Thermal Effects on Shear Fracturing and Injectivity During CO2 Storage

With almost two hundred coal burning power plants in Ohio River valley, this region is considered important for evaluation of CO2 storage potential. In a CO2 storage project, the temperature of the injected CO2 is usually considerably lower than the formation temperature. The heat transfer between the injected fluid and rock has to be investigated in order to test the viability of the target formation to act as an effective storage unit and to optimize the storage process. In our previous work we have introduced the controversial idea of injecting CO2 for storage at fracturing conditions in order to improve injectivity and economics. Here we examine the thermal aspects of such process in a setting typical for Ohio River Valley target formation. A coupled flow, geomechanical and heat transfer model for the potential injection zone and surrounding formations has been developed. All the modeling focuses on a single well performance and considers induced fracturing for both isothermal and thermal injection conditions. The induced thermal effects of CO2 injection on stresses, and fracture pressure, and propagation are investigated. Possibility of shear failure in the caprock resulting from heat transfer between reservoir and the overburden layers is also examined. In the thermal case, the total minimum stress at the wellbore decreases with time and falls below the injection pressure quite early during injection. Therefore, fracturing occurs at considerably lower pressure, when thermal effects are present. The coupled thermal and dynamic fracture model shows that these effects could increase the speed of fracture propa‐ gation in the storage layer depending on the injection rate. These phenomena are dependent primarily on the difference between the injection and reservoir temperature. © 2013 Goodarzi et al.; licensee InTech. This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/3.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Our results show that shortly after injection, the induced expansion in caprock lead to slight increase of total stresses (poroelasticity) which will reduce the chance of shear failure. However as soon as total minimum stress in the caprock decreases due to thermal diffusion between the reservoir and caprock, thermoelasticity dominates and the chance of shear failure increases in the caprock. Incorporation of thermal effects in modeling of CO2 injection is significant for understanding the dynamics of induced fracturing in storage operations. Our work shows that the injection capacity with cold CO2 injection could be significantly lower than expected, and it may be impractical to avoid induced fracture development. In risk assessment studies inclusion of the thermal effects will help prevent the unexpected leakage in storage projects.

[1]  David W. Keith,et al.  Geomechanical modeling for CO2 storage in Nisku aquifer in Wabamun Lake area in Canada , 2012 .

[2]  David William Keith,et al.  A coupled geomechanical reservoir simulation analysis of carbon dioxide storage in a saline aquifer in the Ohio River Valley , 2011 .

[3]  David William Keith,et al.  Thermal Aspects of Geomechanics and Induced Fracturing in CO2 Injection With Application to CO2 Sequestration in Ohio River Valley , 2010 .

[4]  Semere Solomon,et al.  Carbon Dioxide Storage: Geological Security and Environmental Issues - Case Study on the Sleipner Gas Field in Norway , 2007 .

[5]  Neeraj Gupta,et al.  Geomechanical aspects of CO2 sequestration in a deep saline reservoir in the Ohio River Valley region , 2006 .

[6]  Fred Riddiford,et al.  Monitoring geological storage the In Salah Gas CO2 storage project , 2005 .

[7]  Rick Chalaturnyk,et al.  IEA GHG Weyburn CO2 monitoring and storage project , 2005 .

[8]  L. Greene The Bellona Foundation , 2001 .

[9]  E. Fjaer Petroleum Related Rock Mechanics , 1992 .

[10]  M. Zoback,et al.  State of stress and intraplate earthquakes in the United States. , 1981, Science.

[11]  Van Genuchten,et al.  A closed-form equation for predicting the hydraulic conductivity of unsaturated soils , 1980 .

[12]  H. Herman,et al.  The Mechanical and Thermal Properties of Materials and Statistical Physics of Materials , 1975 .

[13]  I. N. Sneddon,et al.  Crack Problems in the Classical Theory of Elasticity , 1969 .

[14]  William C. Maurer,et al.  Bit - Tooth Penetration Under Simulated Borehole Conditions , 1965 .

[15]  J. Sengers,et al.  The thermal conductivity of carbon dioxide in the critical region: I. The thermal conductivity apparatus , 1962 .

[16]  L. A. Guildner THE THERMAL CONDUCTIVITY OF CARBON DIOXIDE IN THE REGION OF THE CRITICAL POINT. , 1958, Proceedings of the National Academy of Sciences of the United States of America.

[17]  Richard Hughes,et al.  The American Association of Petroleum Geologists , 1924, Science.