection reservoirs• <strong>M<strong>in</strong>eral</strong> <strong>storage</strong> <strong>of</strong> CO 2 <strong>in</strong> <strong>basalt</strong>s might be a global alternative•Less energy <strong>in</strong>tensive the <strong>in</strong>jection <strong>of</strong> supercritical CO 2 but large quantities <strong>of</strong> water and <strong>storage</strong>volume are needed. May be used <strong>in</strong> conjunction12 Sigfús Már Pétursson
Global SignificanceExtensive <strong>basalt</strong> shields worldwide13