Controls on CO2 storage security in natural reservoirs and implications for CO2 storage site selection

For carbon capture and storage to successfully contribute to climate mitigation efforts, the captured and stored CO2 must be securely isolated from the atmosphere and oceans for a minimum of 10,000 years. As it is not possible to undertake experiments over such timescales, here we investigate natural occurrences of CO2, trapped for 104 -106 yr to understand the geologic controls on long term storage performance. We present the most comprehensive natural CO2 reservoir dataset compiled to date, containing 76 naturally occurring natural CO2 stores, located in a range of geological environments around the world. We use this dataset to perform a critical analysis of the controls on long-term CO2 retention in the subsurface. We find no evidence of measureable CO2 migration at 66 sites and hence use these sites as examples of secure CO2 retention over geological timescales. We find unequivocal evidence of CO2 migration to the Earth’s surface at only 6 sites, with inconclusive evidence of migration at 4 reservoirs. Our analysis shows that successful CO2 retention is controlled by: thick and multiple caprocks, reservoir depths of >1200m, and high density CO2. Where CO2 has migrated to surface, the pathways by which it has done so are focused along faults, illustrating that CO2 migration via faults is the biggest risk to secure storage. However, we also find that many naturally occurring CO2 reservoirs are fault bound illustrating that faults can also securely retain CO2 over geological timescales. Hence, we conclude that the sealing ability of fault or damage zones to CO2 must be fully characterised during the appraisal process to fully assess the risk of CO2 migration they pose. We propose new engineered storage site selection criteria informed directly from on our observations from naturally occurring CO2 reservoirs. These criteria are similar to, but more prescriptive than, existing best-practise guidance for selecting sites for engineered CO2 storage and we believe that if adopted will increase CO2 storage security in engineered CO2 stores.

[1]  Predicting hydraulic tensile fracture spacing in strata-bound systems $ , 2013 .

[2]  S. Stevens Natural Analogs for Geologic Storage of CO 2 : An Integrated Global Research Program , 2001 .

[3]  Helge Stanjek,et al.  Experimental investigation of the CO2 sealing efficiency of caprocks , 2010 .

[4]  Richard A. Esposito,et al.  Screening considerations for caprock properties in regards to commercial-scale carbon-sequestration operations , 2015 .

[5]  R Stuart Haszeldine,et al.  Assessing the health risks of natural CO2 seeps in Italy , 2011, Proceedings of the National Academy of Sciences.

[6]  F. Gal,et al.  CO2 escapes in the Laacher See region, East Eifel, Germany: application of natural analogue onshore and offshore geochemical monitoring , 2011 .

[7]  Simon Shackley,et al.  Perceptions of sub-seabed carbon dioxide storage in Scotland and implications for policy: A qualitative study , 2014 .

[8]  Zoe K. Shipton,et al.  A review of recent developments concerning the structure, mechanics and fluid flow properties of fault zones , 2010 .

[9]  T. Chidsey,et al.  Gordon Creek, Farnham Dome, and Woodside Fields, Carbon and Emery Counties, Utah , 1991 .

[10]  Joshua A. White,et al.  Geomechanical behavior of the reservoir and caprock system at the In Salah CO2 storage project , 2014, Proceedings of the National Academy of Sciences.

[11]  I. Barnes,et al.  Tectonic relations of carbon dioxide discharges and earthquakes , 1980 .

[12]  N. Kampman,et al.  Pulses of carbon dioxide emissions from intracrustal faults following climatic warming , 2012 .

[13]  C. Tsang,et al.  A study of caprock hydromechanical changes associated with CO2-injection into a brine formation , 2002 .

[14]  Xiaohua Shen,et al.  Geochemistry and occurrence of inorganic gas accumulations in Chinese sedimentary basins , 2005 .

[15]  M. Zoback,et al.  Stress, pore pressure, and dynamically constrained hydrocarbon columns in the South Eugene Island 330 field, northern Gulf of Mexico , 2001 .

[16]  Sam Holloway,et al.  Natural occurrences as analogues for the geological disposal of carbon dioxide , 1996 .

[17]  D. Richey Fault Seal Analysis for CO2 Storage: Fault Zone Architecture, Fault Permeability, and Fluid Migration Pathways in Exposed Analogs in Southeastern Utah , 2013 .

[18]  U. Sauer,et al.  Natural analogues: a potential approach for developing reliable monitoring methods to understand subsurface CO2 migration processes , 2012, Environmental Earth Sciences.

[19]  Salvatore Lombardi,et al.  Gas migration along fault systems and through the vadose zone in the Latera caldera (central Italy): Implications for CO2 geological storage , 2008 .

[20]  Elin Skurtveit,et al.  Experimental percolation of supercritical CO2 through a caprock , 2009 .

[21]  K. E. Starling,et al.  AN ACCURATE EQUATION OF STATE FOR CARBON DIOXIDE , 1985 .

[22]  Pathegama Gamage Ranjith,et al.  A review of studies on CO2 sequestration and caprock integrity , 2010 .

[23]  Richard H. Worden,et al.  The long-term fate of CO2 in the subsurface: natural analogues for CO2 storage , 2004, Geological Society, London, Special Publications.

[24]  K. Ogata,et al.  Fracture corridors as seal-bypass systems in siliciclastic reservoir-cap rock successions: Field-based insights from the Jurassic Entrada Formation (SE Utah, USA) , 2014 .

[25]  Rajesh J. Pawar,et al.  Insights into interconnections between the shallow and deep systems from a natural CO2 reservoir near Springerville, Arizona , 2014 .

[26]  Zoe K. Shipton,et al.  He and Ne as tracers of natural CO2 migration up a fault from a deep reservoir , 2011 .

[27]  A. Fleet,et al.  Some observations on the origins of large volumes of carbon dioxide accumulations in sedimentary basins , 1999 .

[28]  A. Busch,et al.  The Significance of Caprock Sealing Integrity for CO2 Storage , 2010 .

[29]  James P. Evans,et al.  Natural Leaking CO 2 -Charged Systems as Analogs for Failed Geologic Storage Reservoirs , 2005 .

[30]  Johannes M. Miocic,et al.  Mechanisms for CO2 Leakage Prevention – A Global Dataset of Natural Analogues , 2013 .

[31]  Z. Shipton,et al.  Man-made versus natural CO2 leakage: A 400 k.y. history of an analogue for engineered geological storage of CO2 , 2013 .

[32]  Michael Siegrist,et al.  Public perception of carbon capture and storage (CCS): A review , 2014 .

[33]  Odd Magne Mathiassen,et al.  Fault-seal analysis for CO2 storage: an example from the Troll area, Norwegian Continental Shelf , 2011 .

[34]  Dongxiao Zhang,et al.  Comprehensive review of caprock-sealing mechanisms for geologic carbon sequestration. , 2013, Environmental science & technology.

[35]  Ben Dockrill,et al.  Structural controls on leakage from a natural CO2 geologic storage site: Central Utah, U.S.A. , 2010 .

[36]  Barbara Sherwood Lollar,et al.  The noble gas geochemistry of natural CO2 gas reservoirs from the Colorado Plateau and Rocky Mountain provinces, USA , 2008 .

[37]  B. Freeman,et al.  Quantitative Fault Seal Prediction , 1997 .

[38]  D. Vasco,et al.  Coupled reservoir-geomechanical analysis of CO2 injection and ground deformations at In Salah, Algeria , 2010 .

[39]  Barbara Sherwood Lollar,et al.  Solubility trapping in formation water as dominant CO2 sink in natural gas fields , 2009, Nature.

[40]  Pierre Chiquet,et al.  Wettability alteration of caprock minerals by carbon dioxide , 2007 .

[41]  I. Czernichowski-Lauriol,et al.  A review of natural CO2 accumulations in Europe as analogues for geological sequestration , 2004, Geological Society, London, Special Publications.

[42]  Jérémy Rohmer,et al.  Managing the risk of CO2 leakage from deep saline aquifer reservoirs through the creation of a hydraulic barrier , 2011 .

[43]  D. Faulkner,et al.  On the internal structure and mechanics of large strike-slip fault zones: field observations of the Carboneras fault in southeastern Spain , 2001 .

[44]  R. Hillis Pore pressure/stress coupling and its implications for rock failure , 2003, Geological Society, London, Special Publications.

[45]  M. Hesse,et al.  Constraints on the magnitude and rate of CO2 dissolution at Bravo Dome natural gas field , 2014, Proceedings of the National Academy of Sciences.

[46]  Jonny Rutqvist,et al.  Coupled reservoir-geomechanical analysis of CO2 injection at In Salah, Algeria , 2009 .

[47]  R. Hillis Pore Pressure/Stress Coupling and its Implications for Seismicity , 2000 .

[48]  M. Wilkinson,et al.  Surface controls on the characteristics of natural CO2 seeps: implications for engineered CO2 stores , 2015 .

[49]  James P. Evans,et al.  Analysis of CO2 leakage through ‘low-permeability’ faults from natural reservoirs in the Colorado Plateau, east-central Utah , 2004, Geological Society, London, Special Publications.

[50]  P. Deschamps,et al.  Evolution of fault permeability during episodic fluid circulation: Evidence for the effects of fluid–rock interactions from travertine studies (Utah–USA) , 2015 .

[51]  D. Broseta,et al.  CO2/water interfacial tensions under pressure and temperature conditions of CO2 geological storage , 2007 .

[52]  Paul Upham,et al.  The acceptability of CO2 capture and storage (CCS) in Europe: An assessment of the key determining factors. Part 2. The social acceptability of CCS and the wider impacts and repercussions of its implementation , 2009 .

[53]  R. Stuart Haszeldine,et al.  The Sleipner storage site: Capillary flow modeling of a layered CO2 plume requires fractured shale barriers within the Utsira Formation , 2014 .